Phase 1 Diamond Drilling Program - Goldlund Property 2017

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Assessment Report on the 2017 Phase 1 Diamond Drilling Program

Goldlund Property Sioux Lookout, Ontario Patricia and Kenora Mining Divisions

NTS 52F/16SW, SE, NW, NE

Centred at: Latitude/Longitude: 49o52’28.21” N/ 92o19’08.00” W UTM NAD 83, Zone 15: 548940 mE, 5524900 mN

4 January 2018 Submitted by: Miro Mytny P.Geo

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Table of Contents 1 Introduction ...................................................................................................................................................... 1 2 Terms of Reference ........................................................................................................................................ 2

2.1 Units of Measure .............................................................................................................................. 2 2.2 Acronyms ..................................................................................................................................... 2

3 Property Description and Location ........................................................................................................... 3 3.1 Mineral Tenure ................................................................................................................................. 4

4 Property Access ............................................................................................................................................... 8 5 Site Topography, Elevation, and Vegetation ......................................................................................... 8 6 Geologic Setting .............................................................................................................................................. 9

6.1 Regional Geology ............................................................................................................................. 9 6.2 Local Geology ................................................................................................................................. 10

7 History .............................................................................................................................................................. 13 8 Current Program .......................................................................................................................................... 13

8.1 Diamond Drilling ............................................................................................................................ 13 9 Down Hole Surveying ................................................................................................................................. 16 10 Method and Approach ............................................................................................................................... 16 11 Assays ............................................................................................................................................................... 17

11.1 QAQC Analysis ................................................................................................................................ 17 12 DGI Televiewer Survey ............................................................................................................................... 18 13 Results.............................................................................................................................................................. 21 14 Expenditures .................................................................................................................................................. 31 15 Conclusions and Recommendations ..................................................................................................... 31 16 References ...................................................................................................................................................... 33 17 Statement of Qualifications ..................................................................................................................... 34 Appendix A: Claim Map ......................................................................................................................................... 35 Appendix B: Drill Location Map .......................................................................................................................... 36 Appendix C: Drill Logs ............................................................................................................................................ 37 Appendix D: Cross Sections .................................................................................................................................. 38 Appendix E: Assay Certificates ............................................................................................................................ 39 Appendix F: SGS Analytical Guide ...................................................................................................................... 40 Appendix G: DGI Report ........................................................................................................................................ 41

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Tables Table 3.1: Goldlund Unpatented Claims ....................................................................................................... 4 Table 3.2: Goldlund Patented Claims ............................................................................................................ 7 Table 3.3: Goldlund Mining Lease ................................................................................................................. 8 Table 3.4: Goldlund Licence of Occupation ................................................................................................... 8 Table 8.1: Phase 1 Drill Holes ...................................................................................................................... 13 Table 12.1: DGI Downhole Surveys, March 2017 ........................................................................................ 20 Table 13.1: Drill Hole Results ...................................................................................................................... 21 Table 14.1: Expenditure Summary .............................................................................................................. 31 Figures Figure 3.1: Location Map .............................................................................................................................. 3 Figure 6.1: Regional Geology ........................................................................................................................ 9 Figure 6.2: Property Geology ...................................................................................................................... 12 Figure 12.1: Location of Drill Holes with Televiewer Surveys ...................................................................... 19

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1 Introduction The Goldlund Property is located in the Kenora and Patricia mining districts of northwestern Ontario. The property covers a total area of 24,040 hectares and is located approximately 45 kilometers from Sioux Lookout and 60 kilometers from Dryden. The Property is fully owned by First Mining Finance Corp. (First Mining), through its 100%-owned subsidiary company Goldlund Resources Inc.

Historic exploration on the Goldlund Property dates back to the 1930’s and includes surface exploration programs and underground development on the Goldlund deposit. The deposit was mined in the 1980’s by Campbell Chibougamau (Camchib) who recovered 18,000 ounces of gold, at an average grade of 4.7 g/t (Pieterse, 2005).

The Goldlund Property has a number of historic gold occurrences. These consist of the Mistango, Beartrack, Windfall, Goldlund, Tarbush, Loybex, Miller, Eaglelund, Quyta and others. These occurrences have historically undergone various amounts of exploration and mining activities. The Eaglelund, Miles Lake, and Jacobus Creek gold showings all exhibit similar mineralization to that seen in the area of the Goldlund mine. The Miller and Quyta occurrences are classified as shear zone-hosted gold.

Between January and July of 2017, First Mining completed the first phase of its multi-phase diamond drill program. Rodren Drilling of Winnipeg was commissioned to complete the drilling, under the supervision of Miro Mytny, Exploration Manager at First Mining. The drill program was designed based on recommendations from the NI 43-101 compliant technical report and resource estimation update completed by WSP Canada in 2017 (McCracken, 2017). The Phase 1 program, which is the subject of this report, was focused on improving the resource definition of Zone 7 to the west of the Goldlund mine site. During Phase 1, a total of 100 HQ diameter sized holes were drilled, for a total of 24,299 meters.

Historical drilling of Zone 7 lacked continuous sample data throughout the albatized tonalite (“granodiorite” in mine terminology) units, which are the principal hosts of the gold mineralization. Only quartz veining with alteration halos and any visible sulphides were sampled during previous drill campaigns, and one of the purposes of First Mining’s Phase 1 drilling was to fill in these historical data gaps to enable an eventual upgrade in the resource categories of Zone 7 from Inferred to Indicated or Measured. During the Phase 1 program, all the core from the granodiorite, mafic inclusions and porphyries was continuously sampled in 2 meter intervals. Samples from these mineralized zones were analyzed for gold by Bulk Leach Extractable Gold (BLEG) assay technique. Volcanics in the hanging wall and footwall of the granodiorite were sampled intermittently and these samples were sent for gold analysis by fire assay. The Phase 1 drilling both confirmed historical results and improved the definition of the mineralization in Zone 7.

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2 Terms of Reference This report was prepared by First Mining for the purpose of filing assessment work, as required under the Ontario Mining Act. All units of measure are in metric unless otherwise stated. All map units are in UTM coordinates (NAD83 Zone 15) unless otherwise stated. All funds are reported in Canadian dollar (CDN$) unless otherwise stated.

2.1 Units of Measure above mean sea level .................................. amsl centimeter ..................................................... cm cubic meter .................................................... m3 degree ............................................................... ° degrees Celsius................................................ °C dollar (Canadian) ....................................... CDN$ gram ................................................................. g grams per tonne ............................................ g/t greater than ..................................................... > hectare (10,000 m2) ....................................... ha kilogram .......................................................... kg kilometer ....................................................... km less than ........................................................... < meter ............................................................... m meters above sea level ............................... masl

microns ......................................................... µm milligram ....................................................... mg millimeter ..................................................... mm million ............................................................. M million tonnes ................................................ Mt ounce .............................................................. oz ounce/tonne ................................................ oz/t ounce/short ton ......................................... oz/st parts per million .......................................... ppm parts per billion ............................................ ppb percent ............................................................ % short ton (2,000 lb) ......................................... st specific gravity ............................................... SG three-dimensional .......................................... 3D tonne (1,000 kg) (metric tonne) ....................... t

2.2 Acronyms AA ..................................................................................................................................... Atomic Absorption

BLEG ................................................................................................................... Bulk Leach Extractable Gold

FA ................................................................................................................................................... Fire Assay

QAQC ..................................................................................................... Quality Assurance / Quality Control

SG .......................................................................................................................................... Specific Gravity

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3 Property Description and Location The Goldlund Property is located in northwestern Ontario, approximately 60 km northeast of Dryden and stretches over several townships of the Patricia Mining and Kenora Mining Divisions. The Project is centered at 49.900203 north Latitude and 92.341103 west Longitude (UTM Coordinates: 545800E, 5527400N, NAD 83, Zone 15) on National Topographic Sheet 52F/16.

Figure 3.1 shows the location of the Property.

Figure 3.1: Location Map

Coordinates: NAD83 UTMz15 Scale 1 : 750,000

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3.1 Mineral Tenure The Property consists of 149 unpatented claims comprised of 1,469 claim units (23,504 ha) presented in Table 3.1, 27 patented claims (432 ha) presented in Table 3.2, one mining lease (48.56 ha) presented in Table 3.3., and one License of Occupation (Table 3.4), all of which are owned by First Mining Finance Corp., through its 100%-owned subsidiary company Goldlund Resources Inc. The Property covers a total of 24,040 hectares, and lies within both the Patricia (PA) and Kenora (K) Mining Divisions.

Appendix A is a map showing the Goldlund landholdings.

Table 3.1: Goldlund Unpatented Claims

MINING DIVISION

CLAIM NUMBER TOWNSHIP/AREA RECORDING

DATE DUE DATE AREA (UNIT) AREA (HECTARE)

PA 1162943 ECHO 08-Aug-02 08-Aug-18 2 32 PA 1166865 ECHO 29-Mar-00 29-Mar-19 6 96 PA 1191761 ECHO 13-Nov-01 13-Nov-18 4 64 PA 1191762 ECHO 23-Nov-01 23-Nov-17 1 16 PA 1199268 ECHO 30-Nov-01 30-Nov-17 4 64 PA 1247989 ECHO 15-Apr-02 15-Apr-18 4 64 PA 3002714 ECHO 02-Aug-02 02-Aug-18 2 32 PA 3002715 ECHO 18-Nov-02 18-Nov-17 9 144 PA 3002721 ECHO 12-Sep-02 17-Sep-18 1 16 PA 3004264 ECHO 12-Sep-02 17-Sep-18 1 16 PA 3004265 ECHO 05-Nov-02 05-Nov-17 6 96 K 3012443 LAVAL 30-Sep-05 30-Sep-18 12 192 K 3012472 LAVAL 30-Sep-05 30-Sep-18 14 224 K 3012488 LAVAL 30-Sep-05 30-Sep-18 11 176 K 3012489 LAVAL 30-Sep-05 30-Sep-18 16 256 K 3012490 LAVAL 30-Sep-05 30-Sep-18 16 256 K 3012491 LAVAL 30-Sep-05 30-Sep-18 9 144 K 3012492 LAVAL 30-Sep-05 30-Sep-18 6 96 K 3012493 LAVAL 30-Sep-05 30-Sep-18 16 256 K 3012494 LAVAL 30-Sep-05 30-Sep-18 13 208 K 3012496 LAVAL 30-Sep-05 30-Sep-18 6 96

PA 3019655 ECHO 30-Sep-05 30-Sep-18 2 32 PA 3019656 MCAREE 30-Sep-05 30-Sep-18 4 64 PA 3019657 ECHO 30-Sep-05 30-Sep-18 4 64 K 3019677 LAVAL 24-Nov-05 04-Dec-17 16 256 K 3019693 LAVAL 24-Nov-05 04-Dec-17 15 240 K 3019695 LAVAL 24-Nov-05 24-Nov-17 5 80

PA 3019701 MCAREE 04-Nov-05 04-Nov-17 2 32 K 3019749 LAVAL 30-Sep-05 30-Sep-18 12 192 K 3019751 LAVAL 11-Aug-05 12-Feb-18 8 128 K 3019752 LAVAL 11-Aug-05 12-Feb-18 6 96 K 3019753 LAVAL 11-Aug-05 12-Feb-18 9 144 K 3019754 LAVAL 11-Aug-05 12-Feb-18 12 192

PA 3019755 PICKEREL 11-Aug-05 11-Aug-18 7 112 PA 3019756 PICKEREL 11-Aug-05 12-Feb-18 12 192

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MINING DIVISION



PA 3019757 ECHO 11-Aug-05 11-Aug-18 9 144 PA 3019758 MCAREE 05-Aug-05 05-Aug-18 15 240 PA 3019759 MCAREE 05-Aug-05 05-Aug-18 9 144 PA 3019760 MCAREE 05-Aug-05 05-Aug-18 16 256 PA 3019761 MCAREE 05-Aug-05 05-Aug-18 15 240 K 3019762 LAVAL 05-Aug-05 12-Feb-18 9 144 K 3019763 LAVAL 05-Aug-05 05-Aug-18 3 48

PA 3019764 ECHO 11-Aug-05 12-Feb-18 15 240 PA 3019765 ECHO 11-Aug-05 11-Aug-18 8 128 PA 3019766 ECHO 11-Aug-05 11-Aug-18 12 192 PA 3019767 ECHO 11-Aug-05 12-Feb-18 14 224 PA 3019768 ECHO 11-Aug-05 12-Feb-18 10 160 PA 4200304 PICKEREL 13-Jan-06 13-Jan-18 9 144 PA 4200305 PICKEREL 13-Jan-06 13-Jan-18 8 128 PA 4200306 KABIK LAKE AREA 13-Jan-06 13-Jan-18 4 64 PA 4200307 VERMILLION 13-Jan-06 13-Jan-18 6 96 PA 4200342 PICKEREL 13-Jan-06 13-Jan-18 16 256 PA 4200343 PICKEREL 13-Jan-06 13-Jan-18 16 256 PA 4200344 PICKEREL 13-Jan-06 13-Jan-18 16 256 PA 4200345 PICKEREL 13-Jan-06 13-Jan-18 16 256 PA 4200346 PICKEREL 13-Jan-06 13-Jan-18 4 64 PA 4200347 PICKEREL 13-Jan-06 13-Jan-18 16 256 PA 4200348 PICKEREL 13-Jan-06 13-Jan-18 16 256 PA 4200349 KABIK LAKE AREA 13-Jan-06 13-Jan-18 4 64 PA 4200350 KABIK LAKE AREA 13-Jan-06 13-Jan-18 16 256 PA 4200351 PICKEREL 13-Jan-06 13-Jan-18 14 224 PA 4200423 ECHO 13-Jan-06 13-Jan-18 10 160 PA 4200424 ECHO 13-Jan-06 13-Jan-18 13 208 PA 4200425 ECHO 13-Jan-06 13-Jan-18 16 256 PA 4200426 ECHO 13-Jan-06 13-Jan-18 4 64 PA 4200428 ECHO 13-Jan-06 13-Jan-18 10 160 PA 4200429 PICKEREL 13-Jan-06 13-Jan-18 14 224 PA 4200430 PICKEREL 13-Jan-06 13-Jan-18 16 256 PA 4200431 PICKEREL 13-Jan-06 13-Jan-18 6 96 PA 4200432 PICKEREL 13-Jan-06 13-Jan-18 12 192 K 4214543 LAVAL 14-Nov-08 04-Dec-17 16 256

PA 4222883 PICKEREL 31-Jan-08 31-Jan-18 2 32 K 4224123 LAVAL 30-Aug-10 30-Aug-18 15 240 K 4224124 LAVAL 02-Dec-10 04-Dec-17 15 240 K 4241202 LAVAL 31-Oct-08 31-Oct-18 1 16

PA 4241203 MCAREE 27-Oct-08 27-Oct-17 2 32 PA 4253224 WEBB 24-Jan-11 24-Jan-18 6 96 PA 4253225 WEBB 24-Jan-11 24-Jan-18 16 256 K 4253227 LAVAL 24-Jan-11 24-Jan-18 4 64

PA 4253228 WEBB 24-Jan-11 24-Jan-18 16 256 PA 4253229 WEBB 24-Jan-11 24-Jan-18 16 256 PA 4253230 WEBB 24-Jan-11 24-Jan-18 16 256

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MINING DIVISION



K 4253231 LAVAL 24-Jan-11 24-Jan-18 16 256 K 4253232 LAVAL 24-Jan-11 24-Jan-18 14 224

