EX-99.1 2 tm236279d1_ex99-1.htm EXHIBIT 99.1

 

Great Bear Gold Project 

Ontario, Canada

Voluntary National Instrument 43-101 Technical Report

 

 

Prepared for: 

Kinross Gold Corporation

 

Prepared by: 

Nicos Pfeiffer, P.Geo. 

John Sims, CPG 

Yves Breau, P.Eng. 

Rick Greenwood, P.Geo. 

Agung Prawasono, P.Eng.

 

Effective Date: December 31, 2022 

Issue Date: February 13, 2023

 

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Contents

 

 

1. SUMMARY   1
  1.1 Executive Summary   1
  1.2 Technical Summary   6
       
2. INTRODUCTION   12
  2.1 Qualified Persons   12
  2.2 Sources of Information   12
  2.3 Effective Date   13
  2.4 List of Abbreviations   14
       
3. RELIANCE ON OTHER EXPERTS   15
       
4. PROPERTY DESCRIPTION AND LOCATION   16
  4.1 Location   16
  4.2 Mineral Tenure   16
  4.3 Mineral Claim Ownership Details   19
  4.4 Environmental Liabilities and Other Significant Factors   19
  4.5 Permitting   19
  4.6 Other Liabilities   20
       
5. ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY   21
  5.1 Accessibility   21
  5.2 Climate   21
  5.3 Local Resources   22
  5.4 Infrastructure and Community Services   22
  5.5 Physiography and Environment   23
       
6. HISTORY   24
  6.1 88-4 Zone (Limb Zone)   30
  6.2 NS Zone (Hinge Zone)   30
  6.3 LP Zone   31
  6.4 Production   31
       
7. GEOLOGICAL SETTING   32
  7.1 Regional Geology   32
  7.2 Local Geology   38
  7.3 Project Geology   41
  7.4 Mineralization Styles and Target Areas   50
  7.5 Metamorphism and Alteration   59
  7.6 Structural Geology   60
       
8. DEPOSIT TYPES   64
       
9. EXPLORATION   65
       
10. DRILLING   66
  10.1 Summary   66
  10.2 Kinross 2022 Drilling Program   66
       
11. SAMPLE PREPARATION, ANALYSES, AND SECURITY   71
  11.1 Sample Security   71

TOC i 

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

  11.2 Sample Preparation and Analysis   71
  11.3 Quality Assurance/Quality Control   73
  11.4 QP Opinion   106
       
12. DATA VERIFICATION   107
  12.1 AGP Site Inspection   107
  12.2 Independent Sample Analysis   121
  12.3 QP Opinion   123
       
13. MINERAL PROCESSING AND METALLURGICAL TESTING   124
  13.1 Introduction   124
  13.1 Blue Coast Test Programs Results   124
  13.2 SGS Metallurgical Scoping Test Work 2022   132
       
14. MINERAL RESOURCE ESTIMATE   146
  14.1 Summary of Mineral Resources   146
  14.2 LP Zone Mineral Resource Estimate   146
  14.3 Hinge and Limb Zone Mineral Resource Estimate   176
  14.4 Underground Mineral Resource Sensitivity   190
       
15. MINERAL RESERVE ESTIMATE   191
       
16. MINING METHODS   192
       
17. RECOVERY METHODS   193
       
18. PROJECT INFRASTRUCTURE   194
       
19. MARKET STUDIES AND CONTRACTS   195
       
20. ENVIRONMENTAL STUDIES, PERMITTING, AND SOCIAL OR COMMUNITY IMPACT   196
       
21. CAPITAL AND OPERATING COSTS   197
       
22. ECONOMIC ANALYSIS   198
       
23. ADJACENT PROPERTIES   199
       
24. OTHER RELEVANT DATA AND INFORMATION   201
       
25. INTERPRETATION AND CONCLUSIONS   202
  25.1 Geology and Mineral Resources   202
  25.2 Metallurgical Testing   203
       
26. RECOMMENDATIONS   205
  26.1 Exploration Drilling   205
  26.2 Project Development   206
  26.3 Advanced Exploration Program   207
       
27. REFERENCES   208
       
28. DATE AND SIGNATURE PAGE   211
       
29. CERTIFICATE OF QUALIFIED PERSON   212
  29.1 Nicos Pfeiffer   212
  29.2 John Sims   214
  29.3 Yves Breau   216
  29.4 Rick Greenwood   218
  29.5 Agung Prawasono   219

 

30. APPENDIX 1 - LAND TENURE   221

TOC ii 

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Tables

 

 

Table 1-1: Summary of Project Mineral Resources – December 31, 2022   1
Table 2-1: Qualified Persons and their responsibilities   12
Table 6-1: Exploration history 1944-February 2022   24
Table 6-2: Summary of Historical Drilling (1944 to February 2022)   27
Table 7-1: Regional geology from Sanborn-Barrie et al., 2004   35
Table 10-1: Statistics of 2022 drilling   68
Table 11-1: Summary of control samples – 2017 to 2019   74
Table 11-2: Summary of control sample results – 2017 to 2019   75
Table 11-3: Summary of control samples – 2020 – 2022 Great Bear drill programs   90
Table 11-4: Summary of CRMs for 2020 – 2022 Great Bear drill program   92
Table 11-5: Summary of control samples – 2022 Kinross drill program   97
Table 11-6: Summary of CRMs for 2022 Kinross drill program   99
Table 11-7: Summary of control samples – 2022 Kinross RC drill program   102
Table 11-8: Summary of CRMs for 2022 Kinross RC drilling program   103
Table 12-1: Drill hole collar locations - Hinge and Limb Zones   109
Table 12-2: Drill hole collar locations - LP Zone   109
Table 12-3: Summary of selected drill core for review   111
Table 12-4: Summary of independent samples   122
Table 12-5: Independent sample results   122
Table 13-1: Quantitative analysis - Dixie Project composite head assays   125
Table 13-2: Semi-quantitative ICP scan analysis - Dixie Project multi-element ICP scan   126
Table 13-3: Semi-quantitative ICP scan analysis - LP multi-element ICP scan   127
Table 13-4: Leaching results summary   129
Table 13-5: Screened metallics for Au analysis   136
Table 13-6: Screened metallics for Ag analysis   136
Table 13-7: Quantitative analyses of the samples   137
Table 13-8: Semi-quantitative analyses of the samples   138
Table 13-9: XFR analysis of the samples   139
Table 13-10: Comminution parameters   140
Table 13-11: Gold data, coarse bottle roll cyanide leach test results (heap leach amenability)   141
Table 13-12: Silver data, coarse ore bottle roll cyanide leach test results (heap leach amenability)   141
Table 13-13: Gravity separation Au test results   143
Table 13-14: Gravity separation Ag test results   143
Table 13-15: Gravity separation tailing cyanide leach results, the effects of grind size   144
Table 14-1: Summary of Project Mineral Resources – December 31, 2022   146
Table 14-2: LP Zone Mineral Resource summary – December 31, 2022   147
Table 14-3: Open pit Mineral Resource sensitivity - LP Zone   148
Table 14-4: Uncapped statistics of composite data by domain   154
Table 14-5: Capped statistics of composited data by domain   155
Table 14-6: Summary of variogram parameters by domain   158
Table 14-7: Block model extents and the block parameters   159

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Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Table 14-8: Description of block model variables   160
Table 14-9: Variables using majority codes, averages, and weighted averages   161
Table 14-10: Comparison of tonnes, grade, and ounces in common blocks between the ground truth and long term models   171
Table 14-11: Kinross corporate guidance for reconciliation variance   171
Table 14-12: Hinge and Limb Zone Mineral Resource summary – December 31, 2022   176
Table 14-13: Capped and uncapped composite statistics by domain   182
Table 14-14: Block model variables description   185
Table 14-15: Ellipsoid search distances for each estimation domain   186
Table 14-16: Underground Inferred Mineral Resource sensitivity - LP, Hinge, and Limb   190
Table 30-1: Great Bear claim list   222

 

Figures

 

 

Figure 4-1: Location map   17
Figure 4-2: Land tenure for Great Bear Property   18
Figure 5-1: Property access   21
Figure 5-2: Low rolling topography, partially forested, with mature stands and younger growth of black spruce   23
Figure 6-1: Great Bear Project historical diamond drilling   29
Figure 7-1: Regional setting of Great Bear Property within the Uchi Subprovince, on the south margin of the ca. 3 Ga North Caribou Terrane   33
Figure 7-2: Regional Red Lake District geology with active and past producing mines   34
Figure 7-3: Property scale regional geology   35
Figure 7-4: Interpreted geology from drilling, prospecting, and geophysics   38
Figure 7-5: Schematic illustration of documented subaqueous felsic lava deposits   39
Figure 7-6: Schematic stratigraphy column for the Great Bear Project   41
Figure 7-7: Dry core sample of Sediments from BR-051 at 87.5 m   42
Figure 7-8: Dry core sample of Felsic Volcaniclastic from BR-046 at 87.5 m   42
Figure 7-9: Wet core sample of Felsic Volcanic from DNW-011 at 13.2 m   43
Figure 7-10: Dry core photo of Metasediments (2) from BR-065 at 264 m   43
Figure 7-11: Wet core photo of Metasediments (2) from DNW-011 at 133.15 m   44
Figure 7-12: Wet core photo of Felsic Volcanic (2) from DNW-011 at 141.45 m   44
Figure 7-13: Wet core photo of Metasediments (3) from DNW-011 136.3 m and BR-060 315 m   45
Figure 7-14: Wet core photo of Fragmental from BR-036 at 413 m to 420 m   46
Figure 7-15: Wet core photo of Fragmental from DL-018 at 112 m   47
Figure 7-16: Wet core photo of Mafic Volcanic – Fe-Tholeiite – Biotite Calcite Pillows from DL-018 at 136 m   47
Figure 7-17: Dry core photo of Argillite from DHZ-026 at 48 m   48
Figure 7-18: Wet core photo of Mafic Volcanic – High Mg-Tholeiite – Massive Basalt from DL-024 at 145.5 m   49
Figure 7-19: Dry core photo of Mafic Volcanic – High Fe-Tholeiite – Pillow Basalt from DL-024 at 25.0 m   49
Figure 7-20: Wet core photo of Ultramafic from DHZ-039 at 141 m   50
Figure 7-21: Wet core photo of Feldspar Porphyry Dyke from DHZ-001 at 244.3 m   50

TOC iv 

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Figure 7-22: Internal Great Bear Resources Ltd. interpreted geology showing mineralization zones at the Project   51
Figure 7-23: Silica sulphide replacement style mineralization of the Limb Zone   52
Figure 7-24: Limb Zone with significant gold intercepts and MSO shapes looking northeast   53
Figure 7-25: Hinge Zone style vein from DHZ-014 at 184.5 m   54
Figure 7-26: Vertical section of Hinge Zone, looking northeast (± 7.5 m) with significant assays and MSO shapes   55
Figure 7-27: Plan view of gold values >2.3 g/t for the LP Zone with geology and LP sub-zones   56
Figure 7-28: Strong strained Felsic Volcanic with 5% to 10% fine-grained arsenopyrite and 1% fine visible gold in the foliation in BR-020 at 90.15 m 57
Figure 7-29: Visible gold in foliation hosted by strained porphyritic Felsic Volcanic from DNW-011 at 58.25 m   58
Figure 7-30: Recrystallized amphibole overprinting foliation (possible actinolite) and biotite alteration in contact with quartz vein (red line)   59
Figure 7-31: Property structural interpretation showing folded terrains (grey shaded) and the Central (coloured) High Strain Corridor   60
Figure 7-32: Conceptual sequence of Great Bear area deformation events (not to scale)   62
Figure 7-33: Stereonets showing rotated foliation fabrics along the trend of the LP Fault Zone   63
Figure 10-1: Drill holes from the 2022 drill program   67
Figure 11-1: Graphical representation of total samples submitted and failure rates at SGS vs ActLabs   76
Figure 11-2: Blank reference material BL-10   77
Figure 11-3: Control plot for BLK blank material (BL-10 and BLM combined); April 2017 – May 2019   78
Figure 11-4: Control plot for BL-10 blank material; June 2019 to December 2019   78
Figure 11-5: Control plot for BLM blank material; June 2019 to December 2019   79
Figure 11-6: Control plot for SRM GS12A   80
Figure 11-7: Control plot for SRM GS1P5Q   81
Figure 11-8: Control plot for SRM GS1P5R   81
Figure 11-9: Control plot for SRM GS2S   82
Figure 11-10: Control plot for SRM GS4H   82
Figure 11-11: Control plot for SRM GS5W (Fire Assay)   83
Figure 11-12: Control plot for SRM GS5W (Gravimetric Finish)   83
Figure 11-13: Control plot for SRM GSP5E   84
Figure 11-14: Control plot for SRM OREAS 209   84
Figure 11-15: Control plot for SRM OREAS 214   85
Figure 11-16: Control plot for SRM OREAS 221   85
Figure 11-17: Control plot for SRM OREAS 224   86
Figure 11-18: Control plot for SRM OREAS 228   86
Figure 11-19: Scatter plot for field duplicates   88
Figure 11-20: Control plot for coarse reject analyses from SGS, Actlabs and ALS Global   89
Figure 11-21: Control plot BLM   91
Figure 11-22: Control plot for BLK   91
Figure 11-23: Control plot for CDN-GS-1W   93
Figure 11-24: Control plot for CDN-GS-4H   93
Figure 11-25: Control plot for CDN-GS-P5E   94
Figure 11-26: Control plot for OREAS 221   94

TOC v 

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Figure 11-27: Control plot for OREAS 226   95
Figure 11-28: Control plot for OREAS 232   95
Figure 11-29: Control plot for field duplicates; January 2020 to March 2021   96
Figure 11-30: Control plot for BLK   98
Figure 11-31: Control plot for BLK_PStone   98
Figure 11-32: Control plot for OREAS 230   100
Figure 11-33: Control plot for OREAS 233   100
Figure 11-34: Control plot for OREAS 238   101
Figure 11-35: Control plot for OREAS 240   101
Figure 11-36: Control plot for BLK   103
Figure 11-37: Control plot for CDN-GS-12B   104
Figure 11-38: Control plot for OREAS 211   104
Figure 11-39: Control plot for OREAS 233   105
Figure 11-40: Scatter plot for field duplicates   106
Figure 12-1: Drill hole collars BR-207 (left, LP Zone), DHZ-060 and 061 (right, Hinge Zone)   108
Figure 12-2: Drill logging and sampling facility at 117 Forestry Road   112
Figure 12-3: Drill logging table; 117 Forestry Road   113
Figure 12-4: Core cutting area; 117 Forestry Road   113
Figure 12-5: Drill logging and sampling facility at 2 Industrial Park Road and 19 Young Street   115
Figure 12-6: Drill logging tables at the 2 Industrial Park Road facility   116
Figure 12-7: Drill core cutting room at the 2 Industrial Park Road facility   117
Figure 12-8: Strapped core boxes (by drill hole), temporary core storage at the 2 Industrial Park facility   118
Figure 12-9: Core racks at the core storage area; Project site   119
Figure 12-10: Coarse rejects under tarpaulin at the core storage area; Project site   120
Figure 12-11: Historic drill core storage area; near Hinge and Limb Zone   121
Figure 13-1: Metallurgical sample locations from current and historical drill sites for test work programs   135
Figure 13-2: EGRG test summary results   142
Figure 14-1: LP Zone estimation domains, looking northwest   150
Figure 14-2: LP Zone estimation domains segmented by parallel east-west trending shear zones   151
Figure 14-3: LP Zone cumulative log histogram of assay sample lengths   152
Figure 14-4: LP Zone contact plots: transition from background domains to bulk domains (left) and bulk domains to high-grade domains (right)   153
Figure 14-5: LP Zone capping analysis   154
Figure 14-6: Directional variograms for LP Zone domain 1500 estimated using OK   157
Figure 14-7: Experimental variogram models of the Auro domain   165
Figure 14-8: RC drill program assays within the high-grade population supporting strong continuity at 50 m and reasonable continuity at 75 m spacing   166
Figure 14-9: LP Zone classification shells based on drill hole spacing   167
Figure 14-10: Swath plots in major block model directions for gold as compared to the NN estimate for gold   169
Figure 14-11: Ground truth model based on 8 m x 10 m RC grade control drilling   170
Figure 14-12: Comparison of ground truth model to long-term model grade tonnage curves   170
Figure 14-13: LP resource open pit shell in 3D   173

TOC vi 

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Figure 14-14: LP underground resource shapes   175
Figure 14-15: Lithological model section cutting the main Limb vein with the folded metasedimentary layer   178
Figure 14-16: Limb and Hinge histogram of assay sample lengths   179
Figure 14-17: Limb and Hinge contact plot figures   180
Figure 14-18: Limb 101 domain capped and uncapped statistics   181
Figure 14-19: Hinge 201 domain capped and uncapped statistics   182
Figure 14-20: Variogram model for Limb 101 domain estimated using OK   184
Figure 14-21: Octree block model setup in Leapfrog   185
Figure 14-22: Classification for Limb looking northeast (left) and Hinge looking northwest (right)   188
Figure 14-23: Underground Hinge and Limb resource shapes looking northwest   190
Figure 23-1: Location of the Great Bear Project and adjacent projects   199

TOC vii 

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

1.Summary

 

1.1Executive Summary

 

Kinross Gold Corporation (Kinross) has prepared a Technical Report (the Technical Report) for its wholly-owned Great Bear gold project (the Project or the Property), located in northwest Ontario, Canada. This Technical Report conforms to National Instrument 43-101 Standards of Disclosure for Mineral Projects (NI 43-101).

 

The Project is a gold exploration property located within the Red Lake Mining District of Ontario, an area of historic gold mining and exploration. The Project is located 24 km southeast of the town of Red Lake, Ontario and is comprised of 471 unpatented mining claims totalling 9,140 hectares (ha). Kinross acquired the Project through acquisition of Great Bear Resources Ltd. (Great Bear) in February 2022 and now owns a 100% interest in the Property.

 

The purpose of this Technical Report is to support an initial Mineral Resource estimate with an effective date of December 31, 2022.

 

Mineral Resources were estimated for three target areas at the Property, the LP Zone and the satellite Hinge and Limb Zones, and are summarized in Table 1-1 with an effective date of December 31, 2022. Canadian Institute of Mining, Metallurgy and Petroleum (CIM) Definition Standards for Mineral Resources and Mineral Reserves dated May 10, 2014 (CIM (2014) Definitions) were used for classification of Mineral Resources.

 

Table 1-1: Summary of Project Mineral Resources – December 31, 2022

 

Classification  Tonnes
(000)
   Grade
(g/t Au)
   Gold Ounces
(000)
Measured   -   -   - 
Indicated   33,110   2.57   2,737 
TOTAL M&I   33,110   2.57   2,737 
Inferred   20,037   3.56   2,290 

 

Notes:

1.Mineral Resources estimated according to CIM (2014) Definitions.

2.Mineral Resources estimated at a gold price of US$1,700 per ounce.

3.Open pit Mineral Resources are estimated at a cut-off grade of 0.5 g/t Au. The LP Zone pit shell was selected at an input gold price of US$1,400/oz (for volume), but resources are reported based on a US$1,700/oz cut-off value.

4.Underground Mineral Resources are estimated at cut-off grades of 2.3 g/t for the LP and Hinge zones and 2.5 g/t Au for the Limb Zone.

5.Numbers may not add due to rounding.

Page 1

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

The QP is not aware of any environmental, permitting, legal, title, taxation, socio-economic, marketing, political, or other relevant factors that could materially affect the Mineral Resource estimate.

 

Conclusions

 

Geology and Mineral Resources

 

The Project lies within a regional northwest-southeast trending belt of metavolcanic and metasedimentary rocks which are bounded by intrusive batholiths.

 

Three zones of mineralization have been identified within the Project area, LP, Limb, and Hinge, representing three dominant styles of mineralization: silica sulphide replacement, quartz veining, and disseminated gold in a high strain corridor.

 

A combined total of 1,170 drill holes totalling 563,191 m have been drilled by Great Bear and Kinross between January 1, 2017 and December 31, 2022.

 

Mineral Resources conform to CIM (2014) Definitions.

 

As of December 31, 2022, Mineral Resources at the Project consist of:

 

Indicated: 33.1 Mt grading 2.57 g/t Au and containing 2.7 Moz of gold.

 

Inferred: 20.0 Mt grading 3.56 g/t Au and containing 2.3 Moz of gold.

 

The sample preparation and analyses are adequate for this type of deposit and style of gold mineralization and the sample handling and chain of custody, as documented, meet standard industry practice.

 

The quality assurance and quality control (QA/QC) program is in accordance with standard industry practice and CIM Estimation of Mineral Resources and Mineral Reserves Best Practice Guidelines dated November 29, 2019 (MRMR Best Practice Guidelines). Kinross personnel have taken reasonable measures to ensure that the sample analysis completed is sufficiently accurate and precise and that, based on the statistical analysis of the QA/QC results, the assay results are accurate and reliable and are suitable for Mineral Resource estimation.

 

The data used to support a Mineral Resource estimate are subject to validation using built-in software program that automatically triggers a data check for a range of data entry errors. Verification checks on surveys, collar coordinates, lithology, and assay data have been conducted. The checks were appropriate and consistent with industry standards.

Page 2

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

A reverse circulation (RC) drill program was undertaken in 2022 to generate a ground truth model separate from the resource model for validation purposes. A total of 433 drill holes were completed on a 8 m x 10 m grid designed to re-create a grade control drill program on approximately a quarter of a year of estimated production from the open pit across a combination of low, medium, and high grade. The variance between the two models is currently well within Kinross quarterly Key Performance Indicators (KPI) providing good confidence that the resource model is performing well.

 

The sample descriptions, sampling procedures, and data entries were conducted in accordance with industry standards.

 

The database is representative and adequate to support a Mineral Resource estimate for the Project.

 

An open pit and underground scenario was contemplated for the LP Zone and an underground scenario, for the Hinge and Limb zones. The open pit and underground resources were constrained within $1,400 open pit resource shells and $1,700 underground mineable shapes, respectively, and fulfill the CIM (2014) Definitions requirement of “reasonable prospects for eventual economic extraction” (RPEEE).

 

Metallurgical Testing

 

The following conclusions were noted based on the preliminary metallurgical test work carried out by Blue Coast Research Ltd. (Blue Coast Research) in 2020 and 2021:

 

Gold from each composite was readily cyanide soluble with extraction during standard cyanide leach tests ranging from 95% to 99%.

 

The addition of lead nitrate did not improve overall leach recovery from the LP material. Lead nitrate addition improved extraction kinetics from the highest-grade composite only. Extraction kinetics from all other composites were unaffected by the addition of lead nitrate.

 

Cyanide consumption was low, averaging 0.19 kg NaCN/tonne over all tests.

 

Higher sulphide content was noted in the Limb samples.

Page 3

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

The addition of lead nitrate improved overall gold recovery and increased gold dissolution kinetics in the Limb samples. The improvement in gold dissolution kinetics was noted to be up to 24 hours in some instances.

 

Lead nitrate addition reduced the dissolution of sulphur and resulted in lower consumption of cyanide.

 

Pre-treatment with lead nitrate prior to the addition of cyanide did not result in any additional gold recovery, compared to when lead nitrate was added just prior to cyanide.

 

Grinding to 75 microns appeared to improve gold recovery slightly compared to primary grinds of approximately P80=125 μm.

 

A more comprehensive metallurgical testing program is currently underway at SGS Canada Inc. (SGS) and has the purpose of evaluating the metallurgical response of the mineralization, providing the key metallurgical data for selection of a suitable processing flowsheet for plant design, and estimating metallurgical recoveries and processing costs for financial modelling.

 

Recommendations

 

Based on the information presented in this Technical Report and results of the ongoing work on the Project, the QPs’ recommendations are summarized as follows.

 

All three target zones continue to warrant follow-up drilling. There is a three-fold objective for the continued drilling: establishing the extent of the deposit along strike and its depth potential, property-wide exploration, and definition drilling, with the first being the primary focus. The LP Zone is the most attractive target based on its potential size and high gold grades, and therefore continues to be prioritized.

 

Concurrently with drilling, the Project should continue with metallurgical and other technical studies and permitting. The Mineral Resource is substantial enough to initiate more advanced studies.

 

In addition, an Advanced Exploration Program (AEX) is recommended that would enable exploration drilling to be completed from underground, testing the depth of the deposit as well as better defining the deposit for engineering work.

 

Exploration Drilling

 

Exploration drilling at the Project should continue with multiple drill holes targeting both depth and strike potential. A specific focus should be on testing the deposit at and below the 1,000 m vertical depth to define the underground extents. For this purpose, additional drilling is proposed to be carried out on the Property. In conjunction with drilling, the Project should continue its ongoing highly technical program of data collection and analysis. The continued development of the geological model as well as continued geological mapping are considered highly important for Project advancement.

Page 4

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Specific exploration recommendations for 2023 and beyond are as follows:

 

1.Continue diamond drilling to test:

 

Extent of deposit along strike

 

Extent of deposit at depth

 

New targets throughout Property

 

Condemnation for potential infrastructure locations

 

Upgrade Inferred Mineral Resources to Indicated Resources where feasible, to allow for completion of technical studies and future Mineral Reserve estimation

 

Project Development

 

Based on the current Mineral Resources, the Project shows sufficient economic potential to initiate advanced studies.

 

The QPs recommend that Great Bear continue with engineering studies on ground conditions, site layout, metallurgical testing, soil geotechnical drilling and testing, and environmental baseline studies. Great Bear will continue to follow standard project development framework, with both open pit and underground studied. Specific Project recommendations for 2023 and beyond are summarized below:

 

1.Continue baseline environmental studies for input into permitting and engineering studies.

 

2.Continue to engage with our First Nations partners and local stakeholders.

 

3.Study the Project with engineering partners following project stage-gating (Scoping, PFS, FS).

 

4.Although the underground will not be fully defined, it is recommended that site infrastructure considers what the underground may become.

 

5.Further mine plan optimisation of the open pit and underground resource.

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Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

6.Continue with metallurgical studies to test the variability of the deposits considering the significant strike length and depth.

 

7.Implement geotechnical work on both the bedrock and soil geotechnical characterization including geophysics, drilling, and laboratory testing using a speciality consultant.

 

Advanced Exploration Program

 

The Property, centered around the LP Zone deposit, continues to be open at depth and additional drilling is required to estimate the potential at depth, approximately 500 vertical metres from surface. For this purpose, an AEX program should be evaluated which would require a portal and decline to be established to access the underground and drill from depth. The initial concept being contemplated would allow exploration drilling to start from approximately 600 vertical metres from surface and test the depth extent of the deposit. Due to the deposit’s characteristics, drilling from the underground is considered to be more feasible for upgrading the underground resource to a higher category. AEX has proved to be an efficient method to define underground deposits. AEX would also aid in the engineering studies and design of the future Project.

 

It is recommended by the QP that Great Bear complete the engineering and baseline environmental studies on the AEX program be completed as a priority and the Ontario permitting process be initiated.

 

1.2Technical Summary

 

Property Description, Location and Land Tenure

 

The Project is located in northwest Ontario, Canada, at latitude 50.8764°N and longitude 93.6398° (Universal Transverse Mercator (UTM) Zone 15N 455665E, 5633910N (NAD83)). Red Lake, the nearest municipality, is 24 km to the north-northwest of the Property. Red Lake consists of six small communities, Balmertown, Cochenour, Madsen, McKenzie Island, Red Lake, and Starratt-Olsen, and is an enclave within the Unorganized Kenora District. Red Lake is 535 km northwest of Thunder Bay and 250 km east of Winnipeg, Manitoba.

 

The Property consists of a contiguous block comprising 471 unpatented mining claims totaling 9,140 ha. Kinross’ wholly-owned subsidiary Great Bear owns 100% of the claims.

Page 6

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

History

 

The first exploration work on the Property documented by Geology Ontario dates to 1944, with mapping/prospecting, diamond drilling, and geophysical work continuing to present.

 

Prior to acquisition by Kinross in 2022, a total of 974 diamond drill holes (DDH) for 390,227 m had been completed on the Property (historically named the Dixie Lake Property) between 1944 and February 2022. Other exploration activities included geological mapping, airborne and ground-based geophysical surveys, and geochemical sampling.

 

Historically, the most significant drill programs on the Project were completed by Consolidated Silver Standard Mines Ltd. (1988), Teck Resources Ltd. (1989-1990), Alberta Star Mining Corp./Fronteer Development Group Joint Venture (2003-2004), Grandview Gold Inc. (2005-2011), and Great Bear (2017-2022). These programs focused on two main target areas historically identified as the 88-4 Zone and the NS Zone, currently known as the Limb Zone and Hinge Zone respectively. The most recent drill program conducted by Great Bear discovered and drill-tested the third and largest target on the Property, the LP Zone.

 

No production has taken place on the Property.

 

Geology and Mineralization

 

The Property lies within the Red Lake greenstone belt of the Uchi Subprovince of the Archean Superior Province of the Canadian Shield. The belt is one of the most prolific gold camps in Canada, with gold production over 29 million ounces (Moz) from multiple deposits, including the Campbell-Goldcorp (>23 Moz), Cochenor-Willans (1.2 Moz), and Madsen (2.4 Moz) mines.

 

Because of the overburden and lack of outcrop exposure throughout the Property, most of the previous geological interpretation was based on geophysics, limited regional scale mapping, and diamond drilling.

 

The Property area lies within a regional northwest-southeast trending belt of metavolcanic and metasedimentary rocks which are bounded by intrusive batholiths. The southwestern portion of the Property is within the mafic domain and consists of mafic volcanic flows (high Fe-tholeiites and high Mg-tholeiites) intercalated with argillite, siltstone, iron formation, and minor local felsic volcanics. The younger sequence of intermediate to mafic volcanic and volcanic derived sedimentary rocks is located at the centre of the Property and has a similar stratigraphy to the western and eastern portions of the Property. The felsic domain dominates the northeastern portion of the Property. It consists of porphyritic felsic flows (dacites) and volcaniclastics intercalated with sedimentary rocks. The sequence is interpreted as a deformed felsic flow-dome complex. The mafic domain is in contact with a largely felsic/sedimentary domain in the northeast portion of the Property.

Page 7

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Mafic volcanic dykes and sills are common throughout the Property, ranging from lamprophyre to gabbro/diorite. Intermediate felsic intrusive rocks are also noted throughout the region.

 

Three dominant styles of mineralization are observed within three target areas on the Property:

 

1.Silica-sulphide replacement – Limb Zone

 

Mineralization is associated with the rheological and geochemical contact between pillow basalt (Fe-tholeiites) and massive basalt and occurs as replacement of sediments, if present, or as silica flooding and quartz-calcite veining in the absence of sediments. Pyrrhotite (2% to 40%) is the dominant sulphide, with other sulphides including pyrite, arsenopyrite, chalcopyrite, minor sphalerite, and trace magnetite. Visible gold is not uncommon and, where observed, is associated with strong pyrrhotite and weaker arsenopyrite-pyrite mineralization. The zone is approximately 800 m long and has been drilled to a vertical depth exceeding 400 m. Mineralization plunges steeply northwest in a fold limb host dipping steeply to subvertically northeast.

 

2.Quartz veining – Hinge Zone

 

Mineralization is hosted by multiple lithologies including massive basalt (high Mg-tholeiite), argillite, and pillow basalt (high-Fe tholeiite). Individual veins are variable in width ranging from 1 cm to 5 m and can create zones up to 40 m. They are generally mineralized with fine-grained disseminated sulphides including pyrrhotite, pyrite, chalcopyrite, minor arsenopyrite, and trace sphalerite. Visible gold is very common ranging from trace to 5% as pin pricks, centimetre scale clusters, and fracture fill. The Hinge Zone is comprised of several subparallel anastomosing veins formed along the axial trace of a property wide D2 fold.

 

3.Disseminated gold within high strain – LP Zone

 

Mineralization occurs within a wide zone of high strain and increased metamorphic grade. The strain zone is very continuous for over 4 km and is slightly oblique to stratigraphy, intersecting multiple lithologies. The higher-grade gold mineralization appears to be controlled by the intersection of this strain zone and a metasediment unit. Recent drilling results indicate that it occurs within 50 m to 100 m of the metasedimentary/felsic volcanic contact. At least three gold mineralizing events have been recognized, including foliation parallel free gold in host rock, transposed quartz veins, and later quartz veins with visible gold that are slightly oblique to foliation.

Page 8

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Exploration

 

Due to overburden and lack of outcrop in the area, exploration targets at the Project were interpreted from geophysical and surface geochemical surveys. These exploration tools included airborne magnetic and electromagnetic (EM) surveys, ground magnetics, very low frequency electromagnetic (VLF-EM), horizontal loop/Max-Min EM, induced polarization (IP), soil, mobile metal ion (MMI), and rock sampling. Anomalies and conductors from the geophysical surveys predominantly coincide with iron formation, graphitic argillites, and sulphide-bearing (pyrite and/or pyrrhotite) argillites, or mafic volcanics. The geochemical surveys, which were typically completed over the geophysical surveys, were then used to vector in on the most prospective targets for diamond drilling.

 

Diamond drilling has been carried out since 1944 and totals 597,194 m in 1,359 drill holes. Of these, Kinross has drilled 397 holes for a total of 206,967 m. In addition, Kinross has completed an RC drill program for a total of 34,530 m in 433 holes. The objective of the Kinross 2022 drill program was five-fold:

 

1.Test the extents of known drill targets.

 

2.Infill zones of potentially economic mineralization to meet Inferred Mineral Resource classification status.

 

3.Carry out condemnation drilling to identify areas that may be used for capital development.

 

4.Begin drill testing the deep extension of the mineralization at a greater than one kilometre depth.

 

5.Mimic production drilling by drilling a tight grid of RC drill holes that would provide data for a ground truth block model.

 

Metallurgical Testing

 

Two test work programs were completed by Blue Coast Research in 2020 and 2021 to provide an initial understanding of gold dissolution using standard cyanidation methods on composites from the LP, Hinge, and Limb zones of the Great Bear deposit. Additional cyanidation tests were conducted to evaluate the impacts of grind size, cyanide concentration, and lead nitrate addition on gold leaching.

Page 9

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Following the acquisition, Kinross retained SGS to perform a more comprehensive test program, namely the Scoping Test Work program. This metallurgical testing program is underway at SGS. The evaluation program includes a wide range of characterization tests comprised of detailed chemical head analysis, mineralogy, comminution, and ore sorting. Gold recovery testing incorporates a brief investigation of the heap leaching option, and a detailed examination of standard milling circuit options, including gravity separation, flotation, and cyanide leaching. A rheometallurgical program covering thickening, rheology, and filtration is also included as well as a baseline acid rock drainage (ARD) testing on final tailings from selected leach tests. The results of the SGS test program are pending as of the effective date of this Technical Report.

 

Mineral Resource Estimate

 

A summary of the Mineral Resource estimate is provided in Table 1-1.

 

LP Zone

 

Snowden Supervisor v 8.14.2 (Supervisor) was used for geostatistical analysis, Leapfrog Geo 2021.5 (Leapfrog) was used to generate estimation domains, and Vulcan 2022.3 (Vulcan) was used for compositing and estimation. The bulk estimation domains were interpolated by ordinary kriging (OK), while the high-grade estimation domains and background domain were interpolated using inverse distance cubed (ID3).

 

The 2022 Great Bear LP Zone Scoping Study model classification criteria are based upon the geostatistical drill hole spacing analysis supported by historic exploration and deposit growth drilling, as well as the recent 2022 drill campaign designed to upgrade unclassified material to Inferred status in and around the preliminary pit area at the LP Zone. Drill hole distance criteria of 50 m and 75 m were used for classification of Indicated and Inferred material, respectively.

 

The LP zone pit shell was selected at an input gold price of US$1,400/oz (for volume), but resources are reported based on a US$1,700/oz cut-off grade. The US$1,400/oz shell size was selected as a result of initial optimizations between open pit and underground. Furthermore, only the Central section of the LP Zone was considered for open pit resource, with Discovery (NW) and Viggo (SE) areas considered entirely underground resource.

 

As of December 31, 2022, open pit Mineral Resources are estimated to total 33.1 Mt of Indicated material grading 2.57 g/t Au and containing 2.7 Moz of gold and 8.4 Mt of Inferred material grading 2.24 g/t Au and containing 606,000 oz of gold in the Inferred category. The underground Mineral Resources are estimated to total 10.6 Mt grading 4.54 g/t Au and containing 1.5 Moz, all classified as Inferred.

Page 10

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Hinge and Limb Zones

 

Snowden Supervisor v8.14.3.1 was used for geostatistical analysis and Leapfrog Geo/Edge 2022.1.1 for geological and domain modelling, compositing, and estimation. The Limb estimation domains comprise a mineralized zone within metasediments with silica and sulphide replacement hosted in the north limb of the fold. The Hinge estimation domains encompass quartz veins within a tholeiitic basalt in the axial plane of the fold. The main vein at Limb was interpolated using OK and the remaining lenses, using ID3. The model classification criteria are based on drilling spacing analysis, 75 m for Limb and 50 m for Hinge, considering the differences in the mineralization and its continuity between the two zones.