PA 4253233 MCAREE 24-Jan-11 24-Jan-18 3 48 PA 4256201 KABIK LAKE AREA 10-Nov-10 10-Nov-17 6 96 PA 4256202 KABIK LAKE AREA 10-Nov-10 10-Nov-17 14 224 PA 4256204 KABIK LAKE AREA 10-Nov-10 10-Nov-17 16 256 PA 4256211 KABIK LAKE AREA 10-Nov-10 10-Nov-17 4 64 PA 4256212 KABIK LAKE AREA 10-Nov-10 10-Nov-17 6 96 PA 4256213 KABIK LAKE AREA 10-Nov-10 10-Nov-17 10 160 PA 4256214 KABIK LAKE AREA 10-Nov-10 10-Nov-17 9 144 PA 4256223 JORDAN 12-Nov-12 12-Nov-17 7 112 PA 4256224 JORDAN 12-Nov-12 12-Nov-17 12 192 PA 4256225 JORDAN 12-Nov-12 12-Nov-17 16 256 PA 4256226 JORDAN 12-Nov-12 12-Nov-17 8 128 PA 4256235 JORDAN 12-Nov-12 12-Nov-17 8 128 PA 4256236 JORDAN 12-Nov-12 12-Nov-17 16 256 PA 4256237 JORDAN 12-Nov-12 12-Nov-17 12 192 PA 4256238 JORDAN 12-Nov-12 12-Nov-17 8 128 PA 4256239 JORDAN 12-Nov-12 12-Nov-17 16 256 PA 4256240 JORDAN 10-Nov-12 10-Nov-17 16 256 PA 4256242 KABIK LAKE AREA 10-Nov-10 10-Nov-17 9 144 PA 4256603 MCAREE 28-Sep-10 28-Sep-18 6 96 PA 4256604 MCAREE 28-Sep-10 28-Sep-18 10 160 PA 4256605 MCAREE 28-Sep-10 28-Sep-19 1 16 PA 4256606 MCAREE 28-Sep-10 28-Sep-18 16 256 PA 4256607 MCAREE 28-Sep-10 28-Sep-18 10 160 PA 4256608 MCAREE 28-Sep-10 28-Sep-18 16 256 PA 4256609 JORDAN 28-Sep-10 28-Mar-18 12 192 PA 4256610 JORDAN 28-Sep-10 28-Mar-18 12 192 PA 4256611 JORDAN 28-Sep-10 28-Mar-18 13 208 PA 4256615 ECHO 28-Sep-10 28-Sep-18 4 64 PA 4256616 ECHO 28-Sep-10 28-Sep-18 16 256 K 4256869 LAVAL 09-Feb-12 09-Feb-18 4 64

PA 4256871 PICKEREL 27-Oct-10 27-Oct-17 4 64 PA 4256872 KABIK LAKE AREA 27-Oct-10 27-Oct-17 8 128 PA 4256874 PICKEREL 27-Oct-10 27-Oct-17 8 128 PA 4256876 KABIK LAKE AREA 27-Oct-10 27-Oct-17 16 256 PA 4256877 PICKEREL 27-Oct-10 27-Oct-17 9 144 PA 4256879 KABIK LAKE AREA 27-Oct-10 27-Oct-17 16 256 PA 4256882 KABIK LAKE AREA 01-Nov-10 01-Nov-17 8 128 PA 4256883 KABIK LAKE AREA 01-Nov-10 01-Nov-17 16 256 PA 4259021 JORDAN 10-Nov-10 10-Nov-17 12 192 PA 4259026 DRAYTON 12-Nov-10 12-Nov-17 6 96 PA 4259027 PARNES LAKE AREA 12-Nov-10 12-Nov-17 12 192 PA 4259028 PARNES LAKE AREA 10-Nov-10 10-Nov-17 16 256 PA 4259035 DRAYTON 12-Nov-10 12-Nov-17 9 144 PA 4259039 DRAYTON 12-Nov-10 12-Nov-17 9 144

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MINING DIVISION



PA 4259041 DRAYTON 12-Nov-10 12-Nov-17 12 192 PA 4259045 DRAYTON 12-Nov-10 12-Nov-17 8 128 PA 4259707 JORDAN 10-Nov-10 10-Nov-17 16 256 PA 4259709 JORDAN 10-Nov-10 10-Nov-17 16 256 PA 4259712 JORDAN 10-Nov-10 10-Nov-18 8 128 PA 4259717 JORDAN 10-Nov-10 10-Nov-17 3 48 PA 4259718 JORDAN 10-Nov-10 10-Nov-17 8 128 PA 4259719 JORDAN 10-Nov-10 10-Nov-17 6 96 PA 4259720 JORDAN 10-Nov-10 10-Nov-17 5 80 PA 4261478 ECHO 26-Apr-11 26-Apr-18 15 240 PA 4261479 ECHO 26-Apr-11 26-Apr-18 13 208 PA 4262202 MCAREE 09-Dec-13 09-Dec-17 3 48 PA 4262781 KABIK LAKE AREA 18-Apr-11 18-Apr-18 4 64 PA 4262782 KABIK LAKE AREA 18-Apr-11 18-Apr-18 8 128 PA 4262783 JORDAN 18-Apr-11 18-Apr-18 8 128 PA 4262784 JORDAN 18-Apr-11 18-Apr-18 8 128 PA 4262785 JORDAN 20-Apr-11 20-Apr-18 16 256 PA 4263723 ECHO 09-Feb-12 09-Feb-18 9 144 PA 4263724 ECHO 09-Feb-12 09-Feb-18 8 128 PA 4263725 ECHO 09-Feb-12 09-Feb-18 5 80

*Claims with past due dates are currently under a time extension to file assessment work

Table 3.2: Goldlund Patented Claims

PATENT ID RECORDED OWNER TOWNSHIP AREA (HECTARES) KRL18720 Goldlund Resources Inc. ECHO 16.24 KRL18722 Goldlund Resources Inc. ECHO 16.19 KRL18723 Goldlund Resources Inc. ECHO 16.19 KRL18724 Goldlund Resources Inc. ECHO 16.14 KRL18809 Goldlund Resources Inc. ECHO 16.14 KRL18812 Goldlund Resources Inc. ECHO 16.14 KRL23115 Goldlund Resources Inc. ECHO 16 KRL23108 Goldlund Resources Inc. ECHO 16 KRL23111 Goldlund Resources Inc. ECHO 16 KRL23107 Goldlund Resources Inc. ECHO 16 KRL23106 Goldlund Resources Inc. ECHO 16 KRL23123 Goldlund Resources Inc. ECHO 16 KRL23119 Goldlund Resources Inc. ECHO 16 KRL23116 Goldlund Resources Inc. ECHO 16 KRL23117 Goldlund Resources Inc. ECHO 16 KRL23121 Goldlund Resources Inc. ECHO 16 KRL23120 Goldlund Resources Inc. ECHO 16 KRL23122 Goldlund Resources Inc. ECHO 16 KRL23118 Goldlund Resources Inc. ECHO 16 KRL23114 Goldlund Resources Inc. ECHO 16 KRL22735 Goldlund Resources Inc. ECHO 16 KRL22736 Goldlund Resources Inc. ECHO 16

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PATENT ID RECORDED OWNER TOWNSHIP AREA (HECTARES) KRL23110 Goldlund Resources Inc. ECHO 16 KRL23113 Goldlund Resources Inc. ECHO 16 KRL22737 Goldlund Resources Inc. ECHO 16 KRL23112 Goldlund Resources Inc. ECHO 16 KRL23109 Goldlund Resources Inc. ECHO 16

Table 3.3: Goldlund Mining Lease

TOWNSHIP CLAIM NUMBER PIN AREA (HECTARES) Echo 107464 2969DKL 48.56

Table 3.4: Goldlund Licence of Occupation

LICENCE OF OCCUPATION OWNER 12023 Goldlund Resources Inc.

4 Property Access Access to the Property is by road, following Ontario Provincial Highway 72 for approximately 60 km northeast from Dryden, or approximately 45 km southwest from Sioux Lookout. A private, all-weather gravel road leads from the highway turn-off to the Property. The road into the Property would require upgrading to sustain any form of mining operations, but is currently accessible by two-wheel drive vehicle for exploration purposes.

Regularly scheduled passenger air service and charter flights are available to the towns of Dryden and Sioux Lookout.

5 Site Topography, Elevation, and Vegetation (Excerpt from McCracken, 2017)

The Project area has low relief, ranging from 10 to 50 m, and is covered with a number of small lakes and sparse, coniferous forest with locally abundant outcrops. Vegetation consists predominantly of black spruce, balsam fir and tamarack trees, typical of the Canadian Shield. Parts of the Property area are also covered by drumlins and by glacial till. Overburden cover ranges from 1 to 10 m. The elevation on the Property is in the order of 400 masl.

The climate in this part of northern Ontario is continental to subarctic. The mean temperature during the winter months is -17°C and the mean temperature during the summer months is 16°C. The average annual precipitation is approximately 690 mm. The closest weather stations are located in the towns of Dryden and Sioux Lookout.

Exploration on the Property can be conducted year-round.

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6 Geologic Setting

6.1 Regional Geology The Goldlund Project is located in the Sioux Lookout sub-area of the Savant Lake to Crow Lake metavolcanic-metasedimentary belt which is part of the western Wabigoon Subprovince.

The Wabigoon Subprovince is composed mainly of volcanic rocks of tholeiitic to calc-alkaline affinity and sedimentary rocks, which are intruded by large granitoid batholiths. It is over 900 km long and has been divided into three regions: the eastern, central, and western Wabigoon (Blackburn et al.1991).

In the western Wabigoon region (WWR), volcanic rocks comprised of sequences of ultramafic (komatiites) to mafic (tholeiitic) to felsic rocks (mostly calc-alkaline) are organized in a series of interconnected greenstone belts ( Figure 6.1). They surround large granitoid batholiths. Volcanism in the WWR occurred mostly within the 2745 to 2711 Ma interval (Percival, 2007).

Figure 6.1: Regional Geology

Goldlund Project

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Lithostratigraphic assemblages of the WWR have been regrouped into tectonically bounded assemblages. Four main sequences were identified within most of these assemblages (Blackburn et al., 1991). They are from the oldest to youngest:

1) Lower mafic sequences, composed of komatiites and tholeiites, with lesser amounts of andesitic flowsand coeval intrusions;

2) Diverse intermediate to felsic volcanic sequences of calc-alkaline affinity and lesser amounts ofandesites to rhyolites;

3) Upper ultramafic to mafic sequences, composed of komatiitic and tholeiitic flows and;

4) Sedimentary sequences of turbidites, alluvial fans and/or minor platform sequences.

Contacts between these four sequences are either faulted or conformable, depending on the location within the WWR. (Blackburn et al., 1991).

The stratigraphic assemblages have been subdivided into five principal rock groups: the Northern Volcanic Belt, Northern Sedimentary Group (Abram Group), Central Volcanic Belt (Neepawa Group), Southern Sedimentary Group (Minnitaki Group), and the Southern Volcanic Belt. The majority of gold occurrences within these assemblages are located in the Central and Southern Volcanic Belts. This area has been subjected to at least four phases of deformation resulting in a predominantly northeasterly striking structural fabric (Pettigrew, 2012).

In the area of the Goldlund Project, the Neepawa Group can be subdivided into a lower tholeiitic and an upper andesite-basalt division. The lower division consists of tholeiitic mafic and felsic volcanic rocks with associated sub-volcanic intrusions. The upper division consists of intrusive calc-alkaline units and tholeiitic mafic to felsic volcanic units that outcrop around the Beartrack, Troutfly, and Gardner Lakes region (Blackburn et al., 1991).

Two main alteration events have occurred. The first pre-dates the four regional deformation events and results from metasomatic alteration, as evidenced by no structural fabric or tectonic preference associated with the metasomatic event, and occurs at the metavolcanic-metasedimentary contact. The second alteration event is syngenetic with regional deformation stages 3 and 4 and associated gold mineralization including quartz veining, sulphide mineralization, potassic alteration (sericite) and sodic alteration (albite). These can be observed in the rocks and drill core of the Goldlund Project.

6.2 Local Geology The Goldlund Project is located in a volcanic sequence about 1.5 km wide, comprising massive pillowed, often amygdaloidal flows interlayered with andesitic tuffs, lapilli tuff and agglomerate. This northeasterly striking volcanic sequence is intruded by several albitized tonalite (“granodiorite” in mine terminology) sills. These albitized tonalite sills are the host rock of the gold mineralization that occurs at the Goldlund Project. These sills range from 14 to 60 meters in thickness, and dip from vertical to 80° southward, and are subparallel to wallrock strata. These strata-parallel intrusions are known to extend north-eastward beyond the Goldlund Exploration Block and south-westward beyond Crossecho Lake where they reappear just south of Troutfly Lake.

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Two texturally different phases of tonalite exist. A light, fine- to medium-grained phase, which contains the majority of gold mineralization, is surrounded by a dark, fine-grained phase. Distinct alteration zones are present surrounding quartz veins which fill tension fractures in the tonalite dykes. Gabbro sills are observed in the hangingwall of the tonalite sills. These could represent an early phase of volcanism derived from the same source of magma as the tonalite. The mafic volcanic formation hosting the tonalite sills represents a series of basaltic spherulitic flows interlayered with pillow basalts and occasional tuffaceous horizons. Narrow sericitized dacite horizons were observed during logging. Some of these altered dacite intersects may represent hydrothermally altered tonalite.

This metavolcanic stratigraphy was foliated, crosscut by granitoid stocks, folded, displaced on shear zones, and eroded to produce the present geological map pattern (Figure 6.2). During this deformation, a peak biotite-amphibole facies metamorphism was attained in the northwestern sector, coinciding with the emplacement of the stocks. (Chorlton, 1990). Late intrusive porphyries (Quartz Feldspar Porphyry and Feldspar Porphyries) crosscut the tonalite sills. They range from less than 1 meter to several meters in thickness. The porphyries appear to be differentiated fractions of the magma from the Crossecho Stock, and were intruded into the sub-crustal assemblage during active plutonism of during the Kenoran Orogeny (Giddings, 1986).

Three-stages of paragenetic mineralization sequences have been recognized at Goldlund (Giddings, 1986):

1) An early, high temperature stage (pyrite, scheelite, xenotime, magnetite and ilmenite);

2) An intermediate dominantly sulphide stage (pyrite, sphalerite, chalcopyrite, galena), and

3) A late stage, low temperature (~300OC) gold and telluride stage

Native gold, petzite, calaverite, and altaite were deposited in this late, low temperature stage. Geochemical data shows strong correlations between gold and tellurides. Visible gold was often observed in drill core associated with altaite. Gold, in native form and in gold-silver tellurides (calaverite and petzite), occurs in quartz veins and in adjacent zones of metasomatic alteration within the tonalite. Quartz veins fill fractures that trend 005° to 015° and dip 35° to 50° towards the northwest. These fractures are concentrated in zones that display an intermittent, 300 to 400 meter spacing for a strike-length of 3 km.

5,5

35

,00

0 m

N

560,000 mE 565,000 mE

5,5

30

,00

0 m

N5

,52

0,0

00

mN

560,000 mE 565,000 mE

5,5

25

,00

0 m

N

550,000 mE 555,000 mE

550,000 mE 555,000 mE

545,000 mE540,000 mE

540,000 mE 545,000 mE

5,5

20

,00

0 m

N5

,52

5,0

00

mN

5,5

30

,00

0 m

N5

,53

5,0

00

mN

Slough Lake

Jacobus Creek

Two Lakes

Cabin Road

Franciscan Lake

Batch River

Crossecho Lake

Smith Zone

Goldenrod

Tom Chief Lake

0 1 2 4

kilometers

Figure 6.2: Property Geology

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7 History (Excerpt from McCracken, 2017)

Exploration on the Property dates back to the 1940s. Between the late 1940s and through to 1985, 850 ft of shaft sinking, 1,385 ft of ramp, and approximately 19,600 ft of drifting and crosscuts were developed for both exploration and production purposes.

Campbell Chibougamau Mines (Camchib) operated an underground mine and an open pit mine from mid-1982 to early 1985. During this time, they processed material at the mill on site. Underground mine production totalled approximately 100,000 st at an estimated grade of 0.15 oz/st gold, while open pit production totalled approximately 43,000 st, with an estimated grade of 0.17 oz/st gold. Mill records indicate that 132,000 st was processed, to produce 18,000 oz of gold. The head grade was 0.15 oz/st gold and mill recovery of the gold was reported as 86.6% (Pieterse, 2005).

With the exception of the 2017 drill program discussed in this report, First Mining has not conducted any surface exploration on the Property.

8 Current Program

8.1 Diamond Drilling First Mining completed Phase 1 of their planned drilling program at Goldlund between January 2017 and July 2017. A total of 100 holes were drilled over 24,299 m. The drilling was conducted by Rodren Drilling of Manitoba with HQ sized core. All casings were left in place and capped. Collar locations were initially surveyed using a handheld Garmin GPS, then after drilling was completed, collars were surveyed by EXP Geomatics of Dryden using a differential GPS. These final surveyed coordinates are provided in Table 8.1.

Core logging was undertaken by First Mining field geologists and supervised by Miro Mytny, First Mining’s Exploration Manager. Core cutting and geotechnical services were provided by locals from the Wabigoon and Lac Seul First Nation communities, and the nearby towns of Dryden and Sioux Lookout.

Appendix B is a plan map showing the drill hole locations. Cross sections and individual drill hole logs can be found in Appendices C and D respectively.

Table 8.1: Phase 1 Drill Holes

HOLE ID UTM EAST UTM NORTH AZIMUTH ° DIP ° LENGTH (m) GL-17-002 545701 5527232 0 -90 158 GL-17-003 545701 5527231 180 -80 302 GL-17-004 545702 5527213 0 -90 257 GL-17-005 545702 5527213 180 -80 656 GL-17-006 545701 5527191 0 -90 326 GL-17-007 545701 5527176 0 -90 293 GL-17-008 545701 5527156 0 -90 300 GL-17-010 545752 5527244 180 -80 305

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HOLE ID UTM EAST UTM NORTH AZIMUTH ° DIP ° LENGTH (m) GL-17-011 545752 5527235 0 -90 152 GL-17-012 545750 5527224 180 -80 299 GL-17-013 545748 5527213 0 -90 275 GL-17-014 545750 5527195 0 -90 371 GL-17-016 545648 5527228 0 -90 152 GL-17-017 545648 5527228 180 -80 302 GL-17-018 545648 5527213 0 -90 149 GL-17-019 545651 5527183 0 -90 374 GL-17-021 545649 5527159 0 -90 383 GL-17-023 545801 5527255 180 -80 131 GL-17-026 545800 5527215 0 -90 188 GL-17-027 545801 5527238 180 -90 218 GL-17-028 545801 5527238 180 -77 299 GL-17-029 545800 5527187 0 -90 320 GL-17-030 545602 5527234 0 -90 143 GL-17-031 545601 5527214 0 -90 125 GL-17-032 545601 5527197 0 -90 200 GL-17-033 545601 5527197 180 -80 299 GL-17-034 545601 5527177 0 -90 228 GL-17-035 545600 5527155 0 -90 314 GL-17-036 545600 5527157 180 -80 548 GL-17-037 545600 5527136 0 -90 365 GL-17-039 545850 5527265 180 -80 327.6 GL-17-040 545849 5527246 0 -90 173 GL-17-041 545850 5527228 0 -90 347.26 GL-17-042 545851 5527209 0 -90 447 GL-17-043 545550 5527211 0 -90 107 GL-17-044 545550 5527194 0 -90 200 GL-17-045 545549 5527193 180 -80 302 GL-17-046 545549 5527171 0 -90 209 GL-17-047 545550 5527154 0 -90 278 GL-17-048 545550 5527154 180 -80 302 GL-17-049 545552 5527134 0 -90 326 GL-17-050 545950 5527285 0 -90 144 GL-17-051 545951 5527284 180 -80 341 GL-17-052 545951 5527265 0 -90 257 GL-17-053 545952 5527245 0 -90 299 GL-17-054 545950 5527225 0 -90 302 GL-17-055 545499 5527201 0 -90 131 GL-17-056 545501 5527190 180 -80 59 GL-17-057 545501 5527190 180 -80 233 GL-17-058 545500 5527171 0 -90 200 GL-17-059 545501 5527161 180 -80 317 GL-17-060 545503 5527143 0 -90 278 GL-17-061 545501 5527105 0 -90 269 GL-17-062 546000 5527305 0 -90 74 GL-17-063 546000 5527285 0 -90 200 GL-17-064 546000 5527265 0 -90 269

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HOLE ID UTM EAST UTM NORTH AZIMUTH ° DIP ° LENGTH (m) GL-17-065 546000 5527245 0 -90 341 GL-17-066 546050 5527315 0 -90 164 GL-17-067 546050 5527295 0 -90 206 GL-17-068 546050 5527275 0 -90 248 GL-17-069 546050 5527255 0 -90 320 GL-17-070 545450 5527202 0 -90 65 GL-17-071 545449 5527181 0 -90 86 GL-17-072 545450 5527185 180 -80 206 GL-17-073 545450 5527165 0 -90 164 GL-17-074 545447 5527136 0 -90 239 GL-17-075 545448 5527136 180 -80 284 GL-17-076 546100 5527315 0 -90 176 GL-17-077 546100 5527295 0 -90 206 GL-17-078 546100 5527275 0 -90 251 GL-17-079 546150 5527290 0 -90 200 GL-17-080 546150 5527270 0 -90 284 GL-17-081 546150 5527250 0 -90 275 GL-17-082 545399 5527168 0 -90 113 GL-17-083 545402 5527149 0 -90 107 GL-17-084 545399 5527124 0 -90 164 GL-17-085 545400 5527097 0 -90 172.47 GL-17-086 546300 5527305 0 -90 98 GL-17-087 546300 5527285 0 -90 137 GL-17-088 546300 5527265 0 -90 230 GL-17-089 546350 5527315 0 -90 89 GL-17-091 546350 5527275 0 -90 179 GL-17-092 545356 5527126 0 -90 107 GL-17-093 545350 5527085 0 -90 233 GL-17-094 545350 5527059 0 -90 287 GL-17-095 545351 5527033 0 -90 260 GL-17-096 546400 5527315 0 -90 101 GL-17-097 546400 5527295 0 -90 131 GL-17-098 546400 5527275 0 -90 149 GL-17-103 546050 5527200 0 -90 491 GL-17-104 546150 5527205 0 -90 443 GL-17-105 545401 5527072 0 -90 200 GL-17-106 545900 5527275 180 -80 302 GL-17-107 545901 5527254 180 -90 269 GL-17-108 545901 5527254 180 -80 328.5 GL-17-109 546200 5527280 0 -90 251 GL-17-110 546200 5527280 180 -80 431 GL-17-111 546250 5527300 0 -90 102.5 GL-17-112 546250 5527300 180 -80 296 GL-17-113 545900 5527275 0 -90 89

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9 Down Hole Surveying Due to the magnetic nature of the volcanic rocks of the area, an EZ Gyro survey tool was used for determining the deviation of the drill paths. The path of the drill hole was surveyed upon completion of the boring, with readings taken approximately every 30 meters. Optimized readings (consisting of three consecutive readings taken at the same interval and averaged together), were taken at the top and bottom of the drill hole. These were used to create the drill hole paths seen in the cross sections in Appendix D.

10 Method and Approach The core logging methodology and QAQC procedures were overseen by Miro Mytny, P.Geo, Exploration Manager for First Mining. The logging procedures applied during the 2017 program are as follows:

• HQ diameter (47.6 mm) drill core is cleaned and the run blocks checked. After this, the runs are measured for recovery. The recovery percentage is then used to mark off the adjusted meters within the run

• The Rock Quality Designation (RQD) is measured and recorded in an Excel sheet, for importing into DH Logger software

• The core is logged for lithology, alteration, minerology, veining and structure and entered into DH Logger software

• Two meter sample intervals are marked off, except at lithological contacts, and in zones of poor recovery, where sample size could be adjusted accordingly

• Standards and blanks are inserted in the sample stream at the required intervals

• Duplicates are inserted between the blanks and standards, alternating between field and lab duplicates

• Core pieces are selected and measured for SG

• The core is photographed twice, both dry and wet

• The core is sawn in half onsite, with one half bagged and labelled to be sent for assay. For field duplicates, the core is quartered and one quarter is sent for the regular assay and the other quarter for the duplicate assay. For the lab duplicates, an empty sample bag with a sample ID is sent to the lab where a split is taken from the pulverized sample to run a duplicate assay.

• The remaining half core is placed in core boxes which are stored in a secure on-site facility to serve as a permanent record

• Sample bags are placed in zip-tied rice bags and shipped to SGS Laboratory facilities in Red Lake, Ontario and Burnaby, British Columbia for the fire assay and BLEG assaying respectively

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11 Assays Samples from the mineralized granodiorite were shipped to SGS Laboratories in Burnaby, BC for cyanide leach assay using the Bulk Leach Extractable Gold (BLEG) method, which incorporated a LeachWELLTM reagent. To ensure that the cyanide leach is reporting all of the gold, the leach residue was also assayed, which was done by fire assay on a 50 g residue sample. The gold assays for the leach solution and residues are combined for each sample to report the final gold concentration.

The SGS Burnaby sample preparation and assay procedure is as follows:

• Crush entire half core sample

• Pulverize 3,000 g and split pulp into 3 x 1 kg pulps

• Send one of the 1 kg splits for BLEG assay (remainder is retained for duplicates)

• Bottle roll with LeachWELLTM

• Draw off solution and analyze by ICP-MS

• Filter all pulp, wash, dry and analyze for gold by fire assay

A 50g split from each sample sent to the Burnaby lab underwent ICP multi-element analysis by two-acid aqua regia digestion with ICP-MS and AES finish.

Samples from the unmineralized volcanics were sent to the SGS laboratory in Red Lake, Ontario for fire assay.

The assay methods are further detailed in the SGS Analytical Guide, (Appendix F). The assay certificates are included Appendix E. Appendix C contains the drill logs with the sample intervals, and Appendix D includes cross sections displaying the assay results along the drill traces.

11.1 QAQC Analysis The QAQC program for the 2017 drilling consisted of the submission of duplicate samples and the insertion of certified reference materials (standards) and blanks at regular intervals. Blanks and standards were inserted at a rate of one standard for every 20 samples (5% of total) and one blank for every 30 samples (3% of total). Field duplicates from quartered core, as well as ‘pulp’ duplicates taken from 1 kg pulverized splits, were also inserted at regular intervals with an insertion rate of 4% for field duplicates and 4% for pulp duplicates.

After assay results were returned, additional duplicates were run on available 1 kg pulverized splits, including BLEG duplicates and screened metallic duplicates. Selected samples were also sent to an independent umpire laboratory (Activation Labs in Thunder Bay, Ontario) for check assay.

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12 DGI Televiewer Survey At the start of the Phase 1 drill program in January 2017, Terracognita Geological Consulting Inc. (TGC) was contracted by First Mining to assist in the planning and execution of a downhole televiewer survey program at the Goldlund Property, and to undertake a structural analysis of the final data. The principal objective of the televiewer survey program was to gather structural geology data that would allow for the interpretation of the structural setting of the gold mineralization in the deposit. DGI Geoscience Inc. (DGI) of Toronto was the company contracted by First Mining to carry out the surveys.

TGC designed the televiewer survey program following a review of the historical drilling and assay results for two of the mineralized zones at Goldlund, Zone 1 and Zone 7. A priority suite of seven drill holes was identified, representing a total of 5,609 meters, as well as several alternative choices of drill holes in case some of the priority drill holes proved to be inaccessible. The drill holes were chosen based on a requirement for good spatial coverage of Zones 1 and 7, as well as a preference to survey holes that sampled mineralized rocks across the two zones, while avoiding holes that might intersect historical underground workings. The final selection included historical drill holes as well as drill holes from the Phase 1 drilling campaign at Zone 7.

During a site visit from February 1st through February 6th, 2017, TGC worked with First Mining personnel at Goldlund to refine the choice of drill holes to be surveyed based on accessibility as validated in the field. Some Phase 1 drill holes were also included in the program, where mineralization had been identified during core logging.

DGI personnel performed the surveys from March 9th through March 18th, 2017. TGC visited the Goldlund site a second time from March 10th through March 14th in order to consult with the DGI and First Mining personnel to adjust the final survey program. Adjustments were necessary as a function of early results and of some unforeseen problems with drill hole access.

The final program included nine surveyed drill holes. Optical televiewer (OTV) data was gathered for eight of the holes, with K13-146 having been excluded due to the hole being blocked at a rather shallow depth. Acoustic televiewer (ATV) surveys were also carried out for eight of the nine holes, with GL-17-005 being excluded. OTV data is most useful for structural geology studies whereas the ATV surveys are most useful for geotechnical studies. The surveys also included the logging of natural gamma and magnetic susceptibility data from a subset of the nine drill holes.

Following completion of the televiewer surveys, structural picks (i.e. the measurement of structural features from the televiewer data) were performed by DGI personnel and the resulting data was transferred to TGC during the month of April. TGC then carried out a structural analysis and interpretation of the structural picks from the OTV data.

TGC was able to identify multiple vein sets within the granodiorite bodies that host the Goldlund mineralization and to analyze the vein sets in the framework of a Riedel-type brittle-ductile shear system. Veins belonging the PDZ-set and the T-set are abundantly represented in Zone 1. Alteration envelopes are commonly associated with both of those vein sets. Different vein sets are predominant in the rocks that make up Zone 1 (mostly granodiorite with subordinate porphyry) and in the rocks that host it (andesite).

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The T vein set is predominant within the granodiorites of Zone 1 and most of the measured alteration envelopes are associated with that vein set. If the presence of alteration envelopes associated with veins were a reliable indication of potential mineralization then it could be expected that, in Zone 1, gold would be associated mainly with the SSW-striking extensional veins.

The PDZ vein set is predominant within the andesite and most of the measured alteration envelopes are associated with that vein set where it is hosted by that rock type. In Zone 7, OTV analysis reveals the presence of several vein sets, the most prominent being the SSW-striking T-vein set, interpreted to represent extensional veins associated with the same deformation event that gave rise to the brittle shear zones defined by the PDZ (R, P & Y) vein sets. Alteration envelopes identified in the OTV images are predominantly associated with the T-vein set which is itself more prevalent in the granodiorite unit than in the host andesites. If the presence of alteration envelopes associated with veins is a reliable indication of potential mineralization then it can be expected that, in Zone 7, gold will be associated mainly with the SSW-striking extensional veins. The most likely orientation for potential ore shoots would be plunging at moderate angles to the southwest.

A schematic showing the locations of the surveyed drill holes is provided in Figure 12.1. Modeled pits (McCracken, 2017) are shown in black outlines and mineralized zones shown in green. A summary of the drill holes that were surveyed is provided in Table 12.1. The full report from DGI can be found in Appendix G.

Figure 12.1: Location of Drill Holes with Televiewer Surveys

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Table 12.1: DGI Downhole Surveys, March 2017

ACOUSTIC TELEVIEWER

OPTICAL TELEVIEWER

NATURAL GAMMA

MAGNETIC SUSCEPTIBILITY

HOLE ID EOH (m) DUMMIED DEPTH (m)

CASING DEPTH

(m)

DATE FROM (m)

TO (m)

FROM (m)

TO (m)

FROM (m)

TO (m)

FROM (m)

TO (m)

COMMENTS

GL-17-084 167 166 20 2017-03-09 1.6 162.7 3.8 162.3 3.8 162.3

K14-158 605 606 3 2017-03-10 2.5 598.6 2.5 598.6

2017-03-11 6.8 599.7 2.5 598.6 2.5 598.6

K13-150 197 197 0 2017-03-12 8.4 194.9 - 192.0 - 192.0

K13-146 303 280 12.4 2017-03-12 12.0 164.4 Blocked at 165 m

K13-147 177 170 12 2017-03-13 11.0 172.0 2.1 171.8 2.1 171.8

K11-129 486 486 10.5 2017-03-13 10.8 484.4 Artesian, as a result added ATV

2017-03-14 11.5 484.4 9.0 478.0 9.0 478.0 Mag requested

GL-17-032 188 184 13.2 2017-03-15 12.3 172.7 12.5 158.0 12.5 158.0 0.0 174.8 VG at ~90 m

G08-061 471 444 6 2017-03-16 4.9 440.1 4.5 360.0 4.5 360.0 Requested to log OTV only above

~350 m 2017-03-17 7.8 355.5 Mag requested

GL-17-005 667 667 0 2017-03-18 2.8 645.3 2.8 645.3 Requested OTV only

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13 Results A list of the significant drill intercepts from the 2017 Phase 1 drill program, with length-weighted average gold values are provided in Table 13.1.