 

The Mineral Resources were reported within underground reporting shapes generated using the MSO tool, and defined using a minimum stope thickness of 2.0 m, limited to areas of continuous mineralization. The cut-off grades were 2.3 Au g/t for the Hinge Zone and 2.5 Au g/t for the Limb Zone.

 

As of December 31, 2022, the combined Hinge and Limb underground Mineral Resources were estimated to total approximately 1.1 Mt grading 4.07 g/t Au and containing 137K oz of gold in the Inferred category.

Page 11

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

2.Introduction

 

Kinross Gold Corporation (Kinross) has prepared a Technical Report (the Technical Report) for its wholly-owned Great Bear gold project (the Project or the Property), located in northwest Ontario, Canada. This Technical Report conforms to National Instrument 43-101 Standards of Disclosure for Mineral Projects (NI 43-101).

 

The Project is a gold exploration property located within the Red Lake Mining District of Ontario, an area of historic gold mining and exploration. The Project is located 24 km southeast of the town of Red Lake, Ontario and is comprised of 471 unpatented mining claims totalling 9,140 hectares (ha). Kinross acquired the Project through acquisition of Great Bear Resources Ltd. (Great Bear) in February 2022 and now owns a 100% interest in the Property, with Great Bear Resources Ltd. the registered holder.

 

The purpose of this Technical Report is to support an initial Mineral Resource estimate with an effective date of December 31, 2022.

 

2.1Qualified Persons

 

The Qualified Persons (QP) for this Technical Report are summarized in Table 2-1:

 

Table 2-1: Qualified Persons and their responsibilities

 

QP Name, Designation, Title   Site Visit   Responsible for
Nicos Pfeiffer, P.Geo.
Vice President Geology
  Multiple in 2022   Section 14 (except Mineral Resource Reporting)
John Sims, CPG
Company Qualified Person, President of Sims Resources LLC
  October 19 and 20, 2022   Overall preparation of the Technical Report and in particular, Sections 1 to 10, and 23 to 27
Yves Breau, P.Eng.
Vice-President Metallurgy, Engineering and Energy
  March 2022   Section 13
Rick Greenwood, P.Geo.
Exploration Manager
  Full time employee at Project site   Sections 11 and 12
Agung Prawasono, P.Eng., PMP, Senior Director, Mine Planning   June 24, 2022   Section 14 (Mineral Resource Reporting)

 

2.2Sources of Information

 

The Kinross QPs visited the Project as indicated in Table 2-1.

Page 12

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

While at the Project site, the Kinross QPs held discussions with site technical personnel; visited the proposed open pit site, drill rigs in the field, and core logging facility to review core and logging procedures; reviewed data collection and QA/QC procedures, geological interpretations, geological modelling, and resource estimation procedures; and reviewed existing infrastructure.

 

Information used to support this Technical Report has been derived from the reports and documents listed in Section 27 References of this Technical Report.

 

2.3Effective Date

 

The effective date of the Mineral Resource estimate is December 31, 2022. There were no material changes to the information on the Project between the effective date and the signature date of the Technical Report.

Page 13

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

2.4List of Abbreviations

 

Units of measurement used in this Technical Report conform to the metric system. All currency in this Technical Report is in US dollars (US$) unless otherwise noted.

 

µm micrometre kWh kilowatt-hour
°C degree Celsius L litre
a annum m metre
C$ Canadian dollars M mega (million)
cm centimetre m2 square metre
d day m3 cubic metre
dia. diameter Ma million years
g gram MASL metres above sea level
G giga (billion) min minute
Ga billion years mm millimetre
g/L gram per liter Moz million ounces
g/t gram per tonne Mst million short tons
ha hectare Mt million tonnes
in inch oz Troy ounce (31.1035g)
kg kilogram ppm part per million
km kilometre s second
km/h kilometre per hour st short ton
km2 square kilometre t metric tonne
kWh/t kilowatt-hour per tonne US$ United States dollar
kW kilowatt yr year

Page 14

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

3.Reliance on Other Experts

 

In the preparation of the Technical Report, the Qualified Persons relied on information provided by internal Kinross legal counsel for the discussion of claim numbers, title types, anniversary dates and confirmation that the claims are in good standing as of the date of this Technical Report summarized in Sections 1, 4, and Appendix 1.

Page 15

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

4.Property Description and Location

 

4.1Location

 

The Project is located in northwest Ontario, Canada (Figure 4-1) at latitude 50.8764°N and longitude 93.6398° (Universal Transverse Mercator (UTM) Zone 15N 455665E, 5633910N (NAD83)). Red Lake, the nearest municipality, is 24 km north-northwest of the Property. Red Lake consists of six small communities—Balmertown, Cochenour, Madsen, McKenzie Island, Red Lake, and Starratt-Olsen—and is an enclave within the Unorganized Kenora District. Red Lake is 535 km northwest of Thunder Bay, Ontario and 250 km east of Winnipeg, Manitoba.

 

4.2Mineral Tenure

 

The Property consists of a contiguous block comprising 471 unpatented mining claims totalling 9,140 ha, shown in Figure 4-2 and listed in Appendix 1 Table 30-1 of this Technical Report. Kinross’ wholly-owned subsidiary Great Bear Resources Ltd. (Great Bear) owns 100% of the claims.

 

Of the 471 unpatented mining claims, 436 are termed as Single Cell Mining Claims (SCMC) meaning that the claim holder holds the entirety of the mining cell. The remaining 35 unpatented claims are classified as Boundary Cell Mining Claims (BCMC) meaning that the claim is a partial cell and the cell is shared with another property owner. If, at any time, the other claim holder was to abandon or forfeit their portion of any of the BCMC, it would be converted to SCMC and the balance of the map cell would become part of the Great Bear Property. The 471 unpatented mining claims which comprise the Property are currently in good standing and assessment work credits are sufficient to maintain that standing for several years. The government of Ontario requires expenditures of $400 per year per SCMC, prior to expiry, to keep the claims in good standing for the following year(s). BCMC require expenditures of $200 per year. The Assessment Report describing the work completed by the company must be submitted by the expiry date of the claims to which the work credit is to be applied.

Page 16

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

 

Figure 4-1: Location map

Page 17

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Figure 4-2: Land tenure for Great Bear Property

Page 18

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

 

4.3Mineral Claim Ownership Details

 

In February 2022, Kinross completed the acquisition of Great Bear for approximately $1.4 billion. Great Bear Resources Ltd. owns 100% of the Great Bear Property.

 

The Property is subject to a 2% net smelter return (NSR) royalty that was granted by Great Bear to Great Bear Royalties Corp. on January 31, 2020. In September 2022, Great Bear Royalties Corp. was acquired by a wholly-owned subsidiary of Royal Gold Inc.

 

As the land is crown land, legal access to the claims is available by public roads which cross the Property.

 

4.4Environmental Liabilities and Other Significant Factors

 

No known environmental liabilities exist on the Property from historical or present processing or operations. Comprehensive soil and water quality baseline tests commenced in 2022 and are continuing into 2023. There are areas that have been hydraulically and/or mechanically stripped to expose bedrock in the past, and several small trenching programs have taken place. These disturbed areas have been recorded by the Ontario Geological Survey (OGS) and are considered part of the legacy work of the Project area.

 

4.5Permitting

 

Great Bear holds an Exploration Permit valid until November 23, 2025. This permit is issued under the authority of section 78.3 of the Mining Act and the Exploration Plans and Exploration Permits Regulation (O. Reg. 308/12). The permit covers multiple zones of high-grade mineralization across the Property and grants the company the right to use mechanized drilling (assembled weight of the drill >150 kg).

 

Great Bear holds a Land Use Permit (LUP) for a weather station on a 0.25 ha area. The LUP came into effect on May 1, 2022 and is valid until April 30, 2027.

 

Great Bear has a Memorandum of Understanding (MoU) with the Ministry of Natural Resources and Forestry (MNRF) for a bridge that crosses Dixie Creek, situated on public land as defined in section 1 of the Public Lands Act (RSO, 1990, c. P.43). The agreement is valid from February 23, 2020 to February 23, 2025.

Page 19

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

4.6Other Liabilities

 

The QP is not aware of any other factors or risks that would affect or limit access, title, or the right or ability to perform work on the Property.

Page 20

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

5.Accessibility, Climate, Local Resources, Infrastructure and Physiography

 

5.1Accessibility

 

Access to the Property from Red Lake is via Highway 105. From the highway turnoff, the claims are crossed by a network of all-season logging roads and seasonal trails built to service mineral exploration work (Figure 5-1). The southwestern portion of the claim is accessible by the Snake Falls Camp Road, where there is a small seasonal fishing camp.

 

 

 

Figure 5-1: Property access

 

5.2Climate

 

The climate is typically mid-continental. Summers are warm and humid, with frequent rain showers and thunderstorms. Winters are cold. Snow usually starts falling around late October or early November and starts melting around March. Temperatures in the summer range from 15°C to 28°C with temperatures dipping to an average of -10°C to -20°C in the winter, with lows reaching -35°C.

Page 21

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Total annual precipitation averages 6.3 cm. Snow accounts for approximately 24% of the precipitation. The summer months of June, July, August, and September account for more than half of the annual precipitation (54%). February is the driest month of the year, with an average precipitation of just 2.5 mm.

 

Exploration activities may be conducted year-round on the Property. Seasonal exploration activities, such as mapping and field sampling, are best conducted from May to October when there is no snow cover. Ground geophysical and diamond drilling programs can be conducted year-round but are preferred between late October and mid-March, when the lakes, streams, and muskeg are typically frozen, as well as in the drier summer months from May through September. This allows for easy mobilization of the heavy machinery required for drilling operations.

 

5.3Local Resources

 

Water Supply

 

Water is abundant year-round on the Project and in the region. There are numerous lakes, rivers, and swamps on the Project and in the area. Seasonal temperature variations require that heating systems be utilized for water transportation systems (i.e., drilling hose line) during the winter and late fall.

 

Power

 

Hydroelectric power lines follow Highway 105 and cross the northeastern corner of the Property and run parallel to the northeastern boundary.

 

5.4Infrastructure and Community Services

 

Red Lake is the closest community to the Project. It has a population of 4,094 residents, according to Statistics Canada in 2022. There is a fully functional airport that receives daily flights from Winnipeg, Manitoba and Thunder Bay, Ontario, Canada. The district has produced more than 28 million ounces (Moz) of gold since 1949, from four principal mines, only one of which is still in operation (Evolution’s Red Lake Gold Mine). Gold mining and seasonal tourism activity provide a stable economic base and the town offers all necessary facilities in support of mineral exploration efforts. Supplies and experienced, highly trained field personnel are available from the surrounding area and local communities.

Page 22

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

5.5Physiography and Environment

 

The regional topography features low, rolling hills with numerous small lakes and spruce bogs. On the Property, the terrain is gently sloping with an elevation range of 350 MASL to 460 MASL. There are a few streams, including Dixie Creek, that have mature, meandering courses. The Property is partially forested with mature stands and younger growth of black spruce, poplar, birch and jack pine, all typical species of the boreal forest (Figure 5-2).

 

 

Figure 5-2: Low rolling topography, partially forested, with mature stands and younger growth of black spruce

 

Bedrock occurrences are rare on the Property; where observed, they are typically glacially polished. In aid of prospecting activities, overburden has been stripped from some areas of the claims to expose the bedrock underneath. Overburden depth typically ranges from 5 m to 20 m and averages 15 m. Overburden has been observed to be as deep as 50 m in places.

Page 23

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

6.History

 

The first exploration work on the Property documented by Geology Ontario dates to 1944, with mapping/prospecting, diamond drilling, and geophysical work continuing to present.

 

Prior to acquisition by Kinross, a total of 974 diamond drill holes (DDH) for 390,227 m had been completed on the Property (historically named the Dixie Lake Property) between 1944 and February 2022. Other exploration activities included geological mapping, and airborne and ground-based geophysical and geochemical surveys. The exploration history is summarized in Table 6-1.

 

Table 6-1: Exploration history 1944-February 2022

 

Company   Year(s)   Description of Work   Area/Target
Boyle   1944   Drilling, x-ray, metres unknown   A-Zone (Main Zone)
Belgold Mines   1945   Prospecting   Dixie Lake Property
    Trenching   A, B, C, D zones, Dixie Lake Property
Caravelle Consolidated   1969-1972   Mapping   Dixie Lake Property
  1969   Airborne, magnetic (Mag), electromagnetic (EM) – 1/8 mile line spacing.   Dorothy Prospect – covers much of the Property
  1972   Drilling 5 holes, 372.85 m   Dixie Lake Property
Newmont Mining Corp.   1970   6 holes, 679.14 m   Dixie Lake Property
Kerr Addison Mines Ltd   1975   3 DDH, 306 m; EM, 32 line-miles Mag survey   Dixie Lake eastern central portion of the Property
Golden Terrace   1985   Airborne Mag, EM   Dixie Lake Property
Mutual Resources   1988   3 trenches, rock sampling   North, Main, and South showings, Dixie Lake Property
  1988   Ground Mag, very low frequency electromagnetics (VLF-EM), Max-Min – 31-33 line-km   Central part of the Dixie Lake Property
  1989   1 drill hole, 216.5 m   88-4 Zone
Consolidated Silver Standard Mines Ltd.   1988   7 BQ (36.5 mm) drill holes, 465 m   Dixie Lake Property, discovery of 88-4 Zone
    1989   Mapping   Dixie Lake Property

Page 24

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Company   Year(s)   Description of Work   Area/Target
Teck Resources Ltd./National Trust Co.
  1989   Ground Mag, VLF-EM – 217.5 line-km, 25 m stations on 100 m spaced lines   Portions of Main and South Grids, Dixie Lake Property
  1989   Diamond drilling, 28 BQ drill holes, 4,090 m   Dixie Lake Property, 88-4 Zone
  1990   Ground Mag, VLF-EM – 217.5 line-km, 25 m spacing Extensive airborne survey Three induced polarization (IP) test lines   Dixie Lake Property
  1990   Diamond drilling, 12 BQ drill holes, 1,999.48 m   Dixie Lake Property, 88-4 Zone, and other geophysical targets
Noranda   1990   Humus geochemistry, mapping, prospecting   Western Dixie Property
  1993   EM 27.85 LKM and 21.77 LKM MAG Survey, 2 DDH, 174.4 m   Western Dixie Property
  1994   Diamond drilling, 1 NQ (47.6 mm), 104.5 m, mapping, prospecting   Central Dixie Lake, Bruce Lake area
Cross Lake Minerals Ltd   1997   IP Survey 21 km, trenching   Dixie North
  1998   IP Survey 39.2 km, trenching   Dixie North, Dixie Northeast
Canadian Golden Dragon Resources Ltd.   1996   Humus geochemistry   Selected areas around IP anomalies, Dixie Lake Property
  1996-1997   IP – 153.6 line-km at 100 m to 200 m line spacing   Large portion of Dixie Lake Property
  1996   Diamond drilling, 12 NQ drill holes, 1,888 m   Dixie Lake Property, 88-4 Zone
  1997   Diamond drilling, 15 NQ drill holes, 2,566 m, testing IP anomalies   Dixie Lake Property
Cross Lake Minerals Ltd.   1997   Diamond drilling, 5 NQ drill holes, 836 m   Dixie Lake Property
Alberta Star Mining Corp./Fronteer Development Group   2003   Mobile Metal Ion (MMI) Survey   Dixie Lake Property, centered on 88-4 Zone
  2004   Ground Mag, diamond drilling, 12 drill holes, 4,370.9 m   88-4 Zone
Perry English   2004   Magnetic/Magnetometer Survey 43 LKM   Dixie Lake, South of Byshe Area
  2005   EM 27.4 line km, IP Survey 45.6 line km, line cutting   Dixie Lake Area

Page 25

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Company   Year(s)   Description of Work   Area/Target
Grandview Gold Inc./Fronteer Development Group   2003   Diamond drilling, 10 NQ drill holes, 2,185.5 m   88-4 Zone and one hole to the northwest of 88-4 Zone
  2004   MMI Survey, 927 samples, Ground Mag survey, 50 m line spacing   Dixie Lake Property
Grandview Gold Inc.   2005   Diamond drilling, 16 NQ drill holes, 2,772 m   14 DDH west of 88-4 Zone, 2 DDH in 88-4 Zone
  2006   Diamond drilling, 5 NQ drill holes, 1,033 m, MMI sampling   88-4 Zone
  2007   Mapping   Dixie Lake Property
  2007   Diamond drilling, 18 NQ drill holes, 5,117 m   88-4 Zone, Main Zone, South Zone, NS Zone, C-Zone, MMI-East
  2008   Diamond drilling, 3 NQ drill holes, 575.15 m   NS Zone
  2009   Diamond drilling, 7 NQ drill holes, 1,560 m   MMI Zone, Zone, Main, Zone, C- Zone, 88-4 Zone
  2011   Diamond drilling, 8 NQ drill holes, 1,611 m   MMI Zone, East Zone, Main Zone, C-Zone, 88-4 Zone
Larry Kenneth Herbert   2011-2012   Trenching, airborne Mag   East of Dixie Lake – North within Property boundary
Laurentian Goldfields Ltd.   2010-2013   Airborne Magnetometer 7184 line km. Mapping and prospecting   Dixie East
Great Bear Resources Inc.   2017-2022   Diamond drilling 770 NQ drill holes, 355,083 m, airborne Mag and SkyTEM, trenching, mapping, soil geochemistry, grab sampling   Hinge and Limb zones, LP Zone

 

Due to overburden and lack of outcrop in the area, exploration targets were interpreted from geophysical and surface geochemical surveys. These exploration tools include airborne magnetic and EM surveys, ground magnetics, VLF-EM, horizontal loop/Max-Min EM, IP, soil, MMI, and rock sampling. Anomalies and conductors from the geophysical surveys predominantly coincide with iron formation, graphitic argillites, and sulphide-bearing (pyrite and/or pyrrhotite) argillites, or mafic volcanics. The geochemical surveys, which were typically completed over the geophysical surveys, were then used to vector in on the most prospective targets for diamond drilling.

 

Historically, the most significant drill programs on the Project were completed by Consolidated Silver Standard Mines Ltd. (Consolidated Silver Standard, 1988), Teck Resources Ltd. (Teck, 1989-1990), Alberta Star Mining Corp./Fronteer Development Group Joint Venture (Alberta Star/Fronteer JV, 2003-2004), Grandview Gold Inc. (Grandview, 2005-2011), and Great Bear (2017-2022). These programs focused on two main target areas historically identified as the 88-4 Zone and the NS Zone. These zones are currently known as the Limb Zone and Hinge Zone respectively. The most recent drill program conducted by Great Bear discovered and drill-tested the third and largest target on the Property, the LP Zone. 

Page 26

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

A summary of historical drilling on the Project is provided in Table 6-2 and historical drilling is illustrated in Figure 6-1.

 

Table 6-2: Summary of Historical Drilling (1944 to February 2022)

 

Year   Company   Holes   Metres
1944   Drilling, x-ray, metres unknown   8    
1945   Belgold Mines, metres unknown   4    
1950   Unknown   9   284.5
1970   New Mont Mining Corp., Caravelle Mines Ltd, Omar Exploration   9   927.5
1972   Caravelle Mines Ltd   2   124.6
1975   Kerr Addison Mines   3   306.0
1988   Consolidated Silver Standard   7   465.7
1989   Teck Exploration Ltd   28   4,090.6
1990   Teck Exploration Ltd   13   2216
1993   Noranda   2   174.4
1994   Noranda   1   104.5
1996   Canadian Golden Dragon   12   1,888.4
1997   Canadian Golden Dragon, Cross Lake Minerals   20   3,402.3
2003   Fronteer Development Group Inc   10   2,389.5
2004   Fronteer Development Group Inc   12   4,370.9
2005   Grandview Gold Inc/Grandcru Resources   20   3,371.6
2006   Grandview Gold Inc   5   1,033.3
2007   Grandview Gold Inc   18   5,117.0
2008   Grandview Gold Inc/Trueclaim Resources   6   1,706.1
2009   Grandview Gold Inc   7   1,559.5
2011   Grandview Gold Inc   8   1,611.3
2017   Great Bear Resources Ltd   9   1,093.0
2018   Great Bear Resources Ltd   70   16,578.6
2019   Great Bear Resources Ltd   164   68,869.0

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Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Year   Company   Holes   Metres
2020   Great Bear Resources Ltd   192   110,673.5
2021   Great Bear Resources Ltd   305   138,253.1
Jan-Feb 2022   Great Bear Resources Ltd   30   19,616.1
TOTAL   974   390,227

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Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

 

 

Figure 6-1:          Great Bear Project historical diamond drilling 

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

6.188-4 Zone (Limb Zone)

 

This zone was initially identified by Consolidated Silver Standard as a 700 m long geophysical response, characterized by a strong northwest trending EM conductor, with coincident magnetic and VLF-EM anomalies. In 1988, Consolidated Silver Standard drilled this geophysical anomaly and intersected 4.97 g/t Au over 4.2 m (DL-88-4) which led to the discovery of the 88-4 Zone (now known as the Limb Zone). This zone is defined by silica sulphide replacement +/- quartz veining at the contact between a high Fe-tholeiite and high Mg-tholeiite and associated argillite.

 

The Teck exploration program (1989-1990) concentrated on delineating the strike extents of the 88-4 Zone to approximately 200 m depth.

 

Teck produced the only published resource estimate for the Property which was completed on the 88-4 Zone (Janzen, 1989). The estimate used standard methodologies for the time, but this work pre-dates NI 43-101 guidelines and would not meet current standards as defined by the Canadian Institute of Mining, Metallurgy and Petroleum (CIM). This estimate is relevant only for historical interest. The QP has not completed sufficient work to classify the historical estimate as a current Mineral Resource and Kinross is not treating this estimate as a current Mineral Resource. .

 

Great Bear continued to further delineate the Limb Zone through diamond drilling and extended the strike and dip extents of the mineralization with step-out drilling to a depth of 800 m below surface with 400 m of strike extent.

 

6.2NS Zone (Hinge Zone)

 

During 2007, Grandview was exploring the southeast extension of the 88-4 Zone and intersected high-grade mineralized quartz veining identified as the NS Zone. Unlike the 88-4 Zone, this mineralization consisted of relatively sulphide poor quartz veining hosted by mafic volcanics.

 

The discovery hole (DC-10-07) intersected 163.57 g/t Au over 0.46 m between 181.8 m and 182.3 m and 15.05 g/t Au over 2.0 m between 201.1 m and 203.1 m, which prompted further drilling on the zone. Additional results included 4.28 g/t Au over 6.35 m between 176.6-183m(DC-15-07) and 17.2 g/t Au over 2.2 m between 127.6-129.8m (DC-08-01R). Historic drilling at the NS Zone indicated that the mineralization was hosted by up to three massive white quartz veins with sub-vertical dip striking approximately east-west.

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

6.3LP Zone

 

Following a reconnaissance drill campaign in early 2019, Great Bear completed follow-up drilling on its DNW-008 drill hole approximately two kilometres northwest from the Limb Zone. The reconnaissance program had an objective to test the east-west trending structures on the Property responsible for mineralization occurring in the mafic domain southeast of what is known today as the LP Zone. The LP Discovery hole DNW-011 was planned 50 m step back to undercut DNW-008 which returned 0.57 g/t Au over 33.5 m mineralization from its collar to 41.5 m depth. The discovery hole was drilled reporting multiple mineralized horizons including 155 g/t Au over 2.5 m between 57.5 m and 60.0 m, 12.33 g/t Au over 14 m between 75.0 m and 89.0 m, and 0.6 g/t Au over 71.6 m between 98.0 m and 169.6 m.

 

Mineralization consisted of fine gold disseminated throughout porphyritic felsic host rocks associated with increased albitization and silicification. Isolated quartz veining also hosted visible gold within this domain. Great Bear continued drilling along strike of the new mineralization and known stratigraphy stepping out over 1.5 km, and re-logging DC-12-07 and extending DL-03-10, which had been sparsely sampled. This led to the discovery of unsampled high-grade mineralization in DC-12-07 of 2.73 g/t Au over 8.5 m between 190.5 m and 199.0 m (Yuma). The approach of testing geology and mineralization along strike continued by stepping one kilometre east and drilling BR-020 resulting in 4.18 g/t Au over 53.7 m between 81.0 m and 134.7 m (Auro).

 

6.4Production

 

There is no known production from the Property.

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Great Bear Gold Project

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NI 43-101 Technical Report

 

7.Geological Setting

 

7.1Regional Geology

 

The Property lies within the Red Lake greenstone belt of the Uchi Subprovince of the Archean Superior Province of the Canadian Shield (Figure 7-1 and Figure 7-2). The most comprehensive geology description of the belt is provided by Sanborn-Barrie et al. (2001; 2004), compilations of Geological Survey of Canada (Open File 4256), and the Ontario Geological Survey (Preliminary Map P3460). It is briefly summarized here.

 

The Red Lake greenstone belt has 300 Ma history of tectono-magmatic deformation with episodes of magmatism, sedimentation, and intense hydrothermal activity (Sanborn-Barrie et al., 2001).

 

The rocks of the Red Lake (east trending) and Birch-Confederation (north trending) greenstone belts of the Uchi Subprovince are interpreted to have evolved by eruption and deposition of volcanic sedimentary sequences on the active continental margin (the North Caribou Terrane, 3.0 to 2.7 Ga), followed by subduction related arc volcanism (Figure 7-1). Continental collision with the Winnipeg River Terrane at 2.71-2.7 Ga led to subsequent crust thickening and metamorphism (Stott and Corfu, 1991; Sanborn-Barrie et al., 2000, 2001).

 

Both greenstone belts in the Red Lake District are dominated by the Balmer and Confederation Lake assemblages (Sanborn-Barrie et al., 2004).

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Source: Thurston et al., 1991

 

Figure 7-1: Regional setting of Great Bear Property within the Uchi Subprovince, on the south margin of the ca. 3 Ga North Caribou Terrane

 

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Source: Sanborn-Barrie et al., 2004

 

Figure 7-2: Regional Red Lake District geology with active and past producing mines

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The 1:250,000 GSC mapping of the East Uchi Subprovince (Sanborn-Barrie et al., 2004) classified the Project into four main rock types (Figure 7-3 and Table 7-1). These include: an unknown affinity Archean mafic volcanic, an amphibole facies mafic volcanic, Confederation assemblage intermediate to felsic volcanic (possible McNeely assemblage), and undated tonalite/quartz monzonite to granodiorite intrusive rocks. There has been no age dating in this area to confirm the assemblage affinity interpretation.

 

 

Source: Sanborn-Barrie et al., 2004

 

Figure 7-3: Property scale regional geology

 

Table 7-1: Regional geology from Sanborn-Barrie et al., 2004

 

Age/Assemblage Affiliation   Rock Type   Description
Un-subdivided Archean (4000-2500 Ma)   Tonalite to Granodiorite   Medium grained, variably foliated biotite, hornblende biotite tonalite, and associated rocks
  Un-subdivided Mafic Volcanic   Foliated, massive to pillowed basalt, amphibolite, and associated gabbroic rocks; lesser associated intermediate to felsic flows, tuff, and wacke
Un-subdivided Neoarchean (2800-2500 Ma)   Quartz Monzonite to Granodiorite   Variably foliated biotite quartz monzonite, granodiorite and granite; locally leucocratic and quartz and/or K-feldspar porphyritic

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Age/Assemblage Affiliation   Rock Type   Description
Confederation Assemblage (2745-2735 Ma)   Amphibolite   Amphibolite-facies mafic volcanic rocks locally pillowed east of Dixie Lake considered part of the Confederation assemblage, but sequence is not specified
  Intermediate to Felsic Volcanic   Dacitic to rhyodacite pyroclastic rocks associated epiclastic rocks (regionally interpreted as McNeely sequence)

 

Balmer assemblage (2989-2964 Ma)

 

Tholeiitic and komatiitic basalt, with minor felsic volcanic rocks, iron formation, and fine-grained clastic metasedimentary rocks. The assemblage is the host to the majority of Red Lake’s lode gold deposits.

 

Confederation assemblage (2750-2735 Ma)

 

Represented by three sequences: 1) McNeely calc-alkaline sequence (central Red Lake) consisting of intermediate to mafic volcanic rocks; 2) Heyson tholeiitic sequence (southeastern Red Lake) composed of felsic volcanics and interlayered with mafic flows, dacitic tuff, and plagioclase-phyric basaltic andesites; and 3) Graves sequence (northern Red Lake) consisting of basal polymictic conglomerate, intermediate pyroclastic rocks, syn-volcanic diorite, and tonalite.

 

Structure, Metamorphism, and Mineralisation

 

Structure

 

The Red Lake area underwent a complex protracted deformation that culminated in the Kenoran Orogeny which marks collision of the Northern Caribou and Winnipeg River Terranes (Sanborn-Barrie et al., 2004). The east trending Red Lake and north trending Birch-Confederation greenstone belts that form the East Uchi Subprovince are characterized by steeply dipping panels of metamorphosed volcanic and sedimentary rocks. Early, non-penetrative deformation (D0), which resulted in overturning and recumbent folding of Balmer assemblage rocks, is overprinted by two ductile deformation events (D1 and D2) recorded by two generations of folds and penetrative L-S fabrics throughout the belt. D1 fabrics and folds strike northerly, whereas D2 structures are east-northeast striking, except in the Cochenour-Campbell-Red Lake “mine trend”, where a high D2 strain zones strikes east-southeast. Subsequent brittle and semi-brittle structures occur at micro- to macro-scales and have both localized and offset gold mineralization (Dube et al., 2003).

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One of the macro-scale features, trending east-west from the Birch-Uchi belt in the east, through the Property, and then to the northwest, and traceable on high contrast anomalies of regional aeromagnetic data, is interpreted by Lee (2006) to represent a high strain zone.

 

Metamorphism

 

The regional metamorphic grade of the Red Lake and Birch-Uchi belts is characterized by mineral assemblages typical of greenschist facies metamorphism (Thompson, 2003). Amphibolite facies mineral assemblages that occur towards the margins of the greenstone belt and are recognized by the presence of garnet and staurolite in metasedimentary rocks and by hornblende clinopyroxene in mafic rocks are attributed to contact metamorphism with major plutons and minor intrusions.

 

Regional Mineralization

 

The Red Lake greenstone belt is one of the most prolific gold camps in Canada, with gold production over 29 million ounces (Moz) from multiple deposits, including the Campbell-Goldcorp (>23 Moz), Cochenor-Willans (1.2 Moz), and Madsen (2.4 Moz) mines (Armstrong et al., 2018). The largest and highest grade gold deposits are hosted in the Balmer assemblage. According to Dube et al. (2003b), all gold mineralization is epigenetic and structurally controlled, occurring in veins, lenses, fractures, and hinge zones along contacts between rheologically distinct units.

 

The Birch-Uchi belt is a volcanogenic massive sulphide (VMS) camp, host to the past-producing South Bay Mine that yielded 1.6 million tons (Mst) of ore averaging 11.06% Zn, 1.8% Cu, and 2.12 oz/t Ag (Atkinson et al., 1990). The deposit is associated with an exhalative argillaceous chert unit and FIII-type spherulitic flows and porphyries of the Confederation assemblage (Agnew sequence). Although most of the volcanic assemblages of the Red Lake greenstone belt host small zinc, copper, and sulphide occurrences, the most prospective volcanic sequence for VMS mineralization, based on known sulphide mineralization, synvolcanic alteration, and correlation with the Birch-Uchi belt, is the tholeiitic Heyson sequence with its high-temperature FIII-type rhyolitic rocks and associated exhalative units (Parker, 1999).

 

Also, the historic Griffith Mine, located approximately 10 km southeast of the Property, produced 22.8 Mst of iron ore pellets grading 66.7% Fe from 78.8 Mst of crude ore grading 23.9% magnetic iron (29-30% Fe). The mineralization consisted of tightly folded, banded iron formations within sediments of the English River Subprovince.

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7.2Local Geology

 

Because of the overburden and lack of outcrop exposure throughout the Property, most of the previous geological interpretation was based on geophysics, limited regional scale mapping, and diamond drilling.

 

The Property area lies within a regional northwest-southeast trending belt of metavolcanic and metasedimentary rocks which are bounded by intrusive batholiths. The regional tectonostratigraphic assemblages of the East Uchi Subprovince (Sanborn-Barrie et al., 2004) have recently been subdivided by Great Bear into new lithologies based on visual core logging, geochemistry, and petrology. The division between mafic and intermediate-felsic domain still exists.

 

The southwestern portion of the Property is within the mafic domain and consists of mafic volcanic flows (high Fe-tholeiites and high Mg-tholeiites) intercalated with argillite, siltstone, iron formation, and minor local felsic volcanics (Figure 7-4). The association of these rocks is interpreted to be the sequence formed in a marine setting, in proximity to active venting in pre-existing anoxic basins. The strong magnetic response associated within this sequence is related to horizons of iron formation and argillites.

 

 

 

Figure 7-4: Interpreted geology from drilling, prospecting, and geophysics

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The younger sequence of intermediate to mafic volcanic and volcanic derived sedimentary rocks is located at the centre of the Property and has a similar stratigraphy to the western and eastern portions of the Property. However, these areas have a much higher proportion of felsic pyroclastic rocks in the strata. These are also interpreted to have been submarine flows. Basin development is characterized by relatively thin-bedded, silty argillite and common iron formation. The fine-grained volcanic facies suggest quiescent depositional conditions with subdued modification of the sedimentary sequences caused by volcanism.

 

The felsic domain dominates the northeastern portion of the Property. It consists of porphyritic felsic flows (dacites) and volcaniclastics intercalated with sedimentary rocks. The sequence is interpreted as a deformed felsic flow-dome complex (Figure 7-5).

 

 

 

Source: Submarine lava dome, based on the Gold Lake dome and flow complex (modified from Lambert et al., 1990). Illustration adopted from Sylvester et al. (1997) in de Wit & Ashwal (1997).

 

Figure 7-5: Schematic illustration of documented subaqueous felsic lava deposits

 

The mafic domain is in contact with a largely felsic/sedimentary domain in the northeast portion of the Property. The contact between the two domains is best described as gradational from mafic to sedimentary and felsic rocks, and where drilled is marked by a highly strained sedimentary sequence.

 

Topping directions, determined from graded bedding using oriented core data, are generally fining towards the northeast.

 

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Mafic volcanic dykes and sills are common throughout the Property, ranging from lamprophyre to gabbro/diorite (i.e., high level apophyses injected into and disrupting the stratigraphy). Intermediate felsic intrusive rocks are also noted throughout the region. Small intrusive bodies are mapped and have been intersected in both the historic and present drill campaigns.

 

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7.3Project Geology

 

Lithological units have been identified and correlated across the Property and are represented as a schematic stratigraphic column in Figure 7-6. The stratigraphy is remarkably consistent throughout the drilled area. Well documented individual units from drill core are supported with litho-geochemical data and petrological descriptions.

 

 

 

Not to Scale

 

Figure 7-6: Schematic stratigraphy column for the Great Bear Project

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The stratigraphic units are briefly described below:

 

Sediments: Dark to light grey, thinly bedded (<5 cm), fine to medium grained with local argillite beds. Magnetic susceptibility is overall low, but localized high magnetic response is observed in areas with an increased content of argillite. Occasional graded beds are noted with fining direction to the northeast (Figure 7-7).

 

 

 

Figure 7-7: Dry core sample of Sediments from BR-051 at 87.5 m

 

Felsic Volcaniclastic: A fine- to medium-grained, dark grey matrix with sporadic (<5%) less than 4 mm quartz and feldspar crystals. Rounded to angular heterolithic fragments (<5 cm wide) of leucocratic felsic volcanic and dark brown, fine-grained biotite rich fragments are observed. Fragments are often flattened, parallel to foliation (Figure 7-8). The unit is not magnetic and is moderately deformed, with sporadic weak to moderate biotite alteration.

 

 

 

Figure 7-8: Dry core sample of Felsic Volcaniclastic from BR-046 at 87.5 m

 

Felsic Volcanic - Porphyritic: Medium-grained, porphyritic and moderately to strongly foliated. Phenocrysts consist of blue-grey quartz (5%) and up to 10% milky white to yellow feldspar crystals up to 4 mm in diameter. They are stretched out in the foliation and slightly augen shaped. The groundmass is dark grey, composed of very fine grained (<50 µm) interlocking plagioclase and quartz of uncertain proportions. Dark brown biotite (8%) occurs as foliation parallel streaks (Figure 7-9).

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Figure 7-9: Wet core sample of Felsic Volcanic from DNW-011 at 13.2 m

 

Metasediments (2): Massive to thinly bedded, carbonaceous sedimentary rocks. Dark brown to dark grey, fined grained, intensely foliated, biotite rich, overprinted with garnet, staurolite, and andalusite porphyroblasts. Garnets are pink, rounded, up to 4 mm; staurolite is dark yellow, up to 3 mm; and andalusite is light grey, up to 1 cm and angular. Foliation, defined by the alignment of biotite, partially wraps porphyroblasts (Figure 7-10 and Figure 7-11).