The holes with no significant gold mineralization have helped to define the extent and further the understanding of the shape and nature of the deposit. Drill holes that ended in mineralized granodiorite are to be extended in a later phase.

Detailed graphic drill logs and cross sections are provided in Appendices C and D respectively.

Table 13.1: Drill Hole Results

HOLE ID FROM (m) TO (m) LENGTH (m) Au (g/t) GL-17-002 GL-17-002 17 31 14 1.48

inc 17 19 2 8.00 and 69 91 22 0.64 and 129 135 6 1.40 inc 129 131 2 3.83

GL-17-003 GL-17-003 50 76 26 0.29 and 94 96 2 1.24 and 106 108 2 11.12 and 140 168 28 0.85 inc 140 154 14 1.14 and 208.5 209.5 1 2.86 and 245 247 2 1.26 and 269 273 4 1.50 inc 269 271 2 2.57

GL-17-004 GL-17-004 94 100 6 0.38 and 124 130 6 1.09 inc 128 130 2 2.89 and 162 164 2 1.49

GL-17-005 GL-17-005 24 337 313 0.81 inc 24 28 4 4.44

and inc 38 42 4 2.30 and inc 72 74 2 6.65 and inc 82 84 2 1.55 and inc 103.5 104 0.5 14.66 and inc 112 124 12 1.47 and inc 120 120.5 0.5 15.83 and inc 150 156 6 5.43 and inc 154 156 2 12.67 and inc 216 218 2 15.48 and inc 262 266 4 1.23 and inc 270 272 2 42.15 and inc 290 291 1 1.97

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HOLE ID FROM (m) TO (m) LENGTH (m) Au (g/t) and 441 605 164 0.42 inc 461 463 2 1.17

and inc 475 477 2 1.36 and inc 545 575 30 1.44 and inc 555 569 14 2.19 and inc 567 569 2 8.07 and inc 571 573 2 2.68 and inc 599 601 2 3.86

GL-17-006 GL-17-006 108 132 24 0.44 inc 114 120 6 1.03

and inc 130 132 2 1.32 and 182 212 30 0.52 inc 182 186 4 2.67 and 242 244 2 1.99 and 270 272 2 1.07 and 282 298 16 0.47 inc 296 298 2 1.64 and 312 324 12 0.45

GL-17-007 GL-17-007 93 97 4 1.42 and 145 155 10 0.86 inc 149 151 2 2.34 and 183 235 52 0.63 inc 207 213 6 1.81

and inc 207 209 2 2.74 and inc 211 213 2 2.61 and inc 233 235 2 4.70

and 269 271 2 1.83 GL-17-008 GL-17-008 203 205 2 1.05

and 225 233 8 1.40 inc 225 227 2 2.25

and inc 231 233 2 3.33 and 249 265 16 0.40 inc 255 257 2 1.28 and 282 290 8 0.63 inc 285 286 1 3.69

GL-17-010 GL-17-010 12 58 46 0.37 inc 12 14 2 1.45


and 182 184 2 1.20 and 252 256 4 1.53 inc 254 256 2 2.62 and 280 286 6 1.07 inc 284 286 2 2.45

GL-17-011 GL-17-011 44 54 10 0.74 inc 46 48 2 2.46

GL-17-012 GL-17-012 186 208 22 0.71

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HOLE ID FROM (m) TO (m) LENGTH (m) Au (g/t)

inc 200 208 8 1.71 and inc 204 206 2 5.02

and 246 248 2 1.52 GL-17-013 GL-17-013 74 82 8 1.49

inc 74 76 2 4.04 and 166 168 2 2.69 and 266 275 9 0.95 inc 274 275 1 2.92

GL-17-014 GL-17-014 88 90 2 1.45 and 234 246 12 1.72 inc 234 236 2 8.79 and 266 272 6 30.69 inc 270 272 2 91.63 and 288 290 2 2.45 and 338 348 10 0.56

GL-17-016 GL-17-016 40 48 8 0.77 and 54 64 10 0.55

GL-17-017 GL-17-017 5.69 210 204.31 0.45 inc 12 74 62 0.90


and 106 116 10 1.86 inc 106 112 6 2.91

and inc 106 108 2 7.38 and 134 140 6 0.54 and 204 244 40 0.32 inc 236 244 8 0.66

GL-17-018 GL-17-018 30 112 82 0.46 inc 30 38 8 1.06

and inc 52 72 20 0.70 and inc 70 72 2 3.26 and inc 104 110 6 1.33 and inc 108 110 2 3.53

GL-17-019 GL-17-019 118 126 8 0.45 and 152 170 18 0.55 inc 166 170 4 1.82 and 226 232 6 0.98

GL-17-21 GL-17-21 155 365 210 0.85 inc 155 207 52 2.21

and inc 185 203 18 5.14 and inc 201 203 2 43.09 and inc 273 301 28 1.37 and inc 281 283 2 8.80 and inc 289 291 2 6.29

GL-17-023 GL-17-023 48 52 4 1.23 inc 48 50 2 2.05

GL-17-026 GL-17-026 144 146 2 2.07

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GL-17-027 GL-17-027 58 64 6 3.6 inc 58 60 2 8.63

GL-17-028 GL-17-028 150 162 12 0.98 inc 150 152 2 2.10



GL-17-029 GL-17-029 212 222 10 4.11 inc 212 214 2 10.66

and inc 220 222 2 9.76 and 240 248 8 1.28 inc 244 248 4 2.15 and 306 310 4 2.18

GL-17-030 GL-17-030 no significant mineralization GL-17-031 GL-17-031 25 59 34 0.91

inc 51 59 8 2.81 and inc 55 57 2 8.77

GL-17-032 GL-17-032 48 112.5 64.5 3.25 inc 90 112.5 22.5 8.57

and inc 90 90.5 0.5 335.76 GL-17-033 GL-17-033 28 38 10 0.6

inc 28 30 2 1.99 and 110 112 2 2.5 and 126 128 2 1.1 and 154 156 2 1.09

GL-17-034 GL-17-034 104 134 30 0.98 inc 108 110 2 8.75

GL-17-035 GL-17-035 124 166 42 0.51 and 254 260 6 0.53

GL-17-036 GL-17-036 136 150 14 1.44 inc 136 138 2 8.55 and 196 232 36 0.55 inc 208 210 2 2.66

and inc 212 216 4 1.51 and inc 230 232 2 1.29

and 382 386 4 1.65 inc 382 384 2 2.48

GL-17-037 GL-17-037 197 235 38 0.36 inc 197 199 2 1.86

and inc 211 213 2 1.84 and inc 233 235 2 1.38

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GL-17-039 GL-17-039 164 174 10 0.93 inc 172 174 2 2.05 and 184 190 6 1.22 inc 188 190 2 3.06 and 216 220 4 1.06 and 246 302 56 0.90 inc 246 260 14 2.18

and inc 248 250 2 12.54 and inc 278 280 2 4.46


inc 130 136 6 0.99 and 198 200 2 11.50 and 226 286 60 1.02 inc 226 244 18 2.26


GL-17-042 GL-17-042 210 236 26 0.30 inc 210 212 2 1.62 and 278 351 73 0.51 inc 278 279 1 16.38

and inc 331 333 2 2.11 and inc 337 339 2 1.22

and 367 387 20 0.53 inc 367 369 2 1.37

and inc 383 385 2 1.85 and 409 431 22 1.20 inc 409 411 2 9.66

and inc 423 425 2 2.28 GL-17-043 GL-17-043 58 74 16 0.34

inc 72 74 2 1.29 GL-17-044 GL-17-044 80 106 26 2.14

inc 82 92 10 4.85 and inc 88 90 2 18.43

GL-17-045 GL-17-045 24 102 78 1.96 inc 38 50 12 10.81


and 148 150 2 3.94 GL-17-046 GL-17-046 40 156 116 0.62

inc 48 74 26 1.16 and inc 64 68 4 3.31 and inc 128 152 24 1.31 and inc 150 152 2 10.67

GL-17-047 GL-17-047 96 204 108 0.47

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inc 128 130 2 16.95 and 248 254 6 3.55

GL-17-048 GL-17-048 108 160 52 0.36 inc 134 136 2 3.92

GL-17-049 GL-17-049 70 96 26 0.65 inc 70 72 2 1.45

and inc 78 80 2 4.96 and inc 94 96 2 1.13

and 124 136 12 0.52 inc 124 126 2 1.10


and inc 242 244 2 1.49 and inc 246 248 2 1.38

and 296 298 2 2.19 GL-17-050 GL-17-050 5.45 7 1.55 0.99

and 13 15 2 0.73 and 49 51 2 1.30

GL-17-051 GL-17-051 85 87 2 2.94 and 209 229 20 0.90 inc 209 211 2 3.46

and inc 221 223 2 2.13 and 261 263 2 2.31 and 285 287 2 1.28 and 305 323 18 1.54 inc 317 323 6 3.42

GL-17-052 GL-17-052 7 9 2 2.64 and 73 75 2 1.06 and 87 93 6 0.57

GL-17-053 GL-17-053 102 281 179 1.13 inc 102 104 2 8.70

and inc 144 152 8 3.29 and inc 150 152 2 12.07 and inc 180 184 4 2.63 and inc 238 281 43 3.01 and inc 238 242 4 7.29 and inc 245 248 3 8.59 and inc 255 257 2 8.14

GL-17-054 GL-17-054 no significant mineralization GL-17-055 GL-17-055 22 24 2 1.27 GL-17-056 GL-17-056 10 42 32 0.77

inc 22 26 4 1.70 GL-17-057 GL-17-057 10 44 34 0.68

inc 10 12 2 1.20 and inc 14 16 2 1.41 and inc 18 20 2 1.30

27 | P a g e

HOLE ID FROM (m) TO (m) LENGTH (m) Au (g/t) and inc 36 38 2 1.81 and inc 42 44 2 1.42

and 62 66 4 0.81 and 126 128 2 1.47

GL-17-058 GL-17-058 10 12 2 3.2 and 56 58 2 1.03 and 118 138 20 0.68 inc 124 130 6 1.28 and 164 166.1 2.1 2.41

GL-17-059 GL-17-059 82 152.5 70.5 2.5 inc 110 112 2 23.62

and inc 122 132 10 1.05 and inc 152 152.5 0.5 186.49

and 186 188 2 1.09 GL-17-060 GL-17-060 46 60 14 6.05

inc 46 48 2 38.54 and 82 152 70 0.50 inc 88 94 6 1.93

and inc 88 90 2 4.07 and inc 115 116.5 1.5 1.51

GL-17-061 GL-17-061 38 40 2 1.32 and 130 132 2 0.92 and 154 156 2 2.54 and 178 182 4 1.04

GL-17-062 GL-17-062 12 24 12 1.44 inc 16 18 2 5.24

GL-17-063 GL-17-063 46 64 18 2.44 inc 46 48 2 6.49

and inc 62 64 2 6.65 and 96 164 68 0.28 inc 98 100 2 1.82

and inc 124 130 6 0.99 GL-17-064 GL-17-064 45.83 48 2.17 2.78

and 78 80 2 3.64 and 122 174 52 0.46 inc 122 124 2 4.64

and inc 172 174 2 2.99 GL-17-065 GL-17-065 204 294 90 1.32


GL-17-066 GL-17-066 8 30 22 0.38 inc 28 30 2 2.10 and 50 52 2 11.07 and 78 104.92 26.92 0.50 inc 84 86 2 3.44

GL-17-067 GL-17-067 3.8 16 12.2 0.73

28 | P a g e


inc 12 16 4 1.64 and inc 38 40 2 1.92

and 94 96 2 1.39 and 104 106 2 1.43

GL-17-068 GL-17-068 116 184 68 0.91 inc 142 184 42 1.36


GL-17-069 GL-17-069 234 300 66 1.51 inc 234 262 28 2.03


GL-17-070 GL-17-070 no significant mineralization GL-17-071 GL-17-071 10.85 56 45.15 0.97

inc 22 52 30 1.26 and inc 48 52 4 3.71

GL-17-072 GL-17-072 11 87 76 0.66 inc 11 15 4 1.44 and 27 43 16 1.02 and 75 79 4 2.23

GL-17-073 GL-17-073 17 21 4 3.71 and 39 87 48 2.34 inc 39 41 2 9.05 and 75 77 2 36.53

GL-17-074 GL-17-074 26 92 66 0.75 inc 52 56 4 2.95

and inc 66 68 2 2.16 and inc 88 90 2 10.54

GL-17-075 GL-17-075 26 28 2 1.16 and 68 70 2 1.26 and 90 92 2 2.19

GL-17-076 GL-17-076 46 54 8 3.44 inc 46 48 2 12.40

GL-17-077 GL-17-077 32 68 36 0.46 inc 32 34 2 2.08

and inc 66 68 2 1.99 and 104 106 2 1.87 and 124 126 2 1.82 and 134 136 2 1.32

GL-17-078 GL-17-078 no significant mineralization GL-17-079 GL-17-079 no significant mineralization GL-17-080 GL-17-080 no significant mineralization GL-17-081 GL-17-081 no significant mineralization GL-17-082 GL-17-082 no significant mineralization GL-17-083 GL-17-083 32 62 30 0.19

29 | P a g e


GL-17-084 GL-17-084 54 88 34 3.91 inc 54 56 2 41.93

and inc 78 80 2 8.44 GL-17-085 GL-17-085 52 56 4 0.83

and 84 88 4 1.27 GL-17-086 GL-17-086 45 47 2 0.73 GL-17-087 GL-17-087 no significant mineralization GL-17-088 GL-17-088 no significant mineralization GL-17-089 GL-17-089 29 42.7 13.7 0.65

inc 31 35 4 1.30 GL-17-091 GL-17-091 76 84 8 0.55

inc 80 82 2 1.16 and 96 120 24 0.33

GL-17-092 GL-17-092 19 39 20 1.39 inc 23 25 2 7.51

GL-17-093 GL-17-093 40 44 4 0.81 GL-17-094 GL-17-094 23 25 2 3.36 GL-17-095 GL-17-095 105 107 2 1.85 GL-17-096 GL-17-096 16 22 6 0.87

inc 18 20 2 2.05 and 32 50 18 1.02 inc 40 42 2 2.15

GL-17-097 GL-17-097 48 92 44 0.82 inc 48 68 20 1.33

and inc 54 56 2 4.23 and inc 60 62 2 6.18

GL-17-098 GL-17-098 78 98 20 0.36 inc 80 82 2 2.22

GL-17-103 GL-17-103 329 381 52 2.18 inc 329 361 32 3.41 inc 329 331 2 5.76


GL-17-104 GL-17-104 361 369 8 1.04 inc 361 363 2 2.06

GL-17-105 GL-17-105 34 44 10 1.90 inc 34 36 2 9.14 and 84 128 44 0.32 inc 86 88 2 2.86

GL-17-106 GL-17-106 66 268 202 1.39 inc 76 80 4 2.25

and inc 178 194 16 6.66 and inc 188 190 2 43.28 and inc 226 268 42 3.21 and inc 242 244 2 13.51 and inc 262 264 2 13.88

GL-17-107 GL-17-107 82 216 134 0.91

30 | P a g e

HOLE ID FROM (m) TO (m) LENGTH (m) Au (g/t) inc 82 98 16 1.38


GL-17-108 GL-17-108 38 40 2 1.02 and 110 112 2 3.87 and 146 156 10 0.71 and 266 326 60 0.39 inc 296 298 2 4.13

and inc 322 326 4 1.34 GL-17-109 GL-17-109 no significant mineralization GL-17-110 GL-17-110 294 400 106 0.59



inc 282 284 2 3.17 GL-17-113 GL-17-113 no significant mineralization

31 | P a g e

14 Expenditures The total cost of drilling, and associated surveying was $2,424,340 for Phase 1. The total cost of this phase of the drilling program was $4,474,689. A further breakdown can be seen in Table 14.1.