 

 

 

Figure 7-10: Dry core photo of Metasediments (2) from BR-065 at 264 m

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Figure 7-11: Wet core photo of Metasediments (2) from DNW-011 at 133.15 m

 

Felsic Volcanic 2 - Aphyric: White to light grey, strongly deformed with a mottled appearance, this unit has a very fine grained to aphyric matrix, often translucent, with 1% to 7% plagioclase phenocrysts. The groundmass is comprised of very fine grained (<50 µm) plagioclase ± quartz. The plagioclase phenocrysts are partially stretched out in the foliation and overprinted by secondary albite, quartz, muscovite, calcite, and chlorite. Biotite content is less than 2% and partially chlorite altered (Figure 7-12).

 

 

 

Note. Red circle indicates visible gold.

 

Figure 7-12: Wet core photo of Felsic Volcanic (2) from DNW-011 at 141.45 m

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Metasediments (3): Fine-grained, thin to moderately bedded, grey-brown to black banded sericite altered sedimentary rocks. The unit is moderately to strongly foliated and usually has a strong banded appearance due to bedding parallel sericite alteration. Contacts between bands can be sharp or gradational (Figure 7-13). They may represent transposed graded bedding. The darker layers are defined by very fine grained biotite, while the grey layers are denoted by greenish muscovite. A second foliation was noted in thin section defined by kinks in muscovite flakes which are strongly aligned in the dominant foliation.

 

 

 

 

Figure 7-13: Wet core photo of Metasediments (3) from DNW-011 136.3 m and BR-060 315 m

 

Fragmental: Highly strained unit consisting of rounded to subangular lithic fragments set in a dark green-grey fine-grained matrix, with moderate to strong sericite alteration (Figure 7-14). Heterolithic fragments are 0.5 cm to 10 cm in size, varying from fine-grained and massive to quartz-phyric with millimetre phenocrysts. The unit is strongly foliated and brecciated. This unit marks the contact between felsic and mafic domains.

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Figure 7-14: Wet core photo of Fragmental from BR-036 at 413 m to 420 m

 

The mafic domain dominates the southwestern portion of the Property and primarily consists of high Fe-tholeiitic basalt (locally pillowed) and high Mg-tholeiitic basalt (massive) intercalated with argillites and siltstones.

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Mafic Volcanic - Fe-Tholeiite: This unit varies from massive to weak to strongly foliated pillow basalt. When strongly foliated, it has alternating bands of dark green hornblende with subsidiary bands of biotite, and light grey discontinuous wispy bands of calcite. In less strained zones, relic pillow selvages can be observed. Selvages are often centimetre-wide with strong chlorite and biotite alteration (Figure 7-15). Centimetre size metamorphic pink garnet becomes more abundant towards the fragmental contact.

 

 

 

Figure 7-15: Wet core photo of Fragmental from DL-018 at 112 m

 

Mafic Volcanic – Fe-Tholeiite – Biotite Calcite Pillows: This unit is dark green, fine-grained with decimetre scale pillows defined by calcite and biotite selvages. The unit contains fine-grained hornblende crystals mixed with biotite and layers of platy, elongated calcite. It is an Fe-tholeiite but is distinct from the unit described above in higher chalcopyrite concentration. That mineralization may account for a weak copper anomaly observed (Figure 7-16).

 

 

 

Figure 7-16: Wet core photo of Mafic Volcanic – Fe-Tholeiite – Biotite Calcite Pillows from DL-018 at 136 m

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Argillite: Fine-grained black to dark grey, highly deformed with folded and contorted bedding. Bedding is millimetre to less than 5 cm thick and averages approximately 1 cm (Figure 7-17).

 

 

 

Figure 7-17: Dry core photo of Argillite from DHZ-026 at 48 m

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Mafic Volcanic – Mg-Tholeiite – Massive Basalt: Dark green to grey, homogeneous, with no obvious pillow or flow breccia textures. The unit is moderately to strongly foliated. Amphiboles (approximately 5 mm clots) are common, set in a finer-grained quartz-feldspar-biotite groundmass. In a more intensely foliated rock, clots of amphibole are stretched and aligned into a foliation plane (Ross, 2018). These two amphibole forms indicate two separate amphibolite grade metamorphic events that outlasted deformation. The amphibole occurs as two minerals: hornblende and actinolite. The unit also contains minor biotite with weak chlorite and actinolite alteration and minor high-angle calcite veinlets (Figure 7-18).

 

 

 

Figure 7-18: Wet core photo of Mafic Volcanic – High Mg-Tholeiite – Massive Basalt from DL-024 at 145.5 m

 

Mafic Volcanic – High Fe-Tholeiite – Pillowed Basalt: This unit is dark green, coarse grained, with strong amphibole recrystallization. There are clear pillow selvages defined by interstitial calcite and chlorite altered chill margins. It is weakly to moderately foliated. The foliation is partially overprinted by fine-grained clots of amphibole set in a fine-grained groundmass of quartz-albite (Figure 7-19).

 

 

 

Figure 7-19: Dry core photo of Mafic Volcanic – High Fe-Tholeiite – Pillow Basalt from DL-024 at 25.0 m

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Ultramafic: The ultramafic consists of fibrous talc (50% to 55%) intergrown with pale Mg-chlorite or possibly serpentine (10% to 15%), with granules of calcite overprinted by prismatic porphyroblasts of pale amphibole (Figure 7-20). The amphibole crystals occur oblique to foliation but are partially wrapped by it, indicating a late syn-deformation timing (Ross, 2019).

 

 

 

Figure 7-20: Wet core photo of Ultramafic from DHZ-039 at 141 m

 

Feldspar Porphyry Dyke: The feldspar porphyry dyke is made up of 10% to 15% blocky plagioclase phenocrysts (<3 mm) set in a foliated quartz-plagioclase-biotite-calcite groundmass (Figure 7-21). The phenocrysts are unaltered. Pyrite is disseminated in the groundmass. The plagioclase is difficult to distinguish from the quartz in the groundmass due to the very fine grain size. Biotite content is 12% and is aligned in the foliation (Ross, 2019).

 

 

 

Figure 7-21: Wet core photo of Feldspar Porphyry Dyke from DHZ-001 at 244.3 m

 

7.4Mineralization Styles and Target Areas

 

Three dominant styles of mineralization are observed within three target areas on the Property (Figure 7-22):

 

1.Silica-sulphide replacement – Limb Zone

 

2.Quartz veining – Hinge Zone

 

3.Disseminated gold within high strain – LP Zone

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Figure 7-22: Internal Great Bear Resources Ltd. interpreted geology showing mineralization zones at the Project

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Silica Sulphide Replacement – Limb Zone

 

The silica sulphide replacement zones have been the focus of exploration at the Limb Zone (historically the 88-4 Zone target). This zone is associated with the rheological and geochemical contact between pillow basalt (Fe-tholeiites) and massive basalt (Mg-tholeiites). The contact is often marked by argillite/siltstones. Mineralization occurs as replacement of sediments, if present, or as silica flooding and quartz-calcite veining in the absence of sediments. Pyrrhotite is the dominant sulphide, with sulphides ranging in concentrations from 2% to 40% pyrrhotite, 2% to 15% pyrite, 1% to 4% arsenopyrite, 2% chalcopyrite, minor less than 2% sphalerite, and trace magnetite. Visible gold is not uncommon and, where observed, is associated with strong pyrrhotite and weaker arsenopyrite-pyrite mineralization (Figure 7-23). Higher-grade and more intense visible gold correlates well with a thinning or absence of sedimentary host rocks at the contact. An increase in silica flooding at the high Fe-tholeiite basalt and high Mg-tholeiite basalt contact is observed where sediments are thin or not deposited. Petrographic work by Ross (2004) identified the presence of gold-silver and lead-tellurides locally encapsulated within arsenopyrite. All native gold in the polished thin sections occurred as free gold crystals up to 50 microns in size.

 

 

 

Figure 7-23: Silica sulphide replacement style mineralization of the Limb Zone

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Alteration and mineralization are strongly correlated with the sulphidized sedimentary layer, both commonly exhibiting very sharp contacts with unmineralized or unaltered host rock. A strong shear component is present within and adjacent to the mineralized zone. The zone is approximately 800 m long and has been drilled to a vertical depth exceeding 400 m (Figure 7-24). Mineralization plunges steeply northwest in a fold limb host dipping steeply to subvertically northeast. It is generally considered that the Limb Zone lies on the north limb of a property scale F2 fold.

 

 

 

Figure 7-24: Limb Zone with significant gold intercepts and MSO shapes looking northeast

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Quartz Veining – Hinge Zone

 

Quartz veining has been observed throughout the Property and has been the main focus of exploration at the Hinge Zone. The quartz veining is hosted by multiple lithologies including massive basalt (high Mg-tholeiite), argillite, and pillow basalt (high-Fe tholeiite). Individual veins are variable in width ranging from 1 cm to 5 m and can create zones up to 40 m. They are generally mineralized with fine-grained disseminated sulphides consisting of 1% to 3% pyrrhotite, 1% to 2% pyrite, 1% to 2% chalcopyrite, less than 1% arsenopyrite, and trace sphalerite. Visible gold is very common ranging from trace to 5% as pin pricks, centimetre scale clusters, and fracture fill (Figure 7-25). These veins have a weak to strong, patchy to pervasive biotite and carbonate alteration halo ranging from several centimetres to approximately 2 m in width.

 

 

 

Note. Cluster of visible gold above centre of pencil.

 

Figure 7-25: Hinge Zone style vein from DHZ-014 at 184.5 m

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Great Bear Gold Project

Ontario, Canada

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The Hinge Zone vein system is comprised of several subparallel anastomosing veins formed along the axial trace of a property wide D2 fold. The intersection between the fold and stratigraphy marks a plunge control on the higher grades within the veins (Figure 7-26).

 

(GRAPHIC)

 

Figure 7-26: Vertical section of Hinge Zone, looking northeast (± 7.5 m) with significant assays and MSO shapes

 

Disseminated Gold in High Strain Corridor – LP Zone

 

The LP Zone exhibits a style of mineralization which is not observed in other parts of the Red Lake greenstone belt. The zone is associated with a high degree of deformation, widespread alteration, and transposition of primary textures as well as complete flattening of stratigraphy.

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The LP Zone mineralization occurs within a wide zone of high strain and increased metamorphic grade. The strain zone is very continuous for over 4 km and is slightly oblique to stratigraphy, intersecting multiple lithologies including the porphyritic felsic volcanic, metasediment 2, felsic volcanic 2, and metasediment 3. The deformation zone is up to 500 m wide. The higher-grade gold mineralization appears to be controlled by the intersection of this strain zone and the metasediment 2 unit. Ongoing LP Zone drilling has demonstrated that most of the greater than 5.0 g/t Au intercepts and nearly all of the greater than 10 g/t Au intercepts drilled along the LP Zone to date occur within 50 m to 100 m of the metasedimentary/felsic volcanic contact (Figure 7-27).

 

Gangue mineralization is variable across the zone and locally ranges from 0% to any amount of the following: 1% to 15% disseminated pyrite, 1% to 10% arsenopyrite (blebby and matted), 1% to 5% red and yellow sphalerite, 1% to 5% pyrrhotite, 1% to 5% chalcopyrite, 1% to 5% galena, and 1% to 3% scheelite (Figure 7-28). The LP Zone has been further sub-divided into six sub-zones named, from northwest to southeast, Discovery, Bruma, Yuma, Yauro, Auro, and Viggo.

 

(GRAPHIC)

 

Figure 7-27: Plan view of gold values >2.3 g/t for the LP Zone with geology and LP sub-zones

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

(GRAPHIC)

 

Figure 7-28: Strong strained Felsic Volcanic with 5% to 10% fine-grained arsenopyrite and 1% fine visible gold in the foliation in BR-020 at 90.15 m

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Great Bear Gold Project

Ontario, Canada

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At least three gold mineralizing events have been recognized, including foliation parallel free gold in host rock, transposed quartz veins, and later quartz veins with visible gold that are slightly oblique to foliation (Figure 7-29).

 

(GRAPHIC)

 

Figure 7-29: Visible gold in foliation hosted by strained porphyritic Felsic Volcanic from DNW-011 at 58.25 m

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Great Bear Gold Project

Ontario, Canada

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7.5Metamorphism and Alteration

 

This package of rock preserves a greenschist to amphibolite grade metamorphic assemblage with only minor amounts of retrograde chlorite-epidote ± sericite alteration related to younger cross-cutting calcite veinlets and micro fractures. The dominant amphibole minerals present in the area local to the Limb, Hinge, and LP Zones is hornblende with subordinate actinolite. There is evidence of two foliation forming events occurring at amphibolite grade metamorphic conditions, with these high-grade conditions outlasting the deformation and allowing the amphibole to recrystallize and partially overprint foliation (Figure 7-30).

 

(GRAPHIC)

 

Figure 7-30: Recrystallized amphibole overprinting foliation (possible actinolite) and biotite alteration in contact with quartz vein (red line)

 

The Limb Zone exhibits greenschist to lower amphibolite grade metamorphism. The silica sulphide replacement alteration of the Limb Zone consists of dark grey, fine-grained silica replacing and flooding argillite and siltstones at the high Fe-tholeiite and high Mg-tholeiite contact. The alteration is fairly discrete and contained within the mineralization corridor. Weak carbonate quartz alteration is observed as a late stage veining event in wall rocks.

 

Metamorphic grade at the Hinge Zone is upper greenschist to lower amphibolite, consisting of minor late-stage amphibole growth. Alteration of quartz veining at the Hinge Zone consists of pervasive to patchy, dark brown, fine-grained biotite extending into the host rock for up to 2 m.

 

Metamorphic grade of the LP Zone, by contrast to the Hinge Zone and Limb Zone, is mainly amphibolite to upper greenschist facies. The felsic-intermediate units preserve an amphibolite grade metamorphic assemblage of albite, biotite, muscovite, and garnet with the sedimentary units containing garnet and staurolite (Ross, 2019). The LP Zone alteration is variable throughout its extent but can generally be described as strong to pervasive albitization and silicification of the felsic volcanic units and sericite/muscovite alteration of the metasediment units. The sericite/muscovite alteration can be banded (bedding parallel) or completely pervasive. Locally there is patchy biotite, but it does not appear to be associated with gold mineralizing events. Within the metasediments, coarser grained diffuse cordierite crystals (andalusite according to Ross, 2020) have no association with sulphides or visible gold.

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Great Bear Gold Project

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7.6Structural Geology

 

The Property is divided into two main structural domains: the southwest and northeast domains exhibit folding, and the central domain exhibits high strain and mylonitic textures (Figure 7-31).

 

(GRAPHIC)

 

Figure 7-31: Property structural interpretation showing folded terrains (grey shaded) and the Central (coloured) High Strain Corridor

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Great Bear Gold Project

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Structural fabrics are interpreted from airborne magnetic data and where available, oriented core data (Figure 7-31). Detailed drilling at the Hinge and Limb Zones has provided numerous data points which validate the fold model in that area. A possible evolution of the Great Bear volcanic rocks involved early folding and tilting of the rock package followed by later warping or refolding of the main fabric. This model proposes three phases of deformation D1 through D3.

 

D1 deformation: Early compression and uplift of the greenstone belt after the collision of the Caribou and Winnipeg River terranes. (Note that a penetrative foliation fabric is not preserved in the rocks.)

 

D2 deformation: Progressive strain, tilting, and continued uplift and folding, this deformation is marked by a penetrative foliation fabric (F2). Rocks develop a stretch lineation and mineralized veins are emplaced along weaknesses during D2 deformation. Bedding cleavage relationships observed in the Limb and Hinge Zones indicate that the folds verge to the northeast and plunge steeply to the northwest.

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

D3 deformation: A broad scale warping of the F2 foliation fabric, most likely resulting from either emplacement of post-tectonic plutons or re-activation of earlier faults (Figure 7-32).

 

(GRAPHIC)

 

Source: Adamova (2021)

 

Figure 7-32: Conceptual sequence of Great Bear area deformation events (not to scale)

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Great Bear Gold Project

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NI 43-101 Technical Report

 

The LP Zone, or central structural domain, most likely exhibits all of the above phrases of deformation, however, evidence of fold hinges, fold closures, and vergence directions is completely obliterated due to the high degree of flattening and transposition of rocks into the F2 foliation plane (Figure 7-33). The LP Fault, which was first identified by the Lithoprobe project and reported by Zeng and Calvert (2006), may represent a re-activated deep crustal fault which remained active throughout D2 and D3 deformation events. Rocks within the central domain (including mafic dykes and lamprophyres) exhibit a very high degree of strain often showing mylonitic textures. These same dykes in the folded terrains show lesser strain.

 

(GRAPHIC)

 

Figure 7-33: Stereonets showing rotated foliation fabrics along the trend of the LP Fault Zone

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

8.Deposit Types

 

The Great Bear deposit is an Archean mesothermal gold deposit. The prolific Red Lake greenstone belt in Canada hosts numerous high-grade Archean mesothermal gold deposits that have produced more than 28 Moz of gold (Armstrong et al., 2018). The major gold deposits such as the Red Lake, Campbell, and Cochenour-Willans Mines are hosted by the Balmer assemblage and considered as shear-hosted vein-type deposits (Sanborn-Barrie et al., 2000). Madsen is a stratabound, replacement-style disseminated vein-type gold deposit that is hosted by a calc-silicate altered carbonatized mafic volcanic near the margin of a batholith (Dube et al., 2000). Within the Confederation greenstone belt, South Bay is a VMS deposit with bimodal mafic to felsic subaqueous volcanic stratigraphy (Stott and Corfu, 1992).

 

The Red Lake camp produced gold from the following principal types of mineralization (Lee, 2006):

 

Carbonate veins consisting of ferroan dolomite and minor quartz with disseminated arsenopyrite and native gold;

 

Quartz-arsenopyrite replacement zones occurring as irregular sheets and lenses within mafic volcanics;

 

Sulphide replacement bodies composed of disseminated pyrite and pyrrhotite occurring in the mafic volcanics;

 

Of lesser importance, quartz veins containing free gold associated with small scale shear zones within intermediate to felsic intrusive.

 

Gold mineralization styles on the Great Bear property include:

 

Silica-sulphide replacement (Limb Zone)

 

Quartz veining in mafic volcanics (Hinge Zone)

 

Shear hosted; disseminated gold within high strain zones (LP Zone)

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Great Bear Gold Project

Ontario, Canada

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9.Exploration

 

Exploration work prior to the Property acquisition in February 2022 is described in Section 6, History. All exploration work completed by Kinross during 2022 was mainly drilling and is described in Section 10, Drilling.

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Great Bear Gold Project

Ontario, Canada

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10.Drilling

 

10.1Summary

 

To date, a total of 1,359 diamond drill holes for approximately 597,194 m and a total of 433 reverse circulation (RC) holes for approximately 34,530 m have been completed on the Project.

 

Drilling carried out by Kinross’ predecessors is described in Section 6, History and illustrated in Figure 6-1.

 

This section provides details of the Kinross 2022 drilling program.

 

10.2Kinross 2022 Drilling Program

 

From acquisition of the Property in February 2022 to December 31, 2022, Kinross completed a total of 397 drill holes for a total of 206,967 m. Drill hole locations are illustrated in Figure 10-1. All diamond drill holes were drilled with NQ (47.6 mm) rods and core bits. Holes were continuously sampled, and sample widths were between 0.5 m and 1.5 m long. The samples were laid out based on lithology, alteration, mineralization, or structures.

 

The objective of the Kinross 2022 drill program was five-fold:

 

1.Test the extents of known drill targets.

 

2.Infill zones of potentially economic mineralization to meet Inferred Mineral Resource classification status.

 

3.Carry out condemnation drilling to identify areas that may be used for capital development.

 

4.Begin drill testing the deep extension of the mineralization at a greater than one kilometre depth.

 

5.Mimic production drilling by drilling a tight grid of RC drill holes that would provide data for a ground truth block model.

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

(GRAPHIC)

 

Figure 10-1: Drill holes from the 2022 drill program

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Drilling statistics for the Kinross 2022 drill program by zone, are summarized in Table 10-1.

 

Table 10-1: Statistics of 2022 drilling

 

Zone/Sub-zone  Holes   Total Meterage (m) 
Auro   33    27,215 
Yauro   23    20,099 
Yuma   32    23,684 
Bruma   29    25,919 
Discovery   25    16,227 
Viggo   62    28,941 
Limb   50    34,181 
Hinge   1    501 
Exploration and Condemnation Drilling   34    17,3870 
Geotechnical and Metallurgical Drilling   41    11,724 

 

The RC drill program began in March 2022 and was concluded in July 2022. A total of 433 holes were completed for a total of 34,530 m. All RC holes were drilled with a 171 mm drill bit. Holes were under compression to ensure samples were dry. Samples were taken continuously in rock over 2 m intervals targeting 10 kg for each sample.

 

Where possible, best efforts were made to calculate true widths of zones. In established vein zones such as the Hinge and Limb Zones, true widths were calculated by intersecting the drill hole intercept with the vein geometry. In the LP Zone, true widths were calculated from the orientation of the estimation domains. These values range from 75% to 95% of true width and reported on a hole-by-hole basis.

 

Drilling Procedures

 

Chibougamau Diamond Drilling Ltd., Forage FTE Drilling Ltd., Hy-Tech Drilling Ltd., and Major Drilling Group International Inc. were used for the Kinross 2022 drill campaign. The drills were skid mounted diamond core drills and were capable of drilling a range of depths up to greater than 2,000 m. All holes drilled at the Project utilized NQ (47.6 mm) tools and rods. Drill holes were cased in HQ diameter core (63.5 mm) and reduced to NQ (47.6 mm) for the remainder of the drill hole. Regular drill rig visits indicated drill crews used adequate care in handling and boxing the core. Core was placed in wooden boxes with depth markers demarcating the end of every drill run (up to 3 m). Boxes were covered and brought to the core facility in Red Lake twice a day after morning and evening rig checks.

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

All drill holes completed in all programs were initially set up using a handheld Garmin GPS60 unit. At the completion of the hole, casing was left in the hole and capped for diamond drill holes. The cap included the drill hole ID stamped onto a large metal flag for winter safety. At the completion of the program, the drill holes were surveyed with a differential global positioning system (GPS) and this information was added to the “Header” as the final UTM location.

 

Downhole surveys of the drill holes were conducted using a Reflex Gyro, a non-magnetic north seeking tool. In diamond drill holes, the first measurement was taken just past the casing at approximately 10 m, with readings taken every 10 m thereafter and again at the end of the hole. In RC drill holes, the first measurement was taken just past the casing at approximately 5 m, with readings taken every 5 m thereafter and again at the end of the hole. The non-magnetic, north seeking Gyro tool was selected after review of historical drilling which revealed significant erroneous downhole survey measurements due to excessively magnetic rocks.

 

Oriented core measurements were taken for all drill programs with the exception of the RC drill program. Measurements were taken at the end of each run (3 m) or when the core tube was pulled. Drillers used a Reflex ACT III RD Orientation Instrument to obtain the measurements.

 

As a result of competent bedrock and reliable drilling practices, drill core recovery rates were more than 98% for the duration of the Project.

 

Confidence values were assigned to all drill holes, including historic drill holes, based on whether the drill hole has had its collar found and surveyed by a differential GPS, whether the hole had downhole surveys carried out and if that survey was conducted using a non-magnetic device. For all modelling and estimation work, only high confidence drill holes were used (Confidence 1 and 2). To the QP’s knowledge, there are no drilling, sampling, or recovery factors that could materially impact the accuracy and reliability of the results.

 

Drill Core Logging

 

The following describes Kinross’ approach to diamond drill core analysis:

 

The drill core is collected at the end of each shift and brought to the core logging facility in Red Lake.

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Great Bear Gold Project

Ontario, Canada

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The core is geotechnically logged: orientation marks are measured, magnetic susceptibility and specific gravity values are recorded by the geotechnician. All data is recorded electronically on a tablet.

 

If any errors in blocking or box numbers are found, they are reported to the geologist. These errors are then reported to the drill supervisor so they can be corrected at the drill.

 

The drill holes are then logged by the geologist. Data including lithological type, alteration, structural elements, and sulphide content is recorded electronically on a tablet in Logger for the first nine months of the year and in acQuire for the remainder of the year. All data is recorded electronically and backed up automatically.

 

Wet and dry core is photographed for every box then labelled by hole ID and meterage.

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

11.Sample Preparation, Analyses, and Security

 

11.1Sample Security

 

All samples are stored in Great Bear’s (now Kinross) secure core logging facilities. The logging facilities are kept locked and are only accessible to Kinross personnel.

 

Prior to shipping, the samples are manifested on the respective shipping forms. Samples are collected in standard plastic rock sample bags and stapled closed. The sample bags are placed in rice bags, which in turn are placed in plastic bin palettes. The bins are covered with plywood and a numbered security seal is applied. Kinross personnel load the bin palettes onto the transport trucks, operated by Red Lake based freight shipping company Gardewine North. Paper copies of the forms are sent along with the samples and a digital copy is sent to the laboratory via email. A digital copy of the forms is retained by Kinross.

 

Samples are generally shipped two or three times per week, depending on the amount of drilling.

 

11.2Sample Preparation and Analysis

 

Great Bear has used several laboratories to perform their assay analyses on core and rock samples:

 

Activation Laboratories Ltd (Actlabs) from July 2017 to June 2018

 

SGS Ltd. (SGS), in Red Lake, from July 4, 2018, to December 31, 2019.

 

Actlabs, in Thunder Bay, from September 2019 to present.

 

Check assay samples and RC samples were sent to ALS Global (ALS).

 

All assaying laboratories servicing Great Bear and Kinross samples are independent laboratories with ISO/IEC 17025:2017 accreditation from the International Organization for Standardization and Standards Council of Canada.

 

All pulps and coarse reject material from both laboratories were packaged and shipped to Kinross’s facility (Great Bear’s prior to acquisition) in Red Lake, at 2 Industrial Park, or at their core storage (core laydown) area on the Property.

 

Descriptions of the sample preparation and analyses conducted at Actlabs and SGS are presented below.

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Great Bear Gold Project

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Actlabs

 

Upon receipt at Actlabs in Thunder Bay, the entire sample is weighed (kg) and recorded (prep code RX10). The samples (<7 kg) are crushed up to 80% passing 2 mm, mechanically split to obtain a representative sample (250 g), and then pulverized to at least 95% -105 microns (µm). All the steel mills used in this process are mild steel and do not introduce Cr or Ni contamination (prep code RX1).

 

All samples were subject to near total digestion, using four acid digestion, and were analyzed for 36 elements by Inductively Coupled Plasma Mass Spectrometry (ICP-MS) (Actlabs Code: 8-4).

 

The samples were assayed for gold by fire assay (50 g) with an atomic absorption (AA) finish (Actlabs Code: 1A2-50). Sample results above the 10,000 ppb gold over limit were re-assayed using a gravimetric finish (Actlabs Code: 1A3). Samples with highly variable gold results, or that contained visible gold, had a 500 g split taken and sieved to 149 µm, and a metallic screen assay performed (Actlabs Code: 1A4).

 

In 2020, density measurements were also completed by Actlabs.

 

The Actlabs analytical codes and description are summarized as follows.

 

1A2-50 (Au Fire Assay – AA, 50 g sample)

 

1A3 (Au Fire Assay – Gravimetric, 50 g sample, over limit)

 

1F2 (Au Fire Assay – AA, 30 g sample)

 

8-4 (4 Acid ICP-MS, 0.5 g sample, over limit)

 

1A4 (Au Fire Assay - Metallic Screen, 500 g sample)

 

SGS

 

Once received at SGS in Red Lake, samples are weighed and dried. The sample (<3 kg) is then crushed to 75% passing a 2 mm screen. A 250 g split is then taken and pulverized to 85% passing 75 µm (SGS code: PRP89).

 

All samples were subject to near total digestion with four acids, 33 element geochemical analysis by Inductively Coupled Plasma Optical Emission Spectrometry (ICP-OES) (SGS code: ICP40B). Detection limits for some of the metals of interest were: Ag 2 ppm to 100 ppm, Sb 5 ppm to 1%, Zn 1 ppm to 1%.

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Great Bear Gold Project

Ontario, Canada

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A larger 50 g sample was also analyzed for gold using fire assay and AA (SGS code: FAA515), which has a lower and upper detection limit of 5 ppb Au and 10,000 ppb Au, respectively. Samples that were greater than 10,000 ppb Au were analyzed by lead fusion fire assay with a gravimetric finish (SGS Code: FAG505). This method’s lower and upper limits are 0.5 ppm and 3,000 ppm, respectively.

 

Metallic screens were also requested by the field geologist if visible gold was noted or suspected during the logging process, or if the results from the fire assay were highly variable. In this case, a one kilogram split was taken and screened through a 160 mesh screen. The entire plus size sample fraction was assayed by fire assay. A 50 g minus size sample fraction was run in duplicate. The average of the two minus fraction assays and the plus fraction assay were combined by weight for total grade calculation.

 

The SGS analytical codes and description are summarized as follows:

 

ICP40B (4 Acid ICP-OES, 0.2 g sample)

 

FAA515 (Au Fire Assay – AA, 50 g sample)

 

FAG505 (Au Fire Assay – Gravimetric, 50 g sample)

 

GO_FAS50M (Au, Ag, screen metallic)

 

11.3Quality Assurance/Quality Control

 

Great Bear and Kinross have carried out a quality assurance/quality control (QA/QC) program on all its drill core sampling since 2017 consisting of the insertion and analysis of blanks, Certified Reference Materials (CRM or standards), and duplicate samples to monitor the precision and accuracy or the reliability of the assay results from its drilling and sampling program. This is in addition to the quality control samples that are inserted by the assay laboratory and consist of blanks, standards, and duplicates.

 

Between May and August 2020, Great Bear retained Analytical Solutions Ltd. (ASL) to carry out a comparison of the two analytical methods used, fire assay and screen metallics, based on 54 drill core samples (from 2019 drill holes).

 

In August 2020, ASL reviewed 2,622 drill core duplicates obtained by the quartering of half core samples from Great Bear’s 2019 and 2020 drill holes. Due to the variability of the values typical of an orogenic gold project, ASL recommended that core duplicate collection be discontinued during the sampling program.

 

In September 2020, ASL completed guidelines for sampling and assay quality control for Great Bear. These procedures serve as the basis of Great Bear’s QA/QC program.

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

11.3.1QA/QC – 2017 to 2019 by Great Bear

 

The following has been modified from Adamova (2021). Kinross has reviewed the 2017-2019 QA/QC data with accompanying report and the QP is of the opinion that the assay results are accurate and reliable and suitable for Mineral Resource estimation.

 

Between 2017 to 2019, a total of 9,454 QA/QC samples, consisting of two types of blanks and 14 different CRMs, were inserted into the drill core sample stream nominally every 30 samples.

 

When selecting control sample types, Great Bear’s approach was to insert a blank, a sample representing low grade (approximately 1 g/t Au to 2 g/t Au), a standard representing mid-grade (approximately 3 g/t Au to 5 g/t Au), and a high-grade sample which should trigger a gravimetric analysis at greater than 10 g/t Au. CRMs were used to completion and if unable to obtain more of the same standard, Great Bear replaced it with a standard with the same approximate gold grade.

 

Table 11-1 provides a summary of control samples for blanks and CRMs.

 

Table 11-1: Summary of control samples – 2017 to 2019

 

Description  2017 - 2019  Comments
Total Number of Samples  83,574   
Number of Control Samples  9,454 (11.3%)   
Distribution      
Blanks  4,726 (5.7%)   
BLM  1,701  Actlabs + SGS
BLK  1,591  Actlabs + SGS
BM-10  1,436  Actlabs + SGS
Standards (CRMs)  4,726 (5.7%)   
CDN-GS12A  102  Actlabs + SGS
CDN-GS1P5Q  748  SGS
CDN-GS1P5R  824  Actlabs + SGS
CDN-GS2S  474  SGS
CDN-GS4H  467  Actlabs + SGS
CDN-GS5W  350  SGS
CDN-GSP5E  659  Actlabs + SGS
OREAS 209  360  Actlabs + SGS
OREAS 214  109  SGS
OREAS 215  30  Actlabs

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Description  2017 - 2019  Comments
OREAS 221  400  Actlabs + SGS
OREAS 224  171  SGS
OREAS 228  32  Actlabs

 

Note: summation errors may occur due to rounding. 

  

Blank material that returns assays greater than 10 ppb Au is considered in the warning range. CRMs that return assays of ± 3 standard deviations (SD) from the certified value are considered outside the tolerable limits.

 

Sources of error in QA/QC samples can occur from data entry errors, sample mix-ups before, during or after shipping, switched samples at the laboratory, errors in the standard itself, and laboratory assaying errors.

 

Every QA/QC failure is followed up by the database manager in an attempt to recognize the most likely cause. Multiple failures on a single certificate and gradual migration of values over time are the two most likely causes for re-running certificates and batches. In general, single errors and outliers will be recognized as a warning but will not trigger re-assaying.

 

Table 11-2 shows a summary of the QA/QC control samples results for drilling programs between 2017 and 2019. These results are further broken down by laboratory where the sample analysis was completed. Figure 11-1 presents a graphical comparison of QA/QC results for control samples between 2017 and 2019.

 

Table 11-2: Summary of control sample results – 2017 to 2019

 

   Total
Count
   %
Failures
   Actlabs
Count
   Actlabs
% Failures
   SGS
Count
   SGS
% Failures
 
Blanks 
BL10   1,701    2%   323    1%   1,378    3%
BLK   1,591    5%   193    0%   1,398    6%
BLM   1,436    1%   331    1%   1,105    2%
CRMs 
CDN-GS12A   102    6%   23    4%   79    7%
CDN-GS1P5Q   748    17%   -    -    748    17%
CDN-GS1P5R   824    6%   206    5%   618    6%
CDN-GS2S   474    14%   -    -    474    14%
CDN-GS4H   467    8%   211    1%   256    13%
CDN-GS5W   350    5%   -    -    350    5%

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Ontario, Canada

NI 43-101 Technical Report

 

   Total
Count
   %
Failures
   Actlabs
Count
   Actlabs
% Failures
   SGS
Count
   SGS
% Failures
 
CDN-GSP5E   659    5%   207    7%   452    4%
OREAS 209   360    14%   50    0%   310    17%
OREAS 214   109    20%   -    -    109    20%
OREAS 215   30    0%   30    0%   -    - 
OREAS 221   400    9%   72    3%   328    10%
OREAS 224   171    14%   -    -    171    14%
OREAS 228   32    3%   32    3%   -    - 

 

Note: summation errors may occur due to rounding.

 

 

 

Source: Adamova (2021)

 

Figure 11-1: Graphical representation of total samples submitted and failure rates at SGS vs ActLabs

 

Blanks

 

From 2017 to May 2019, two types of blank reference material were combined under the label BLK. The two types of blank materials were:

 

BL-10: a commercially available ¾ inch unmineralized limestone marble gravel, purchased from a local hardware store

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BLM: a certified blank purchased from CDN Resources Laboratories Ltd. (CDNRL) (Figure 11-2).

 

From June 2019, the two types of blank material were differentiated from each other in the database as “BL-10”, from CDNRL, and the commercial marble material as “BLM”.

 

 

 

Source: AGP (2021)

 

Figure 11-2: Blank reference material BL-10

 

Blanks are used to monitor the laboratory’s cleanliness between samples and provide a benchmark by which to monitor contamination. Generally, 100 g of the blank material was inserted into the sample series nominally every 20 samples and/or after an obvious mineralized interval. A blank failure was defined as having an assay value greater than 0.01 ppm Au.

 

Sample batches were often not re-run due to blank failures unless significant contamination is found. Failure of a blank sample may be due to contamination and, for this reason, any re-assaying of samples is completed on the sample batch. Typically, the sample range, including the last passed blank to the next passed blank, is re-analyzed if contamination is suspected.

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Figure 11-3 to Figure 11-5 present control plots of blank material for BLK, BL-10 and BLM, by laboratory. The red bars depict the warning limit of 0.01 g/t Au.

 

 

 

Source: Adamova (2021)

 

Figure 11-3: Control plot for BLK blank material (BL-10 and BLM combined); April 2017 – May 2019

  

 

 

Source: Adamova (2021)

 

Figure 11-4: Control plot for BL-10 blank material; June 2019 to December 2019

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Source: Adamova (2021)

 

Figure 11-5: Control plot for BLM blank material; June 2019 to December 2019

 

Standards

 

Commercial CRMs, or standards, are used to test the precision and accuracy of gold assays and to monitor the consistency of the laboratory’s performance. The standards were purchased in pre-measured individual packets weighing approximately 100 g and were sourced from ORE Research & Exploration PL (OREAS) and CDNRL. The CRMs were randomly inserted into the sample sequences, nominally every 20 to 30 samples.

 

A CRM outside of the acceptable tolerance levels was defined by analytical values that were greater than 3SD above or below the expected certified gold value. The results of the standard were reviewed in the context of the results of the batch, and the assay laboratory was notified of the CRM failure if deemed appropriate. In the event of a standard outside the tolerance limits, 10 samples above and 10 below the failed standard within a laboratory defined batch were selected for re-analysis. In cases where the standard failures occurred in “unmineralized” rock (generally in zones returning < 0.10 g/t Au) no action was taken but a note was made in the QA/QC sample tracking spreadsheet. Extreme outliers were often determined to be a result of the incorrect standard sample being inserted into the sample stream or errors in the sample data entry; these samples have been corrected in the database.

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Figure 11-6 to Figure 11-18 represent the control plots for each standard used in the 2017, 2018, and 2019 drill programs. The red solid lines denote the upper and lower tolerance levels of three standard deviations. Typically, only two or three different CRMs are used during any given time. The CRMs have overlapping insertion dates between 2017 and 2019 (Adamova, 2021).

 

 

 

Source: Adamova (2021)

 

Figure 11-6: Control plot for SRM GS12A

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Source: Adamova (2021)

 

Figure 11-7: Control plot for SRM GS1P5Q

 

 

 

Source: Adamova (2021)

 

Figure 11-8: Control plot for SRM GS1P5R

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Source: Adamova (2021)

 

Figure 11-9: Control plot for SRM GS2S

 

 

 

Source: Adamova (2021)

 

Figure 11-10: Control plot for SRM GS4H

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Source: Adamova (2021)

 

Figure 11-11: Control plot for SRM GS5W (Fire Assay)

 

 

 

Source: Adamova (2021)

 

Figure 11-12: Control plot for SRM GS5W (Gravimetric Finish)

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Source: Adamova (2021)

 

Figure 11-13: Control plot for SRM GSP5E

 

 

 

Source: Adamova (2021)

 

Figure 11-14: Control plot for SRM OREAS 209

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Source: Adamova (2021)

 

Figure 11-15: Control plot for SRM OREAS 214

 

 

 

Source: Adamova (2021)

 

Figure 11-16: Control plot for SRM OREAS 221

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Source: Adamova (2021)

 

Figure 11-17: Control plot for SRM OREAS 224

 

 

 

Source: Adamova (2021)

 

Figure 11-18: Control plot for SRM OREAS 228

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Field Duplicates

 

Field duplicate samples are used to monitor sample batches for potential sample mix-ups and monitor the data variability as a function of both laboratory error and sample homogeneity.

 

The duplicate samples were produced by quartering the half core sample into two quarter splits, with one sample recorded as the “original” sample and the other, the duplicate. Field duplicates were inserted every 40 to 60 samples.

 

Given the highly variable and nuggety nature of the mineralization, the field duplicates may produce assay samples that vary considerably. Thus, the results of the field duplicates do not fail, but highlight the variability of the different styles of mineralization. If the duplicate was selected from unmineralized rock and contained significant gold values, the sample was selected for re-assay using the coarse reject material.

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Figure 11-19 presents the scatter plot for the results of the field duplicates.

 

 

Figure 11-19: Scatter plot for field duplicates

 

Check Assays

 

Approximately 5% of gold bearing samples were sent for check assays to a different analytical laboratory. Check assays were completed on both pulps of the original sample and coarse rejects. A total of 179 samples were selected from drill holes BR-024, BR-035, and BR-050.

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Figure 11-20 presents the comparison of gold assays of original assays and coarse rejects for the 179 samples that were initially assayed at SGS and were sent to both Actlabs and ALS for check analyses.

 

 

 

Source: Adamova (2021)

 

Figure 11-20: Control plot for coarse reject analyses from SGS, Actlabs and ALS Global

 

Duplicate sampling of cut core and check assays preformed at Actlabs and ALS did not reveal any bias in assay results for Great Bear’s exploration programs.

 

11.3.2QA/QC – 2020 to February 2022 by Great Bear

 

Between January 2020 and February 2022, Great Bear followed the same QA/QC procedures and insertion rates for the control samples used in its 2017 to 2019 drill programs.

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Eight of the thirteen CRMs were discontinued and six new CRMs were utilized during the 2020-2022 drilling programs.

 

Table 11-3 summarizes the blanks and CRMs used in the 2020-2022 drill programs.

 

Table 11-3: Summary of control samples – 2020 – 2022 Great Bear drill programs

 

Description  2020 – 2022  Comments
Total Number of Samples  245,460   
Number of Control Samples  25,613 (10.4%)   
Distribution      
Blanks  12,670 (5.1%)   
BLK  9,215   
BLM  1,707  to Sep 2020
BL-10  1,748  to Sep 2020
Standards (CRMs)  12,943 (5.3%)   
CDN-GS-12A  102  to Jul 2020
CDN-GS-12B  332   
CDN-GS-1P5R  562  to Aug 2020
CDN-GS-1W  962  to Oct 2020
CDN-GS-4H  514   to May 2020
CDN-GS-P5E  1,499  to Oct 2020
OREAS 216b  1,135   
OREAS 221  1,093  to Feb 2021
OREAS 226  3,257   
OREAS 232  3.305   
OREAS 238  182   

 

Blanks

 

Similar to 2019, Great Bear employed the two types of blank reference materials: BL-10 and BLM. Starting from August 2020, and on the recommendation of ASL, the certified blank exclusively used by Great Bear was the coarse silica material from OREAS (BLK).

 

Generally, 100 g of the blank material was inserted into the sample series nominally every 20 samples and/or after an obvious mineralized interval. A blank failure was defined as having an assay value greater than 0.025 ppm Au, which is equivalent to five times the detection limit of the Au FA-AA analytical method.

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Figure 11-21 and Figure 11-22 present the control plots of blank material for BLM and BLK, respectively. The failure rate from all three blank samples was 0.1% during the period (only 13 failures out of 12,670 blank samples inserted).

 

 

 

Figure 11-21: Control plot BLM

 

 

Figure 11-22: Control plot for BLK

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Standards

 

In 2020 to 2022, Great Bear followed the same QA/QC procedures used in its previous drill programs. The CRMs were inserted into the sample sequences, nominally every 20 to 30 samples.

 

Table 11-4 presents a summary of results for CRMs used between January 2020 and February 2022. Figure 11-23 to Figure 11-28 present the control plots for selected CRMs used during this period.

 

Table 11-4: Summary of CRMs for 2020 – 2022 Great Bear drill program

 

CRM Name  Assay
Lab.
  Method   Count   Certified
Value Au
(g/t)
   Standard
Deviation
   Average
Assay Au
(g/t)
   No. of
Failures
   %
Failures
 
CDN-GS-12A  Actlabs  FA-GRAV    102    12.31    0.27    12.38    8    7.8%
CDN-GS-12B  Actlabs  FA-GRAV    332    11.88    0.285    11.99    17    5.1%
CDN-GS-1P5R  Actlabs  FA-AA    562    1.81    0.07    1.80    22    3.9%
CDN-GS-1W  Actlabs  FA-AA    962    1.063    0.038    1.047    55    5.7%
CDN-GS-4H  Actlabs  FA-AA    514    5.01    0.15    5.01    16    3.1%
CDN-GS-P5E  Actlabs  FA-AA    1,499    0.655    0.031    0.640    102    6.8%
OREAS 216b  Actlabs  FA-AA    1,135    6.66    0.158    6.76    7    0.6%
OREAS 221  Actlabs  FA-AA    1,093    1.062    0.036    1.057    9    0.8%
OREAS 226  Actlabs  FA-AA    3,257    5.45    0.126    5.46    52    1.6%
OREAS 232  Actlabs  FA-AA    3,305    0.902    0.023    0.901    39    1.2%
OREAS 238  Actlabs  FA-AA    182    3.03    0.080    3.06    9    4.9%
Total & Avg     All    12,943                   336    2.6%

 

FA-AA – fire assay AAS finish, FS-GRAV –fire assay gravimetric finish

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Figure 11-23: Control plot for CDN-GS-1W

 

 

 

Figure 11-24: Control plot for CDN-GS-4H

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Figure 11-25: Control plot for CDN-GS-P5E

 

 

 

Figure 11-26: Control plot for OREAS 221

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Figure 11-27: Control plot for OREAS 226

 

 

 

Figure 11-28: Control plot for OREAS 232

 

Field Duplicates

 

A similar procedure was followed during 2020 to February 2022 to those used in 2017 to 2019. Field duplicates were inserted every 40 to 60 samples.

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Figure 11-29 presents the scatter plot for the results of the field duplicates completed between January 2020 and March 2021. Field duplicate samples did not reveal any bias in assay results for Great Bear’s 2020-2021 exploration programs.

 

 

 

Figure 11-29: Control plot for field duplicates; January 2020 to March 2021

 

11.3.3QA/QC – March to December 2022 by Kinross

 

Between March and December 2022, Kinross followed the same QA/QC procedures and insertion rates for the control samples used by Great Bear in its previous drilling programs.

 

Six of the eleven CRMs were discontinued and five new CRMs were utilized during the 2022 Kinross drill program.

 

Table 11-5 summarizes the blanks and CRMs used in the 2022 sampling program.

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Table 11-5: Summary of control samples – 2022 Kinross drill program

 

Description  2022   Comments 
Total Number of Samples  134,291     
Number of Control Samples  14,224 (10.6%)     
Distribution        
Blanks  7,084 (5.3%)     
BLK  6,268     
BLK_PStone  816   from Oct 2022 
Standards (CRMs)  7.140 (5.3%)     
CDN-GS-12B  76     
OREAS 211  1,116     
OREAS 216B  715   to Jul 2022 
OREAS 226  5   to May 2022 
OREAS 230  1,103     
OREAS 232  1,266     
OREAS 233  502     
OREAS 237B  179     
OREAS 238  1,149     
OREAS 240  1,029     

 

Blanks

 

During 2022, Kinross continued using the certified coarse silica blank from OREAS (BLK) and employed one additional blank reference material (BLK_PStone) in October 2022.

 

Generally, 250 g of the blank material was inserted into the sample series nominally every 20 samples and/or after an obvious mineralized interval or if visible gold was noted. A blank failure was defined as having an assay value greater than 0.025 ppm Au.

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Figure 11-30 and Figure 11-31 present the control plots of blank material for BLK and BLK_PStone, respectively.

 

 

  

Figure 11-30: Control plot for BLK

 

 

 

Figure 11-31: Control plot for BLK_PStone

 

During the 2022 Kinross drill program, the failure rate from all blank samples was 0.2% (only 12 failures out of 7,084 blank samples inserted).

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Standards

 

For the 2022 drill program, Kinross followed the QA/QC procedures used by Great Bear in its previous drill programs. The CRMs are inserted into the sample sequences, nominally every 20 samples.

 

Table 11-6 presents a summary of results for CRMs used between March and December 2022. Figure 11-32 to Figure 11-35 present the control plots for CRMs used during this period.

 

Table 11-6: Summary of CRMs for 2022 Kinross drill program

 

CRM Name  Assay Lab.  Method  Count  Certified Value Au (g/t)  Standard Deviation  Average Assay Au (g/t)  No. of Failures  % Failures 
GS12B  Actlabs  FA-GRAV  76  11.88  0.285  11.92  2  2.6%
OR211  Actlabs  FA-AA  1,116  0.768  0.027  0.758  17  1.5%
OR216B  Actlabs  FA-AA  715  6.66  0.158  6.73  17  2.4%
OR226  Actlabs  FA-AA  5  5.45  0.126  5.37  0  0.0%
OR230  Actlabs  FA-AA  1,103  0.337  0.013  0.332  19  1.7%
OR232  Actlabs  FA-AA  1,266  0.902  0.023  0.899  19  1.5%
OR233  Actlabs  FA-AA  502  1.05  0.029  1.05  9  1.8%
OR237B  Actlabs  FA-AA  179  2.26  0.067  2.28  7  3.9%
OR238  Actlabs  FA-AA  1,149  3.03  0.080  3.04  23  2.0%
OR240  Actlabs  FA-AA  1,029  5.51  0.139  5.53  18  1.7%
Total & Avg     All  7,140           131  1.8%

 

FA-AA – fire assay AAS finish, FA-GRAV – fire assay gravimetric finish

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Figure 11-32: Control plot for OREAS 230

 

 

 

Figure 11-33: Control plot for OREAS 233

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Figure 11-34: Control plot for OREAS 238

 

 

 

Figure 11-35: Control plot for OREAS 240

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11.3.4        QA/QC – 2022 RC Drilling by Kinross

 

During the 2022 RC drill program, Kinross applied similar QA/QC procedures and insertion rates for the control samples to the diamond drill samples.

 

Table 11-7 summarizes the blanks and CRMs used in the 2022 Kinross RC drill program.

 

Table 11-7: Summary of control samples – 2022 Kinross RC drill program

 

Description  2022   Comments 
Total Number of Samples  14,273     
Number of Control Samples  2,081 (14.6%)     
Distribution        
Blanks  427 (3.0%)     
BLK  427     
Standards (CRMs)  1,654 (11.6%)     
CDN-GS-12B  117     
OREAS 211  274     
OREAS 216B  66   to Jul 2022 
OREAS 230  308     
OREAS 232  106   to Jul 2022 
OREAS 233  178     
OREAS 238  281     
OREAS 240  187     
OREAS 243  137     

 

Blanks

 

Similar to 2020, Kinross employed one blank reference material (BLK) in the sample stream. The blank failure rate for the RC program was relatively high at 6.3%. This was due mainly to the powdery nature of the RC samples that created a cloud of dust when poured into the crusher. This was identified at the early stage of the RC drill program and proactive measures, such as longer and more rigorous cleaning of the crusher by compressed air between each sample, were implemented.

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Figure 11-36 presents the control plot of blank material (BLK) inserted during the 2022 Kinross RC drill program. 

  

 

 

Figure 11-36: Control plot for BLK

 

Standards

 

For the 2022 Kinross RC drill program, the CRMs were inserted into the sample sequences nominally every 10 samples.

 

Table 11-8 presents a summary of results for CRMs used for 2022 Kinross RC drill program. Figure 11-37 to Figure 11-39 present the control plots for CRMs used for this program.

 

Table 11-8: Summary of CRMs for 2022 Kinross RC drilling program

 

CRM Name  Assay Lab.  Method   Count   Certified Value Au (g/t)   Standard Deviation   Average Assay Au (g/t)   No. of Failures   % Failures 
CDN-GS-12B  ALS  FA-GRAV   117   11.88   0.285   11.88   7   6.0%
OREAS 211  ALS  FA-AA   274   0.768   0.027   0.766   5   1.8%
OREAS 216B  ALS  FA-AA   66   6.66   0.158   6.66   2   3.0%
OREAS 230  ALS  FA-AA   308   0.337   0.013   0.335   3   1.0%
OREAS 232  ALS  FA-AA   106   0.902   0.062   0.904   1   0.9%
OREAS 233  ALS  FA-AA   178   1.05   0.029   1.06   2   1.1%
OREAS 238  ALS  FA-AA   281   3.03   0.080   3.03   7   2.5%
OREAS 240  ALS  FA-AA   187   5.51   0.139   5.46   9   4.8%
OREAS 243  ALS  FA-AA   137   12.39   0.306   12.53   4   2.9%
Total & Avg     All   1,654               40   2.4%

 

Note. FA-AA – fire assay AAS finish, FA-GRAV – fire assay gravimetric finish

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Figure 11-37: Control plot for CDN-GS-12B

 

 

 

Figure 11-38: Control plot for OREAS 211

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Figure 11-39: Control plot for OREAS 233

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Field Duplicates

 

Figure 11-40 presents the scatter plot for the results of the field duplicates collected from the RC drill program. Field duplicate assays from 2022 RC drill program showed typical scatteredness of the nuggety gold mineralization but did not reveal any bias.

 

 

  

Figure 11-40: Scatter plot for field duplicates

 

11.4QP Opinion

 

The QP is of the opinion that the preparation and analyses of the samples are adequate for this type of deposit and style of gold mineralization and that the sample handling and chain of custody, as documented, meet standard industry practice.

 

The QP has reviewed the QA/QC programs and is of the opinion that it is in accordance with standard industry practice and CIM Estimation of Mineral Resource & Mineral Reserve Best Practice Guidelines (CIM, 2019), Great Bear and Kinross personnel have taken reasonable measures to ensure that the sample analysis completed is sufficiently accurate and precise and that based on the statistical analysis of the QA/QC results, the assay results are accurate and reliable and suitable for Mineral Resource estimation.

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12.Data Verification

 

Technical information in this report has been derived from exploration programs by Great Bear and Kinross and from the existing reports and data collected by previous exploration companies that were reviewed by the QP. The QP has visited the site multiple times during 2021 and 2022 and reviewed all the procedures for collection and handling of the data from the drilling program, which includes but is not limited to the following.

 

Historical drill hole collar coordinates

 

Core handling and storage procedures

 

Core logging and sampling procedures

 

QA/QC sample insertion procedure

 

Sample packing and shipment procedures

 

In September 2022 Kinross transferred the drill hole data from Logger to acQuire database. Drill hole assays and survey data were reimported from the original certificates to ensure that accurate information is stored in the database. The data was compared between Logger and acQuire to verify the data was migrated correctly.

 

In July 2021, a consulting company, AGP Mining Consultants (AGP), was requested to review the data collection and handling procedures of Great Bear’s drilling program. The following chapters 12.1 and 12.2 are from AGP’s site visit report and follow-up work on independent sample analysis.

 

12.1AGP Site Inspection

 

The site visit to the Property was conducted by Mr. Paul Daigle, a QP from AGP from July 12 to 15, 2021, with three days on site and exploration offices in Red Lake. The 2021 drill program was underway and near completion at the time of the visit. The author was accompanied on the site visit by:

 

Dylan Langille, Project Geologist, Rimini for Great Bear

 

Rick Greenwood, Project Geologist, Rimini for Great Bear

 

The site visit included an inspection of the Project site to review drill hole collars and collar coordinates; and an inspection of the two core logging, sampling, and storage facilities in Red Lake. The visit also included a review of selected drill core and drill logs.

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Drill Hole Collar Locations

 

AGP located 60 of the 299 drill hole collars (up to March 31, 2021) at the Hinge, Limb, and LP Zones; approximately 14% of Great Bear’s drill holes. The locations of diamond drill hole collars were surveyed in the field using a handheld GPS device (Garmin GPS map 62s) and using the NAD83 datum, the same datum used by Great Bear.

 

Casing is left in the hole and Great Bear drill hole collars are capped by an aluminum screw cap that is punched with the drill hole number with a threaded rod and metal tag welded at the top. The drill hole number on some of the red flags is still legible. Some drill hole casings use a red cap covering the top of the casing. Figure 12-1 shows the drill hole collars at the LP and Hinge Zones.

 

 

 

Source: AGP (2021)

 

Figure 12-1: Drill hole collars BR-207 (left, LP Zone), DHZ-060 and 061 (right, Hinge Zone)

 

The collar coordinates measured by AGP occurred within a 4 m tolerance of those reported in the drill hole database. In the QP’s opinion, the coordinates are acceptable, given the accuracy of the handheld GPS used to check the drill hole collar locations.

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Table 12-1 and Table 12-2 present the comparison of the AGP coordinates and the Great Bear surveyed drill hole coordinates for verified drill holes in the Hinge and Limb Zones and the LP Zone, respectively.

 

Table 12-1: Drill hole collar locations - Hinge and Limb Zones

 

Drill Hole  Great Bear
Easting
(UTM E)
  Great Bear
Northing
(UTM N)
  AGP
Easting
(UTM E)
  AGP
Northing
(UTM N)
  Δ Easting
(m)
  Δ Northing
(m)
 
BR-11-A  455347  5635500  455350  5635500  -3  0  
DSL-16 -17 -18  456384  5633306  456384  5633307  0  -1  
DHZ-061  456395  5633309  456395  5633309  0  0  
DHZ-060  456395  5633309  456397  5633312  -2  -3  
DHZ-055  456455  5633339  456456  5633340  -1  -1  
DHZ-044  456479  5633298  456479  5633300  0  -2  
DHZ-044  456479  5633298  456479  5633299  0  -1  
DHZ-046 -047  456478  5633299  456478  5633295  0  4  
DHZ-036 035  456509  5633273  456508  5633271  1  2  
DHZ-037  456523  5633275  456526  5633273  -3  2  
DHZ-038A  456524  5633277  456526  5633273  -2  4  
DHZ-028 -029  456540  5633276  456541  5633275  -1  1  
DHZ-032 -033 -034  456511  5633228  456508  5633226  3  2  
DSL-009 -010 -011  456501  5633200  456497  5633200  4  0  
DHZ -022 -021  456523  5633162  456523  5633160  0  2  
DHZ -050 -051 -052  456457  5633218  456457  5633218  0  0  
DSL-019 - 020 -021  456428  5633209  456430  5633209  -2  0  
DL-58-59  456348  5633545  456350  5633544  -2  1  
DL-047  456168  5633745  456171  5633743  -3  2  

 

Source: AGP (2021)

 

Note: Datum is NAD 83 Zone 15 U.

 

Table 12-2: Drill hole collar locations - LP Zone

 

Drill Hole  Great Bear
Easting
(UTM E)
  Great Bear
Northing
(UTM N)
  AGP
Easting
(UTM E)
  AGP
Northing
(UTM N)
  Δ Easting
(m)
  Δ Northing
(m)
 
BR-207  457306  5634010  457305  5634011  1  -1  
BR-206  457347  5634028  457348  5634025  -1  3  
BR-237  457332  5633989  457329  5633987  3  2  
BR-203 BR-204  457374  5633984  457371  5633983  3  1  

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Drill Hole  Great Bear
Easting
(UTM E)
  Great Bear
Northing
(UTM N)
  AGP
Easting
(UTM E)
  AGP
Northing
(UTM N)
  Δ Easting
(m)
  Δ Northing
(m)
 
BR-208  457353  5633943  457349  5633945  4  -2  
BR-236  457271  5634080  457272  5634081  -1  -1  
BR-233  457221  5634118  457219  5634117  2  1  
BR-232  457196  5634144  457194  5634147  2  -3  
BR-038  457155  5634131  457154  5634131  1  0  
BR-144  457118  5634163  457120  5634164  -2  -1  
BR-143  457081  5634208  457081  5634206  0  2  
BR-212  456977  5634200  456975  5634201  2  -1  
BR-140  456955  5634239  456955  5634241  0  -2  
BR-164  457493  5634178  457492  5634177  1  1  
BR-220  457435  5634149  457432  5634149  3  0  
BR-109  457413  5634095  457410  5634096  3  -1  
BR-216  457412  5634095  457409  5634095  3  0  
BR-228  457512  5634241  457511  5634242  1  -2  
BR-103  457736  5634241  457738  5634240  -2  1  
REG-001  455916  5634199  455918  5634202  -2  -3  
BR-080  455975  5634707  455978  5634708  -3  -1  
DNW-006  455479  5635086  455478  5635084  1  2  
DNW-005 DNW-006  455507  5635074  455508  5635074  -1  0  
DNW-008  455489  5635139  455489  5635141  0  -2  

 

Source: AGP (2021)

 

Note: Datum is NAD 83 Zone 15 U.

 

Drill Core Review

 

The site visit included a review of drill logs and their comparison to selected drill core intervals. Mineralized intervals were selected for the review. The lithological descriptions and sample intervals recorded in the drill logs were consistent with the drill core intervals reviewed. Visible gold, where logged, was observed.

 

Table 12-3 lists the selected drill core intervals examined during the site visit.

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Table 12-3: Summary of selected drill core for review

 

Drill Hole  From
(m)
  To
(m)
  Interval
(m)
  Core
Boxes
  Target  
BR-118  52.45  66.5  14.05  10 – 14  LP/Auro  
BR-118  144.10  166.10  22.00  44 – 49  LP/Auro  
BR-196  153.35  176.40  23.05  43 – 50  LP/Auro  
BR-198  185.10  207.40  22.30  53 – 60  LP/Auro  
BR-101  184.20  221.90  37.70  59 – 71  LP/Auro  
BR-167  280.15  311.65  31.50  95 – 106  LP/Auro  
BR-243  59.25  90.80  31.55  62 – 72  LP/Auro  
BR-251  59.25  90.80  31.55  11 – 21  LP/Auro  
DL-042  131.45  145.80  14.35  42 – 46  Limb  
DHZ-031  134.20  145.60  11.40  45 – 48  Hinge  
DHZ-020  181.26  192.80  11.54  60 - 65  Hinge  

 

Source: AGP (2021)

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Drill Core Logging and Sampling Facilities

 

Great Bear maintains two logging and sampling facilities in Red Lake. The first facility is situated approximately 2.5 km northwest of Red Lake at 117 Forestry Road. This facility is a refurbished sawmill with a large warehouse split into a logging area and a core cutting area. Two ATCO trailers installed outside serve as an administration and exploration office at this site (Figure 12-2).

 

The interior of the core logging and sampling facility is clean and well maintained. 

  

 

 

Source: AGP (2021)

 

Figure 12-2: Drill logging and sampling facility at 117 Forestry Road

 

Figure 12-3 and Figure 12-4 show the core logging tables and core cutting area, respectively.

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Source: AGP (2021)

 

Figure 12-3: Drill logging table; 117 Forestry Road

 

 

 

Source: AGP (2021)

 

Figure 12-4: Core cutting area; 117 Forestry Road

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Great Bear’s second facility is housed in three rented buildings in Red Lake, located at 2 Industrial Park Road and 19 Young Street, and a garage. These facilities were the original logging and sampling facilities when Great Bear initiated its drilling programs (Figure 12-5).

 

Each building contains logging tables and core cutting facilities (Figure 12-6 and Figure 12-7). There is a large yard where core boxes are temporarily stored before being sent to the core storage/core laydown yard on the Property. This facility is the staging area for shipping samples (from both facilities). It is secured by a lock and is located next to Gardewine North, the transport company used to ship samples to Actlabs in Thunder Bay.

 

The interior of this core logging and sampling facility is kept clean and is well maintained.

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Source: AGP (2021)

 

Figure 12-5: Drill logging and sampling facility at 2 Industrial Park Road and 19 Young Street

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Source: AGP (2021)

 

Figure 12-6: Drill logging tables at the 2 Industrial Park Road facility

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Source: AGP (2021)

 

Figure 12-7: Drill core cutting room at the 2 Industrial Park Road facility

 

Core Storage

 

Drill core from the field is kept within secured logging facilities with access only for Great Bear or Rimini personnel.

 

Once the drill core is sampled, the core boxes are stacked criss-cross and strapped together for security. The core boxes are held temporarily at the 2 Industrial Park Road facility (Figure 12-8) until transported to the core storage area (core laydown area) on the Project site (Figure 12-9). Coarse rejects have also been transported to this area for storage (Figure 12-10).

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Source: AGP (2021)

 

Figure 12-8: Strapped core boxes (by drill hole), temporary core storage at the 2 Industrial Park facility

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Source: AGP (2021)

 

Figure 12-9: Core racks at the core storage area; Project site

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Source: AGP (2021)

 

Figure 12-10: Coarse rejects under tarpaulin at the core storage area; Project site

 

Historic Drill Core

 

On the Project site, historic drill core is stored close to the Hinge and Limb Zones. The core boxes are stack in criss-cross, covered with empty core boxes, and strapped (Figure 12-11). The site is overgrown; however, the boxes appear to be in good condition. Any permanent marker labels are faded but many of the boxes have etched aluminum tags with information including drill hole number, drill hole interval, and box number.

 

Kinross has reviewed and mapped these drill holes and plans to transport the core to its core storage area on the Property.

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Source: AGP (2021)

 

Figure 12-11: Historic drill core storage area; near Hinge and Limb Zone

 

12.2Independent Sample Analysis

 

The collection of independent samples is meant to demonstrate the presence of mineralization on the Property in similar ranges as reported by the issuer. These samples are not intended to act as duplicate samples.

 

AGP collected six samples by selecting sample intervals from the Great Bear drill core. The samples were collected from the same sample interval as noted in the drill hole database for comparison.

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AGP supervised the quartering of the drill core and collection of the selected sample intervals at Great Bear’s cutting room at the Forestry Road facility. The samples were placed in plastic sample bags with a sample tag inserted and sealed with a stapler. The six samples were placed in a rice bag and zip tied and kept under supervision by the QP. The samples were placed in a second rice bag and sealed with a numbered seal. The samples were shipped within one of Great Bear’s shipping bins by Gardewine North to Actlabs in Thunder Bay for sample preparation and analysis. Once received at Actlabs, the samples were:

 

prepared by crushing the samples to 80% passing 2 mm and then a split of 250 g was pulverized to 95% passing 105 µm (Actlabs Code RX1).

 

Analyzed for gold by fire assay with an AA finish (Actlabs Code 1A2B-50).

 

The six independent samples are shown in Table 12-4 and the comparison of gold results is presented in Table 12-5.

 

Table 12-4: Summary of independent samples

 

AGP Sample No.  Great Bear
Sample No.
  Drill Hole  Sample Interval
(m)
  Interval
(m)
  Target
A1047851  DX156790  BR-118  156.00 – 157.00  1.00  LP (Yuma)
A1047852  DX106614  BR-198  197.00 – 198.20  1.20  LP (Auro)
A1047853  DX150087  BR-167  289.60 – 290.35  0.75  LP (Auro)
A1047854  A00370962  DL-042  139.80 – 140.30  0.50  Limb
A1047855  A00361035  DHZ-020  185.10 – 185.85  0.75  Hinge
A1047856  DX130522  BR-243  65.00 – 65.70  0.70  LP (NW)

 

Source: AGP (2021)

 

Table 12-5: Independent sample results

 

GBR
Sample No.
  AGP
Sample No.
  Great Bear Au
(gpt Au)
  AGP Au
(gpt Au)
  Δ Au
(gpt Au)
 
DX156790  A1047851  4.94  4.14  0.80  
DX106614  A1047852  13.70  8.92  4.78  
DX150087  A1047853  6.00  5.28  0.72  
A00370962  A1047854  7.15  2.23  4.92  
A00361035  A1047855  2.43  1.70  0.73  
DX130522  A1047856  3.23  3.86  -0.63  

 

Source: AGP (2021)

 

The results of the independent samples have demonstrated the presence of gold mineralization on the Property. AGP interprets the differences of the gold grades in the independent samples to be due to the degree of variability of the gold mineralization. It should be noted that all samples, except one, returned values less than those of Great Bear, however, they are all in the range of those of Great Bear. It should also be noted that samples collected by AGP were quarter core, in lieu of half core collected by Great Bear.

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12.3QP Opinion

 

The data used to support a Mineral Resource estimate are subject to validation, using built-in software program that automatically triggers a data check for a range of data entry errors. Verification checks on surveys, collar coordinates, lithology, and assay data have been conducted. The checks were appropriate and consistent with industry standards.

 

The QP for this section is of the opinion that the sample descriptions, sampling procedures, and data entries were conducted in accordance with industry standards.

 

The QP is also of the opinion that the database is representative and adequate to support a Mineral Resource estimate for the Project.

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Ontario, Canada

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13.Mineral Processing and Metallurgical Testing

 

13.1Introduction

 

Kinross acquired Great Bear in 2022 following metallurgical test work performed at Blue Coast Research Ltd (Blue Coast Research) in 2020 and 2021. The two test work programs were designed to provide an initial understanding of gold dissolution using standard cyanidation methods on composites from the LP, Hinge, and Limb zones of the Great Bear deposit. Additional cyanidation tests were conducted to evaluate the impacts of grind size, cyanide concentration, and lead nitrate addition on gold leaching.

 

Following the acquisition, Kinross retained SGS Canada Inc. (SGS) to perform a more comprehensive test program, namely the Scoping Test Work program. This metallurgical testing program is still underway at the time of writing this report. The evaluation program includes a wide range of characterization tests comprised of detailed chemical head analysis, mineralogy, comminution, and ore sorting. Gold recovery testing incorporates a brief investigation of the heap leaching option, and a detailed examination of standard milling circuit options, including gravity separation, flotation, and cyanide leaching. A rheometallurgical program covering thickening, rheology, and filtration is also included as well as a baseline acid rock drainage (ARD) testing on final tailings from selected leach tests. Kinross notes that limited SGS Scoping Test Work results will be presented as the test work was underway at the time of writing this Technical Report.

 

As of the effective date of this Technical Report, the QP is not aware of any processing factors or deleterious elements that could have a significant effect on potential economic extraction.

 

13.1Blue Coast Test Programs Results

 

Blue Coast Research completed two preliminary metallurgical test work programs on the Project (then Dixie Project) in 2020 and 2021.

 

Sampling Program

 

In 2020, three composites were selected by representatives from Great Bear. Each composite weighed approximately 20 kg and was comprised of drill core and/or assay rejects. The three composites are listed below:

 

Hinge Zone Comp – a single composite from the Hinge Zone.

 

Dixie Limb (DL) Argillite Comp – a composite comprised of argillite rock type, within the Limb Zone.

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DL High Sulphide Comp – a composite that consists of higher sulphide material within the Limb Zone. The samples were all noted as being from the silica sulphide replacement rock type.

 

In 2021, five composites were submitted by Great Bear. Four of the five composites were designed to represent variations in grade across the deposit, while the fifth composite was selected to evaluate the impact that higher arsenic zones may have on gold recovery. The composites were:

 

LP Fault High Arsenic Comp – a composite selected to represent the LP material containing elevated quantities of arsenopyrite.

 

LP Fault 8-10 Comp – a composite with an expected average grade of 8 g/t to10 g/t Au.

 

LP Fault 3.5 Comp – a composite with an expected average grade of 3.5 g/t Au.

 

LP Fault 1.5 Comp – a composite with an expected average grade of 1.5 g/t Au.

 

LP Fault 0.5 Comp – a composite with an expected average grade of 0.5 g/t Au.

 

Sample Head Analysis

 

A chemical characterization of the composites was performed at the Blue Coast Research laboratory through the following analysis:

 

Quantitative Analysis (Au, sulphur, and carbon)

 

FA-GRAV for gold

 

ELTRA for carbon and total sulphur (Stot) and sulphide sulphur (S2)

 

CO3—ELTRA for total carbon (Ctot)

 

HCl-ELTRA for organic carbon (Corg)

 

Semi-Quantitative ICP Scan Analysis

 

The samples and head assays are listed in Table 13-1 to Table 13-3.