Table 14.1: Expenditure Summary

EXPENDITURE TYPE CAD$

Professional Time

Management & Supervision $94,074

Camp Management & Logistics $40,257

Geologists $186,485

Geotechs $171,406

TOTAL PROFESSIONAL TIME $492,221

Drilling & Surveying $2,424,340

Assaying & Field Supplies $1,151,467

Accommodation, Food, Travel and other Expenses $399,661

Report Writing $7,000

GRAND TOTAL $4,474,689

15 Conclusions and Recommendations The Phase 1 drilling program has confirmed historical results and has better defined the mineralization in Zone 7. The albitized tonalite (granodiorite) and immediate hangingwall and footwall were entirely sampled and assayed to allow for a more accurate resource estimate with no data gaps. Also, this new drilling has extended the known Zone 7 mineralization to 650 meters depth.

Eight mineralized zones are known in the Goldlund resource area. Only Zones 1, 2, 4 and parts of Zone 8 have sufficient drilling to be classified as Indicated resource. With the new drilling however, the Zone 7 could potentially be upgraded from Inferred to Indicated category. The remaining three zones have insufficient data to be included in the current resource (McCracken, 2017).

It is recommended that an exploration program be designed to further identify any additional gold mineralization on the Property and to better define the known gold-bearing zones at the Goldlund Project. The main focus should be on the zones included within the current pit shell, as published in the most recent technical report (WSP, 2017).

32 | P a g e

There are a number of known historical gold occurrences elsewhere within the Goldlund Property which have only limited drill data. Mistango, Beartrack, Windfall, Goldlund, Tarbush, Loybex, Miller, Eaglelund, Quyta and other occurrences have all undergone varying degrees of exploration and mining activity.

It is recommended that surface exploration programs be implemented to follow up on the above-mentioned occurrences, with geological mapping and grab sampling to confirm historical data. A 2,500 m drill program is recommended to follow up on the results of the geological mapping and sampling programs. These exploration programs would utilize the knowledge gained from the Goldlund main Project by drilling vertical (-90º) to -80º holes down-dip of the tonalite sills, which would allow for the most efficient assessment of mineralization within these occurrences.

33 | P a g e

16 References Blackburn, C.E., Johns, G.W., Ayer, J.L, and Davis, D.W. 1991. Wabigoon Subprovince; in Geology of

Ontario; Ontario Geological. Survey, Special Volume 4, Part 1, p. 303–381

Chorlton, L. 1990. Regional Setting of Vein-style Gold Mineralization around the Goldlund Mine, Sandybeach Lake Area, Northwestern Ontario

Fingas, J. 2012. Assessment Report on Regional Geological Mapping and Soil Sampling Program, Tamaka Gold Corporation, Goldlund Project, Kenora & Patricia Mining Divisions, Ontario, Canada

Giddings, S. D. 1986. Petrology, Mineralogy, and Geochemistry of the Goldlund Deposit, Northwestern Ontario. M.Sc. Thesis, University of North Dakota, Grand Forks, ND.

McCracken, Todd. 2017. Technical Report and Resource Estimation Update on the Goldlund Project. Patricia Mining Division: NI 43-101

McCracken, T. 2016. Technical Report and Resource Estimate Update on the Goldlund Deposit, Goldlund Project, Sioux Lookout, Ontario, WSP Canada Inc.

McCracken, T. 2014. Technical Report and Resource Estimate Update on the Goldlund Deposit, Goldlund Project, Sioux Lookout, Ontario, Tetra Tech Inc.

McCracken, T. 2012. Technical Report and Resource Estimate on the Goldlund Deposit, Goldlund Project, Sioux Lookout, Ontario, Tetra Tech Inc.

Page, R.O., 1984. Geology of the Lateral Lake Area, District of Kenora: Ministry of Northern Development.

Percival, J.A. and Easton, R.M., 2007. Geology of the Canadian Shield in Ontario: An Update, Ontario Geological Survey Open File Report 6196

Pieterse, R.K., 2005. Summation and Extracts from Historical Technical Reports on Goldlund Property of Tamaka Holdings Inc., November 2005

Pettigrew, N, 2012. Report on Structural Observations and Interpretations, Sioux Lookout, Ontario, October 2012

SGS Mineral Services. 2017. SGS Analytical Guide. http://www.sgs.com/-/media/global/documents/brochures/sgs-analytical-guide.pdf

Sheridan, K. 2011. Assessment Report on Regional Geological Mapping and 2011 Diamond Drill Program, Tamaka Gold Corporation, Goldlund Project, Kenora & Patricia Mining Divisions, Ontario, Canada. March 2011

Zellerer, S. 2013. Technical Report and Resource Estimate Update on the Goldlund Deposit, Sioux Lookout, Ontario, December 2013

http://www.sgs.com/-/media/global/documents/brochures/sgs-analytical-guide.pdf

34 | P a g e

17 Statement of Qualifications

Miro Mytny, M.Sc., P.Geo. First Mining Finance Corp.

1800 - 925 West Georgia Street, Vancouver, BC, Canada

Telephone: 1-844-306-8827 Email: [email protected]

CERTIFICATE of Author

I, Miro Mytny, M.Sc., P.Geo. do hereby certify that:

1. I am Senior Exploration Manager of: First Mining Finance Corp. 1800 - 925 West Georgia Street, Vancouver, BC, Canada, V6C 3L2

2. I graduated with a degree in Geochemistry, General Geology and Geology of Mineral Deposits from the Comenius University, Bratislava, Slovakia in 1986. In addition, I have obtained a RNDr. (Doctor of Natural Sciences) from Comenius University.

3. I am a member of the Association of Professional Geoscientists of Ontario, APGO.

4. I have worked as a geologist for a total of 30 years since my graduation from university.

Dated this 20th Day of December, 2017.

__________________________________

35 | P a g e

Appendix A: Claim Map

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¢

¢

g¢

¢

g"

§̈¦72

§̈¦72

WinwardGoldlund

ECHO

KABIK LAKEWEBB

LAVALKEIKEWABIK LAKE

MCAREE

PARNES LAKE

LOMOND

JORDANVERMILION

MCILRAITH

LARDER LAKE

PICKEREL

MACFIEHARTMAN

DRAYTON DRAYTON

Camp

3012493

4256883

4256606

4200350

3019760

4256876

3019677

4256879

4259028

4262785

3019758

4253231

4253229

4200430

4200347

4256239

4200342

4200344

4200343

4200425

4253230

4259707

3012489

4200345

4256236 4256240

4256204

4200348

4253225

4259709

3019764

4256608

4256225

4261478

4253228

4256610

3019761

4256202

4200351

3019767

4253232

3012490

4214543

4200429

3019693

3012443

4224124

4261479

3012472

4256611

4256616

4200424

3012494

4259027

3019756

3019766

3019749

4200432

4224123

42562244259021

3019754

4256237

4259041

3012488

4256214

4256609

4256604

3019768

4256213

4200423

4256607

4200428

3019753

3019757

3002715

42627844200304

4263723

4256882

4256877

4262783

3012491

3019759

3019762

4256874

42590394259035

4259718

42003054262782

4256235

4256226

4256872

4256238

4263724

3019751

4259045

3019765

3012492

3019755

4259712

4256603

4256223

4253224

3019752

4200307

4259026

1166865

3004265

4200431

4256201

4259719

3012496

4263725

4256242

4259720

4262781

3019695

4253227

1191761

1247989

4256212

4256871

1199268

3019657

4200346

4200349

4256869

4256615

3019656

4256211

3019763

4259717

4262202 3019701

3019655

1162943

3002714

4222883

4241203

4200426

4200306

4253233

1191762

4256605

30042643002721

4241202

534000

534000

536000

536000

538000

538000

540000

540000

542000

542000

544000

544000

546000

546000

548000

548000

550000

550000

552000

552000

554000

554000

556000

556000

558000

558000

560000

560000

562000

562000

564000

564000

566000

566000

568000

568000

570000

570000

572000

572000

574000

574000

576000

576000

578000

578000

551700

0

551700

0

551900

0

551900

0

552100

0

552100

0

552300

0

552300

0

552500

0

552500

0

552700

0

552700

0

552900

0

552900

0

553100

0

553100

0

553300

0

553300

0

553500

0

553500

0

553700

0

553700

0

553900

0

553900

0

554100

0

554100

0

554300

0

554300

0

Goldlund TenureProperty OutlinePatented Claim

Mining Lease

License of OccupationUnpatented Claim

4

NTS Reference: 52J04, 52K01, 02, 52G13, 52F15, 16Patricia & Kenora Mining Divisions, Ontario

Coordinates: NAD83 UTMz15 Date: 20-Nov-2017 Scale 1 : 50,000

0 5Kilometers

Vermilion Lake

Minnitaki Lake

Big Sandy Lake

KABIKWABIK LAKE

LittleVermilion

Lake

Goldlund Land Tenure

!.

!.

!. !.

!.

_̂

Ottawa

Kenora

Toronto

TimminsThunder Bay

0 500

Kilometers

Manitoba

USA

Goldlund PropertyLocation Ontario Quebec

¢

¢

g

¢

¢

g

"

Mining Lease107464

WinwardGoldlund

ECHO

MCAREE

Camp

KRL18809

PA436895

PA436896

KRL22736 PA436897

KRL23117

KRL23122

KRL23118KRL23116

KRL23108

KRL18812

KRL23121

KRL18720

KRL23107

KRL23119

KRL18724

KRL23109

KRL18722

KRL23120

KRL23115

KRL23111

KRL18723

KRL22737

KRL23113KRL23112

KRL23123

KRL23106

KRL22735

KRL23114

KRL23110

4263724

30197644263723

4256606

1166865

1191761

1247989

3019657

3019656

3019758

4262202

4256604

3019701

3004265

3019655

1162943

3002714

4200423

42637251191762

4256605

3004264 3002721

4256616

4261478

42566151199268

0 1Kilometers

CrossechoLake

LegendRoadway

! Power Line¢

¢

g ShaftTownship Grid

36 | P a g e

Appendix B: Drill Location Map

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Goldlund Camp

GL-17-113

GL-17-112GL-17-111

GL-17-110GL-17-109

GL-17-108GL-17-107

GL-17-106

GL-17-105

GL-17-104GL-17-103

GL-17-098

GL-17-097

GL-17-096

GL-17-095

GL-17-094

GL-17-093

GL-17-092

GL-17-091

GL-17-089

GL-17-088

GL-17-087

GL-17-086

GL-17-085

GL-17-084

GL-17-083

GL-17-082

GL-17-081

GL-17-080

GL-17-079GL-17-078

GL-17-077

GL-17-076

GL-17-075GL-17-074

GL-17-073

GL-17-072GL-17-071

GL-17-070

GL-17-069

GL-17-068

GL-17-067

GL-17-066

GL-17-065

GL-17-064

GL-17-063

GL-17-062

GL-17-061

GL-17-060

GL-17-059

GL-17-058GL-17-057GL-17-056

GL-17-055

GL-17-054

GL-17-053

GL-17-052

GL-17-051GL-17-050

GL-17-049

GL-17-048GL-17-047

GL-17-046

GL-17-045GL-17-044

GL-17-043 GL-17-042

GL-17-041

GL-17-040

GL-17-039

GL-17-037

GL-17-036GL-17-035

GL-17-034

GL-17-033GL-17-032

GL-17-031

GL-17-030

GL-17-029

GL-17-028GL-17-027

GL-17-026

GL-17-023

GL-17-021

GL-17-019

GL-17-018

GL-17-017GL-17-016

GL-17-014

GL-17-013GL-17-012

GL-17-011GL-17-010

GL-17-008

GL-17-007

GL-17-006

GL-17-005

GL-17-003

GL-17-004

GL-17-002

1166865

3019657

1247989

3004264 3002721

1191762

KRL18809KRL18812

KRL18724KRL23113

KRL18723

KRL23114

KRL23112

KRL23112

KRL23112

KRL23114

KRL23113

395

390

385

400

405

410

415

420

425

425

410

415

410

415

420

405

400

410

410

415

410

410

405

410

420

420

Goldlund Shaft

Windfall Shaft

545400

545400

545600

545600

545800

545800

546000

546000

546200

546200

546400

546400

546600

546600

546800

546800

547000

547000

547200

5472005526

800

5526

800

5527

000

5527

000

5527

200

5527

200

5527

400

5527

400

5527

600

5527

600

License of OccupationPatented ClaimUnpatented Claim

é

é Shaft! 2017 Phase 1 Drill Hole Collar

2017 Phase 1 Drill Hole Trace

HighwayLogging RoadTopography Contours (5m Interval)

Buildings / InfrastructureWater Body

0 300Meters

Map Extent

4

Goldlund Property Outline

0 20Kilometers

Scale 1 : 3,500NAD83 UTM Zone 15NNov. 2017

Goldlund Property, Ontario2017 Phase 1 Drill Location Map

NTS Reference: 52J04, K01, K02, G13, F15, F16Patricia & Kenora Mining Divisions

§̈¦72

37 | P a g e

Appendix C: Drill Logs

GL-17-002 GL-17-050 GL-17-092 GL-17-003 GL-17-051 GL-17-093 GL-17-004 GL-17-052 GL-17-094 GL-17-005 GL-17-053 GL-17-095 GL-17-006 GL-17-054 GL-17-096 GL-17-007 GL-17-055 GL-17-097 GL-17-008 GL-17-056 GL-17-098 GL-17-010 GL-17-057 GL-17-103 GL-17-011 GL-17-058 GL-17-104 GL-17-012 GL-17-059 GL-17-105 GL-17-013 GL-17-060 GL-17-106 GL-17-014 GL-17-061 GL-17-107 GL-17-016 GL-17-062 GL-17-108 GL-17-017 GL-17-063 GL-17-109 GL-17-018 GL-17-064 GL-17-110 GL-17-019 GL-17-065 GL-17-111 GL-17-021 GL-17-066 GL-17-112 GL-17-023 GL-17-067 GL-17-113 GL-17-026 GL-17-068 GL-17-027 GL-17-069 GL-17-028 GL-17-070 GL-17-029 GL-17-071 GL-17-030 GL-17-072 GL-17-031 GL-17-073 GL-17-032 GL-17-074 GL-17-033 GL-17-075 GL-17-034 GL-17-076 GL-17-035 GL-17-077 GL-17-036 GL-17-078 GL-17-037 GL-17-079 GL-17-039 GL-17-080 GL-17-040 GL-17-081 GL-17-041 GL-17-082 GL-17-042 GL-17-083 GL-17-043 GL-17-084 GL-17-044 GL-17-085 GL-17-045 GL-17-086 GL-17-046 GL-17-087 GL-17-047 GL-17-088 GL-17-048 GL-17-089 GL-17-049 GL-17-091

Gold Values (g/t)0 - 0.20.2 - 0.50.5 - 11 - 55 - 1010 - 500

Alteration StyleBDisFFFHALINTMOPPCHPDSP

Banded Disseminated FractureFracture Filling HaloesInterstitial MottledPervasivePatchyPods Spots

AlterationAbAnkBtCarbChlEpHemKSausSerSil

AlbiteAnkeriteBiotiteCarbonateChloriteEpidoteHematitePotassicSaussuriteSericiteSilica

LithologyCasOvbMdkGabDioDiaDacAndBasGrdPorQVVoid

CasingOverburdenMafic DykeGabbroDioriteDiabaseDaciteAndesiteBasaltGranodioritePorphyryQuartz VeinVoid

Vein StylesFLDMASSHTSTKSTRVNLVUG

FloodedMassiveSheetedStockworkStringersVeinletsVuggy

IntensityISMW

IntenseStrongModerateWeak

TextureAmyPillMassGAphFGMGCGBPPhePyVarVes

AmygdaloidalPillowedMassiveGlassyAphaniticFine GrainedMedium GrainedCoarse GrainedBimodalPorphyriticPhenocrysticPyroclasticVarioliticVesicular

Vein TypeCQQAQBQCQCBQCChlQChlQT

CarbonateQuartzQuartz-AlbiteQuartz-BiotiteQuartz-Carb Qtz-Carb-BtQtz-Carb-ChlQuartz-ChloriteQtz-Tourmaline

Structure tadpoles on logsare oriented according to angle to core axis

StructureBDBOUDBXCNTRFDFLTFOLFRGGNJNTSMYLSSHRSLK

Bedding BoudinageBrecciation Contorted FoldedFaultFoliated Fractured Fault with GougeGneissicJointsMyloniticSchistoseShearFault with Slickensides

> 10

MineralizationStyle

BlBxCxDisFFIntRimSMSeTrVnWs

BlebbyBreccia CrystalsDisseminatedFracture filling Interstitial RimsSemi-Massive Seams TraceVeinsWisps

MineralizationCcpHemMagMolPoPyTelVG

ChalcopyriteHematiteMagnetiteMolybdenitePyrrhotitePyriteTellurideVisible Gold

Legend

90

80

70

60

50

40

30

20

10

0

light greenish gray moderately chloritized and very weakly carb altd grd transitioning below 113.0m to medium gray less chloritic and more carb altered grd; unit is massive crosscut by numerous qtz and qtz-carb veins with alteration halos supporting variable sulphide concentrations

0.090.020.17

80.270.260.620.40.2

0.610.0050.020.1

0.010.04

0.0050.0050.23

0.0050.170.010.030.320.250.030.220.190.060.1

0.860.210.530.3

0.250.771.310.920.570.39

F00001303F00001304F00001305F00001306F00001307F00001308F00001309F00001310F00001311F00001312F00001313F00001314F00001315F00001316F00001318F00001319F00001320F00001321F00001323F00001324F00001325F00001328F00001329F00001330F00001331F00001332F00001333F00001334F00001335F00001336F00001337F00001338F00001340F00001341F00001343F00001344F00001345F00001346F00001347

Depth(m)

Lithology Alteration Mineralization Veining AssaysStructure

Claim ID: 1166865Easting: 545700.53 mENorthing: 5527231.75 mNElevation: 391.82 mASL Core Size: HQ

Casing Depth: 11 mEOH: 158 m

Start Date: March-30-17End Date: April-01-17Drill Contractor: Rodren Drilling

Au g/t Sample IDPrimary 2nd 3rd 4th Primary nd 3rd th nd Primary nd

Azimuth: 0 degreesDip: -90 degreesUTM NAD 83 - Zone 15

Project: GoldlundLogged by: John CamierLog Completed: April-01-17Core Location: TENT

GL-17-002 1 of 2 151050 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

160

150

140

130

120

110

100

dark olive green intensely chloritized and moderately silicified meta-mafic greenschist with carb-filled stretched amygdules and crosscutting qtz-carb veins and veinlets

0.970.280.170.1

0.320.5

0.310.360.110.270.070.070.020.030.040.120.030.020.040.073.830.040.340.060.180.19

0.0050.020.03

0.0050.0050.005

0.00250.00250.0025

F00001348F00001349F00001350F00001352F00001353F00001354F00001355F00001356F00001358F00001359F00001360F00001361F00001363F00001364F00001365F00001366F00001367F00001368F00001369F00001370F00001371F00001373F00001374F00001375F00001376F00001377F00001378F00001379F00001380F00001381F00001383F00001385F00001386F00001387F00001388

Depth(m)

Lithology Alteration Mineralization Veining AssaysStructureAu g/t Sample IDPrimary 2nd 3rd 4th Primary nd 3rd th nd Primary nd

GL-17-002 2 of 2 151050 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0 overburden to 10.45m depth; casing drilled to 12m depth for water return seal

massive light gray fg-mg moderately chloritized blue-qtz-eyed grd crosscut by numerous qtz + qtz-carb + qtz-albite veins with variable width alteration halos comprised of strongly to intensely silicified + weakly to moderately K +/- Na +/- carb (cte) with/without ankerite +/- hem altered; with halos supporting varying amounts of sulphides +/- Pb-tellurides;

massive mg-cg light to medium gray plag (~60%) + Kspr (20-30%) supported in a fg qtz-feldspathic-mt-amph-bio groundmass +/- trace sulphides (py); Kspr appears to contain white plag cores. Feldspars are bimodal in distribution and rock is weakly magnetic

0.0050.220.060.750.10.3

0.360.02

0.0050.04

0.0050.51

0.0050.2

0.040.005

0.30.2

0.070.090.390.010.510.790.170.150.650.080.050.530.05

0.0050.320.030.09

0.0050.0050.210.090.15

F00000251F00000252F00000253F00000254F00000255F00000256F00000257F00000258F00000259F00000260F00000262F00000263F00000264F00000265F00000266F00000267F00000268F00000269F00000271F00000272F00000274F00000276F00000277F00000278F00000279F00000280F00000281F00000282F00000283F00000285F00000286F00000287F00000288F00000289F00000291F00000292F00000293F00000294F00000295F00000296

Depth(m)




Start Date: April-01-17End Date: April-05-17Drill Contractor: Rodren Drilling




GL-17-003 1 of 4 3210 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

180

160

140

120

100

chloritized blue-qtz-eyed grd crosscut by numerous qtz + qtz-carb + qtz-albite veins with variable width alteration halos comprised of strongly to intensely silicified + weakly to moderately K +/- Na +/- carb (cte) with/without ankerite +/- hem altered; with halos supporting varying amounts of sulphides +/- Pb-tellurides; lower contact is somewhat irregular;

0.030.021.240.040.210.280.120.28

11.120.12

0.0050.0050.0050.010.1

0.050.06

0.0050.09

0.0050.02

0.0050.010.060.091.071.140.391.360.471.242.330.270.490.690.6

0.720.071.020.09

0.0050.220.040.040.22

0.0050.130.680.020.04

0.005

F00000297F00000298F00000300F00000301F00000302F00000303F00000304F00000306F00000307F00000309F00000311F00000312F00000313F00000314F00000315F00000316F00000317F00000318F00000319F00000321F00000322F00000323F00000324F00000325F00000326F00000327F00000328F00000329F00000331F00000333F00000334F00000336F00000337F00000338F00000339F00000340F00000341F00000342F00000343F00000345F00000346F00000347F00000348F00000349F00000351F00000352F00000353F00000354F00000355F00000356F00000357

Depth(m)


GL-17-003 2 of 4 3210 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

280

260

240

220

200

massive medium to coarse-grained bimodal feldspar porphyry

massive light grey fine to medium grained magnetic granodiorite; lower contact was not intercepted; Note drill hole intercept a previous cemented drill hole at 202.9 m

0.0050.0050.0050.330.330.030.060.030.052.860.230.040.090.050.260.170.05

0.0050.110.1

0.110.070.330.030.010.160.02

0.0051.260.180.030.360.76

0.0050.005

0.20.050.260.160.212.570.420.030.020.020.020.030.080.030.070.490.01

F00000358F00000360F00000361F00000362F00000363F00000364F00000366F00000368F00000369F00000371F00000372F00000373F00000374F00000375F00000376F00000377F00000378F00000380F00000381F00000382F00000383F00000384F00000385F00000386F00000387F00000388F00000389F00000391F00000392F00000394F00000396F00000397F00000398F00000399F00000400F00000401F00000402F00000404F00000405F00000406F00000407F00000408F00000409F00000411F00000412F00000413F00000414F00000415F00000416F00000417F00000418F00000420

Depth(m)


GL-17-003 3 of 4 3210 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

320

300

0.880.1

0.050.0050.18

F00000421F00000422F00000423F00000424F00000426

Depth(m)


GL-17-003 4 of 4 3210 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

80

60

40

20

0 casing set at 14m in highly fractured rock with only moderate water return; drilling cored from 11.71m; rod count at 95m; back oriented to top of hole from correct depth at 95m coring depth

fg-mg; light gray; massive grd that is highly fractured and displays ridge-and-groove slickensides and well developed slickenfibres parallel and oblique to the core axis and fractures; fractures are longitudinal near parallel TCA; fault zone

Fsp-porphyry with plag>kspr; fg groundmass of qtz-bio-mt and 1.0-1.5% disseminated py grains; subhedral to euhedral plag at 10-15%; subhedral kspr is 5-10%; sharp irregular upper and lower intrusive contactsfg-mg light gray to darker gray; sil-chl-mt altered grd; relatively competent rock with

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.05

0.0050.02

0.0050.1

0.0050.030.1

0.390.040.01

0.0050.2

0.0050.0050.0050.030.31

0.0050.01

0.0050.01

0.0050.0050.010.010.18


Depth(m)




Start Date: March-02-17End Date: March-06-17Drill Contractor: Rodren Drilling



Project: GoldlundLogged by: John CamierLog Completed: March-06-17Core Location: TENT

GL-17-004 1 of 3 3210 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

and qtz-carb veins some of which display sil-kspr-alb alteration haloes supporting cg py min

0.070.030.420.130.580.060.080.03

0.0050.0050.59

0.0050.220.170.13

0.0050.0050.37

0.0052.890.020.070.05

0.0050.080.69

0.0050.08

0.0050.0050.520.020.010.2

0.180.041.490.01

0.0050.04

0.0050.0050.040.250.210.050.130.15

0.0050.050.02


Depth(m)


GL-17-004 2 of 3 3210 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

260

240

220

200

cg fsp porphyry (plag ~70%) with subhedral to euhedral plag phenocrysts supported in a fg bluish qtz + mt + bio matrix that has been ankerite altered; with weak ser alteration to fsp; sharp contactsfg-mg light gray massive grd in sharp contact with upper porphyry unit and brecciated lower contact with protomylonitic (sheared) strongly chl-ank-carb altered maficstrongly schistose (protomylonitic) silicified mafic unit (and) with schistosity at 20 degTCA; unit may be a xenolith caught in grd-mafic contact zone; brecciated lower contactfg-mg light gray massive grd in sharp brecciated contact with mafic unitmg fsp porphyry (plag~60-70%) minor kspr phenocrysts supported in a vfg-fg bluish qtz-mt-bio matrix; EOH at 257.0m

0.160.070.020.09

0.0050.050.5

0.110.020.140.040.060.520.050.030.020.010.320.2

0.040.0050.040.040.080.4

0.020.23

0.0050.005

0.00250.00250.0320.005

F00013308F00013309F00013310F00013311F00013312F00013313F00013314F00013316F00013317F00013318F00013319F00013321F00013323F00013324F00013325F00013326F00013327F00013328F00013329F00013330F00013331F00013332F00013333F00013334F00013336F00013337F00013338F00013339F00013341F00013342F00013343F00013344F00013345

Depth(m)


GL-17-004 3 of 3 3210 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

40

0

Magnetic. 0.0050.0050.0050.02

0.0050.0050.967.910.250.070.030.30.22.71.9

0.020.160.060.1

0.050.790.01

0.0050.680.1

0.310.020.55

0.0050.0056.650.190.030.050.061.550.07

0.0050.005


Depth(m)



Casing Depth: 13.5 mEOH: 656 m




Project: GoldlundLogged by: Harvey BuckLog Completed: March-17-17Core Location: TENT

GL-17-005 1 of 7 151050 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

160

120

Lower contact is highly irregular and possibly partly sheeted; angle at last section of contact; magneticLower contact is slightly undulatingLower contact is very slightly undulating; magnetic

Lower contact is highly irregular; medium angle to core accessLower contact is slightly irregular; but easily readable; magnetic

0.010.070.11

0.0050.0050.03

0.00514.660.070.010.06

0.0050.970.470.070.97

15.830.042.330.040.020.020.120.040.010.140.030.140.080.490.040.3

1.532.1

12.670.150.090.070.120.130.020.070.430.130.040.040.040.560.080.080.430.030.1

F00000696F00000697F00000698

F00000699AF00000701AF00000702AF00000703AF00000704AF00000706AF00000707AF00000708AF00000709AF00000711AF00000712F00000713F00000714F00000716F00000717F00000718F00000719F00000720F00000721F00000722F00000723F00000724F00000725F00000726F00000727F00000728F00000729F00000731F00000733F00000734F00000736F00000737F00000738F00000739F00000740F00000741F00000742F00000744F00000745F00000746F00000747F00000748F00000749F00000751F00000752F00000753F00000754F00000755F00000757F00000758

Depth(m)


GL-17-005 2 of 7 151050 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

280

240

200

0.490.0050.080.040.020.240.080.060.010.050.01

0.00515.480.090.020.060.07

0.0050.190.020.01

0.0050.09

0.0050.060.060.060.02

0.0050.051.270.170.040.09

0.0050.931.520.060.02

42.150.3

0.010.010.44

0.0050.0050.49

0.0050.041.970.11


Depth(m)


GL-17-005 3 of 7 151050 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

360

320

0.450.0050.150.090.17

0.0050.05

0.0050.030.35

0.0050.02

0.0050.0050.0050.180.040.030.03

0.0050.0050.750.08

0.0050.0050.0050.04

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.02

0.0050.01

0.0050.04

0.0050.0050.010.060.01

0.0050.0050.210.01


Depth(m)


GL-17-005 4 of 7 151050 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

480

440

400

Mafic dyke; has a small xenolith near the downhole contact; nonmagneticSmall mafic dyke between 430.05-430.15 m; Grd is magnetic; mafic dyke is not magnetic; well mineralized 548-575.5 m; highly altered andesite between 586.25 and 587.0 m with mostly sharp; highly irregular contact at 2-3 degrees; section mostly granodiorite; lower contact undulating and partly irregular; approx. 22 degrees

0.0050.0050.0050.0050.0050.02

0.0050.02

0.0050.14

0.0050.67

0.0050.0050.0050.0050.01

0.0050.0050.0050.060.1

0.020.451.31

0.0050.0050.0050.040.030.030.020.021.170.12

0.0050.0050.0050.0050.231.360.440.020.010.030.04

0.0050.070.06

0.0050.05


Depth(m)


GL-17-005 5 of 7 151050 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

600

560

520

Possible stretched amygdules in the centre of the unit; lower contact is slightly undulating

0.0050.0050.350.2

0.0050.0050.0050.0050.04

0.0050.0050.0050.0050.0050.29

0.0050.01

0.0050.0050.020.330.260.110.170.7

0.480.690.470.271.651.571.3

0.711.040.998.070.252.680.670.10.1

0.090.27

0.0050.0050.030.04

0.0050.0050.060.02


Depth(m)


GL-17-005 6 of 7 151050 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

680

640

Possible pillow selvages at 617.3; 621.9; 622.3; 622.9; 629.45 and 629.65; possible amygdules at 622.9; 629.9; 630.1 and 630.4; lower contact is slightly irregular

Lower contact is indistinct in strong alteration and is taken at a quartz vein which appears to be the contact; lowermost 1.1 m is strongly bleached; zone is generally very weakly magnetic

Lower contact was not drilled; bimodal feldspar crystals to 17 mm long; end of hole

3.860.050.490.150.110.170.03

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005

F00013405F00013406F00013407F00013408F00013409F00013411F00013413F00013414F00013416F00013417F00013418F00013420F00013421F00013422F00013423F00013424F00013425F00013426F00013427F00013428F00013429F00013431F00013433F00013434F00013436F00013437F00013438F00013439F00013440

Depth(m)


GL-17-005 7 of 7 151050 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

80

60

40

20

0

Lower contact is undulating;