 

Table 13-1: Quantitative analysis - Dixie Project composite head assays

 

Composite  Au (g/t)   Stot (%)   S2- (%)   Ctot (%)   Corg (%) 
Method  FA-GRAV   ELTRA   CO3—ELTRA   ELTRA   HCl-ELTRA 
Hinge Zone Comp  13.07   0.66   0.49   1.01   0.03 

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Composite  Au (g/t)   Stot (%)   S2- (%)   Ctot (%)   Corg (%) 
DL Argillite Comp  10.64   6.29   4.81   2.55   0.37 
DL High Sulphide Comp  8.02   6.74   6.11   2.35   0.21 
LP Fault High Arsenic Comp  9.43   1.13   1.07   0.56   0.02 
LP Fault 8-10 Comp  21.9   0.94   0.79   0.26   0.06 
LP Fault 3.5 Comp  3.97   1   0.9   0.22   0.04 
LP Fault 1.5 Comp  1.54   0.86   0.6   0.21   0.02 
LP Fault 0.5 Comp  0.65   0.79   0.59   0.25   0.02 

 

Table 13-2: Semi-quantitative ICP scan analysis - Dixie Project multi-element ICP scan

 

Element   Detection
Limit
   Units   Method   Hinge Zone Composite   DL Argillite Composite   DL HS Composite 
Ag   0.2   ppm   4AD-ICP   0.7   1.4   2.1 
Al   0.01   %   4AD-ICP   5   4.5   2.9 
As   2   ppm   4AD-ICP   28.3   2,887.40   3,798.10 
Ba   2   ppm   4AD-ICP   191.6   184.8   104 
Be   0.2   ppm   4AD-ICP   0.8   0.3   <0.2 
Bi   2   ppm   4AD-ICP   <2   <2   <2 
Ca   0.01   %   4AD-ICP   5.9   6.7   6.3 
Cd   0.2   ppm   4AD-ICP   4   8.1   1.9 
Co   2   ppm   4AD-ICP   27.7   36.7   32.6 
Cr   1   ppm   4AD-ICP   197.6   116.4   92.9 
Cu   1   ppm   4AD-ICP   111.7   296.3   317.7 
Fe   0.01   %   4AD-ICP   5.7   11.2   12.2 
Ga   20   ppm   4AD-ICP   <20   <20   <20 
Ge   20   ppm   4AD-ICP   <20   <20   <20 
Hf   20   ppm   4AD-ICP   <20   <20   <20 
Hg   1   ppm   4AD-ICP   N/A   N/A   N/A 
In   20   ppm   4AD-ICP   <20   <20   <20 
K   0.01   %   4AD-ICP   0.7   0.5   0.2 
Li   2   ppm   4AD-ICP   24.2   18.6   12.1 
Mg   0.01   %   4AD-ICP   2.1   2.2   1.5 
Mn   2   ppm   4AD-ICP   1,124.40   1,466.50   1,933.30 
Mo   1   ppm   4AD-ICP   1.6   2.1   2.7 
Na   0.01   %   4AD-ICP   1.4   2.7   1.6 

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Element   Detection
Limit
   Units   Method   Hinge Zone Composite   DL Argillite Composite   DL HS Composite 
Nb   10   ppm   4AD-ICP   <10   <10   <10 
Ni   1   ppm   4AD-ICP   72.6   71.2   50.7 
P   0.002   %   4AD-ICP   0   0   0 
Pb   2   ppm   4AD-ICP   4.3   43.5   15.1 
Rb   20   ppm   4AD-ICP   33   <20   <20 
Re   20   ppm   4AD-ICP   <20   <20   <20 
S   0.01   %   4AD-ICP   0.7   6.3   7.1 
Sb   2   ppm   4AD-ICP   <2   <2   9 
Se   10   ppm   4AD-ICP   <10   <10   <10 
Sn   10   ppm   4AD-ICP   <10   <10   <10 
Sr   1   ppm   4AD-ICP   123.5   330.8   269.1 
Ta   10   ppm   4AD-ICP   <10   <10   <10 
Te   10   ppm   4AD-ICP   <10   11.6   15.8 
Ti   0.01   %   4AD-ICP   0.3   0.3   0.1 
Tl   2   ppm   4AD-ICP   <2   <2   <2 
V   1   ppm   4AD-ICP   190.3   103.4   65.9 
W   10   ppm   4AD-ICP   549.2   20.4   22.9 
Zn   2   ppm   4AD-ICP   344.5   641.1   502.2 
Zr   4   ppm   4AD-ICP   51   91.1   45.5 

 

Table 13-3: Semi-quantitative ICP scan analysis - LP multi-element ICP scan

 

Element   Detection Limit   Units   Method   LP Fault
0.5g Comp
   LP Fault
1.5g Comp
   LP Fault
3.5g Comp
   LP Fault
8-10Comp
   LP Fault High As
Comp
 
Ag   0.2   ppm   AR-ICP   <0.2   <0.2   0.8   2.4   1.9 
Al   0.01   %   AR-ICP   1.36   1.26   1.06   0.6   0.81 
As   2   ppm   AR-ICP   147   506   421   3474   640 
Ba   2   ppm   AR-ICP   59   84   75   64   93 
Be   0.2   ppm   AR-ICP   0.4   0.2   0.5   <0.2   0.2 
Bi   2   ppm   AR-ICP   <2   <2   <2   <2   <2 
Ca   0.01   %   AR-ICP   1.11   0.91   0.9   0.87   1.79 
Cd   0.2   ppm   AR-ICP   3.1   <0.2   0.2   0.3   0.5 
Co   2   ppm   AR-ICP   10   9   10   9   9 

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Element   Detection Limit   Units   Method   LP Fault
0.5g Comp
   LP Fault
1.5g Comp
   LP Fault
3.5g Comp
   LP Fault
8-10Comp
   LP Fault High As
Comp
 
Cr   1   ppm   AR-ICP   47   68   61   64   46 
Cu   1   ppm   AR-ICP   47   26   46   31   29 
Fe   0.01   %   AR-ICP   2.73   2.51   2.71   2.07   2.45 
Ga   20   ppm   AR-ICP   <20   <20   <20   <20   <20 
Ge   20   ppm   AR-ICP   <20   <20   <20   <20   <20 
Hf   20   ppm   AR-ICP   <20   <20   <20   <20   <20 
Hg   1   ppm   AR-ICP   <3   <3   <3   <3   <3 
In   20   ppm   AR-ICP   <20   <20   <20   <20   <20 
K   0.01   %   AR-ICP   0.77   0.73   0.81   0.4   0.54 
Li   2   ppm   AR-ICP   12   12   14   7   9 
Mg   0.01   %   AR-ICP   0.91   0.85   0.79   0.49   0.72 
Mn   2   ppm   AR-ICP   533   488   469   443   669 
Mo   1   ppm   AR-ICP   6   7   6   8   6 
Na   0.01   %   AR-ICP   0.05   0.06   0.04   0.04   0.04 
Nb   10   ppm   AR-ICP   <10   <10   <10   <10   <10 
Ni   1   ppm   AR-ICP   16   17   17   14   17 
P   0.002   %   AR-ICP   0.06   0.054   0.063   0.04   0.055 
Pb   2   ppm   AR-ICP   139   18   59   46   15 
Rb   20   ppm   AR-ICP   59   54   52   22   30 
Re   20   ppm   AR-ICP   <20   <20   <20   <20   <20 
S   0.01   %   AR-ICP   0.84   0.83   1.09   1   1.22 
Sb   2   ppm   AR-ICP   6   6   8   9   7 
Se   10   ppm   AR-ICP   <10   <10   <10   <10   <10 
Sn   10   ppm   AR-ICP   <10   <10   <10   <10   <10 
Sr   1   ppm   AR-ICP   16   19   10   25   25 
Ta   10   ppm   AR-ICP   <10   <10   <10   <10   <10 
Te   10   ppm   AR-ICP   <10   <10   <10   <10   <10 
Ti   0.01   %   AR-ICP   0.15   0.13   0.16   0.07   0.1 
Tl   2   ppm   AR-ICP   6   3   <2   5   2 
V   1   ppm   AR-ICP   38   38   44   22   32 
W   10   ppm   AR-ICP   12   <10   12   15   26 
Zn   2   ppm   AR-ICP   513   67   116   96   111 
Zr   4   ppm   AR-ICP   19   11   16   12   11 

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Head assays results indicate the following:

 

Silver content was relatively low and was not expected to influence carbon loadings or elution performance significantly.

 

Higher sulphide content was noted in the Limb samples.

 

Mercury levels were low.

 

Arsenic and antimony levels were low and are not expected to influence recoveries.

 

Organic carbon levels were low indicating that the preg-robbing potential should be low.

 

Base metal concentrations were low and should not influence carbon loadings.

 

Telluride levels were low and are not expected to adversely influence gold leaching kinetics or recovery.

 

Leaching

 

A total of 22 bottle roll cyanidation tests were conducted on the composites. The following leach conditions were used:

 

Residence time: 48-hour bottle

 

Pulp density: 40% solids

 

Cyanide concentration maintained: 1.0 g/L

 

pH was maintained: 10.5 and 11 with the addition of lime

 

Primary grind size: 80% passing 75 μm

 

Lead nitrate addition: 250 g/t

 

A summary of test conditions and results is presented in Table 134.

 

Table 13-4: Leaching results summary

 

Test ID  Feed  Purpose  Primary Grind
(P80, µm)
  NaCN Consumption
(kg/t)
  48 hr Au Recovery
(%)
  Residue Grade
(Au, g/t)
  Calculated Head Grade (Au, g/t) 
CN-1  Hinge Zone Comp  Effect of Primary Grind  112  0.37  95.4  0.640  14.0 

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NI 43-101 Technical Report

 

Test ID  Feed  Purpose  Primary Grind
(P80, µm)
  NaCN Consumption
(kg/t)
  48 hr Au Recovery
(%)
  Residue Grade
(Au, g/t)
  Calculated Head Grade (Au, g/t) 
CN-2  Hinge Zone Comp  Effect of Primary Grind  74  0.43  97.2  0.390  13.9 
CN-3  DL Argillite Comp  Effect of Primary Grind  138  1.10  92.9  0.720  10.1 
CN-4  DL Argillite Comp  Effect of Primary Grind  77  4.47  88.3  1.272  10.9 
CN-5  DL High Sulphide Comp  Effect of Primary Grind  121  1.11  93.1  0.620  9.0 
CN-6  DL High Sulphide Comp  Effect of Primary Grind  74  1.91  96.1  0.347  8.9 
CN-7  DL Argillite Comp  Effect of Lead Nitrate  78  1.66  97.0  0.313  10.4 
CN-8  DL Argillite Comp  Effect of Lead Nitrate  76  1.43  97.4  0.287  11.1 
CN-9  DL Argillite Comp  Effect of Cyanide Concentration  74  3.30  97.5  0.287  11.5 
CN-10  DL Argillite Comp  Effect of Lead Nitrate / Pre-treatment  79  1.56  97.1  0.288  10.1 
CN-11  DL High Sulphide Comp  Effect of Lead Nitrate  76  1.55  96.9  0.292  9.4 
CN-12  DL High Sulphide Comp  Effect of Lead Nitrate / Pre-treatment  77  1.35  96.7  0.289  8.8 
CN-13  LP Fault High As Comp  Baseline  77  0.19  98.0  0.183  9.2 
CN-14  LP Fault High As Comp  Effect of Lead Nitrate / Pre-treatment  75  0.22  97.7  0.211  9.2 
CN-15  LP Fault 8-10 Comp  Baseline  75  0.23  99.2  0.190  23.0 
CN-16  LP Fault 8-10 Comp  Effect of Lead Nitrate / Pre-treatment  74  0.27  98.7  0.341  26.6 
CN-17  LP Fault 3.5 Comp  Baseline  75  0.18  97.5  0.106  4.2 
CN-18  LP Fault 3.5 Comp  Effect of Lead Nitrate / Pre-treatment  74  0.12  97.3  0.111  4.1 

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Ontario, Canada

NI 43-101 Technical Report

 

Test ID  Feed  Purpose  Primary Grind
(P80, µm)
  NaCN Consumption
(kg/t)
  48 hr Au Recovery
(%)
  Residue Grade
(Au, g/t)
  Calculated Head Grade (Au, g/t) 
CN-19  LP Fault 1.5 Comp  Baseline  75  0.12  96.3  0.058  1.6 
CN-20  LP Fault 1.5 Comp  Effect of Lead Nitrate / Pre-treatment  74  0.19  96.4  0.049  1.4 
CN-21  LP Fault 0.5 Comp  Baseline  77  0.23  95.2  0.036  0.7 
CN-22  LP Fault 0.5 Comp  Effect of Lead Nitrate / Pre-treatment  74  0.12  95.9  0.040  1.0 

 

Test Work Conclusions

 

The following conclusions were noted from Blue Coast Research test work programs conducted on the Great Bear mineralization:

 

Gold from each composite was readily cyanide soluble with extraction during standard cyanide leach tests ranging from 95% to 99% for LP.

 

The addition of lead nitrate did not improve overall leach recovery from the LP material. Lead nitrate addition improved extraction kinetics from the highest-grade composite only. Extraction kinetics from all other composites were unaffected by the addition of lead nitrate.

 

Cyanide consumption was low, averaging 0.19 kg NaCN/tonne over all tests.

 

Higher sulphide content was noted in the Limb samples.

 

The addition of lead nitrate improved overall gold recovery and increased gold dissolution kinetics in the Limb samples. The improvement in gold dissolution kinetics was noted to be up to 24 hours in some instances.

 

Lead nitrate addition reduced the dissolution of sulphur and resulted in lower consumption of cyanide.

 

Pre-treatment with lead nitrate prior to the addition of cyanide did not result in any additional gold recovery, compared to when lead nitrate was added just prior to cyanide.

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Grinding to 75 microns appeared to improve gold recovery slightly compared to primary grinds of approximately P80=125 μm.

 

Test Work Recommendations

 

Based on results produced from the Blue Coast Research testing programs, the following recommendations were made for future work:

 

Conduct a cyanide leach optimization program exploring:

 

the gold extraction at coarser grind sizes.

 

the impact of lower concentrations of sodium cyanide and the impact they have on gold dissolution.

 

Conduct gravity recoverable gold test work to determine the potential for gravity concentration on material from the Great Bear deposit.

 

Conduct comminution test work including Bond Ball Mill Work Index and Semi-autogenous Grinding (SAG) Mill Comminution (SMC) tests to determine grindability parameters.

 

Conduct a flotation test work program to determine how the material responds to flotation.

 

Conduct additional cyanidation test work.

 

Evaluate the benefits of lead nitrate addition in the Hinge Zone material.

 

Examine the impact of primary grind size when lead nitrate is applied.

 

Carry out a variability cyanidation study on discrete spatial samples to determine the variability of metallurgical response within the deposit and to provide a link to discrete 3D space.

 

13.2SGS Metallurgical Scoping Test Work 2022

 

Sampling Program

 

Following the metallurgical test work performed at Blue Coast Research in 2020 and 2021, a more comprehensive test program was initiated by Kinross in 2022 after the acquisition of the Project. Samples were selected from different zones of the Great Bear deposit and sent to SGS for testing. This test work is underway at the time of writing this report. The purpose of the investigation is to evaluate the metallurgical response of the mineralization, provide the key metallurgical data for selection of a suitable processing flowsheet for plant design, and estimate metallurgical recoveries and processing costs for financial modelling.

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The method of preparing composite samples for the test work was based on grades and the need to obtain composites representative of the three mineralized zones of the Great Bear deposit, namely the LP Zone, Hinge Zone, and Limb Zone. The samples were predominantly NQ half drill cores from all three mineralized zones of the Great Bear deposit, with the exception of two LP samples which were PQ whole drill cores. The NQ half drill cores were from drilling programs executed prior to the acquisition. The two PQ whole drill cores consisted of fresh drill cores, BRP002 and BRP001, drilled following the Kinross acquisition in 2022.

 

Nine composite samples representative of the deposit were designed from the drill cores collected to represent the three different zones of the deposit. However, due to limited samples available, a single composite was generated from the Limb drill core collected. The nine composites are listed below:

 

C01: LP composite made of BRP002 selected PQ whole core intervals

 

C02: LP composite made of BRP001 selected PQ whole core intervals

 

C03: LP composite made of selected NQ half core intervals

 

C04: LP composite made of selected NQ half core intervals

 

C05: LP composite made of selected NQ half core intervals

 

C06: LP composite made of selected NQ half core intervals

 

C07: Hinge composite made of selected NQ half core intervals

 

C08: Hinge composite made of selected NQ half core intervals

 

C09: Limb composite made of selected NQ half core intervals

 

Figure 13-1 depicts the locations of the drill holes from where metallurgical samples for the three test work progssrams were retrieved in the Project area.

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(GRAPHIC)

 

Figure 13-1: Metallurgical sample locations from current and historical drill sites for test work programs

 

Head Assays

 

One-kilogram sub-samples of minus 1.7 mm material representing each of the 20 samples were subjected to standard screened metallics analysis for gold and silver as follows:

 

Samples were initially sieved at +/-106 μm. The minus 106 μm fraction was set aside, while the +106 μm fraction was briefly pulverized and the pulverized material re-sieved.

 

The minus 106 μm generated was combined with the previous minus 106 μm material and the process was repeated several times until only approximately 30 g remains on the sieve.

 

The +106 μm (metallics) fraction was fire assayed for gold and silver in its entirety. The combined minus 106 μm fraction was homogenized and two separately riffled approximately 30 g aliquots were submitted for fire assay for gold and silver to extinction.

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Depending on the anticipated (or known) silver grade of the sample, a separate undersize screen cut was typically retained and potentially subjected to acid digestion before being read for Ag by AAS.

 

Screened metallic analysis was used due to coarse gold in the samples. Silver assay in the +150 mesh product was less than 5 g/t Ag in some samples. For purposes of calculating, the values are set at 5 g/t Ag.

 

Duplicate gold assays on the -150 mesh fraction of the samples listed in Table 13-5 reveal some differences in the gold grades. This appears to be a nugget effect. Screened metallic gold analysis indicated that gold concentration in the -150 mesh in samples C02, C03, C05, C06, C07, C08, and C09 was higher than in the +150 mesh fraction. Silver head analysis presented in Table 13-6 shows that more than 77% of silver in samples is in the -150 mesh fraction.

 

Table 13-5: Screened metallics for Au analysis

 

       Head   +150 Mesh   -150 Mesh   % Au Distribution 
       Grade                 Au, g/t         
Ore Type  Comp   (Au, g/t)   % Mass   Au, g/t   % Mass   a   b   +150 Mesh   -150 Mesh 
LP  C01   2.08   2.8   40.9   97.2   1.22   0.70   55.1   44.9 
LP  C02   3.29   2.5   55.6   97.5   2.12   1.72   43.1   56.9 
LP  C03   2.03   3.0   13.7   97.0   1.77   1.56   20.5   79.5 
LP  C04   1.97   2.1   46.3   97.9   0.90   1.11   50.0   50.0 
LP  C05   2.64   3.0   22.7   97.0   1.53   2.51   25.8   74.2 
LP  C06   3.72   3.1   19.0   96.9   3.22   3.25   15.6   84.4 
Hinge  C07   4.25   3.0   29.5   97.0   4.08   2.89   20.5   79.5 
Hinge  C08   4.36   2.6   24.6   97.4   3.92   3.71   14.7   85.3 
Limb  C09   9.73   2.7   128.0   97.3   7.16   5.73   35.6   64.4 

 

Table 13-6: Screened metallics for Ag analysis

 

       Head   +150 Mesh   -150 Mesh   % Ag Distribution 
       Grade                 Ag, g/t         
Ore Type  Comp   (Ag, g/t)   % Mass   Ag, g/t   % Mass   a   b   +150 Mesh   -150 Mesh 
LP  C01   0.63   2.8   5   97.2   0.5   --   22.3   77.7 
LP  C02   1.72   2.5   10   97.5   1.5   --   14.8   85.2 
LP  C03   0.83   3.0   5   97.0   0.70   --   18.3   81.7 

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       Head   +150 Mesh   -150 Mesh   % Ag Distribution 
       Grade                 Ag, g/t         
Ore Type  Comp   (Ag, g/t)   % Mass   Ag, g/t   % Mass   a   b   +150 Mesh   -150 Mesh 
LP  C04   0.89   2.1   5   97.9   0.80   --   11.9   88.1 
LP  C05   0.93   3.0   5   97.0   0.80   --   16.2   83.8 
LP  C06   0.83   3.1   5   96.9   0.70   --   18.4   81.6 
Hinge  C07   0.50   --   --   --   --   --   --   -- 
Hinge  C08   0.50   --   --   --   --   --   --   -- 
Limb  C09   0.70   --   --   --   --   --   --   -- 

 

Separate, smaller representative cuts were pulverized and submitted for LECO analyses including S(T), S2-, C(T), C(graphitic) and CO32-, and for 30 element semi-quantitative ICP scan (aqua regia digest). The specific gravity of each sample was determined by gas comparison pycnometer.

 

S(total) and S(sulphide) have been performed as part of the head analysis. Ratios of S=/S(tot) presented in Table 13-7 indicate that 86% to 97% of the sulphur in the samples is present in the sulphide form. Gold deportment studies, on selected samples, will undoubtedly identify other sulphide minerals if sufficient amounts are present.

 

Results presented in Table 13-7 to Table 13-9 indicate that silver content is relatively low and is not expected to influence carbon loadings or elution performance significantly. Antimony levels are low and are not expected to influence recoveries. Organic carbon levels are low indicating that the preg-robbing potential should be low. Base metal concentrations are low and should not influence carbon loadings. The mercury analysis result is not yet available.

 

Table 13-7: Quantitative analyses of the samples

 

   LP   Hinge   Limb 
Element  C01   C02   C03   C04   C05   C06   C07   C08   C09 
Au, g/t  2.08   3.29   2.03   1.97   2.64   3.72   4.25   4.36   9.73 
Ag, g/t  0.6   1.7   0.8   0.9   0.9   0.8   0.5   0.5   0.7 
Au/Ag Ratio  3.3   1.9   2.4   2.2   2.9   4.5   8.5   8.7   13.9 
As, %  0.027   0.002   --   --   --   --   --   --   -- 
S, %  0.69   2.85   1.22   1.89   0.62   1.3   0.44   0.49   4.11 
S=, %  0.62   2.44   1.12   1.84   0.56   1.19   0.39   0.45   3.74 
S= /S %  89.9   85.6   91.8   97.4   90.3   91.5   88.6   91.8   91.0 

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   LP   Hinge   Limb 
Element  C01   C02   C03   C04   C05   C06   C07   C08   C09 
C(t), %  0.21   0.07   0.24   0.28   0.45   0.45   1.05   1.2   2.18 
C(g), %  < 0.05   < 0.05   < 0.05   < 0.05   < 0.05   < 0.05   < 0.05   < 0.05   0.22 
CO3, %  1.06   0.4   0.52   0.65   2.4   2.26   4.79   5.69   9.37 

 

Table 13-8: Semi-quantitative analyses of the samples

 

Element  C01   C02   C03   C04   C05   C06   C07   C08   C09 
Ag, g/t  < 0.8   1.4   < 0.8   < 0.8   < 0.8   < 0.8   1.1   < 0.8   < 0.8 
Al, g/t  15,600   14,400   8,280   8,730   13,200   9,610   16,500   14,000   8,230 
As, g/t  292   32   256   < 30   365   135   30   85   1770 
Ba, g/t  137   86   85.2   89.6   133   155   145   97.9   152 
Be, g/t  0.06   0.29   0.1   0.06   0.11   0.12   < 0.05   < 0.05   0.12 
Bi, g/t  < 10   < 10   < 10   < 10   < 10   < 10   < 10   < 10   < 10 
Ca, g/t  9,500   8,080   10,100   11,400   17,200   16,400   38,700   45,000   51,600 
Cd, g/t  < 2   < 2   < 4   < 4   < 4   < 4   < 4   < 4   < 4 
Co, g/t  17   16   9   12   11   11   25   22   36 
Cr, g/t  75   60   78   86   77   88   122   95   116 
Cu, g/t  43   28   46   206   31   53   108   121   235 
Fe, g/t  30,700   35,000   21,800   24,800   22,800   24,000   30,300   32,600   79,900 
K, g/t  10,300   6,910   4,340   5,470   8,410   5,500   3,810   2,420   2,530 
Li, g/t  < 20   < 20   < 20   < 20   < 20   < 20   < 20   < 20   < 20 
Mg, g/t  9,940   7,040   5,740   7,700   8,260   8,010   12,500   9,520   10,800 
Mn, g/t  399   398   334   408   890   598   674   851   1270 
Mo, g/t  < 6   < 6   7   28   < 6   < 6   < 6   < 6   < 6 
Na, g/t  430   901   691   697   939   680   851   918   413 
Ni, g/t  33   28   14   19   20   20   67   47   78 
P, g/t  558   590   469   605   608   509   233   268   335 
Pb, g/t  < 20   123   < 20   < 20   < 20   38   < 20   < 20   < 20 
Sb, g/t  < 10   < 10   < 10   < 10   < 10   < 10   < 10   < 10   < 10 
Se, g/t  < 30   < 30   < 30   < 30   < 30   < 30   < 30   < 30   < 30 
Sn, g/t  < 20   < 20   < 20   < 20   < 20   < 20   < 20   < 20   < 20 
Sr, g/t  19.3   30.7   17.5   16.7   30.8   27.2   25.4   20.1   120 
Ti, g/t  1,580   791   742   979   1490   1060   998   830   514 
Tl, g/t  < 30   < 30   < 30   < 30   < 30   < 30   < 30   < 30   < 30 
V, g/t  45   14   20   28   38   34   82   76   60 

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Element  C01   C02   C03   C04   C05   C06   C07   C08   C09 
Y, g/t  5.9   5.5   6.6   5.2   5.6   5.3   5.5   5.7   5.7 
Zn, g/t  70   159   65   89   288   166   42   35   276 

 

Table 13-9: XFR analysis of the samples

 

Oxide   C01   C02   C03   C04   C05   C06   C07   C08   C09 
SiO2 %   66.4   66.2   69.4   67   65.5   67.3   58   52.2   49.3 
Al2O3 %   14.0   14.1   13   14   14   13   11   12   8 
Fe2O3 %   5.14   5.67   3.83   4.06   4.11   4.17   9.46   12.2   14.8 
MgO %   1.98   1.65   1.13   1.76   1.77   1.65   4.9   4.42   3.84 
CaO %   3.15   2.34   2.72   3.43   3.89   3.27   8.64   10.8   8.98 
Na2O %   2.7   1.35   3.82   3.77   3.69   4.24   1.8   1.88   2.89 
K2O %   3.06   3.61   2   2   3   2   1   1   0 
TiO2 %   0.48   0.42   0.36   0.43   0.44   0.39   0.66   0.81   0.56 
P2O5 %   0.14   0.15   0.11   0.16   0.13   0.11   0.04   0.06   0.07 
MnO %   0.07   0.11   0.05   0.05   0.15   0.08   0.18   0.27   0.28 
Cr2O3 %   0.02   0.02   0.04   < 0.01   0.02   0.02   0.04   0.05   0.04 
V2O5 %   0.01   < 0.01   < 0.01   0   < 0.01   < 0.01   0   0   0 
LOI %   1.66   3   3   2   2   2   4   4   5 
Sum %   98.8   98.9   99.7   98.9   98.5   98.4   98.9   99.1   94.3 

 

Comminution

 

Several comminution tests were performed to evaluate hardness, abrasiveness, and energy requirements for ore breakage. The tests include:

 

JK drop-weight tests to determine ore resistance to the impact breakage

 

SMC tests (SAG Mill Comminution)

 

RWi - rod mill work index

 

BWi - Bond ball mill work index

 

CWi - impact crushing index

 

Ai - abrasion index

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The results from the comminution testing are summarized in Table 13-10. 

 

Table 13-10: Comminution parameters

 

                    Bond Indices 
Sample   Relative   JK Parameters   CWI   RWI   BWI   Mbi   AI 
Name   Density   A x b 1   ta   SCSE   (kWh/t)   (kWh/t)   (kWh/t)   (kWh/t)   (g) 
C01    2.77    37.05    0.35    10.39    17.0    11.5    11.3    14.8    0.323 
C02    2.79    33.5    0.31    11.0    20.40    12.8    11.9    15.8    0.269 
C03    2.72    --    --    --    --    --    13.0    18.6    -- 
C04    2.74    --    --    --    --    --    --    --    -- 
C05    2.73    --    --    --    --    --    --    --    -- 
C06    2.73    --    --    --    --    --    --    --    -- 
C07    2.87    --    --    --    --    --    15.7    23.4    0.506 
C08    2.94    --    --    --    --    15.2    14.3    21.1    0.544 
C09    2.93    --    --    --    --    15.8    15.0    22.2    0.440 

  

1 A x b from SMC Test. SCSE – Semi-autogenous Grinding Circuit Specific Energy

 

The determined Axb and SCSE parameters are categorized as “hard” ore, according to JKTech’s database; these values reflect the SAG energy requirement. BWi tests were conducted at a closing screen sizing of 90 and 75 microns. The results ranged between 11.3 kWh/t and 13.0 kWh/t for LP samples. Similar to the Limb sample, Hinge samples have an average BWi of 15 kWh/t. In comparison to the SGS hardness database, Hinge and Limb samples are hard materials whereas the LP mineralization falls in the range of moderately soft materials. From the SGS Ai database perspective, the comminution results indicate that Hinge and Limb are relatively more abrasive than LP.

 

Physical characteristics testing was conducted as part of comminution characteristics testing in the SGS Scoping Test Work program. Average rock densities of 2.75 g/cm3 and 2.91 g/cm3 were calculated for LP and Hinge samples, respectively. Only one Limb sample has been tested and gave a rock density of 2.93 g/cm3.

 

Heap Leach

 

Coarse Bottle Roll Tests

 

Heap leach amenability (COBR) tests were completed on crushed 2 kg charges in bottles on rolls on each of the samples: LP Fault C01, 02, and 03; Hinge C08; and Limb C09. The following conditions were applied:

 

Feed Mass: 2,000 g

 

Feed size: -10 and -5 mm (two tests)

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Pulp Density: 50% solids (w/w)

 

Slurry pH: 10.5 – 11.0, maintained with lime

 

Cyanide Concentration: 1 g/L NaCN, maintained

 

Leach duration: 14 days, pregnant solutions subsampled and assayed for Au-Ag after 1, 2, 4, 7, 9, 10, and 14 days

 

Coarse bottle roll cyanide leach test results are presented in Table 13-11 and Table 13-12. Results indicate a 20% increase in gold recovery with a finer grind. Limb recovery is the lowest and Hinge yielded the highest gold recovery. Silver recovery results showed that finer grinding had no major impact on LP silver recovery. LP samples produced the highest average silver recovery of 37.9%.

 

Table 13-11: Gold data, coarse bottle roll cyanide leach test results (heap leach amenability)

 

Feed Size,

P100 mm

 

NaCN

added

  

CaO

added

  

NaCN

consumed

  

CaO

consumed

  

Au

Rec. (%)

  

Residue

Grade

(Au, g/t)

  

Head

Grade

(Au, g/t)

 
All   1.803    0.473    1.252    0.313    34.9    2.13    3.18 
All -10 mm   1.778    0.444    1.242    0.272    24.9    2.39    3.18 
All -5 mm   1.827    0.502    1.261    0.355    44.8    1.86    3.18 
LP   1.673    0.512    1.035    0.369    35.1    1.92    2.83 
Hinge   1.856    0.397    1.391    0.202    41.7    2.04    3.50 
Limb   2.139    0.432    1.764    0.257    27.4    2.83    3.90 

 

Table 13-12: Silver data, coarse ore bottle roll cyanide leach test results (heap leach amenability)

 

Feed Size,

P100 mm

 

NaCN

added

  

CaO

added

  

NaCN

consumed

  

CaO

consumed

  

Ag

Rec. (%)

  

Residue

Grade

(Ag, g/t)

  

Head
Grade

(Ag, g/t)

 
All   1.80    0.47    1.25    0.31    32.2    0.70    1.05 
All -10 mm   1.78    0.44    1.24    0.27    31.6    0.71    1.05 
All -5 mm   1.83    0.50    1.26    0.35    32.9    0.69    1.05 
LP   1.67    0.51    1.03    0.37    37.9    0.82    1.30 
Hinge   1.86    0.40    1.39    0.20    23.8    0.50    0.66 
Limb   2.14    0.43    1.76    0.26    23.7    0.55    0.72 

Page 140

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Gravity

 

Milling test work is focused on gravity separation, gravity tailing cyanide leaching, and gravity tailing flotation. The majority of the tests are underway, and the results are not available yet.

 

Extended Gravity Recoverable Gold (E-GRG) Testing

 

The test consisted of three sequential liberation (stage grind) and recovery stages using 20 kg of material. The laboratory standard Knelson MD-3 concentrator was utilized to perform gravity separation after each grinding stage. The entire Knelson concentrate and a representative subsample of tailing from each stage were submitted for size fraction analysis for gold (gravity concentrate fractions were assayed to extinction). Assays from the three stages were used to construct a metallurgical balance from which the GRG number could be calculated. Note that 10 kg of the feed material (at -0.85 mm) was used for grind calibration.

 

The results of the E-GRG tests are summarized in Figure 13-2.

 

 

 

Figure 13-2: EGRG test summary results

 

Bulk Gravity Separation

 

Two-stage combined Knelson + Mozley procedure was performed on samples using standard operating procedures determined by SGS to simulate and investigate the action of a Knelson (or similar) centrifugal concentrator in commercial operation. The Mozley mass pull targets were set to be typical of the mass pull range in commercial production.

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Gold and silver recovery results are summarized in Table 13-13 and Table 13-14, respectively. Gravity recoveries of about 26% were achieved on LP samples, C02, and C04. Hinge and Limb achieved very high gold recoveries, with Hinge samples yielding the highest gold gravity recoveries. C09 showing the highest silver recovery of 49.7%.

 

Table 13-13: Gravity separation Au test results

 

           Concentrate   Tailing   Head (Au, g/t) 
Comp   Test   Grind Size
P80 µm
   % Mass   Grade
(Au, g/t)
   Recovery Au (%)   Grade
(Au, g/t)
   Calc   Direct Assay 
C02   G2    176    0.052    1,349    26.1    1.98    2.68    3.29 
C04   G4    142    0.055    613    26.6    0.93    1.26    1.97 
C07   G7    132    0.033    18,093    69.7    2.57    8.47    4.25 
C08   G8    126    0.031    11,240    67.8    1.63    5.06    4.36 
C09   G9    122    0.043    8,753    63.1    2.23    6.03    9.73 

 

Table 13-14: Gravity separation Ag test results

 

           Concentrate   Tailing   Head (Ag, g/t) 
Comp   Test   Grind Size
P80 µm
   % Mass   Grade
(Ag, g/t)
   Recovery Ag (%)   Grade,
(Ag, g/t)
   Calc   Direct Assay 
C02   G2    176    0.052    267    8.1    1.6    1.7    1.7 
C04   G4    142    0.055    101    4.6    1.1    1.2    0.9 
C07   G7    132    0.033    993    26.7    0.9    1.2    0.5 
C08   G8    126    0.031    617    21.6    0.7    0.9    0.5 
C09   G9    122    0.043    1,740    49.7    0.8    1.5    0.7 

 

Gravity + leach

 

Cyanide leach tests were completed on gravity separation tailing. All tests were conducted in bottles on rolls and included three kinetic subsamples for gold and silver analyses to monitor rates of extraction. Four tests were conducted on each gravity tailing for the purpose of semi-optimizing grind size between approximately 149 μm and 43 μm (P80). The following baseline leach conditions were recommended for the initial tests:

 

Feed Mass: 1,000 g

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Ontario, Canada

NI 43-101 Technical Report

 

Pulp Density: 50% solids (w/w)

 

Slurry pH: 10.5 – 11.0, maintained with lime

 

Cyanide Concentration: 1 g/L NaCN, maintained

 

Dissolved oxygen: 7 mg/L to 8 mg/L, maintained with air sparge at 1 L/min

 

Leach duration: 48 hours, pregnant solutions subsampled and assayed for gold and silver after 6, 24, and 48 hours.

 

Table 13-15 summarizes the gravity separation tailing cyanide leach results. Normalized recovery values were calculated with the actual assayed residue grades and the average overall calculated gravity separation head grade. The results indicate that high gold leach recoveries were achieved across all grind sizes with an average overall gold leach recovery of 95.4%.

 

Table 13-15: Gravity separation tailing cyanide leach results, the effects of grind size

 

          Reagents (kg/t of CN Feed)   Au Extraction/ Recovery (%)   Leach   Head Grade
(Au, g/t)
 
Deposit  Gravity  Grind Size   Consumed       Normalized   Residue   CN Test   Grav Test 
& Comp  Test No.  P80 µm   NaCN   CaO   Grav Sep   Overall   (Au, g/t)   (calc)   (calc) 
LP                                   
C02  G2  176   0.72    0.37   26.1   92.7   0.20   2.09   2.68 
   G2  103   0.15    0.39   26.1   96.6   0.09   1.69   2.68 
   G2  ~75   1.22    0.29   26.1   96.3   0.10   1.76   2.68 
   G2  53   1.57    0.26   26.1   95.3   0.13   1.59   2.68 
C04  G4  142   0.73    0.32   26.6   90.5   0.12   0.91   1.26 
   G4  92   0.19    0.33   26.6   92.9   0.09   0.85   1.26 
   G4  72   0.82    0.35   26.6   95.2   0.06   1.34   1.26 
   G4  53   1.13    0.32   26.6   94.1   0.08   1.36   1.26 
Hinge                                    
C07  G7  132   0.67    0.52   69.7   95.8   0.36   2.38   8.47 
   G7  88   1.20    0.51   69.7   97.1   0.25   2.44   8.47 
   G7  59   1.38    0.47   69.7   98.3   0.14   2.25   8.47 
C08  G8  126   0.80    0.49   67.8   93.3   0.34   1.50   5.06 
   G8  84   1.32    0.45   67.8   97.2   0.14   1.38   5.06 
   G8  53   1.40    0.49   67.8   98.3   0.09   1.62   5.06 

Page 143

 

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

          Reagents (kg/t of CN Feed)   Au Extraction/ Recovery (%)   Leach    Head Grade
(Au, g/t)
 
Deposit  Gravity  Grind Size   Consumed       Normalized   Residue   CN Test   Grav Test 
& Comp  Test No.  P80 µm   NaCN   CaO   Grav Sep   Overall   (Au, g/t)   (calc)   (calc) 
Limb                                    
C09  G9  122   1.45    0.81   63.1   96.7   0.20   2.20   6.03 
   G9  81   1.95    0.85   63.1   97.0   0.18   2.03   6.03 
   G9  52   2.54    0.90   63.1   97.8   0.14   1.73   6.03 

 

Gravity + flotation

 

Following gravity separation, flotation tests were completed on gravity tailings using standard operating procedures as dictated by SGS Lakefield. All rougher flotation development testing were conducted on 2 kg (dry equivalent) charges of gravity separation tailing in Denver (type) D-12 flotation machines and flotation was performed using local municipal tap water at 35% solids pulp density. A simple and proven set of reagents was used for this test work:

 

Potassium amyl xanthate (PAX)

 

Solvay Aerofloat 208

 

Methyl isobutyl carbinol (MIBC)

 

Testing at the natural pH

 

Results of the flotation tests were not available at the time of the writing of this report.

Page 144

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

14.Mineral Resource Estimate

 

14.1Summary of Mineral Resources

 

Mineral Resources are stated in accordance with Canadian Institute of Mining, Metallurgy and Petroleum (CIM) Definition Standards for Mineral Resources and Mineral Reserves dated May 10, 2014 (CIM (2014) Definitions) as incorporated by reference into NI 43-101. Mineral Resources are estimated for the Project’s LP Zone and satellite Hinge and Limb Zones and have an effective date of December 31, 2022 (Table 14-1).

 

Table 14-1: Summary of Project Mineral Resources – December 31, 2022

 

   Tonnes   Grade   Gold Ounces 
Classification  (000)  (g/t Au)   (000)
Measured   -    -    - 
Indicated   33,110    2.57    2,737 
TOTAL M&I   33,110    2.57    2,737 
Inferred   20,037    3.56    2,290 

 

Notes:

 

1.Mineral Resources estimated according to CIM (2014) Definitions.

2.Mineral Resources estimated at a gold price of US$1,700 per ounce.

3.Open pit Mineral Resources are estimated at a cut-off grade of 0.5 g/t Au. The LP Zone pit shell was selected at an input gold price of US$1,400/oz (for volume), but resources are reported based on a US$1,700/oz cut-off value. Please see Open Pit Shell and Cut-off Grade subsection for details.

4.Underground Mineral Resources are estimated at cut-off grades of 2.3 g/t Au for the LP and Hinge zones and 2.5 g/t Au for the Limb Zone.

5.Numbers may not add due to rounding.

 

The QP is not aware of any environmental, permitting, legal, title, taxation, socio-economic, marketing, political, or other relevant factors that could materially affect the Mineral Resource estimate.

 

14.2LP Zone Mineral Resource Estimate

 

Summary

 

Snowden Supervisor v 8.14.2 (Supervisor) was used for geostatistical analysis, Leapfrog Geo 2021.5 (Leapfrog) was used to generate estimation domains, and Vulcan 2022.3 (Vulcan) was used for compositing and estimation. The bulk estimation domains were interpolated by ordinary kriging (OK), while the high-grade estimation domains and background domain were interpolated using inverse distance cubed (ID3). Validation of the 2022 Great Bear LP Zone Scoping Study model (GB_LP_SS.bmf) against grade control data using the ground truth model (GT_LP_RC.bmf) showed a 0.1% difference at a 0 g/t Au cut-off grade in ounces of gold.

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

The 2022 Great Bear LP Zone Scoping Study model classification criteria are based upon the geostatistical drill hole spacing analysis supported by historic exploration and deposit growth drilling, as well as the recent 2022 drill campaign designed to upgrade unclassified material to Inferred status in and around the preliminary pit area at the LP Zone. The open pit and underground Mineral Resource estimates for the LP Zone are summarized in Table 14-2.

 

Table 14-2: LP Zone Mineral Resource summary – December 31, 2022

 

            Tonnes   Grade   Gold Ounces  
Zone       Classification   (000)   (g/t Au)   (000)  

LP

Zone

  OP   Measured   -   -   -  
    Indicated   33,110   2.57   2,737  
    TOTAL M&I   33,110   2.57   2,737  
    Inferred   8,400   2.24   606  
  UG   Measured   -   -   -  
    Indicated   -   -   -  
    TOTAL M&I   -   -   -  
    Inferred   10,585   4.54   1,547  

 

Notes:

 

1.Mineral Resources estimated according to CIM (2014) Definitions.

2.Mineral Resources estimated at a gold price of US$1,700 per ounce.

3.Open pit Mineral Resources are estimated at a cut-off grade of 0.5 g/t Au. The LP Zone pit shell was selected at an input gold price of US$1,400/oz (for volume), but resources are reported based on a US$1,700/oz cut-off value. Please see Open Pit Shell and Cut-off Grade subsection for details.

4.Underground Mineral Resources are estimated at a cut-off grade of 2.3 g/t Au.

5.Numbers may not add due to rounding.

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

LP Zone Open Pit Mineral Resource Sensitivity

 

The cut-off grade sensitivity of the open pit Indicated and Inferred Mineral Resource estimates for the LP Zone are summarized in Table 14-3. The QP notes that the contained ounces are relatively insensitive to gold cut-off grades.

 

Table 14-3: Open pit Mineral Resource sensitivity - LP Zone

 

INDICATED   CoG
(g/t Au)
  Tonnes
(000)
  Grade
(g/t Au)
  Gold Ounces
(000)
 

Open Pit 

Indicated

 

  0.5   33,110   2.57   2,737  
  0.6   29,278   2.84   2,670  
  0.7   26,095   3.10   2,603  
  0.8   23,619   3.35   2,544  
  0.9   21,686   3.57   2,491  
  1.0   20,048   3.79   2,441  
  1.1   18,537   4.01   2,390  
  1.2   17,293   4.22   2,344  
  1.3   16,226   4.41   2,302  
  1.4   15,343   4.59   2,263  
  1.5   14,508   4.77   2,224  

 

INFERRED   CoG
(g/t Au)
  Tonnes
(000)
  Grade
(g/t Au)
  Gold Ounces
(000)
 

Open Pit 

Inferred

 

  0.5   8,400   2.24   606  
  0.6   7,202   2.53   585  
  0.7   6,217   2.82   565  
  0.8   5,588   3.06   550  
  0.9   5,076   3.28   536  
  1.0   4,598   3.52   521  
  1.1   4,215   3.75   508  
  1.2   3,884   3.97   496  
  1.3   3,606   4.18   485  
  1.4   3,381   4.37   475  
  1.5   3,166   4.57   465  

 

Resource Database

 

Only diamond drill core drilled from surface was considered in this estimate and no combined data types (RC, channel, trench, etc.) were used in the resource estimate.

 

All diamond drill holes were drilled with NQ sized drill bits. The Reflex ACT III core orientation tool was used to orient 100% of the drill core at site. Drill core is split for sampling leaving the orientation line behind in the unsampled core.

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NI 43-101 Technical Report

 

In deposit areas, where recent closely spaced drilling was carried out with the purpose of upgrading resource classifications, whole core sampling accounts for approximately 5% of the total core drilled.

 

Only drill holes classified as Confidence 1 or 2 were used in the estimate.

 

The database cut-off and export date for the resource estimation was September 7, 2022. A total of 644 high-confidence drill holes in the LP Zone totalling 320,370 m of drill core and 287,942 raw assay samples were exported from acQuire to be used in the estimate.

 

Geological Model and Estimation Domains

 

Geologic logging and geostatistical analysis indicate that two broad grade populations exist in the mineralized rock. The first is a low-grade population that is made up of a large number of spatially continuous samples. This population has been modelled as broad, continuous domains that are referred to as the bulk domains. The second population is substantially higher grade and more limited in extent, falling completely within the bulk domains. This population has been modelled as limited strike, high-grade cores within the bulk domains and are referred to as the high-grade domains.

 

Current understanding suggests that the overburden on the Property is unmineralized and therefore all estimation domains are terminated on the lower contact of the alluvium model.

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Gold in the bulk and high-grade domains is predominantly found within the E31 (felsic volcaniclastics) rock unit within approximately 50 m to 100 m of the metasediment 2 contact. The E32 (fine-grained felsic volcaniclastics), metasedimentary, and fragmental (Felsic Volcaniclastics with Fragmentals) rock units are observed to contain minor gold mineralization, however, this mineralization is generally less continuous and lower grade than the mineralisation found in E31. Both bulk and high-grade domains were built considering these constraints and, where possible, follow the metasediment 2 contact rather than cross it (Figure 14-1).

 

 

 

Figure 14-1: LP Zone estimation domains, looking northwest

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The current understanding of the structural geology in the LP Zone is that two shear zones act as discontinuities to both mineralization and lithology. The LP_Shear and Yauro_Shear cross-cut the mineralization in approximately east-west striking, subvertical planes between Auro and Yauro, and Yauro and Yuma respectively. Estimation domains are truncated on these shear zones (Figure 14-2).

 

 

 

Figure 14-2: LP Zone estimation domains segmented by parallel east-west trending shear zones

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Great Bear Gold Project

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NI 43-101 Technical Report

 

Compositing

 

Sample intervals are predominantly one metre in length with 69% of samples equal to or less than one metre in length (Figure 14-3). The block size for the model is 5 m x 1 m x 5 m to support underground mine planning. A composite size of one metre was selected as it does not split too many samples while representing the block dimensions well.

 

 

 

Figure 14-3: LP Zone cumulative log histogram of assay sample lengths

 

The contacts between mineralization domains and background domains were determined to be hard boundaries. To maintain this relationship, run-length composites were generated in Vulcan breaking on estimation domains. Remnant, short intervals were then distributed back over the composites of the domain. The composites were flagged by estimation domain during the compositing process.

 

Exploratory Data Analysis

 

The composite database flagged by estimation domain was exported to .csv and imported to Supervisor for further evaluation.

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Statistics

 

Contact Analysis

 

As the high-grade domains are internal to the bulk domains, two contact analysis plots were run on composites to determine whether a soft or hard boundary should be implemented between domains including:

 

High-grade and bulk domains

 

Bulk domains and background domains

 

The contact analysis indicated that a hard boundary was appropriate both between the high-grade and bulk domains and the bulk and background domains (Figure 14-4).

 

 

 

Figure 14-4: LP Zone contact plots: transition from background domains to bulk domains (left) and bulk domains to high-grade domains (right)

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Capping

 

Capping was reviewed based on the mineralization domains. Each of the domains was capped independently. Background mineralization was also analyzed and capped. Figure 14-5 presents a log histogram, log probability plot, and capped and uncapped statistics.

 

 

 

Figure 14-5: LP Zone capping analysis

 

Uncapped and capped statistical analyses for composite data by domain are shown below in Table 14-4 and Table 14-5, respectively.

 

Table 14-4: Uncapped statistics of composite data by domain

 

Domain   N   Uncapped Mean
(g/t Au)
   Uncapped Median
(g/t Au)
   Uncapped SD
(g/t Au)
   Uncapped CV   Minimum
(g/t Au)
   Maximum
(g/t Au)
 
1   1,042   8.44   1.577   25.61   3.04   0.006   413.60 
2   1,025   4.75   1.413   18.39   3.87   0.017   384.20 
3   656   4.35   1.113   10.00   2.30   0.013   133.30 
4   101   7.41   1.118   30.17   4.07   0.020   284.20 
5   210   3.68   1.338   7.12   1.94   0.010   42.80 
6   180   3.58   0.754   9.80   2.74   0.021   87.12 
7   158   2.88   0.992   7.56   2.63   0.008   75.57 
8   383   1.42   0.869   1.66   1.17   0.006   11.27 
9   179   2.47   1.120   6.75   2.74   0.054   73.13 
10   70   3.36   0.773   9.13   2.72   0.009   54.51 
1000   3,111   0.88   0.234   3.97   4.49   0.003   119.60 
1100   514   0.73   0.269   2.91   3.97   0.003   60.75 
1200   911   1.06   0.162   5.63   5.30   0.003   114.85 
1300   607   1.19   0.171   5.14   4.31   0.003   71.21 
1400   1,061   0.46   0.080   1.43   3.08   0.003   24.41 

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Ontario, Canada

NI 43-101 Technical Report

 

Domain   N   Uncapped Mean
(g/t Au)
   Uncapped Median
(g/t Au)
   Uncapped SD
(g/t Au)
   Uncapped CV   Minimum
(g/t Au)
   Maximum
(g/t Au)
 
1500   6,177   0.29   0.072   1.56   5.37   0.003   56.72 
1600   2,089   0.19   0.023   1.33   6.89   0.003   46.26 
1700   1,767   0.42   0.128   1.19   2.83   0.003   27.35 
1800   637   0.28   0.067   0.58   2.07   0.003   5.16 
1900   156   0.37   0.089   0.87   2.37   0.003   8.63 
2000   6,586   0.44   0.172   1.86   4.20   0.003   71.75 
2100   2,579   0.66   0.114   5.04   7.63   0.003   169.40 
2200   696   0.72   0.079   4.62   6.39   0.005   84.66 
2300   2,579   0.58   0.087   3.79   6.48   0.003   135.40 
2400   439   0.83   0.043   6.58   7.94   0.003   127.00 
3000   11,172   0.48   0.189   3.89   8.05   0.003   380.00 
3100   3,465   0.36   0.077   1.98   5.54   0.003   93.44 
3200   1,259   0.46   0.046   2.77   5.98   0.003   53.70 
3300   2,089   0.34   0.036   1.82   5.44   0.003   42.76 
3400   402   0.42   0.058   1.06   2.51   0.003   10.34 
4000   1,756   0.28   0.048   0.95   3.36   0.003   17.31 
9999   330,188   0.06   0.006   1.94   31.16   0.003   949.50 

 

Table 14-5: Capped statistics of composited data by domain

 

Domain   Capping Value
(g/t Au)
   Capped Mean
(g/t Au)
   Capped SD
(g/t Au)
   Capped CV 
1   205   8.07   21.22   2.63 
2   100   4.22   10.78   2.55 
3   90   4.28   9.26   2.16 
4   90   5.48   14.65   2.67 
5   40   3.65   6.98   1.91 
6   50   3.28   7.68   2.34 
7   45   2.68   5.91   2.20 
8   10   1.41   1.63   1.16 
9   50   2.34   5.50   2.35 
10   50   3.29   8.78   2.67 
1000   35   0.82   2.87   3.50 
1100   20   0.65   1.47   2.25 

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Domain   Capping Value
(g/t Au)
   Capped Mean
(g/t Au)
   Capped SD
(g/t Au)
   Capped CV 
1200   65   0.98   4.16   4.26 
1300   60   1.17   4.90   4.17 
1400   20   0.46   1.37   2.97 
1500   45   0.29   1.44   5.02 
1600   30   0.19   1.09   5.87 
1700   20   0.42   1.11   2.66 
1800   20   0.28   0.58   2.07 
1900   5   0.35   0.67   1.93 
2000   50   0.44   1.73   3.94 
2100   70   0.61   3.83   6.26 
2200   50   0.66   3.65   5.53 
2300   50   0.54   2.68   4.94 
2400   45   0.64   3.38   5.27 
3000   60   0.45   1.40   3.11 
3100   30   0.34   1.29   3.80 
3200   45   0.45   2.62   5.75 
3300   40   0.33   1.79   5.37 
3400   20   0.42   1.06   2.51 
4000   20   0.28   0.95   3.36 
9999   20   0.05   0.44   8.33 

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Great Bear Gold Project

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NI 43-101 Technical Report

 

Variography

 

Only the bulk domains were estimated using OK. Each bulk domain had independent variography completed. The capped composite file flagged by estimation domains were imported into Supervisor and used to calculate the variograms for each domain and model the experimental variograms (Figure 14-6). Table 14-6 presents the breakdown of variogram parameters and directions.  

 

 

 

Figure 14-6: Directional variograms for LP Zone domain 1500 estimated using OK

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NI 43-101 Technical Report

 

Table 14-6: Summary of variogram parameters by domain

 

            Ranges in the Variogram Directions (m)   Orientations of the Variogram Directions (Vulcan)(degrees) 
Domain   Nugget   Sill Differential   Major Axis   Semi-major Axis   Minor Axis   Bearing   Plunge   Dip 
        0.841   68   46   13             
1000   0.106   0.0534   506   215   25   352.4   -63.2   159.6 
        0.848   83   64   20             
1100   0.1   0.515   278   95   40   341.9   -65.2   144.6 
        0.874   92   87   15             
1200   0.0983   0.0276   366   211   21   1.3   -74.2   162.0 
        0.897   98   89   20             
1300   0.0531   0.0498   311   297   40   340.7   -72.0   147.1 
        0.858   132   107   20             
1400   0.0427   0.0991   312   289   40   356.3   -74.2   162.0 
        0.834   62   42   8             
1500   0.141   0.0243   397   405   96   356.3   -74.2   162.0 
        0.877   88   42   20             
1600   0.108   0.0152   457   68   40   340.7   -72.0   147.1 
        0.798   124   118   20             
1700   0.0659   0.136   589   297   43   334.6   -75.9   135.4 
        0.819   95   46   20             
1800   0.0507   0.13   326   176   40   345.7   -72.0   147.1 
        0.559   134   270   20             
1900   0.0895   0.352   226   307   40   356.3   -74.2   162.0 
        0.777   82   73   53             
2000   0.192   0.0309   804   743   70   320.4   -65.2   128.1 
        0.826   104   108   20             
2100   0.0679   0.106   293   187   40   350.7   -72.0   147.1 
        0.893   129   68   20             
2200   0.0957   0.0117   268   374   40   345.7   -72.0   147.1 
        0.851   187   104   20             
2300   0.125   0.0244   372   293   40   333.2   -62.0   136.8 
        0.797   162   161   20             
2400   0.144   0.0591   445   356   40   339.0   -68.9   136.0 
        0.756   63   50   18             

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            Ranges in the Variogram Directions (m)   Orientations of the Variogram Directions (Vulcan)(degrees) 
Domain   Nugget   Sill Differential   Major Axis   Semi-major Axis   Minor Axis   Bearing   Plunge   Dip 
3000   0.236   0.00838   434   378   20   316.7   -49.0   105.3 
        0.8   60   47   20             
3100   0.164   0.0357   382   354   40   0.0   -75.9   135.4 
        0.847   117   32   20             
3200   0.131   0.0218   130   154   40   5.7   -72.0   147.1 
        0.862   69   63   29             
3300   0.114   0.0232   471   268   30   13.3   -78.8   153.7 
        0.761   91   68   20          
3400   0.0927   0.147   232   115   40   40   -85   180 
        0.773   200   123   20             
4000   0.19   0.0373   687   651   40   345.7   -72.0   147.1 

  

Variogram orientations were visually confirmed in Vulcan by plotting the orientations and reviewing them with the estimation domains.

 

Dynamic Anisotropy

 

The morphology of the mineralized body is curviplanar in nature. To capture the appropriate variogram and search ellipse directions within domains that exhibit significant changes in orientation, dynamic anisotropy was used. A centre plane was generated in Leapfrog for each of the domains and transferred from Leapfrog to Vulcan to generate an anisotropy model to assign to the block model.

 

Block Modelling

 

Model Setup

 

The block model is a Vulcan extended model with a parent cell size of 5 m x 1 m x 5 m and no subcells. The block model extents are presented in Table 14-7 below.

 

Table 14-7: Block model extents and the block parameters

 

Base Point
(lower left corner)
   Extents
(m)
   Block Size
(m)
   Rotation 
East   North   Z   East   North   Z   East   North   Z   Bearing   Dip   Plunge 
454,650   5,634,560   -675   4,420   1,325   1,080   5   1   5   117.2°       

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As the LP Zone has a considerable strike length, it was decided not to include subcells to keep the block model to a reasonable working size.

 

Once the block model was constructed, it was flagged using the Leapfrog estimation domains, rock model, overburden model, and classification solids, and the block fraction below topography was assigned from the high resolution LiDAR survey topography model (19_GBear_DEM_1m.00t).

 

The GB_LP_SS.bmf block model variables, variable type, and defaults are listed in Table 14-8 below.

 

Table 14-8: Description of block model variables

 

Variable   Type   Default   Description
au   Double   0   Final gold grade estimate
aupass   Int   0   Estimation pass the block was estimated on
class   Int   4   Classification domain
domain   Int   9999   Estimation domain
rock   Int   99   Rock code
sg   Double   2.715   Density (g/cm3)
topo   Double   0   Fraction of block below topo (0 = entirely above, 1 = entirely below)
vo_bearing   Double   -99   Bearing flagged from anisotropy model for dynamic anisotropy
vo_plunge   Double   -99   Plunge flagged from anisotropy model for dynamic anisotropy
vo_dip   Double   -99   Dip flagged from anisotropy model for dynamic anisotropy

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A reblocked model was generated from the GB_LP_SS.bmf block model for open pit mine planning purposes. The reblocked model has a block size of 10 m x 5 m x 10 m with each block containing twenty 5 m x 1 m x 5 m block model blocks. The criteria used for combining data from multiple blocks to create one reblocked block are listed in Table 14-9.

 

Table 14-9: Variables using majority codes, averages, and weighted averages

 

Variable  Accumulation Type  Weighting
au  Weighted average  sg
sg  Average  -

 

The rock, domain, class, and topo fields were then reassigned from wireframes.

 

Bulk Density

 

A density database was exported as part of the resource data export from acQuire. The database contained 6,717 density measurements from diamond drill core taken by the analysing assay laboratory. The rock codes from the geological model were assigned to the density samples and average density values were calculated for each rock code after accounting for statistical outliers. Those average densities were then flagged into the block model by rock code.

 

As there are currently no overburden density samples taken on the Property, the overburden density used was generated through review of similar overburden types in the region. A temporary value of 1.9 g/cm3 was used until a full density study of the overburden is complete.

 

Above Topography 0
Overburden 1.9 t/m3
Biotite_Calcite_Pillows_E1PBT 2.96 t/m3
Calc-Alk_Basalt_Undifferentiated_Arrow 2.996 t/m3
Dacite_BR_Disc 2.85 t/m3
Dyke 1 2.793 t/m3
E31 2.715 t/m3
E31_01 2.715 t/m3
E31_02 2.715 t/m3
E31_Vuggy 2.676 t/m3
E31M_magnetic_Combined 2.72 t/m3
E32_Fine_grained_felsic_combined 2.673 t/m3
Felsic_porphyry_dyke_combined 2.71 t/m3
Fragmental_1_Combined 2.729 t/m3
Fragmental_2_E3F2 2.695 t/m3
Gabbro_BK_Limb 2.793 t/m3
Granite 2.793 t/m3
High_Fe_Tholeiite_Combined 2.794 t/m3
High_Mg_Dyke_combined 2.974 t/m3
High_Mg_Tholeiitic_basalt_Combined 2.974 t/m3
High_Mg_Tholeiitic_Basalt_Massive_E1M 2.974 t/m3
High_Mg_Tholeiitic_Basalt_Viggo 2.974 t/m3
Metasediment1_MS1 2.736 t/m3
Metasediment2_MS2_combined 2.768 t/m3
Metasediment3_MS3 2.726 t/m3
Rhyolite_combined 2.73 t/m3
Sediment_combined 2.78 t/m3
Sericite_schist_Combined 2.709 t/m3
Talcy_Ultramafic_Dyke_Combined 2.83 t/m3
Tonalite_Combined 2.83 t/m3
Ultramafic_dyke_02_Br_disc 2.83 t/m3
Ultramafic_dyke_03_Br_disc 2.83 t/m3
Ultramafic_dyke_Combined 2.83 t/m3
Amphibole_Schist_Viggo 2.69 t/m3
Barren Dykes 2.69 t/m3

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Estimation

 

The 2022 Great Bear LP Zone Scoping Study model was built and estimated using Vulcan. The bulk estimation domains were estimated using OK, while the high-grade and background estimation domains were estimated using ID3. The estimate uses a two pass strategy in the bulk and high-grade estimation domains with a 200 m x 150 m x 50 m ellipse for pass one and a 100 m x 75 m x 25 m ellipse for pass two. The background estimation domain uses a single pass estimation strategy with a 250 m x 120 m x 40 m ellipse. Multiple estimates were run using various high-yield restriction radii and high-yield restriction grade thresholds, capping levels, estimation methodology (OK vs. ID3), and minimum and maximum samples included in order to align with the ground truth model.

 

High-grade Domains

 

The block model estimation used ID3 with the following implementation strategy:

 

1.5 m x 1 m x 5 m block discretization.

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2.A two pass search strategy was used, with a pass one ellipse diameter distance of 200 m x 150 m x 50 m and pass two ellipse diameter distance of 100 m x 75 m x 25 m.

 

3.Pass one required a minimum of three and maximum of eight samples. Pass two required a minimum of two and maximum of eight samples.

 

4.Passes one and two both used a maximum of two samples per drill hole.

 

5.Capping was applied during the estimation process in Vulcan.

 

6.Hard boundaries were used for all domains.

 

7.Dynamic anisotropy block model variables were used for local search ellipse orientations.

 

Bulk Domains

 

The block model estimation used OK with the following implementation strategy:

 

1.5 m x 1 m x 5 m block discretization.

 

2.A two pass search strategy was used, with a pass one ellipse diameter distance of 200 m x 150 m x 50 m and pass two ellipse diameter distance of 100 m x 75 m x 25 m.

 

3.Pass one required a minimum of three and maximum of 16 samples. Pass two required a minimum of two and maximum of 16 samples.

 

4.Passes one and two both used a maximum of two samples per drill hole.

 

5.Capping was applied during the estimation process in Vulcan.

 

6.Hard boundaries were used for all domains.

 

7.Dynamic anisotropy block model variables were used for search ellipse and variogram orientations.

 

Background Mineralization

 

The block model estimation used ID3 with the following implementation strategy:

 

1.5 m x 1 m x 5 m block discretization

 

2.A single pass search strategy was used, with the ellipse used of 250 m x 120 m x 40 m diameter.

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3.A minimum of three and maximum of eight samples were used.

 

4.A maximum of two samples per drill hole were used.

 

5.Capping was applied during the estimation process in Vulcan.

 

6.Hard boundaries were used for all domains.

 

7.Dynamic anisotropy block model variables were used for search ellipse orientation.

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Classification

 

A preliminary drill hole spacing analysis was carried out using the variograms for the major bulk and high-grade domains. A normalized gamma of 0.8 (80% of the sill) corresponds approximately with a 50 m range while a normalized gamma of 0.9 (90% of the sill) corresponds approximately with a 75 m range across those experimental variogram models (Figure 14-7). From a preliminary classification perspective, those ranges were considered as the drill spacing criteria to be used for assigning the Indicated and Inferred classifications in the 2022 Great Bear LP Zone Scoping Study model.

 

 

 

Figure 14-7: Experimental variogram models of the Auro domain

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The RC program drilling supports the analyses suggesting that there is continuity in the high-grade gold population at 50 m and reasonable continuity at 75 m (Figure 14-8).

 

 

 

Figure 14-8: RC drill program assays within the high-grade population supporting strong continuity at 50 m and reasonable continuity at 75 m spacing

 

Classification shells for Indicated and Inferred were built around drill hole traces in Leapfrog (Figure 14-9). Buffers around traces were set at a 25 m radius for Indicated and 37.5 m radius for Inferred and polylines were built around contiguous or nearly contiguous buffer shapes. The shells outline areas with drill densities meeting the spacing criteria for Indicated and Inferred and show consistent continuity, which was then used to flag the model in Vulcan. This drill hole spacing analysis is currently only applicable to the open pit material, whereas all underground material is classified as Inferred. The Measured classification was not used at this stage of the Project.

 

Classification is updated after the estimation using a block model script. Blocks estimated in pass 2 are downgraded from Indicated to Inferred.

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Figure 14-9: LP Zone classification shells based on drill hole spacing

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Validation

 

Swath plots were constructed to review estimation results (Figure 14-10) for the gold estimate compared to a nearest neighbour (NN) estimate which replicates declustered raw composite data. Overall, in areas of dense data, the estimates replicate raw data very well.

    

 

 

 

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Figure 14-10: Swath plots in major block model directions for gold as compared to the NN estimate for gold

 

Ground Truth Model Validation

 

Independent of the 2022 Great Bear LP Zone Scoping Study model, a ground truth model was built using tightly spaced (433 collar locations, 8 m across strike x 10 m along strike) RC grade control drilling that covered a volume equivalent to approximately a quarter of a year of estimated production from the open pit to a depth of approximately five benches (Figure 14-11). The location selected included a combination of high grade, low grade, and waste. No estimation domains were used due to the data density within this model. The ground truth model applied a single cap across all drill holes at 150 g/t Au. No high-yield restriction search was used. The interpolation method used was inverse distance squared (ID2).

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Comparisons to the Great Bear ground truth model were run to validate the 2022 Great Bear LP Zone Scoping Study model. A grade tonnage curve (Figure 14-12) shows that at lower cut-off grades, the ground truth model has slightly higher grades and equal tonnes, with the difference becoming slightly more pronounced at higher cut-off grades where the ground truth model has lower tonnes and a higher grade. A comparison of tonnes, grades, and ounces between the two models at various cut-off grades is summarized in Table 14-10. The variance between the two models is currently well within Kinross quarterly Key Performance Indicators (KPI) as shown in Table 14-11.

 

 

 

Figure 14-11: Ground truth model based on 8 m x 10 m RC grade control drilling 

 

 

 

Figure 14-12: Comparison of ground truth model to long-term model grade tonnage curves

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Table 14-10: Comparison of tonnes, grade, and ounces in common blocks between the ground truth and long term models

 

   Percent Difference 
Cut-off Grade (g/t Au)   Tonnes   Grade   Metal 
0.0    0%   -3%   -3%
0.6    -8%   7%   1%
3.0    -1%   2%   1%

  

Table 14-11: Kinross corporate guidance for reconciliation variance

 

KPIs    Month    Quarter    Year 
F1    ±25%   ±15%   ±10%
F2    ±10%   ±7.5%   ±5%
F3    ±25%   ±15%   ±10%

 

Mineral Resource Reporting

 

Mineral Resources are reported as per the Mineral Resource estimation methodologies and classification criteria detailed in this Technical Report. The open pit and underground resources, as of December 31, 2022, were constrained with open pit resource shells and underground mineable shapes, respectively, in order to fulfill the CIM (2014) Definitions requirement of “reasonable prospects for eventual economic extraction” (RPEEE).

 

Open Pit Shell and Cut-off Grade

 

The Kinross QP prepared a preliminary open pit shell to constrain the block model for resource reporting purposes. The preliminary pit shell was generated using Datamine Studio NPVS software using the Lerchs-Grossmann (LG) algorithm. That part of the block model that falls within the preliminary pit shell was considered to have RPEEE and is reported as a Mineral Resource at a specified cut-off grade. The Kinross QP confirmed that most of the blocks above the cut-off grade located in the resource pit shell show good continuity (Figure 14-13).

 

The LP zone pit shell was selected at an input gold price of US$1,400/oz (for volume), but resources are reported based on a US$1,700/oz cut-off grade. The US$1,400/oz shell size was selected as a result of initial optimizations between open pit and underground. Furthermore, only the Central section of the LP Zone was considered for open pit resource, with Discovery (NW) and Viggo (SE) areas considered entirely underground resource.

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Assumptions used in the preliminary LG pit shell analysis were:

 

Gold price: US$1,700/oz (C$2,210/oz)

 

Exchange rate: US$1.00 = C$1.30

 

Pit slope angles:

 

Overburden 0-5m Thick: 18°

 

Overburden 5-15m Thick: 14°

 

Overburden 15-40m Thick: 14.1°

 

Overburden 40m+ Thick: 10°

 

Hard Rock: 46°

 

Process recovery of gold: 95.3% overall

 

Mining cost for waste: C$3.69 per tonne

 

Mining cost for mineralized material: C$3.69 per tonne

 

Processing cost: C$18.68 per tonne

 

General and administrative (G&A) costs: C$12.10 per tonne

 

The LG analysis produced a pit discard cut-off grade of 0.50 g/t Au.

 

Process recovery of gold was calculated based on a feed grade recovery formula. The mining cost was derived from a base unit cost of C$3.38 per tonne and incremental vertical bench (10 m) cost of C$0.026 per tonne per bench below reference and C$0.017 per tonne per bench above reference.

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Figure 14-13: LP resource open pit shell in 3D

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Underground Reporting and Cut-off Grade

 

Underground Mineral Resources are reported within underground reporting shapes generated using the Mineable Shape Optimizer (MSO) tool, and defined using a minimum stope thickness of 2.5 m, limited to areas of continuous mineralization. A cut-off grade of 2.3 Au g/t was used for the LP Zone underground. All blocks within the underground constraining shapes have been included within the Mineral Resource estimate, and underground reporting shapes are presented in Figure 14-14. Underground resource is reported using $1700 MSOs up to the open pit resource shell. It was assumed that the crown pillars to surface and underneath the pits can be recovered. No surface water bodies are present in the breakthrough areas. Stope shapes that were considered too isolated or small to be reasonably accessed and extracted were excluded from the resource.

 

The Underground Mineral Resource cut-off grade was calculated with the gold price and full operating costs including mining, processing, and G&A. The cut-off grade has been calculated based on longitudinal long-hole stoping mining method with cemented backfilling, with underground extraction concurrent with the open pit mining.

 

Assumptions used to estimate the underground cut-off grade were:

 

Gold price: US$1,700/oz (C$2,210/oz)

 

Exchange rate: US$1.00 = C$1.30

 

Process recovery of gold: 95.9%

 

Mining cost: C$104.0 per tonne

 

Processing cost: C$18.68 per tonne

 

G&A costs: C$12.10 per tonne

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Figure 14-14: LP underground resource shapes

 

Comparison to Previous Models

 

The 2022 Great Bear LP Zone Scoping Study model is the first model to be released for the zone and as such has no previous models to compare to.

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14.3Hinge and Limb Zone Mineral Resource Estimate

 

Great Bear’s Hinge and Limb Zones are satellite deposits located approximately 750 m southwest of the main LP Zone. The resource inventory was built using Snowden Supervisor v8.14.3.1 for geostatistical analysis and Leapfrog Geo/Edge 2022.1.1 for geological and domain modelling, compositing, and estimation. The Limb estimation domains comprise a mineralized zone within metasediments with silica and sulphide replacement hosted in the north limb of the fold. The Hinge estimation domains encompass quartz veins within a tholeiitic basalt in the axial plane of the fold. The main vein at Limb was interpolated using OK and the remaining lenses, using ID3.

 

The model classification criteria are based on drilling spacing analysis, 75 m for Limb and 50 m for Hinge, considering the differences in the mineralization and its continuity between the two zones. The Mineral Resource estimate for the Hinge and Limb Zones are summarized in Table 14-12.

 

Table 14-12: Hinge and Limb Zone Mineral Resource summary – December 31, 2022

 

Zone       Classification  

Tonnes

(000)

Grade

(g/t Au)

Gold Ounces

(000)

Hinge Zone   UG   Measured   -   -   -  
Indicated   -   -   -  
TOTAL M&I   -   -   -  
Inferred   263   5.93   50  
Limb Zone   UG   Measured   -   -   -  
Indicated   -   -   -  
TOTAL M&I   -   -   -  
Inferred   788   3.44   87  
Total   UG   Measured   -   -   -  
Indicated   -   -   -  
TOTAL M&I   -   -   -  
Inferred   1,052   4.06   138  

 

Notes:

 

1.Mineral Resources estimated according to CIM (2014) Definitions.

2.Mineral Resources estimated at a gold price of US$1,700 per ounce.

3.Underground Mineral Resources are estimated at a cut-off grade of 2.50 g/t Au for Limb and 2.30 g/t Au for Hinge.

4.Numbers may not add due to rounding.

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Resource Database

 

The database cut-off and export date for the resource estimation was November 24, 2022. The database was exported from acQuire and consists of:

 

227 drill holes, totalling 88,676 m.

 

2,996 samples for a total length of 2,064 m.

 

Historical data that did not have collar positions and survey data were removed from the resource database.

 

Geological Model and Estimation Domains

 

The Limb estimation domains comprise a continuous mineralized zone within metasediments, occurring between high Fe tholeiite and calc-alkaline basalt in the north limb of the fold (Figure 14-15). The Hinge estimation domains comprise quartz veins within high Fe tholeiitic basalt in the axial plane of the fold. A total of six (101 to 106) estimation domains were built for Limb and 19 (201 to 219) estimation domains were built for Hinge.

 

The current understanding of the deposit suggests that the overburden on the Property is unmineralized, and therefore all estimation domains are terminated on the lower contact of the overburden model.

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Figure 14-15: Lithological model section cutting the main Limb vein with the folded metasedimentary layer

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Compositing

 

The sample intervals are predominantly 0.5 m in length and 90% of the samples are equal to or less than one metre in length (Figure 14-16). The minimum block size in the octree block model is 0.625 m x 0.625 m x 1 m to support underground planning. A composite size of one metre was selected as it covers the majority of the sample length while representing the block dimensions well at both Limb and Hinge.

 

 

 

Figure 14-16: Limb and Hinge histogram of assay sample lengths

 

The contacts between mineralization domains and background were determined to be hard boundaries. The composites were generated in Leapfrog inside estimation domains and flagged with the corresponding domain code. Remnant, short intervals were then added to the previous interval.

 

Exploratory Data Analysis

 

The composite database flagged by the estimation domains was exported to .csv and imported to Supervisor for further evaluation.

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Statistics

 

Contact Analysis

 

The contact analysis shows that hard boundaries are appropriate and the estimation data should be constrained by the domains (Figure 14-17).

 

Grade transition from Limb 101 domain to background

 

 

 

Grade transition from Hinge 201 domain to background

 

 

 

Figure 14-17: Limb and Hinge contact plot figures

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Capping

 

Capping was carried out on a domain by domain basis and analyzed in four different graphs. The uncapped and capped statistics are shown to the right of the graphs in Figure 14-18 for Limb and Figure 14-19 for Hinge and summarized in Table 14-13 for both zones. Each domain was capped independently.