Lower contact is slightly irregular and very weakly undulating; porphyry is weakly magnetic and moderately bimodalLower contact is sharp and highly irregular; approximately 10 or so degrees??; granodiorite is magnetic

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.01

0.0050.0050.0050.030.010.020.030.080.02

0.0050.0050.0050.47

F00000851F00000852F00000853F00000854F00000855F00000856F00000857F00000858F00000859F00000860F00000861F00000862F00000864F00000865F00000866F00000867F00000868F00000869F00000871F00000872F00000873F00000876F00000877F00000878F00000879F00000880F00000881F00000882F00000883F00000884F00000885F00000886F00000888F00000889F00000891F00000892F00000893F00000894F00000895F00000896F00000897F00000898

Depth(m)








GL-17-006 1 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

180

160

140

120

100

lower contact is sharp; slightly undulating and has a sliver of Granodiorite xenolith paralleling it; nonmagnetic; very weakly bimodal; highly seritized; bleached; altered; about 35% groundmass lacking larger feldspar crystal; which in places are much lower from alteration

Lower contact is straight; granodiorite is magnetic;

Lower contact is straight; feldspar porphyry is nonmagnetic and strongly bimodalfg to mg light greenish gray granodiorite (tonalitic) with fg albitic plag; blueish qtz eyes and groundmass matrix; with interstitial chl

0.0050.89

0.0050.26

0.0050.0050.0050.020.060.55

0.0050.040.860.4

1.830.070.070.05

0.0050.061.32

0.0050.0050.0050.0050.01

0.0050.0050.0050.02

0.0050.32

0.0050.650.280.020.380.050.2

0.030.520.050.020.050.080.05

23.340.31

0.0050.05


Depth(m)


GL-17-006 2 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

280

260

240

220

200

mt that displays a moderate to locally strong magnetism in groundmass; EOH at 326.0m

0.0050.260.4

0.040.06

0.0050.0050.310.490.5

0.120.180.020.130.140.020.080.160.030.060.040.230.050.050.061.990.010.010.060.190.14

0.0050.190.7

0.0050.010.040.010.1

1.070.010.020.03

0.0050.020.830.07

0.0050.020.860.21


Depth(m)


GL-17-006 3 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

340

320

300

0.091.640.190.04

0.0050.180.030.120.030.7

0.690.77

0.0050.0050.510.29

F00001020F00001021F00001022F00001023F00001024F00001026F00001028F00001029F00001031F00001032F00001033F00001034F00001035F00001036F00001037F00001038

Depth(m)


GL-17-006 4 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

80

60

40

20

0

medium olive green to greenish gray to light greenish gray in strongly silicified sections near lower contact; unit comprised of alternating mafic flows and tuffs; strongly foliated and metamorphosed; intensely chloritized and carb altered; unit is variably magnetic with subhedral mt grains supported in the chloritic greenschist groundmass

light greenish gray massive flow banded grd with >30% blue qtz eyes supported in a fg greenish gray groundmass of interstitial chl-mt-fspfeldspar porphyry with 35-40% white plag with albite twining; 20-25% pinkish kspr with minor

0.0140.01

0.00250.00250.00250.0050.390.04

0.0050.0050.005

F00001051F00001052F00001053F00001054F00001055F00001056F00001057F00001058F00001059F00001060F00001061

Depth(m)








GL-17-007 1 of 4 7550250 100% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

180

160

140

120

100

qtzo-feldspathic-amph-mt-bio groundmass with disseminated fg sulphideslight greenish gray massive flow banded grd with >30% blue qtz eyes supported in a fg greenish gray groundmass of interstitial chl-mt-fsp

dark purple gray to reddish/pinkish brown cg to fg feldspar porphyry with >50% euhedral to subhedral albitic plag intermixed with kspr that occasionally display rapakivi textures of alternating plag-kspr growth zonations in large xtalslight greenish gray massive occasionally flow banded grd with 10-30% blue qtz eyes supported in a fg greenish gray groundmass of interstitial chl-mt-fsp

0.060.0051.551.290.08

0.0050.06

0.0050.55

0.0050.19

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.44

0.0050.0050.0050.0050.010.020.940.1

2.340.020.9

0.080.03

0.0050.0050.030.010.340.160.110.020.110.030.090.040.690.1

0.060.22

F00001062F00001063F00001064F00001065F00001066F00001067

F00001068AF00001069AF00001071AF00001072AF00001073AF00001074AF00001076AF00001077F00001078F00001079F00001080F00001081F00001082F00001083F00001084F00001085F00001086F00001087F00001088F00001089F00001091F00001092F00001093F00001094F00001096F00001097F00001098F00001099F00001101F00001102F00001103F00001104F00001106F00001107F00001108F00001109F00001111F00001112F00001113F00001114F00001115F00001117F00001118F00001119F00001120

Depth(m)


GL-17-007 2 of 4 7550250 100% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

280

260

240

220

200

0.580.710.240.010.350.070.080.212.740.072.610.110.930.590.580.03

0.0050.005

0.20.080.44.7

0.090.070.02

0.0050.150.040.250.030.030.010.040.250.2

0.410.110.04

0.0051.830.01

0.0050.0050.750.020.020.040.030.75

0.0050.16


Depth(m)


GL-17-007 3 of 4 7550250 100% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

300

Depth(m)


GL-17-007 4 of 4 7550250 100% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

80

60

40

20

0

medium olive green fg massive intensely chloritized andesite; schistose groundmass comprised of vfg to fg felty masses of chlorite + act/trem + carb (cal) + vfg mt + qtz + vfg euhedral to subhedral plag + diss sulphides (py +/- ccp)

60-75% subhedral to euhedral greenish to white plag with occasional overgrowths of kspr with plag cores set in a dark chlorite altered vfg qtzo-feldspathic + bio + mt + sulphide (tr-0.5% locally) groundmassmedium olive green fg massive intensely chloritized andesite; schistose groundmass comprised of vfg to fg felty masses of chlorite + act/trem + carb (cal) + vfg mt + qtz + vfg euhedral to subhedral plag + diss sulphides (py +/- ccp)medium to dark olive green intensely chloritized massive gabbro with cg completely chloritized pyx and amph set in a fg massive weakly schistose chlorite-act/trem + sulphide (trace py-ccp) groundmassmedium olive green fg massive intensely chloritized andesite; schistose groundmass comprised of vfg to fg felty masses of chlorite + act/trem + carb (cal) + vfg mt + qtz + vfg euhedral to subhedral plag + diss sulphides (py +/- ccp)medium to dark olive green intensely chloritized massive gabbro with cg completely chloritized pyx and amph set in a fg massive weakly schistose chlorite-act/trem + sulphide (trace py-ccp) groundmass

medium olive green; intensely chloritized variolitic textured with elongated carbonate spherulites parallel to foliation (schistosity) set

Depth(m)








GL-17-008 1 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

crosscut by carb veinlets and displaying fold textures; including a fold nose 112.50m; unit grades into tuffaceous silicified tuffs +/- argillaceous vol seds then back into vesicular mafic rocks; lower contact sharp and structural

light gray fg-mg chloritized grd 10-15%+; 1-2(+)mm sized blue qtz eyes supported in a darker gray vfg to fg qtzo-feldspathic + mt + act/trem + plag groundmass with interstitial moderate chl-alteration to ferro-magnesian minerals plus disseminated vfg-fg sulphides of py +/- polight grayish green silicified andesite as described between 82.10m and 115.02m

light greenish gray fg-mg chloritized grd with occasional light whitish gray subrounded tonalite xenoliths supported within the grd groundmass displaying medium gray alteration rims; a 2.4m wide zone of propylitization occurs between 178.3-180.7m depth with strong cte and euhedral py as fracture fillings; zone of qtz + qtz-carb veining occurs below 278.2 to 297m depth; hole ended at 300.0m in brittle fault

0.00250.00250.009

0.00250.1

0.090.0050.020.03

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.670.030.11

0.0050.01

F00001184F00001185F00001186F00001187F00001188F00001189F00001190F00001191F00001193F00001194F00001195F00001196F00001197F00001198F00001199F00001200F00001201F00001202F00001204F00001205F00001207F00001209F00001210F00001211F00001212F00001213F00001214F00001216F00001217F00001218F00001219F00001220F00001221F00001222F00001224F00001225F00001226F00001227F00001228F00001230F00001231F00001232F00001233

Depth(m)


GL-17-008 2 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

0.0050.0050.0050.84

0.0050.0051.050.020.02

0.0050.0050.005

0.10.0050.0050.020.042.25

0.0050.0053.33

0.0050.0050.010.020.26

0.0050.0050.0050.99

0.0050.0051.280.260.070.010.6

0.050.04

0.0050.0050.03

0.0050.0050.020.060.47

0.0050.0053.690.050.050.39

F00001234F00001235F00001236F00001237F00001239F00001240F00001242F00001244F00001245F00001246F00001247F00001248F00001249F00001250F00001251F00001252F00001253F00001255F00001256F00001257F00001258F00001259F00001260F00001261F00001262F00001264F00001265F00001267F00001269F00001270F00001271F00001272F00001273F00001274F00001275F00001277

F00001278AF00001279AF00001280AF00001281AF00001282AF00001284AF00001285AF00001286AF00001287AF00001288AF00001290F00001291F00001292F00001293F00001294F00001295

Depth(m)


GL-17-008 3 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

300

0.030.030.040.030.12

F00001296F00001297F00001299F00001300F00001301F00001302

Depth(m)


GL-17-008 4 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

40

0

fine grained; greenish grey granodiorite. Pervasive chlorite and silica alteration; with sil/kspr alt haloes around Q; QA veins. 1-2% fine grained dis py and po. Several faults within unit

fine grained; dark green vesicular Andesite (basalt). Chlorite and Carb altered. Visible leucoxenesfine grained; greenish grey granodiorite. Pervasive chlorite and silica alteration; localized sil/kspr alt haloes around Q; QA veins. 1-2% fine grained dis py and po; trace-1% FF py and po within QA veins

0.0051.45

0.0050.040.010.051.410.050.021.660.020.170.180.140.160.170.5

0.520.1

0.020.191.070.020.61

0.0050.0050.0050.020.040.020.02

0.0050.0050.0050.0050.02

0.0050.0050.0050.02


Depth(m)







Project: GoldlundLogged by: Joseph WiebeLog Completed: March-30-17Core Location: TENT

GL-17-010 1 of 7 6040200 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

160

120

fine grained; pillowed amygdular green andesite (basalt)fine grained; greenish grey granodiorite. Pervasive chlorite and silica alteration; with localized carb/hem alt and localized sil/kspr alt haloes around Q; QA veins. 1-2% fine grained dis py and po; trace-1% FF py and po within QA veins. Localized in situ Bxcoarse grained grey quartz feldspar porphyry. 1% dis py. Sharp upper and lower contactsfine grained; blueish grey granodiorite. Pervasive silica and chlorite alteration; with localized sil/kspr alt haloes around Q; QA veins. 1-2% fine grained dis py; 2% FF and Cx py within QA veins and alt haloes. Localized offset of Q; QA veins and localized in situ brecciation. Several fault/shear zones. Localized foliation

0.350.16

0.0050.050.04

0.0050.0050.0050.0050.0050.0050.0050.09

0.0050.290.070.020.07

0.0050.17

0.0050.120.040.07

0.280.005

0.20.01

0.0050.0050.0050.0050.0050.020.030.02

0.0050.13

0.0050.0050.050.02

0.0050.050.040.090.241.2

0.080.030.010.07


Depth(m)


GL-17-010 2 of 7 6040200 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

280

240

200

Added by BB by core photos

0.030.060.190.2

0.0050.0050.080.190.180.06

0.0050.2

0.010.240.130.020.240.020.12

0.0050.060.160.010.02

0.0050.060.090.010.04

0.0050.432.620.11

0.0050.170.14

0.0050.010.050.120.06

0.0050.040.230.360.412.45

0.0050.0050.05

0.005


Depth(m)


GL-17-010 3 of 7 6040200 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

360

320

fg pale grey grd; pervasive silica/chl alteration; sil/kspr alteration halos - strong around QA veins; fg chl-mt-bt-carb in groundmass; approx. 2m contact zone with blocks of AND and GRD; brecciated portions of GRD

very fine grained mafic rock; groundmass chl-bt with fg feldspars; extensive chl-bt-carb alteration; carbonate filled amygdules over 3m in middle of interval

pale grey; fg; minimal veining and mineralization; sil/carb pervasive alteration; interstitial chl-carb-bt

dark greenish grey; stretched amygdules

0.0050.0050.0050.04

0.03

F00013621F00013622F00013623F00013624F00013626

Depth(m)


GL-17-010 4 of 7 6040200 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

480

440

400pale grey; fg; predominately qc veins with some qa; sil/carb pervasive alteration; interstitial chl-carb-bt; occasional pervasive kspar/hem

Depth(m)


GL-17-010 5 of 7 6040200 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

600

560

520

margin -> microliteslight gray to medium gray grd with minor qtz veins to 538.5m depth where qtz veins and alteration halos become plentiful with some VG occurring along vein walls and associated with sulphides; local sulphides within the haloes are between 10-25% with several fracture filling and massive veins of bright pyrite

Depth(m)


GL-17-010 6 of 7 6040200 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

640

fg to mg glassy sheared fsp porphyry with strong silica and potassic alterationlight gray fg-mg granodioritefg amygdaloidal silicified and chloritized andesitic unit - possible xenolithlight gray fg-mg granodioritefg massive light grayish green gabbro; moderately chloritized and silicified

Depth(m)


GL-17-010 7 of 7 6040200 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

Fine grained; blueish grey; chlorite/sil altered granodiorite. 1-2% dis py and FF py around veins/veinlets. Unit has a fault running through it. Localized foliation; localized ptygmatic folding of veinlets and localized offset of stringers/veins

blueish grey coarse grained Quartz-feldspar POR; sharp upper and lower contacts. Coarse grained phenocrysts within a fine grained matrix. Minor chlorite alt. 1% py mineralizationfine grained dark green amygdaloidal andesite. Contains carbonate stringers. Sharp upper and lower contacts

Fine grained; blueish grey; chlorite/sil altered granodiorite. Mineralization occurs predominantly around massive quartz and

0.010.02

0.0050.0050.0050.010.040.040.05

0.0050.0050.0050.030.03

0.0050.240.312.460.020.040.850.060.060.19

0.0050.16

0.010.0050.040.01

0.0050.0050.0050.0050.010.02

0.0050.0050.005


Depth(m)







Project: GoldlundLogged by: Joseph WiebeLog Completed: April-01-17Core Location: TENT

GL-17-011 1 of 2 2

1.751.

5

1.251 3

2.52

% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

160

150

140

130

120

110

100

haloes. BQE's throughout. Sheared; mylonitic zone at around 140m approx. 80cm's long; contains lithic fragment of Andesite.

Fine grained; green; chlorite altered Andesite (Basalt). Contains autocataclastic lapilli's

0.0050.0050.010.040.020.13

0.0050.0050.040.040.120.020.040.050.040.630.120.120.230.080.03

0.0050.070.270.250.55

0.0050.0050.0050.01

0.0025

F00013696F00013697F00013698F00013699F00013701F00013702F00013703F00013704F00013706F00013707F00013709F00013711F00013712F00013713F00013714F00013715F00013716F00013717F00013718F00013719F00013720F00013721F00013722F00013723F00013724F00013726F00013727F00013728F00013729F00013731F00013732

Depth(m)


GL-17-011 2 of 2 2

1.751.