 

 

 

Figure 14-18: Limb 101 domain capped and uncapped statistics

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Figure 14-19: Hinge 201 domain capped and uncapped statistics

 

Table 14-13: Capped and uncapped composite statistics by domain

 

        Uncapped   Capped  
Domain   Samples   Mean
(g/t Au)
  Median
(g/t Au)
  SD
(g/t Au)
  CV   Min
(g/t Au)
  Max
(g/t Au)
  Capping
Value
(g/t Au)
  Mean
(g/t Au)
  SD
(g/t Au)
  CV  
101   1,275   2.66   1.49   5.68   2.14   0.003   117.02   47   2.56   4.18   1.64  
102   28   1.34   0.96   1.13   0.84   0.005   5.44   -   -   -   -  
103   10   2.01   1.28   1.78   0.88   0.120   6.72   -   -   -   -  
104   6   2.12   0.55   3.44   1.63   0.397   9.81   -   -   -   -  
105   25   2.19   0.09   6.09   2.79   0.003   30.20   10   1.38   2.74   1.99  
106   94   2.41   1.65   3.17   1.32   0.003   25.61   10   2.24   2.22   0.99  
201   166   6.17   1.19   18.32   2.97   0.003   174.77   70   5.35   12.58   2.35  
202   80   3.20   1.35   6.58   2.05   0.006   50.09   30   2.95   4.98   1.69  
203   65   2.17   0.65   5.86   2.7   0.003   41.21   23   1.89   4.18   2.21  
204   15   1.83   1.31   1.77   0.97   0.003   6.60   -   -   -   -  
205   7   16.59   10.32   16.85   1.02   3.256   56.82   30   12.75   7.98   0.63  

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        Uncapped   Capped  
Domain   Samples   Mean
(g/t Au)
  Median
(g/t Au)
  SD
(g/t Au)
  CV   Min
(g/t Au)
  Max
(g/t Au)
  Capping
Value
(g/t Au)
  Mean
(g/t Au)
  SD
(g/t Au)
  CV  
206   25   14.21   0.86   27.8   1.96   0.003   121.10   40   9.51   13.87   1.46  
207   10   2.05   1.62   1.41   0.69   0.115   5.18   -   -   -   -  
208   96   20.49   1.16   92.83   4.53   0.003   863.70   135   11.45   27.14   2.37  
209   79   4.53   0.62   11.42   2.52   0.003   58.40   30   3.58   7.5   2.1  
210   11   4.28   0.93   6.36   1.49   0.136   19.36   -   -   -   -  
211   14   3.83   0.54   8.31   2.17   0.049   32.66   10   2.21   3.14   1.42  
212   37   0.79   0.56   0.79   0.99   0.007   2.79   -   -   -   -  
213   14   1.45   0.67   1.36   0.94   0.003   4.15   -   -   -   -  
214   6   7.84   0.93   9.11   1.16   0.019   25.50   15   6.09   6.04   0.99  
215   9   3.18   1.82   3.65   1.15   0.095   12.28   -   -   -   -  
216   7   0.51   0.53   0.24   0.46   0.003   0.82   -   -   -   -  
217   39   2.64   0.16   6.78   2.57   0.003   33.94   22   2.33   5.51   2.36  
218   7   3.42   0.92   3.47   1.02   0.133   9.72   -   -   -   -  
219   13   6.56   0.66   12.88   1.96   0.162   49.10   -   -   -   -  

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Variography

 

Only the main Limb domain (code 101) was estimated using OK (Figure 14-20). The variograms were modelled in both Supervisor and Leapfrog with very similar results.

 

 

 

Figure 14-20: Variogram model for Limb 101 domain estimated using OK

 

Dynamic Anisotropy

 

Dynamic anisotropy was applied during the estimation in Leapfrog Edge due to the curviplanar nature of the veins. The wireframes were used to calculate the orientation of search ellipses for each block.

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Block Modelling

 

Model Setup

 

The block model was built in Leapfrog and the octree option was chosen in order to have small blocks to better fill the wireframes, replicate the solids volume, and minimize dilution in the optimization (Figure 14-21).

 

 

 

Figure 14-21: Octree block model setup in Leapfrog

 

A list of variables and their descriptions is presented in Table 14-14.

 

Table 14-14: Block model variables description

 

Variable   Description
Auppm   Final gold grade estimate
Density   Density assigned by lithology and estimation domain
Domain   Estimation domain codes
Class   Classification domains
Litho   Lithology codes
Topo   Above and below topography code

 

Bulk Density

 

The cores were sampled for specific gravity analysis and they are well spatially distributed throughout the deposit. A descriptive statistic was made for each rock code assigned from the geological model and an average density was assigned to lithology and estimation domains.

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As there are currently no overburden density samples taken on the Property, the overburden density used was generated through review of similar overburden types in the region. A temporary value of 1.9 g/cm3 was used until a full density study of the overburden is complete.

 

Above Topography = 0

 

Overburden = 1.9 t/m³

 

Limb Domains = 2.9 t/m³

 

Hinge Domains = 2.78 t/m³

 

Rhyolite = 2.79 t/m³

 

Metasediment = 2.8 t/m³

 

Basalt = 2.89 t/m³

 

Gabbro = 2.89 t/m³

 

Ultramafic Dyke = 2.99 t/m³

 

Estimation

 

The main Limb estimation domain (code 101) was estimated using OK, while all the other veins from Limb and Hinge were estimated using ID3. The estimate employs a two pass strategy using the same search distance, varying the minimum number of samples (five samples in the first pass and one sample in the second pass). Both passes used a maximum of two samples per drill hole. High-grade restriction was used in the second pass in domains 101, 201, 202, and 203 to avoid spreading high grade in areas with sparse drilling support.

 

Table 14-15 lists search distances for each estimation domain.

 

Table 14-15: Ellipsoid search distances for each estimation domain

 

   Search Distance (m)  
Domain  Maximum  Intermediate  Minimum  
101  280  90  20  
102  100  50  10  
103  50  25  10  
104  200  100  20  
105  100  50  10  

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   Search Distance (m)  
Domain  Maximum  Intermediate  Minimum  
106  100  50  10  
201  150  50  10  
202  70  40  10  
203  70  40  10  
204  70  40  10  
205  70  40  10  
206  70  40  10  
207  70  40  10  
208  70  40  10  
209  70  40  10  
210  150  75  10  
211  200  150  30  
212  150  75  20  
213  150  100  10  
214  150  75  10  
215  75  50  10  
216  75  50  10  
217  150  75  10  
218  150  100  10  
219  100  75  10  

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Classification

 

All Inferred material is estimated in pass 1, which estimates blocks using at least five samples and a minimum of three drill holes. A drilling spacing of 75 m for Limb and 50 m for Hinge were also considered, as well as the mineralization continuity. The material that does not fit the specification above (including blocks estimated in pass 1) is coded as unclassified material (Figure 14-22).

 

 

 

Figure 14-22: Classification for Limb looking northeast (left) and Hinge looking northwest (right)

 

Validation

 

Swath plots in the X, Y, and Z directions were used to validate the Au estimation on the Limb and Hinge domains comparing them to the declustered data as an NN interpolator. Overall, the Inferred blocks show the same trends as the declustered data, with some discrepancies due to the use of high-grade restriction on the OK and ID3 estimators.

 

Mineral Resource Reporting

 

Mineral Resources are reported as per the Mineral Resource estimation methodologies and classification criteria detailed in this Technical Report. The underground resources, as of December 31, 2022, were constrained with underground mineable shapes in order to fulfill the RPEEE requirement of the CIM (2014) Definitions.

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Underground Reporting and Cut-Off Grade

 

Underground Mineral Resources are reported within underground reporting shapes generated using the MSO tool, and defined using a minimum stope thickness of 2.0 m, limited to areas of continuous mineralization. The cut-off grades were 2.3 Au g/t for the Hinge Zone and 2.5 Au g/t for the Limb Zone. All blocks within the underground constraining shapes have been included within the Mineral Resource estimate, and underground reporting shapes are presented in Figure 14-23. It was assumed that the crown pillars to surface and underneath the pits can be recovered. No surface water bodies are present in the breakthrough areas. Stope shapes that were considered too isolated or small to be reasonably accessed and extracted were excluded from the resource.

 

The Underground Mineral Resource cut-off grades were calculated with the gold price and full operating costs including mining, processing, and G&A. The cut-off grades have been calculated based on longitudinal long-hole stoping mining method with cemented backfilling, with underground extraction concurrent with the open pit mining.

 

Assumptions used to estimate the underground cut-off grades were:

 

Gold price: US$1,700/oz (C$2,210/oz)

 

Exchange rate: US$1.00 = C$1.30

 

Process recovery of gold: 93.7% for Limb and 93.6% for Hinge

 

Mining cost: C$104.00 per tonne

 

Processing cost per tonne: C$28.41 for Limb and C$19.79 for Hinge

 

G&A costs: C$12.10 per tonne

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Figure 14-23: Underground Hinge and Limb resource shapes looking northwest

 

14.4Underground Mineral Resource Sensitivity

 

The cut-off grade sensitivity of the underground Mineral Resource estimate for the LP, Hinge, and Limb zones is summarized in Table 14-16. The QP notes that the contained ounces are relatively insensitive to gold cut-off grades.

 

Table 14-16: Underground Inferred Mineral Resource sensitivity - LP, Hinge, and Limb

 

    CoG
(g/t Au)
  Tonnes
(000)
  Grade
(g/t Au)
  Gold Ounces
(000)
 

Underground
Inferred

  2.3   11,636   4.50   1,684  
  2.5   10,575   4.71   1,602  
  3.0   7,825   5.41   1,361  
  3.5   5,989   6.07   1,169  
  4.0   4,824   6.64   1,029  
  4.5   3,904   7.20   904  
  5.0   3,029   7.90   770  

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15.Mineral Reserve Estimate

 

There are no Mineral Reserves estimated for this Project.

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16.Mining Methods

 

This section is not applicable.

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17.Recovery Methods

 

This section is not applicable.

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18.Project Infrastructure

 

This section is not applicable.

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19.Market Studies and Contracts

 

This section is not applicable.

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20.Environmental Studies, Permitting, and Social or Community Impact

 

This section is not applicable.

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21.Capital and Operating Costs

 

This section is not applicable.

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22.Economic Analysis

 

This section is not applicable.

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23.Adjacent Properties

 

There is significant historic and present gold production in the Red Lake mining camp. The entire Red Lake/Birch-Uchi Greenstone Belt continues to be explored by major and junior mining companies. Significant mining, preproduction, and greenfields exploration programs are taking place proximal to the Project (Figure 23-1).

 

(graphic) 

 

Figure 23-1: Location of the Great Bear Project and adjacent projects

 

The Project lies approximately 24 km southeast of Evolution Mining Limited’s Red Lake Gold Mine complex. The Red Lake Gold Mine complex is situated within the Red Lake Greenstone Belt and comprised of the historic, Campbell, Dickenson and Red Lake Mines which have produced approximately 24 million ounces of gold between 1948 and 2021 (Malegus, 2022).

 

Pure Gold Mining Inc., the owners of the 47 km2 claims that encompass the Madsen Mine project located 15km northwest of the Great Bear Project, suspended operations and placed the mine on care and maintenance on October 24, 2022. The historic Madsen and Starratt Olsen Mines combined, produced 2.6 million ounces (Malegus, 2022).

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A total of 25 junior companies and individual prospectors are significant claimholders in the Project area. A number of these claimholders are conducting current exploration programs. BTU Metals Corp. owns 19,723 ha directly south of the Great Bear property boundary. They have completed various exploration activities including till sampling, ground/airborne geophysical surveys, and diamond drilling.

 

The QP has compiled this information from publicly available data but has not personally verified data from adjacent properties. Results from neighbouring properties, verified or not, may not necessarily be indicative of the mineralization on the Project.

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24.Other Relevant Data and Information

 

No additional information or explanation is necessary to make this Technical Report understandable and not misleading.

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25.Interpretation and Conclusions

 

25.1Geology and Mineral Resources

 

The Project lies within a regional northwest-southeast trending belt of metavolcanic and metasedimentary rocks which are bounded by intrusive batholiths.

 

Three zones of mineralization have been identified within the Project area, LP, Limb, and Hinge, representing three dominant styles of mineralization: silica sulphide replacement, quartz veining, and disseminated gold in a high strain corridor.

 

A combined total of 1,170 drill holes totalling 563,191 m have been drilled by Great Bear and Kinross between January 1, 2017 and December 31, 2022.

 

Mineral Resources conform to CIM (2014) Definitions.

 

As of December 31, 2022, Mineral Resources at the Project consist of:

 

Indicated: 33.1 Mt grading 2.57 g/t Au and containing 2.7 Moz of gold.

 

Inferred: 20.0 Mt grading 3.56 g/t Au and containing 2.3 Moz of gold.

 

The sample preparation and analyses are adequate for this type of deposit and style of gold mineralization and the sample handling and chain of custody, as documented, meet standard industry practice.

 

The QA/QC program is in accordance with standard industry practice and CIM MRMR Best Practice Guidelines. Kinross personnel have taken reasonable measures to ensure that the sample analysis completed is sufficiently accurate and precise and that, based on the statistical analysis of the QA/QC results, the assay results are accurate and reliable and are suitable for Mineral Resource estimation.

 

The data used to support a Mineral Resource estimate are subject to validation using built-in software program that automatically triggers a data check for a range of data entry errors. Verification checks on surveys, collar coordinates, lithology, and assay data have been conducted. The checks were appropriate and consistent with industry standards.

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An RC drill program was undertaken in 2022 to generate a ground truth model separate from the resource model for validation purposes. A total of 433 drill holes were completed on a 8 m x 10 m grid designed to re-create a grade control drill program on approximately a quarter of a year of estimated production from the open pit across a combination of low, medium, and high grade. The variance between the two models is currently well within Kinross quarterly KPIs providing good confidence that the resource model is performing well.

 

The sample descriptions, sampling procedures, and data entries were conducted in accordance with industry standards.

 

The database is representative and adequate to support a Mineral Resource estimate for the Project.

 

An open pit and underground scenario was contemplated for the LP Zone and an underground scenario, for the Hinge and Limb zones. The open pit and underground resources were constrained within $1,400 open pit resource shells and $1,700 underground mineable shapes, respectively, and fulfill the CIM (2014) Definitions requirement of “reasonable prospects for eventual economic extraction” (RPEEE).

 

25.2Metallurgical Testing

 

The following conclusions were noted based on the preliminary metallurgical test work carried out by Blue Coast Research in 2020 and 2021:

 

Gold from each composite was readily cyanide soluble with extraction during standard cyanide leach tests ranging from 95% to 99%.

 

The addition of lead nitrate did not improve overall leach recovery from the LP material. Lead nitrate addition improved extraction kinetics from the highest-grade composite only. Extraction kinetics from all other composites were unaffected by the addition of lead nitrate.

 

Cyanide consumption was low, averaging 0.19 kg NaCN/tonne over all tests.

 

Higher sulphide content was noted in the Limb samples.

 

The addition of lead nitrate improved overall gold recovery and increased gold dissolution kinetics in the Limb samples. The improvement in gold dissolution kinetics was noted to be up to 24 hours in some instances.

 

Lead nitrate addition reduced the dissolution of sulphur and resulted in lower consumption of cyanide.

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Pre-treatment with lead nitrate prior to the addition of cyanide did not result in any additional gold recovery, compared to when lead nitrate was added just prior to cyanide.

 

Grinding to 75 microns appeared to improve gold recovery slightly compared to primary grinds of approximately P80=125 μm.

 

A more comprehensive metallurgical testing program is currently underway at SGS and has the purpose of evaluating the metallurgical response of the mineralization, providing the key metallurgical data for selection of a suitable processing flowsheet for plant design, and estimating metallurgical recoveries and processing costs for financial modelling.

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26.Recommendations

 

Based on the information presented in this Technical Report and results of the ongoing work on the Project, the QPs’ recommendations are summarized as follows.

 

All three target zones continue to warrant follow-up drilling. There is a three-fold objective for the continued drilling: establishing the extent of the deposit along strike and its depth potential, property-wide exploration, and definition drilling, with the first being the primary focus. The LP Zone is the most attractive target based on its potential size and high gold grades, and therefore continues to be prioritized.

 

Concurrently with drilling, the Project should continue with metallurgical and other technical studies and permitting. The Mineral Resource is substantial enough to initiate more advanced studies.

 

In addition, an Advanced Exploration Program (AEX) is recommended that would enable exploration drilling to be completed from underground, testing the depth of the deposit as well as better defining the deposit for engineering work.

 

26.1Exploration Drilling

 

Exploration drilling at the Project should continue with multiple drill holes targeting both depth and strike potential. A specific focus should be on testing the deposit at and below the 1,000 m vertical depth to define the underground extents. For this purpose, additional drilling is proposed to be carried out on the Property. In conjunction with drilling, the Project should continue its ongoing highly technical program of data collection and analysis. The continued development of the geological model as well as continued geological mapping are considered highly important for Project advancement.

 

Specific exploration recommendations for 2023 and beyond are as follows:

 

1.Continue diamond drilling to test:

 

Extent of deposit along strike

 

Extent of deposit at depth

 

New targets throughout Property

 

Condemnation for potential infrastructure locations

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Upgrade Inferred Mineral Resources to Indicated Resources where feasible, to allow for completion of technical studies and future Mineral Reserve estimation

 

26.2Project Development

 

Based on the current Mineral Resources, the Project shows sufficient economic potential to initiate advanced studies.

 

The QPs recommend that Great Bear continue with engineering studies on ground conditions, site layout, metallurgical testing, soil geotechnical drilling and testing, and environmental baseline studies. Great Bear will continue to follow standard project development framework, with both open pit and underground studied. Specific Project recommendations for 2023 and beyond are summarized below:

 

1.Continue baseline environmental studies for input into permitting and engineering studies.

 

2.Continue to engage with our First Nations partners and local stakeholders.

 

3.Study the Project with engineering partners following project stage-gating (Scoping, PFS, FS).

 

4.Although the underground will not be fully defined, it is recommended that site infrastructure considers what the underground may become.

 

5.Further mine plan optimisation of the open pit and underground resource.

 

6.Continue with metallurgical studies to test the variability of the deposits considering the significant strike length and depth.

 

7.Implement geotechnical work on both the bedrock and soil geotechnical characterization including geophysics, drilling, and laboratory testing using a speciality consultant.

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26.3Advanced Exploration Program

 

The Property, centered around the LP Zone deposit, continues to be open at depth and additional drilling is required to estimate the potential at depth, approximately 500 vertical metres from surface. For this purpose, an AEX program should be evaluated which would require a portal and decline to be established to access the underground and drill from depth. The initial concept being contemplated would allow exploration drilling to start from approximately 600 vertical metres from surface and test the depth extent of the deposit. Due to the deposit’s characteristics, drilling from the underground is considered to be more feasible for upgrading the underground resource to a higher category. AEX has proved to be an efficient method to define underground deposits. AEX would also aid in the engineering studies and design of the future Project.

 

It is recommended by the QP that Great Bear complete the engineering and baseline environmental studies on the AEX program be completed as a priority and the Ontario permitting process be initiated.

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27.References

 

Adamova, A., 2021. Technical Report on the Dixie Property, Red Lake, Ontario, a NI 43-101 report prepared for Great Bear Resources Ltd., with an effective date of January 1, 2020, amended on April 6, 2021.

 

Armstrong B., Kolb, M., Hmidi, N., 2018. Red Lake Operations Ontario, Canada NI 43-101 Technical Report (published on SEDAR).

 

Canadian Institute of Mining, Metallurgy and Petroleum (CIM), 2014. CIM Definition Standards for Mineral Resources and Mineral Reserves, adopted by the CIM Council on May 10, 2014.

 

CIM, 2019. CIM Estimation of Mineral Resources & Mineral Reserves Best Practice Guidelines, adopted by the CIM Council on November 29, 2019.

 

Dube et al., 2003a. Geology of the Archean Goldcorp High-Grade Zone, Red Lake Mine, Ontario: implications for exploration and potential analogy with the Timmins camp; Abstract: CIMM Mining Industry Conference; Montreal 2003.

 

Dube et al., 2003b. Gold mineralization within the Red Lake mine trend: example from the Cochenour-Willians mine area, Red Lake, Ontario, with new key information from the Red Lake mine and potential analogy with the Timmins camp; Geological Survey of Canada Current Research, 2003C-21, 15p.

 

Dube et al., 2000. A preliminary report on amphibolite-facies, disseminated replacement-style mineralization at the Madsen gold mine, Red Lake, Ontario. Geological Survey of Canada, Current Research2000-C17, 12p.

 

Lee, C., 2006. Independent Technical Report on the Dixie Lake Project, Red Lake, Ontario. Fronteer Development Group 43-101 report prepared by SRK (published on SEDAR).

 

Lambert, M B; Burbidge, G; Jefferson, C W; Beaumont-smith, C; Lustwerk, R (1990). “Stratigraphy, Facies and Structure in Volcanic and Sedimentary Rocks of the Archean Back River Volcanic Complex, N.w.t.” Current Research, Part C, Geological Survey of Canada, Paper 90-IC: 151–165.

 

Malegus, P.M., Amyotte, E.G., Adrianwalla, C.J., Wiebe, K.E., Bousquet, P., Daniels, C.M., Pettigrew, T.K. and Dorland, G. 2022. Report of Activities 2021, Resident Geologist Program, Red Lake Regional Resident Geologist Report: Red Lake and Kenora Districts; Ontario Geological Survey, Open File Report 6381, 10p.

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Parker, J.R. 1999a. Gold potential in Ball, Todd and Fairlie township, Red Lake greenstone belt; in Summary of Field Work and Other Activities, Ontario Geological Survey, Open File Report 6000, p.20-1 to 20-11.

 

Parker, J.R. 1999b. Exploration potential for volcanogenic massive sulphide deposits (VMS) in the Red Lake greenstone belt; in Summary of Field Work and Other Activities, Ontario Geological Survey, Open File Report 6000, p.19-1 to 19-24.

 

Ross, K., 2004. Petrographic Report of Five Samples from the Dixie Lake Project, Red Lake District, Ontario. Panterra Geoservices Inc. Unpublished

 

Ross, K., 2018. Petrographic Report on the Dixie Gold Project, Red Lake District, Ontario. Panterra Geoservices Inc. Unpublished

 

Ross K., 2019. Petrographic Report on the Dixie Gold Project, Red Lake District, Ontario. Panterra Geoservices Inc. Unpublished

 

Ross K., 2020. Petrographic Report on the Dixie Gold Project, Red Lake District, Ontario. Panterra Geoservices Inc. Unpublished

 

Sanborn-Barrie, M., et al., 2001. Three hundred million years of tectonic history recorded by the Red Lake greenstone belt, Ontario; Geological Survey of Canada, Current Research2001-C19, 29p.

 

Sanborn-Barrie, M., Skulski, T., and Parker, J., 2001. Three hundred million years of tectonic history recorded in the Red Lake greenstone belt, Ontario; GSC, Current Research 2001-C19.

 

Sanborn-Barrie, M., Rogers, N., Skulski, T., Parker, J., McNicoll, V., and Devaney, J., 2004. Geology and Tectonostratigraphic Assemblages, East Uchi Subprovince, Red Lake and Birch-Uchi belts, Ontario; Geological Survey of Canada, open File 4256; Ontario Geological Survey, Preliminary Map P. 3460, scale 1:250,000

 

Sanborn-Barrie, M., et al., 2004. Geology, Red Lake greenstone belt, western Superior Province, Ontario, 1:50,000 map sheet; Geological Survey of Canada Open File 4594.Singh R., 2019. A Near Surface, High Grade Gold Discovery Dixie Project, Red Lake, Ontario https://greatbearresources.ca/wp-content/uploads/2019/02/GBR-MAR-Technical-PPT-1.pdf

 

Stott, G.M., and Corfu, F., 1991. Uchi Sub-province, in Geology of Ontario, Ontario Geological Survey, Special Volume 4, Pt. 1, pp. 145-236, ed. Thurston P. C. et al.

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Sylvester, P. J.; Harper, G. D.; Byerly, G. R.; Thurston, P. C. (1997). “Volcanic Aspects”. In De Wit, Maarten J.; Ashwal, Lewis D. (eds.). Greenstone belts. Oxford: Clarendon Press. pp. 55–90.

 

Thompson P., 2003. Toward a new metamorphic framework for gold exploration in the Red Lake greenstone belt. Ontario Geological Survey Open File report 6122, 51p.

 

Thurston, P.C., Osmani, I.A. and Stone, D., 1991. Northwestern Superior Province: Review and terrane analysis; in Geology of Ontario, Ontario Geological Survey, Special Volume 4, Part 1, p.81-144.

 

Zeng F. AJ Calvert, 2006, Imaging the upper part of the Red Lake greenstone belt, Northwestern Ontario, with 3D traveltime tomography, Canadian Journal of Earth Sciences 43 (7), p.849- 863.

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28.Date and Signature Page

 

This Technical Report entitled “Great Bear Gold Project Ontario, Canada - Voluntary National Instrument 43-101 Technical Report” with an effective date of December 31, 2022 was prepared by the following authors:

 

“Signed and sealed”

 

Nicos Pfeiffer, P.Geo.
Vice President Geology
February 13, 2023

 

“Signed and sealed”

 

John Sims, CPG
Company Qualified Person
President of Sims Resources LLC
February 13, 2023

 

“Signed and sealed”

 

Yves Breau, P.Eng.
Vice-President Metallurgy, Engineering and Energy
February 13, 2023

 

“Signed and sealed”

 

Rick Greenwood, P.Geo.
Exploration Manager
February 13, 2023

 

“Signed and sealed”

 

Agung Prawasono, P.Eng.
Senior Director, Mine Planning
February 13, 2023

Page 210

 

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Ontario, Canada

NI 43-101 Technical Report

 

29.Certificate of Qualified Person

 

29.1Nicos Pfeiffer

 

I, Nicos Pfeiffer, P.Geo., as an author of this report entitled “Great Bear Gold Project Ontario, Canada - Voluntary National Instrument 43-101 Technical Report” with an effective date of December 31, 2022, prepared for Kinross Gold Corporation, do hereby certify that:

 

1)I am Vice President Geology with Kinross Gold Corp. of 25 York Street, 17th floor Toronto On.

 

2)I am a graduate of Carleton University, Ottawa, Ontario in 2009 with an Honours B.Sc. Earth Science.

 

3)I am registered as a Professional Geologist in the Province of Ontario (Reg# 2354). I have worked in geology for a total of 15 years. My relevant experience for the purpose of the Technical Report is:

 

Domestic and international experience in both underground and open pit operation geology roles.

 

Extensive experience in gold exploration and resource estimation.

 

Experience leading multi-disciplinary technical teams in both a corporate and operational capacity.

 

4)I have read the definition of “qualified person” set out in National Instrument 43-101 (NI 43-101) and certify that by reason of my education, affiliation with a professional association (as defined in NI 43-101) and past relevant work experience, I fulfill the requirements to be a “qualified person” for the purposes of NI 43-101.

 

5)I visited the Great Bear Project on numerous regular intervals throughout 2022.

 

6)I am responsible for Section 14 (except Mineral Resource Reporting) of the Technical Report.

 

7)I am not independent of the Issuer applying the test set out in Section 1.5 of NI 43-101.

 

8)I have had prior involvement with the property that is the subject of the Technical Report.

 

9)I have read NI 43-101, and the Technical Report has been prepared in compliance with NI 43-101 and Form 43-101F1.

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Ontario, Canada

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10)At the effective date of the Technical Report, to the best of my knowledge, information, and belief, Section 14 (except Mineral Resource Reporting) in the Technical Report for which I am responsible contains all scientific and technical information that is required to be disclosed to make the Technical Report not misleading.

 

Dated this 13th of February 2023

 

(Signed and Sealed)

 

Nicos Pfeiffer, P.Geo.

Page 212

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

29.2John Sims

 

I, John Sims, C.P.G., as an author of this report entitled “Great Bear Gold Project Ontario, Canada - Voluntary National Instrument 43-101 Technical Report” with an effective date of December 31, 2022, prepared for Kinross Gold Corporation, do hereby certify that:

 

1)I am President of Sims Resources LLC, of 945 Wyoming Street Unit 214 Missoula, MT 59801.

 

2)I am a graduate of University of Montana, in 1992 with a BS Degree(s) in Geology and Mathematics.

 

3)My relevant experience for the purpose of this Technical Report is:

 

I have over 30 years of mining industry experience. My experience with respect to mineral resources and reserves includes resource exploration geologist in Chile, Honduras, Mexico, Tanzania and USA; exploration project manager in Nicaragua; mine site project manager and geologist at underground and open pit mines in western USA, Central and South America; 20 years of resource modelling and reserve optimization experience for deposits in Argentina, Australia, Chile, Bolivia, Ecuador, Ghana, Mauritania, Mexico, Russia, Tanzania and USA. I have 19 years of experience as a site and corporate Qualified Person which includes positions as a Senior Project Mine Geologist, then Director of Technical Services for Coeur d’Alene Mines Corporation, and as Director, then VP & SVP of Technical Services for Kinross Gold Corporation. I have contributed to, and project managed multi-disciplinary teams that required close interaction with mining engineers for mineral reserve estimation, as well as consideration of recovery methods, project infrastructure, costs and economics including Scoping, Prefeasibility and Feasibility studies.

 

4)I have read the definition of “qualified person” set out in National Instrument 43-101 (NI 43-101) and certify that by reason of my education, affiliation with a professional association (as defined in NI 43-101) and past relevant work experience, I fulfill the requirements to be a “qualified person” for the purposes of NI 43-101.

 

5)I visited the Great Bear Project on October 19 and 20, 2022.

 

6)I am responsible for the overall preparation of the Technical Report and in particular, Sections 1 to 10, and 23 to 27 of the Technical Report.

 

7)I am independent of the Issuer applying the test set out in Section 1.5 of NI 43-101.

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

8)I have had no prior involvement with the property that is the subject of the Technical Report.

 

9)I have read NI 43-101, and the Technical Report has been prepared in compliance with NI 43-101 and Form 43-101F1.

 

10)At the effective date of the Technical Report, to the best of my knowledge, information, and belief, the Technical Report contains all scientific and technical information that is required to be disclosed to make the Technical Report not misleading.

 

Dated this this 13th of February 2023

 

(Signed and Sealed)

 

John Sims, C.P.G.

Page 214

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

29.3Yves Breau

 

I, Yves Breau, P.Eng., as an author of this report entitled “Great Bear Gold Project Ontario, Canada – Voluntary National Instrument 43-101 Technical Report” with an effective date of December 31, 2022, prepared for Kinross Gold Corporation, do hereby certify that:

 

1)I am Vice-President Metallurgy, Engineering and Energy with Kinross Gold Corporation, of 25 York Street, 17th Floor, Toronto, Ontario, M5J 2V5.

 

2)I am a graduate of University of Laval, Québec City in 1997 with a bachelors in Materials and Metallurgy Engineering.

 

3)I am registered as a Professional Engineer in the Province of Ontario (Reg.# 100194755). I have worked as an engineer for a total of 23 years since my graduation. My relevant experience for the purpose of the Technical Report is:

 

My work experience has included multiple operations roles from metallurgist to process manager and multiple mining company corporate roles from manager to Vice-President.

 

In my roles in operations and corporate, I have completed many studies related to gold mineral processing.

 

4)I have read the definition of “qualified person” set out in National Instrument 43-101 (NI 43-101) and certify that by reason of my education, affiliation with a professional association (as defined in NI 43-101) and past relevant work experience, I fulfill the requirements to be a “qualified person” for the purposes of NI 43-101.

 

5)I visited the Great Bear Project in March 2022.

 

6)I am responsible for Section 13 of the Technical Report.

 

7)I am not independent of the Issuer applying the test set out in Section 1.5 of NI 43-101.

 

8)I have had no prior involvement with the property that is the subject of the Technical Report.

 

9)I have read NI 43-101, and the Technical Report has been prepared in compliance with NI 43-101 and Form 43-101F1.

 

10)At the effective date of the Technical Report, to the best of my knowledge, information, and belief, Section 13 in the Technical Report for which I am responsible contains all scientific and technical information that is required to be disclosed to make the Technical Report not misleading.

Page 215

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

  

Dated this this 13th of February 2023

 

(Signed and Sealed)

 

Yves Breau, P.Eng.

Page 216

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

29.4Rick Greenwood

 

I, Rick Greenwood, P.Geo., as an author of this report entitled “Great Bear Gold Project Ontario, Canada – Voluntary National Instrument 43-101 Technical Report” with an effective date of December 31, 2022, prepared for Kinross Gold Corporation, do hereby certify that:

 

1)I am Exploration Manager with Kinross Gold Corp., of Red Lake, Ontario, Canada.

 

2)I am a graduate of Memorial University of Newfoundland and Labrador in 2004 with a Bachelor of Science (Hons.) Degree in Earth Science.

 

3)I am registered as a Professional Geologist in the Province of Ontario (Reg.# 2390). I have worked as a geologist for 19 years since my graduation. My relevant experience for the purpose of the Technical Report is:

 

16+ years experience working in Archean Greenstone belt environments in the North West of Ontario as a Geologist to Exploration Manager.

 

4)I have read the definition of “qualified person” set out in National Instrument 43-101 (NI 43-101) and certify that by reason of my education, affiliation with a professional association (as defined in NI 43-101) and past relevant work experience, I fulfill the requirements to be a “qualified person” for the purposes of NI 43-101.

 

5)I am a full time employee at the Great Bear Gold Project site.

 

6)I am responsible for Sections 11 and 12 of the Technical Report.

 

7)I am not independent of the Issuer applying the test set out in Section 1.5 of NI 43-101.

 

8)I have been actively involved since March of 2018 on the project that is the subject of the Technical Report.

 

9)I have read NI 43-101, and the Technical Report has been prepared in compliance with NI 43-101 and Form 43-101F1.

 

10)At the effective date of the Technical Report, to the best of my knowledge, information, and belief, Sections 11 and 12 in the Technical Report for which I am responsible contain all scientific and technical information that is required to be disclosed to make the Technical Report not misleading.

 

Dated this this 13th of February 2023

 

(Signed and Sealed)

 

Rick Greenwood, P.Geo.

Page 217

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

29.5Agung Prawasono

 

I, Agung Prawasono, P.Eng., PMP, as an author of this report entitled “Great Bear Gold Project Ontario, Canada – Voluntary National Instrument 43-101 Technical Report” with an effective date of December 31, 2022, prepared for Kinross Gold Corporation, do hereby certify that:

 

1)I am a Senior Director, Mine Planning with Kinross Gold Corporation, of 25 York Street, 17th Floor, Toronto, Ontario M5J 2V5.

 

2)I am a graduate of UPN “Veteran” Yogyakarta, Indonesia in 1999 with a Bachelor of Engineering Degree in Mining Engineering program.

 

3)I am registered as a Professional Engineer in the Province of Ontario (Reg.#100533117). I have worked as a mining engineer for a total of 23 years since my graduation. My relevant experience for the purpose of the Technical Report is 23 years’ experience in resource optimization related works that includes mine designs and mine planning for precious and base metal operations and projects in Indonesia, India, Africa, North America and South America.

 

4)I have read the definition of “qualified person” set out in National Instrument 43-101 (NI 43-101) and certify that by reason of my education, affiliation with a professional association (as defined in NI 43-101) and past relevant work experience, I fulfill the requirements to be a “qualified person” for the purposes of NI 43-101.

 

5)I visited the Great Bear Project on June 24, 2022.

 

6)I am responsible for the portion of Section 14 that covers Mineral Resource Reporting.

 

7)I am not independent of the Issuer applying the test set out in Section 1.5 of NI 43-101.

 

8)I have been actively involved since February of 2022 on the project that is the subject of the Technical Report.

 

9)I have read NI 43-101, and the Technical Report has been prepared in compliance with NI 43-101 and Form 43-101F1.

 

10)At the effective date of the Technical Report, to the best of my knowledge, information, and belief, Section 14 (Mineral Resource Reporting) in the Technical Report for which I am responsible contains all scientific and technical information that is required to be disclosed to make the Technical Report not misleading.

Page 218

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Dated this this 13th of February 2023

 

(Signed and Sealed)

 

Agung Prawasono, P.Eng., PMP

Page 219

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

30.Appendix 1 - Land Tenure

Page 220

 

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Table 30-1: Great Bear claim list

 

Tenure

Number

 

Title

Type

 

Tenure

Status

 

Issue

Date

 

Anniversary

Date

  Area
(ha)
 
100967  SCMC  Active  2018-04-10  2024-09-13  20.3838  
101494  SCMC  Active  2018-04-10  2024-09-13  20.3801  
101530  SCMC  Active  2018-04-10  2024-08-03  20.3901  
101612  SCMC  Active  2018-04-10  2026-08-03  20.3979  
101895  SCMC  Active  2018-04-10  2024-08-04  20.3855  
102017  SCMC  Active  2018-04-10  2024-06-21  20.3874  
102839  SCMC  Active  2018-04-10  2024-02-08  20.3891  
103070  SCMC  Active  2018-04-10  2024-08-04  20.3891  
103309  SCMC  Active  2018-04-10  2024-08-03  20.3784  
111854  SCMC  Active  2018-04-10  2024-08-03  20.3874  
111855  SCMC  Active  2018-04-10  2024-08-03  20.3875  
111856  SCMC  Active  2018-04-10  2024-09-08  20.3893  
111882  SCMC  Active  2018-04-10  2024-08-03  20.3713  
112519  BCMC  Active  2018-04-10  2025-08-03  3.3254  
112520  SCMC  Active  2018-04-10  2024-08-03  20.3962  
113713  SCMC  Active  2018-04-10  2024-08-03  20.3681  
114024  SCMC  Active  2018-04-10  2024-08-03  20.3822  
114025  SCMC  Active  2018-04-10  2024-08-03  20.3653  
114026  SCMC  Active  2018-04-10  2024-08-03  20.3714  
114064  SCMC  Active  2018-04-10  2024-08-03  20.3697  
114065  SCMC  Active  2018-04-10  2024-08-03  20.3715  
114070  SCMC  Active  2018-04-10  2024-08-03  20.3698  
114071  SCMC  Active  2018-04-10  2024-08-03  20.3717  
114072  SCMC  Active  2018-04-10  2024-08-03  20.3753  
114286  SCMC  Active  2018-04-10  2024-08-03  20.3752  
114299  SCMC  Active  2018-04-10  2024-08-03  20.3894  
114301  SCMC  Active  2018-04-10  2024-08-03  20.3785  
114302  SCMC  Active  2018-04-10  2024-08-03  20.3786  
114303  SCMC  Active  2018-04-10  2024-08-03  20.3804  
114304  SCMC  Active  2018-04-10  2024-08-03  20.3839  
114652  SCMC  Active  2018-04-10  2024-09-13  20.3802  
116114  SCMC  Active  2018-04-10  2024-08-03  20.3907  
116131  SCMC  Active  2018-04-10  2024-09-13  20.3910  
116196  SCMC  Active  2018-04-10  2024-06-06  20.3892  

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Tenure

Number

 

Title

Type

 

Tenure

Status

 

Issue

Date

 

Anniversary

Date

  Area
(ha)
 
116197  SCMC  Active  2018-04-10  2024-06-21  20.3892  
116500  SCMC  Active  2018-04-10  2024-08-03  20.3802  
116858  SCMC  Active  2018-04-10  2024-08-03  20.3919  
117355  SCMC  Active  2018-04-10  2024-08-03  20.3725  
117356  SCMC  Active  2018-04-10  2026-08-03  20.3730  
117357  SCMC  Active  2018-04-10  2024-08-03  20.3766  
117411  SCMC  Active  2018-04-10  2024-08-03  20.3889  
117462  SCMC  Active  2018-04-10  2024-08-03  20.3854  
118161  SCMC  Active  2018-04-10  2024-08-04  20.3891  
118232  SCMC  Active  2018-04-10  2024-08-03  20.3872  
119141  SCMC  Active  2018-04-10  2024-09-13  20.3855  
121662  SCMC  Active  2018-04-10  2024-08-03  20.3943  
121663  SCMC  Active  2018-04-10  2024-08-03  20.3960  
121774  SCMC  Active  2018-04-10  2024-08-03  20.3979  
121820  SCMC  Active  2018-04-10  2024-02-05  20.3783  
125191  SCMC  Active  2018-04-10  2024-08-04  20.3909  
125336  SCMC  Active  2018-04-10  2024-06-29  20.3874  
125688  BCMC  Active  2018-04-10  2025-02-08  2.3268  
125785  BCMC  Active  2018-04-10  2024-08-03  11.2340  
126417  SCMC  Active  2018-04-10  2024-08-03  20.3846  
127173  SCMC  Active  2018-04-10  2024-08-03  20.3785  
127174  SCMC  Active  2018-04-10  2024-08-03  20.3785  
127175  SCMC  Active  2018-04-10  2024-08-03  20.3802  
127704  SCMC  Active  2018-04-10  2024-08-03  20.3872  
128876  SCMC  Active  2018-04-10  2024-02-05  20.3818  
128877  SCMC  Active  2018-04-10  2024-01-05  20.3837  
128878  SCMC  Active  2018-04-10  2024-09-13  20.3837  
130582  SCMC  Active  2018-04-10  2024-08-03  20.3661  
131296  SCMC  Active  2018-04-10  2024-08-03  20.3698  
131305  SCMC  Active  2018-04-10  2024-08-03  20.3876  
131309  SCMC  Active  2018-04-10  2024-08-03  20.3821  
132390  BCMC  Active  2018-04-10  2024-09-08  6.1323  
132391  BCMC  Active  2018-04-10  2024-09-08  6.4141  
132392  SCMC  Active  2018-04-10  2026-08-03  20.3712  
132557  SCMC  Active  2018-04-10  2024-08-03  20.3662  

Page 222

 

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Ontario, Canada

NI 43-101 Technical Report

 

Tenure

Number

 

Title

Type

 

Tenure

Status

 

Issue

Date

 

Anniversary

Date

  Area
(ha)
 
138479  BCMC  Active  2018-04-10  2025-08-03  3.4707  
138480  SCMC  Active  2018-04-10  2024-08-03  20.3944  
139245  SCMC  Active  2018-04-10  2024-09-13  20.3783  
139246  SCMC  Active  2018-04-10  2024-09-13  20.3784  
143920  SCMC  Active  2018-04-10  2026-08-03  20.3925  
144522  SCMC  Active  2018-04-10  2024-08-03  20.3749  
146647  SCMC  Active  2018-04-10  2024-08-03  20.3698  
146648  SCMC  Active  2018-04-10  2024-08-03  20.3716  
146649  SCMC  Active  2018-04-10  2024-08-03  20.3752  
147364  SCMC  Active  2018-04-10  2024-08-03  20.3642  
147882  SCMC  Active  2018-04-10  2024-08-03  20.3875  
147887  SCMC  Active  2018-04-10  2024-08-03  20.3785  
147888  SCMC  Active  2018-04-10  2024-08-03  20.3858  
147969  SCMC  Active  2018-04-10  2024-08-03  20.3694  
151438  SCMC  Active  2018-04-10  2024-08-03  20.3680  
151443  SCMC  Active  2018-04-10  2024-08-03  20.3751  
151959  SCMC  Active  2018-04-10  2024-09-08  20.3893  
154397  BCMC  Active  2018-04-10  2024-08-04  1.2305  
155096  SCMC  Active  2018-04-10  2024-08-03  20.3871  
155097  SCMC  Active  2018-04-10  2024-08-03  20.3871  
155098  SCMC  Active  2018-04-10  2024-08-03  20.3889  
155608  SCMC  Active  2018-04-10  2024-08-03  20.3821  
155648  SCMC  Active  2018-04-10  2024-08-03  20.3890  
156818  SCMC  Active  2018-04-10  2024-09-08  20.3910  
158073  SCMC  Active  2018-04-10  2024-08-03  20.3749  
160649  SCMC  Active  2018-04-10  2024-08-03  20.3786  
160650  SCMC  Active  2018-04-10  2024-08-03  20.3804  
160652  SCMC  Active  2018-04-10  2024-08-03  20.3660  
160653  SCMC  Active  2018-04-10  2024-08-03  20.3678  
160654  SCMC  Active  2018-04-10  2024-08-03  20.3696  
160690  SCMC  Active  2018-04-10  2024-08-03  20.3661  
160695  SCMC  Active  2018-04-10  2024-08-03  20.3734  
160898  SCMC  Active  2018-04-10  2024-08-03  20.3907  
160939  SCMC  Active  2018-04-10  2024-02-05  20.3801  
161433  SCMC  Active  2018-04-10  2024-08-03  20.3822  

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Ontario, Canada

NI 43-101 Technical Report

 

Tenure

Number

 

Title

Type

 

Tenure

Status

 

Issue

Date

 

Anniversary

Date

  Area
(ha)
 
161434  SCMC  Active  2018-04-10  2024-08-03  20.3858  
162005  SCMC  Active  2018-04-10  2024-08-03  20.3750  
162006  SCMC  Active  2018-04-10  2024-08-03  20.3787  
162318  BCMC  Active  2018-04-10  2024-09-08  4.9728  
162792  SCMC  Active  2018-04-10  2024-08-03  20.3926  
162793  SCMC  Active  2018-04-10  2024-08-03  20.3926  
163391  SCMC  Active  2018-04-10  2024-08-03  20.3767  
164901  BCMC  Active  2018-04-10  2024-09-13  14.2817  
165478  SCMC  Active  2018-04-10  2024-08-03  20.3659  
166020  SCMC  Active  2018-04-10  2024-08-03  20.3661  
166024  SCMC  Active  2018-04-10  2024-08-03  20.3717  
166308  SCMC  Active  2018-04-10  2024-08-03  20.3907  
166309  SCMC  Active  2018-04-10  2024-08-03  20.3937  
166310  SCMC  Active  2018-04-10  2024-08-03  20.3955  
166311  SCMC  Active  2018-04-10  2024-08-03  20.3978  
166752  SCMC  Active  2018-04-10  2024-08-03  20.3893  
166753  BCMC  Active  2018-04-10  2025-08-03  6.8282  
166757  SCMC  Active  2018-04-10  2024-08-03  20.3858  
166823  SCMC  Active  2018-04-10  2024-08-03  20.3694  
166824  SCMC  Active  2018-04-10  2024-08-03  20.3713  
166894  SCMC  Active  2018-04-10  2024-08-03  20.3907  
166895  SCMC  Active  2018-04-10  2024-08-03  20.3925  
166896  SCMC  Active  2018-04-10  2024-08-03  20.3961  
167506  SCMC  Active  2018-04-10  2024-08-03  20.3733  
170319  SCMC  Active  2018-04-10  2024-02-08  20.3909  
170893  SCMC  Active  2018-04-10  2024-08-03  20.3890  
171031  SCMC  Active  2018-04-10  2024-08-04  20.3891  
172297  SCMC  Active  2018-04-10  2024-08-03  20.3872  
173077  SCMC  Active  2018-04-10  2024-08-03  20.3854  
173078  BCMC  Active  2018-04-10  2024-08-04  14.9481  
173190  SCMC  Active  2018-04-10  2024-08-03  20.3871  
173746  SCMC  Active  2018-04-10  2024-08-04  20.3909  
174508  SCMC  Active  2018-04-10  2024-08-03  20.3803  
174543  SCMC  Active  2018-04-10  2026-08-03  20.3871  
174544  SCMC  Active  2018-04-10  2024-08-03  20.3908  

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Tenure

Number

 

Title

Type

 

Tenure

Status

 

Issue

Date

 

Anniversary

Date

  Area
(ha)
 
175718  SCMC  Active  2018-04-10  2024-08-03  20.3856  
175743  SCMC  Active  2018-04-10  2024-08-03  20.3693  
177634  SCMC  Active  2018-04-10  2024-07-31  20.3856  
178443  SCMC  Active  2018-04-10  2024-09-13  20.3910  
179661  SCMC  Active  2018-04-10  2024-08-03  20.3907  
179662  SCMC  Active  2018-04-10  2024-08-03  20.3942  
180358  SCMC  Active  2018-04-10  2024-09-13  20.3819  
183121  SCMC  Active  2018-04-10  2024-09-26  20.3820  
183122  SCMC  Active  2018-04-10  2024-09-26  20.3839  
183133  SCMC  Active  2018-04-10  2024-02-08  20.3891  
183134  SCMC  Active  2018-04-10  2024-02-08  20.3910  
183135  BCMC  Active  2018-04-10  2024-08-04  2.9022  
183942  SCMC  Active  2018-04-10  2024-09-13  20.3855  
185056  SCMC  Active  2018-04-10  2024-08-03  20.3838  
185075  SCMC  Active  2018-04-10  2024-08-03  20.3693  
189773  SCMC  Active  2018-04-10  2024-08-03  20.3864  
189774  SCMC  Active  2018-04-10  2024-08-03  20.3871  
190450  SCMC  Active  2018-04-10  2024-08-03  20.3748  
190451  SCMC  Active  2018-04-10  2024-08-03  20.3748  
190510  SCMC  Active  2018-04-10  2024-08-03  20.3853  
190529  SCMC  Active  2018-04-10  2024-08-03  20.3839  
190530  SCMC  Active  2018-04-10  2024-08-03  20.3839  
194179  SCMC  Active  2018-04-10  2024-09-13  20.3820  
194753  SCMC  Active  2018-04-10  2026-08-03  20.3786  
194754  SCMC  Active  2018-04-10  2024-08-03  20.3822  
194758  SCMC  Active  2018-04-10  2024-08-03  20.3696  
194796  SCMC  Active  2018-04-10  2024-08-03  20.3679  
194797  SCMC  Active  2018-04-10  2024-08-03  20.3679  
194798  SCMC  Active  2018-04-10  2024-08-03  20.3697  
194799  SCMC  Active  2018-04-10  2024-08-03  20.3715  
194846  SCMC  Active  2018-04-10  2024-09-13  20.3838  
195647  SCMC  Active  2018-04-10  2024-08-03  20.3943  
195648  SCMC  Active  2018-04-10  2024-08-03  20.3961  
196042  SCMC  Active  2018-04-10  2026-08-03  20.3804  
196043  SCMC  Active  2018-04-10  2024-08-03  20.3840  

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Tenure

Number

 

Title

Type

 

Tenure

Status

 

Issue

Date

 

Anniversary

Date

  Area
(ha)
 
196617  SCMC  Active  2018-04-10  2024-09-08  20.3911  
196618  SCMC  Active  2018-04-10  2024-08-03  20.3693  
196755  SCMC  Active  2018-04-10  2024-08-03  20.3749  
196768  BCMC  Active  2018-04-10  2025-08-03  0.7950  
196769  SCMC  Active  2018-04-10  2024-08-03  20.3662  
203213  SCMC  Active  2018-04-10  2024-08-03  20.3748  
203214  SCMC  Active  2018-04-10  2024-08-03  20.3767  
203461  SCMC  Active  2018-04-10  2024-02-05  20.3819  
204777  BCMC  Active  2018-04-10  2025-08-03  18.8916  
206957  SCMC  Active  2018-04-10  2024-08-03  20.3871  
208273  SCMC  Active  2018-04-10  2024-02-08  20.3909  
208274  BCMC  Active  2018-04-10  2025-02-08  2.1127  
208970  SCMC  Active  2018-04-10  2024-08-03  20.3730  
209018  SCMC  Active  2018-04-10  2024-08-03  20.3871  
209033  SCMC  Active  2018-04-10  2024-08-03  20.3857  
210200  BCMC  Active  2018-04-10  2024-09-08  15.0122  
210640  BCMC  Active  2018-04-10  2025-08-03  1.0084  
211240  SCMC  Active  2018-04-10  2024-08-03  20.3749  
211435  BCMC  Active  2018-04-10  2024-09-08  0.4142  
211438  SCMC  Active  2018-04-10  2024-08-03  20.3820  
211554  SCMC  Active  2018-04-10  2024-01-05  20.3836  
212738  SCMC  Active  2018-04-10  2024-08-03  20.3784  
213301  SCMC  Active  2018-04-10  2024-08-03  20.3673  
213302  SCMC  Active  2018-04-10  2024-08-03  20.3732  
213342  SCMC  Active  2018-04-10  2024-08-03  20.3734  
213343  SCMC  Active  2018-04-10  2024-08-03  20.3734  
214064  SCMC  Active  2018-04-10  2024-08-03  20.3733  
214086  SCMC  Active  2018-04-10  2024-08-03  20.3804  
214206  SCMC  Active  2018-04-10  2024-06-06  20.3783  
214243  SCMC  Active  2018-04-10  2024-08-03  20.3942  
214244  SCMC  Active  2018-04-10  2024-08-03  20.3961  
214245  SCMC  Active  2018-04-10  2024-08-03  20.3961  
214884  SCMC  Active  2018-04-10  2024-02-05  20.3783  
214885  SCMC  Active  2018-04-10  2024-02-05  20.3801  
214970  SCMC  Active  2018-04-10  2024-06-06  20.3801  

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Tenure

Number

 

Title

Type

 

Tenure

Status

 

Issue

Date

 

Anniversary

Date

  Area
(ha)
 
215002  SCMC  Active  2018-04-10  2024-08-03  20.3973  
215076  SCMC  Active  2018-04-10  2024-08-03  20.3961  
215583  SCMC  Active  2018-04-10  2024-08-03  20.3734  
215600  SCMC  Active  2018-04-10  2024-08-03  20.3911  
215604  SCMC  Active  2018-04-10  2024-08-03  20.3840  
215698  SCMC  Active  2018-04-10  2024-09-13  20.3837  
216179  SCMC  Active  2018-04-10  2024-08-03  20.3751  
216182  SCMC  Active  2018-04-10  2024-08-03  20.3694  
216871  SCMC  Active  2018-04-10  2026-08-03  20.3731  
216872  SCMC  Active  2018-04-10  2026-08-03  20.3732  
216889  BCMC  Active  2018-04-10  2025-08-03  19.0623  
219093  SCMC  Active  2018-04-10  2024-08-03  20.3854  
219094  SCMC  Active  2018-04-10  2024-08-04  20.3890  
219753  SCMC  Active  2018-04-10  2024-08-04  20.3873  
219754  SCMC  Active  2018-04-10  2024-08-04  20.3873  
219755  SCMC  Active  2018-04-10  2024-08-04  20.3873  
219756  SCMC  Active  2018-04-10  2024-08-04  20.3891  
220084  SCMC  Active  2018-04-10  2024-01-05  20.3873  
220387  SCMC  Active  2018-04-10  2024-08-03  20.3748  
220491  SCMC  Active  2018-04-10  2024-08-03  20.3854  
220492  SCMC  Active  2018-04-10  2026-08-03  20.3889  
220493  SCMC  Active  2018-04-10  2024-08-03  20.3890  
223477  SCMC  Active  2018-04-10  2024-09-13  20.3783  
224337  SCMC  Active  2018-04-10  2024-09-13  20.3837  
225358  SCMC  Active  2018-04-10  2024-08-03  20.3678  
225359  SCMC  Active  2018-04-10  2024-08-03  20.3696  
225399  SCMC  Active  2018-04-10  2024-08-03  20.3636  
225400  SCMC  Active  2018-04-10  2024-08-03  20.3697  
226147  SCMC  Active  2018-04-10  2024-06-29  20.3856  
227046  SCMC  Active  2018-04-10  2024-08-03  20.3890  
227047  BCMC  Active  2018-04-10  2025-08-03  12.8692  
227692  SCMC  Active  2018-04-10  2024-08-04  20.3909  
227758  SCMC  Active  2018-04-10  2024-08-03  20.3705  
228366  SCMC  Active  2018-04-10  2024-08-03  20.3710  
228367  SCMC  Active  2018-04-10  2024-08-03  20.3766  

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Tenure

Number

 

Title

Type

 

Tenure

Status

 

Issue

Date

 

Anniversary

Date

  Area
(ha)
 
228368  SCMC  Active  2018-04-10  2024-08-03  20.3766  
228423  SCMC  Active  2018-04-10  2024-08-03  20.3853  
230251  BCMC  Active  2018-04-10  2024-09-08  15.8928  
230256  SCMC  Active  2018-04-10  2024-08-03  20.3820  
230862  SCMC  Active  2018-04-10  2024-01-05  20.3837  
230995  SCMC  Active  2018-04-10  2024-07-31  20.3856  
231498  SCMC  Active  2018-04-10  2024-08-03  20.3696  
231499  SCMC  Active  2018-04-10  2024-08-03  20.3714  
232022  SCMC  Active  2018-04-10  2024-08-03  20.3679  
232023  SCMC  Active  2018-04-10  2024-08-03  20.3715  
232026  SCMC  Active  2018-04-10  2024-08-03  20.3716  
232027  SCMC  Active  2018-04-10  2026-08-03  20.3750  
232749  SCMC  Active  2018-04-10  2024-08-03  20.3680  
232822  SCMC  Active  2018-04-10  2024-08-03  20.3713  
233502  SCMC  Active  2018-04-10  2024-08-03  20.3749  
233503  SCMC  Active  2018-04-10  2024-08-03  20.3768  
233525  SCMC  Active  2018-04-10  2024-08-03  20.3680  
237571  SCMC  Active  2018-04-10  2024-06-21  20.3856  
240469  SCMC  Active  2018-04-10  2026-08-03  20.3962  
240559  SCMC  Active  2018-04-10  2026-08-03  20.3731  
243808  SCMC  Active  2018-04-10  2024-08-03  20.3712  
249285  SCMC  Active  2018-04-10  2024-08-03  20.3716  
249300  SCMC  Active  2018-04-10  2024-08-03  20.3840  
249354  SCMC  Active  2018-04-10  2024-08-03  20.3769  
250047  SCMC  Active  2018-04-10  2024-08-03  20.3732  
250588  SCMC  Active  2018-04-10  2024-08-03  20.3641  
250589  SCMC  Active  2018-04-10  2024-08-03  20.3642  
251392  SCMC  Active  2018-04-10  2024-08-03  20.3662  
251828  SCMC  Active  2018-04-10  2024-08-03  20.3693  
257281  SCMC  Active  2018-04-10  2024-08-03  20.3962  
257282  BCMC  Active  2018-04-10  2025-08-03  3.1801  
257283  SCMC  Active  2018-04-10  2024-08-03  20.3980  
257656  SCMC  Active  2018-04-10  2024-08-03  20.3821  
257657  SCMC  Active  2018-04-10  2024-08-03  20.3857  
257658  SCMC  Active  2018-04-10  2024-08-03  20.3857  

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Tenure

Number

 

Title

Type

 

Tenure

Status

 

Issue

Date

 

Anniversary

Date

  Area
(ha)
 
258749  SCMC  Active  2018-04-10  2026-08-03  20.3730  
259546  SCMC  Active  2018-04-10  2024-02-05  20.3819  
260267  BCMC  Active  2018-04-10  2024-09-08  2.7368  
260775  SCMC  Active  2018-04-10  2024-08-03  20.3714  
260810  SCMC  Active  2018-04-10  2024-09-13  20.3802  
260900  SCMC  Active  2018-04-10  2024-06-21  20.3838  
261312  SCMC  Active  2018-04-10  2024-08-03  20.3641  
261313  SCMC  Active  2018-04-10  2024-08-03  20.3661  
261501  SCMC  Active  2018-04-10  2024-09-13  20.3820  
262023  SCMC  Active  2018-04-10  2024-08-03  20.3662  
262024  SCMC  Active  2018-04-10  2024-08-03  20.3680  
262043  SCMC  Active  2018-04-10  2024-08-03  20.3893  
262104  SCMC  Active  2018-04-10  2024-08-03  20.3768  
262155  SCMC  Active  2018-04-10  2024-09-13  20.3819  
262202  SCMC  Active  2018-04-10  2024-08-03  20.3906  
262203  SCMC  Active  2018-04-10  2024-08-03  20.3925  
262204  SCMC  Active  2018-04-10  2024-08-03  20.3943  
262782  SCMC  Active  2018-04-10  2026-08-03  20.3731  
262797  SCMC  Active  2018-04-10  2024-08-03  20.3661  
262798  SCMC  Active  2018-04-10  2024-08-03  20.3681  
262800  SCMC  Active  2018-04-10  2024-08-03  20.3751  
262808  SCMC  Active  2018-04-10  2024-08-03  20.3943  
262856  SCMC  Active  2018-04-10  2024-02-05  20.3801  
263838  SCMC  Active  2018-04-10  2024-08-03  20.3713  
263839  SCMC  Active  2018-04-10  2024-08-03  20.3713  
266221  SCMC  Active  2018-04-10  2024-09-08  20.3892  
266297  SCMC  Active  2018-04-10  2024-08-03  20.3872  
266890  SCMC  Active  2018-04-10  2024-08-03  20.3851  
266891  SCMC  Active  2018-04-10  2024-08-03  20.3888  
266892  SCMC  Active  2018-04-10  2024-08-03  20.3889  
267609  SCMC  Active  2018-04-10  2024-08-03  20.3730  
268724  SCMC  Active  2018-04-10  2024-08-03  20.3804  
268725  SCMC  Active  2018-04-10  2024-08-03  20.3714  
268759  SCMC  Active  2018-04-10  2024-08-03  20.3679  
268761  SCMC  Active  2018-04-10  2024-08-03  20.3698  

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Tenure

Number

 

Title

Type

 

Tenure

Status

 

Issue

Date

 

Anniversary

Date

  Area
(ha)
 
268762  SCMC  Active  2018-04-10  2024-08-03  20.3699  
269493  SCMC  Active  2018-04-10  2024-08-03  20.3893  
269495  SCMC  Active  2018-04-10  2024-08-03  20.3857  
269657  SCMC  Active  2018-04-10  2024-08-03  20.3906  
270090  SCMC  Active  2018-04-10  2024-08-03  20.3768  
270256  SCMC  Active  2018-04-10  2024-08-03  20.3925  
270257  SCMC  Active  2018-04-10  2024-08-03  20.3925  
270274  BCMC  Active  2018-04-10  2024-09-13  2.2056  
270305  SCMC  Active  2018-04-10  2024-02-05  20.3782  
270578  SCMC  Active  2018-04-10  2024-09-08  20.3911  
270786  SCMC  Active  2018-04-10  2024-08-03  20.3733  
273668  SCMC  Active  2018-04-10  2024-09-26  20.3820  
273682  SCMC  Active  2018-04-10  2024-09-08  20.3892  
274264  SCMC  Active  2018-04-10  2024-08-03  20.3854  
274386  SCMC  Active  2018-04-10  2024-08-03  20.3851  
274387  SCMC  Active  2018-04-10  2024-08-03  20.3883  
274915  SCMC  Active  2018-04-10  2024-08-04  20.3873  
274981  SCMC  Active  2018-04-10  2024-08-03  20.3710  
275583  SCMC  Active  2018-04-10  2024-08-03  20.3766  
275648  SCMC  Active  2018-04-10  2024-08-03  20.3889  
275662  SCMC  Active  2018-04-10  2024-08-03  20.3821  
276608  SCMC  Active  2018-04-10  2024-08-03  20.3944  
276609  SCMC  Active  2018-04-10  2024-08-03  20.3980  
278973  BCMC  Active  2018-04-10  2024-09-08  3.7772  
282263  SCMC  Active  2018-04-10  2024-08-03  20.3925  
282264  SCMC  Active  2018-04-10  2024-08-03  20.3961  
282351  SCMC  Active  2018-04-10  2024-08-03  20.3943  
282352  SCMC  Active  2018-04-10  2024-08-03  20.3979  
285771  BCMC  Active  2018-04-10  2025-02-08  2.1528  
287654  SCMC  Active  2018-04-10  2024-08-03  20.3748  
287704  SCMC  Active  2018-04-10  2024-08-03  20.3853  
289641  SCMC  Active  2018-04-10  2024-08-03  20.3924  
289642  SCMC  Active  2018-04-10  2024-08-03  20.3925  
289643  SCMC  Active  2018-04-10  2024-08-03  20.3979  
289644  SCMC  Active  2018-04-10  2024-08-03  20.3979  

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Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Tenure

Number

 

Title

Type

 

Tenure

Status

 

Issue

Date

 

Anniversary

Date

  Area
(ha)
 
289645  SCMC  Active  2018-04-10  2024-08-03  20.3979  
293160  SCMC  Active  2018-04-10  2024-08-04  20.3872  
293161  BCMC  Active  2018-04-10  2024-08-03  11.2639  
293784  SCMC  Active  2018-04-10  2024-08-03  20.3870  
293812  SCMC  Active  2018-04-10  2024-08-04  20.3909  
293813  BCMC  Active  2018-04-10  2024-08-04  3.5823  
295044  SCMC  Active  2018-04-10  2024-08-03  20.3784  
295045  SCMC  Active  2018-04-10  2024-08-03  20.3839  
295081  SCMC  Active  2018-04-10  2026-08-03  20.3853  
295082  SCMC  Active  2018-04-10  2024-08-03  20.3908  
295570  SCMC  Active  2018-04-10  2024-09-08  20.3910  
296298  BCMC  Active  2018-04-10  2024-09-08  1.3014  
299899  SCMC  Active  2018-04-10  2026-08-03  20.3768  
299901  SCMC  Active  2018-04-10  2024-08-03  20.3714  
300610  BCMC  Active  2018-04-10  2025-08-03  18.7210  
303859  SCMC  Active  2018-04-10  2024-01-05  20.3874  
308584  SCMC  Active  2018-04-10  2024-08-03  20.3784  
309145  SCMC  Active  2018-04-10  2026-08-03  20.3822  
309190  SCMC  Active  2018-04-10  2024-08-03  20.3716  
309191  SCMC  Active  2018-04-10  2024-08-03  20.3734  
309192  SCMC  Active  2018-04-10  2024-08-03  20.3752  
309916  SCMC  Active  2018-04-10  2024-08-03  20.3662  
309927  SCMC  Active  2018-04-10  2024-08-03  20.3876  
312652  SCMC  Active  2018-04-10  2024-09-13  20.3819  
312653  SCMC  Active  2018-04-10  2024-08-04  20.3855  
312786  SCMC  Active  2018-04-10  2024-06-21  20.3874  
313814  SCMC  Active  2018-04-10  2024-08-03  20.3767  
315879  SCMC  Active  2018-04-10  2024-08-03  20.3658  
315880  SCMC  Active  2018-04-10  2024-08-03  20.3678  
315881  SCMC  Active  2018-04-10  2024-08-03  20.3732  
315914  SCMC  Active  2018-04-10  2024-08-03  20.3641  
315917  SCMC  Active  2018-04-10  2024-08-03  20.3752  
315919  SCMC  Active  2018-04-10  2024-08-03  20.3750  
316626  BCMC  Active  2018-04-10  2025-08-03  19.2346  
316627  SCMC  Active  2018-04-10  2024-08-03  20.3751  

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Ontario, Canada

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Number

 

Title

Type

 

Tenure

Status

 

Issue

Date

 

Anniversary

Date

  Area
(ha)
 
316642  SCMC  Active  2018-04-10  2024-08-03  20.3875  
316644  SCMC  Active  2018-04-10  2024-08-03  20.3803  
316645  SCMC  Active  2018-04-10  2024-08-03  20.3821  
317831  SCMC  Active  2018-04-10  2024-08-03  20.3688  
317874  SCMC  Active  2018-04-10  2024-08-03  20.3767  
317890  SCMC  Active  2018-04-10  2024-08-03  20.3751  
321860  SCMC  Active  2018-04-10  2024-06-21  20.3874  
322398  SCMC  Active  2018-04-10  2024-08-04  20.3854  
322399  SCMC  Active  2018-04-10  2024-08-03  20.3872  
323006  SCMC  Active  2018-04-10  2024-08-03  20.3889  
323026  BCMC  Active  2018-04-10  2024-08-04  4.2910  
323736  SCMC  Active  2018-04-10  2024-08-03  20.3857  
325968  SCMC  Active  2018-04-10  2026-08-03  20.3943  
326071  SCMC  Active  2018-04-10  2024-08-03  20.3767  
326180  SCMC  Active  2018-04-10  2024-08-04  20.3855  
326181  SCMC  Active  2018-04-10  2024-09-13  20.3855  
326847  SCMC  Active  2018-04-10  2024-09-08  20.3911  
328159  BCMC  Active  2018-04-10  2024-09-08  5.5901  
328677  SCMC  Active  2018-04-10  2024-08-03  20.3697  
328793  SCMC  Active  2018-04-10  2024-09-13  20.3783  
330514  SCMC  Active  2018-04-10  2024-08-03  20.3875  
330705  SCMC  Active  2018-04-10  2024-08-03  20.3768  
330731  SCMC  Active  2018-04-10  2024-08-03  20.3733  
331593  SCMC  Active  2018-04-10  2026-08-03  20.3731  
331594  SCMC  Active  2018-04-10  2026-08-03  20.3731  
331769  SCMC  Active  2018-04-10  2024-09-13  20.3801  
332096  SCMC  Active  2018-04-10  2024-08-03  20.3802  
332151  SCMC  Active  2018-04-10  2024-08-03  20.3786  
332154  SCMC  Active  2018-04-10  2026-08-03  20.3732  
332188  SCMC  Active  2018-04-10  2024-08-03  20.3715  
332190  SCMC  Active  2018-04-10  2024-08-03  20.3698  
332450  SCMC  Active  2018-04-10  2024-08-03  20.3911  
332451  BCMC  Active  2018-04-10  2025-08-03  6.6487  
332843  SCMC  Active  2018-04-10  2024-08-03  20.3750  
335323  BCMC  Active  2018-04-10  2024-08-04  4.9998  

Page 232

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Tenure

Number

 

Title

Type

 

Tenure

Status

 

Issue

Date

 

Anniversary

Date

  Area
(ha)
 
336083  SCMC  Active  2018-04-10  2024-08-03  20.3785  
336084  SCMC  Active  2018-04-10  2024-08-03  20.3803  
336085  SCMC  Active  2018-04-10  2024-08-03  20.3803  
336086  SCMC  Active  2018-04-10  2024-08-03  20.3803  
336134  SCMC  Active  2018-04-10  2026-08-03  20.3907  
341289  SCMC  Active  2018-04-10  2024-08-03  20.3979  
341326  SCMC  Active  2018-04-10  2024-06-29  20.3838  
342166  SCMC  Active  2018-04-10  2024-09-08  20.3892  
345290  SCMC  Active  2018-04-10  2024-08-03  20.3890  
345391  SCMC  Active  2018-04-10  2024-08-03  20.3851  
345392  SCMC  Active  2018-04-10  2024-08-03  20.3889  
521875  SCMC  Active  2018-05-22  2025-05-22  20.3765  
521876  SCMC  Active  2018-05-22  2025-05-22  20.3745  
521877  SCMC  Active  2018-05-22  2025-05-22  20.3759  
521878  SCMC  Active  2018-05-22  2025-05-22  20.3740  
521879  SCMC  Active  2018-05-22  2025-05-22  20.3745  
521880  SCMC  Active  2018-05-22  2025-05-22  20.3746  
521881  SCMC  Active  2018-05-22  2025-05-22  20.3765  
521882  SCMC  Active  2018-05-22  2025-05-22  20.3746  
521883  SCMC  Active  2018-05-22  2025-05-22  20.3765  
521884  SCMC  Active  2018-05-22  2025-05-22  20.3764  
521885  SCMC  Active  2018-05-22  2025-05-22  20.3765  
521886  SCMC  Active  2018-05-22  2025-05-22  20.3765  
521887  SCMC  Active  2018-05-22  2025-05-22  20.3746  
521888  SCMC  Active  2018-05-22  2025-05-22  20.3745  
521889  SCMC  Active  2018-05-22  2025-05-22  20.3745  
521890  SCMC  Active  2018-05-22  2025-05-22  20.3766  
521891  SCMC  Active  2018-05-22  2025-05-22  20.3765  
521892  SCMC  Active  2018-05-22  2025-05-22  20.3746  
521893  SCMC  Active  2018-05-22  2025-05-22  20.3782  
521894  SCMC  Active  2018-05-22  2025-05-22  20.3800  
521895  SCMC  Active  2018-05-22  2025-05-22  20.3836  
521896  SCMC  Active  2018-05-22  2025-05-22  20.3795  
521897  SCMC  Active  2018-05-22  2025-05-22  20.3818  
521898  SCMC  Active  2018-05-22  2025-05-22  20.3818  

Page 233

 

Kinross Gold Corporation

Great Bear Gold Project

Ontario, Canada

NI 43-101 Technical Report

 

Tenure

Number

 

Title

Type

 

Tenure

Status

 

Issue

Date

 

Anniversary

Date

  Area
(ha)
 
521899  SCMC  Active  2018-05-22  2025-05-22  20.3777  
521900  SCMC  Active  2018-05-22  2025-05-22  20.3836  
521901  SCMC  Active  2018-05-22  2025-05-22  20.3835  
521902  SCMC  Active  2018-05-22  2025-05-22  20.3836  
521903  SCMC  Active  2018-05-22  2025-05-22  20.3835  
521904  SCMC  Active  2018-05-22  2025-05-22  20.3811  
521905  SCMC  Active  2018-05-22  2025-05-22  20.3816  
521906  SCMC  Active  2018-05-22  2025-05-22  20.3816  
521907  SCMC  Active  2018-05-22  2025-05-22  20.3835  
521908  SCMC  Active  2018-05-22  2025-05-22  20.3817  
521909  SCMC  Active  2018-05-22  2025-05-22  20.3816  
521910  SCMC  Active  2018-05-22  2025-05-22  20.3816  
521911  SCMC  Active  2018-05-22  2025-05-22  20.3835  
521912  SCMC  Active  2018-05-22  2025-05-22  20.3816  
521913  SCMC  Active  2018-05-22  2025-05-22  20.3836  
521914  SCMC  Active  2018-05-22  2025-05-22  20.3835  
521915  SCMC  Active  2018-05-22  2025-05-22  20.3828  
Totals  471 claims  9,139.9622  

Page 234