5

1.251 3

2.52

% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

80

60

40

20

0

fine grained; greenish blue grey; pervasive silica/chlorite altered granodiorite. Blue quartz eyes throughout. moderate-Strongly magnetic. Locally foliated; faulted and sheared. Contains few massive quartz veins; crosscut by calcite stringers. Crosscut by >1m Por. Sharp lower contact

coarse grained feldspar-quartz phenocrysts in a fine grained matrix. Euhedral-subhedral crystal faces. 60%-40% feldspar-quartz. Chlorite and kspar alteration. Sharp lower contactfine grained; greenish blue grey; pervasive silica/chlorite altered granodiorite. Blue quartz eyes throughout. Moderate-strongly magnetic. 50cm portion of mylonitic grd. Locally foliated; faulted and sheared. Foliation planes range from 50 degrees tca to sub parallel to core axis. Contains few massive quartz veins; crosscut by calcite stringers. Crosscut by Por. Sharp lower contact

coarse grained quartz-feldspar phenocrysts in a fine grained matrix. Crosscut by granodiorite xenoliths and massive quartz carbonate biotite veins set in a kspar alteration halo. 2% dis and FF py

fine grained; greenish blue grey; pervasive silica/chlorite altered granodiorite. Blue quartz

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.01

0.0050.0050.0050.030.030.1

0.120.090.050.070.330.11

0.005


Depth(m)








GL-17-012 1 of 4 2

1.51

0.50 3

2.52

% % %

Angle toCore Axis3.

532.

52

%

10.

750.5

0.250

180

160

140

120

100

magnetic. Contains few massive quartz veins; crosscut by calcite stringers. Sharp lower contact

Fine grained; dark greenish grey; pervasive sil altered; amygdaloidal Andesite (basalt). Crosscut by carbonate veinlets/stringers at irregular orientations. Trace dis py. Sharp upper and lower contactsfine grained; greenish blue grey; pervasive silica/chlorite altered granodiorite. Blue quartz eyes throughout. Moderate-strongly magnetic. Contains few massive quartz veins; crosscut by calcite stringers. Several faults running through. Sharp lower contact

0.020.0050.0050.04

0.0050.070.21

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.11

0.0050.29

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.03

0.005

0.005

0.040.040.020.640.090.01


F00013847F00013848F00013851F00013852F00013853F00013854F00013855

Depth(m)


GL-17-012 2 of 4 2

1.51

0.50 3

2.52

% % %

Angle toCore Axis3.

532.

52

%

10.

750.5

0.250

280

260

240

220

200

0.060.050.13

0.0050.380.375.021.050.010.02

0.0050.060.110.20.1

0.020.020.030.160.140.040.150.030.03

0.0050.0050.0051.52

0.005

0.050.010.02

0.0050.0050.0050.0050.0050.01

0.0050.0050.0050.005

0.40.020.410.030.350.010.050.03


Depth(m)


GL-17-012 3 of 4 2

1.51

0.50 3

2.52

% % %

Angle toCore Axis3.

532.

52

%

10.

750.5

0.250

300

0.0050.050.02

F00013918F00013919F00013920

Depth(m)


GL-17-012 4 of 4 2

1.51

0.50 3

2.52

% % %

Angle toCore Axis3.

532.

52

%

10.

750.5

0.250

80

60

40

20

0

0.010.040.040.080.020.050.01

0.0050.0050.0050.0050.0050.0050.02

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.010.034.040.070.091.760.2

0.040.0050.04

F00013921F00013922F00013923F00013924F00013925F00013926F00013927F00013929F00013930F00013931F00013932F00013933F00013934F00013935F00013936F00013937F00013938F00013939F00013941F00013943F00013944F00013946F00013947F00013948F00013949F00013950F00013951F00013952F00013953F00013954F00013955F00013956F00013958F00013959F00013960F00013961F00013962F00013963

Depth(m)







Project: GoldlundLogged by: Adam RichardsonLog Completed: April-09-17Core Location: TENT

GL-17-013 1 of 3 3210 1

0.50

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

0.0050.0050.0050.0050.0050.0050.02

0.0050.06

0.0050.0050.04

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.25

0.0050.0050.060.04

0.0050.0050.020.020.4

0.030.0050.020.050.010.030.022.690.01

0.0050.030.050.020.020.02

0.0050.0050.090.070.04


Depth(m)


GL-17-013 2 of 3 3210 1

0.50

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

0.010.0050.0050.020.020.010.040.07

0.0050.240.040.03

0.0050.0050.0050.020.09

0.0050.060.070.070.050.120.110.110.07

0.0050.230.020.030.260.060.110.340.050.2

0.180.641.5

0.080.6

2.92


Depth(m)


GL-17-013 3 of 3 3210 1

0.50

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

green; fine grained; weakly to moderately foliated; pervasively chloritic with trace to locally 1% fg dis pyrite and fg trace magnetite throughout.

green; very similar to above unit but has 1-2% fine grained blue quartz porphyroblasts

green; fine grained; as above minus the blue qtz. Likely a basalt

grey green feldspar porphyry sharp upper and lower contact

very fine grained; greyish green ""andesite"". Likely interflow sediments as well

as above porphyry unit

fine grained granodiorite with blue quartz

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.020.01

0.0050.020.141.45


Depth(m)







Project: GoldlundLogged by: Adam RichardsonLog Completed: March-11-17Core Location: TENT

GL-17-014 1 of 4 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

0.0050.0050.0050.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.99

0.0050.010.080.010.090.020.230.010.03

0.0050.040.010.190.030.030.210.010.070.010.060.010.090.020.040.170.02


Depth(m)


GL-17-014 2 of 4 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

0.430.470.210.150.120.240.130.120.640.3

0.040.030.010.030.010.760.080.040.190.1

0.0058.790.040.440.72

0.0050.320.120.050.250.02

0.0050.040.2

0.030.030.180.410.04

91.630.160.130.10.3

0.110.030.080.2

2.450.230.05


Depth(m)


GL-17-014 3 of 4 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

380

360

340

320

300

fine grained granodiorite; moderate pervasive chlorite alteration

0.040.040.040.020.380.160.080.3

0.010.320.020.02

0.0050.0050.020.040.020.1

0.0050.04

0.0050.0050.570.1

1.210.390.530.020.05

0.0050.030.43

0.00250.00250.00250.00250.00250.0025


Depth(m)


GL-17-014 4 of 4 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

Lower contact obscured in rubble; contact angle is the joint angleBlue Quartz Eye; gradational boundary occurs until 83.41

very fine grained; dark green colour; amygdules concentrated around salvages

0.260.130.030.450.02

0.0050.0050.0050.0050.030.08

0.0050.040.030.050.190.042.55

0.0050.190.320.060.030.020.190.210.112.090.16

0.0050.0050.020.05

0.0050.0050.0050.0050.0050.0050.005

0.00250.0025


Depth(m)




Start Date: January-20-17End Date: January-23-17Drill Contractor: Rodren Drilling



Project: GoldlundLogged by: Andrew WiebeLog Completed: January-23-17Core Location: TENT

GL-17-016 1 of 2 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

160

150

140

130

120

110

100

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.006

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.0025


Depth(m)


GL-17-016 2 of 2 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

xenoliths of GRD in POR; wavy contact trending 15 deg but with well defined boundaries

0.130.0050.083.620.530.340.030.6

1.220.080.070.280.16

12.740.043.610.070.1

0.590.0050.270.150.040.450.610.050.360.43

0.0050.090.020.01

0.0050.0051.34

0.0050.02

0.0050.150.010.070.040.18


Depth(m)








GL-17-017 1 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

0.0050.01

0.0050.0050.0050.03

0.0050.027.380.031.310.130.440.2

0.0050.010.08

0.0050.0050.08

0.0050.091.020.060.550.050.02

0.0050.2

0.020.0050.0050.06

0.0050.040.08

0.0050.020.3

0.020.040.460.030.011.430.180.020.030.041.420.08


F00002745AF00002746AF00002747AF00002748AF00002749AF00002751AF00002752AF00002753AF00002754AF00002755AF00002756F00002757F00002758F00002760F00002761

Depth(m)


GL-17-017 2 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

xenoliths of GRD in POR; wavy contact trending 15 deg but with well defined boundaries

0.020.030.030.020.040.020.420.390.1

0.660.160.2

0.150.050.720.250.010.020.020.150.270.1

0.370.050.5

1.720.040.05

0.0050.03

0.0050.01

0.0050.240.010.020.02

0.0050.090.020.04

0.0050.030.04

0.0050.0050.0050.040.020.060.04


Depth(m)


GL-17-017 3 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

320

300

0.090.05

0.0050.005

F00002823F00002824F00002826F00002827

Depth(m)


GL-17-017 4 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

0.120.11

0.0050.0050.0050.0050.120.030.020.090.011.2

0.360.022.67

0.0050.04

0.0050.11

0.0050.370.130.420.970.480.020.550.480.160.020.483.260.160.140.010.780.120.020.080.090.06

F00002851F00002852F00002853F00002854F00002856F00002857F00002858F00002859F00002860F00002861F00002862F00002863

F00002865AF00002866AF00002867AF00002868AF00002869AF00002871AF00002872AF00002873AF00002874AF00002875AF00002876F00002878F00002879F00002880F00002881F00002882F00002883F00002884F00002886F00002887F00002889F00002891F00002892F00002893F00002894F00002895F00002896F00002897F00002898

Depth(m)








GL-17-018 1 of 2 151050 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

150

140

130

120

110

100

Blue Quartz Eyes alteration

very fine grained; dark green pillows with well defined pillow salvages up to 3cm.

0.120.790.130.060.12

0.0050.040.330.133.530.170.02

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005

0.005


Depth(m)


GL-17-018 2 of 2 151050 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

80

60

40

20

0

No visible salvages; amygdules evenly distributed/carbonate filledFine grained GRD; Blue Quartz Eyes; felsic xenolith at 20.60m; very little ore mineralization

extensive pink colour from K-spar throughout POR; trace chlorite and tourmalinefelsic xenolith at 34.85m; very little ore mineralization; one blue qtz eye observed at 89.08; Qtz Alk. POR inclusion (xenolith?) at 89.0m same lithology as POR unit from 89.96 to 93.20

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.02

0.0050.0050.0050.0050.0050.0050.06

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005

F00002951F00002952F00002953F00002954F00002955F00002956F00002957F00002958F00002959F00002960F00002962F00002963F00002964F00002965F00002966F00002967F00002968F00002969F00002971F00002973F00002974F00002976F00002977F00002978F00002979F00002980F00002981F00002982F00002983F00002985F00002986F00002987F00002988F00002989F00002991F00002992F00002993F00002994F00002995F00002996F00002997

Depth(m)




Start Date: January-29-17End Date: February-05-17Drill Contractor: Rodren Drilling



Project: GoldlundLogged by: Andrew WiebeLog Completed: February-05-17Core Location: TENT

GL-17-019 1 of 4 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

GRD xenolith in POR at lower contact 0.050.0050.0050.0050.0050.0050.0050.0050.080.110.02

0.0050.0050.005

0.70.490.210.4

0.050.04

0.0050.050.02

0.0050.0050.05

0.0050.0050.070.040.030.5

0.160.020.61

0.0050.0050.061.152.480.280.010.01

0.0050.26

0.0050.020.070.060.080.01


Depth(m)


GL-17-019 2 of 4 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

contact is along rock jointirregular lower contact

irregular upper and lower contactfine to med grained with 10% larger qtz phenos to 5mmfine grained

0.040.0050.170.02

0.0050.070.070.010.060.020.040.16

0.0050.060.1

0.150.142.360.220.37

0.0050.040.030.01

0.0050.01

0.0050.050.060.050.020.020.450.020.95

0.0050.030.140.080.060.130.040.02

0.0050.0050.020.140.220.5

0.290.24


Depth(m)


GL-17-019 3 of 4 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

380

360

340

320

300

fine grained; shallow irreg upper and lower contactirregular and undulating contacts; may be a large inclusion of GD between adjacent porphyry units20% phenos 5-10mm in finer grained groundmass; undulating LCfine grained; dark; bluish to blue qtz; weak foliation; ; irregular lower contact with porphyry

plag phenos to 12mm; qtz generally 2-4mmfine grained; numerous irregular qtz-ank +/- albite stringers and veinlets generally shallow to locally 40 deg TCA; 10-15% small blue qtz; lower contact irregular and shallowfspar phenos to 10mm; intensely altered 331.5-334.3 with silica flooding and k; several angular fg GD xenolithslower contact semi regular; porphyry remnant 2X20cmlocal mod foliation 30 deg TCA15% small blue qtzfine to medium grained andesite; numerous qtz-ank stringerswith small blue qtz; lower contact shallow and irregular5-7% locally 10-15% small blue quartzmedium to coarse andesite; frequent primary qtz-carb stringers and irregular veinlets; locally weakly foliated

0.0050.0050.0050.0050.04

0.0050.05

0.0050.0050.0050.02

0.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005


Depth(m)


GL-17-019 4 of 4 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

medium to locally fine grained; weak to locally moderate foliation; decreasing to weakly foliated patches @40m; small blue qtz eyes

10cm mass QV at contact with porphyry

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.120.060.420.03

0.0050.430.020.020.130.020.12


Depth(m)




Start Date: February-05-17End Date: February-12-17Drill Contractor: Rodren Drilling



Project: GoldlundLogged by: Richard KowalskiLog Completed: February-12-17Core Location: TENT

GL-17-021 1 of 5 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

strongly to intensely silica flooded; UC is irregular and comprised of 50% porphyry and 50% GD as xenoliths of varying size; lower contact shallow and irregular

0.0050.031.91

0.0050.0050.0050.070.08

0.0050.0050.0050.040.05

0.0050.0050.0050.0050.0050.0050.0050.0050.01

0.0050.030.020.070.130.060.08

0.0050.090.070.060.470.50.1

0.080.510.030.140.1

0.090.23

0.0058.110.060.08

0.0050.990.080.46


Depth(m)


GL-17-021 2 of 5 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

strong silica flooding

foliatedlocal fine grained intervals

0.10.421.070.040.01

43.090.060.520.040.250.090.1

0.040.030.050.050.060.070.080.080.020.590.110.120.14

0.0050.510.220.190.260.250.140.012.990.180.020.080.090.040.030.040.530.430.290.518.8

0.380.120.686.290.15

F00003461F00003462F00003463F00003464F00003465F00003467F00003468F00003469F00003472F00003473F00003474F00003475F00003476F00003477F00003478F00003479F00003480F00003481F00003482F00003484F00003485

F00003486AF00003487AF00003488AF00003489AF00003490AF00003492AF00003493AF00003495AF00003497AF00003498AF00003499F00003500F00003501F00003502F00003503F00003504F00003505F00003506F00003507F00003509F00003510F00003512F00003513F00003514F00003517F00003518F00003519F00003520F00003521F00003522

Depth(m)


GL-17-021 3 of 5 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

380

360

340

320

300

0.560.070.090.330.070.18

0.0050.030.020.24

0.0050.0050.08

0.0050.0050.250.09

0.0050.0050.02

0.0050.760.370.6

0.0050.0050.130.03

0.0050.390.880.660.030.130.110.38

0.0050.0050.0050.005

0.00250.00250.00250.00250.006

0.0025

F00003523F00003524

F00003525AF00003527AF00003528AF00003529AF00003530AF00003532AF00003533AF00003534AF00003537AF00003538AF00003539F00003540F00003541F00003542F00003543F00003544F00003545F00003546F00003547F00003548F00003550F00007801F00007802F00007803F00007804F00007805F00007807F00007808F00007810F00007812F00007813F00007814F00007815F00007816F00007818F00007819F00007820F00007821F00007822F00007823F00007824F00007825F00007826F00007827

Depth(m)


GL-17-021 4 of 5 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

400

Depth(m)


GL-17-021 5 of 5 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

very fine grained-fine grained (more FG than GRD); medium grey with purplish hue; dacite. Well defined banding. 30cm POR at 24.4m. QCCHL; and QC veins throughout. Localized boudinage of QC veins. Weak-moderately magnetic. Trace dis py

Fine-medium grained; dark green; chloritic

0.0050.03

0.0050.0050.15

0.0050.0050.0050.0050.0050.04

0.0050.0050.0050.0050.02

0.0050.230.142.050.41

0.0050.030.040.010.030.010.08

0.0050.06

0.0050.0050.0050.0050.0050.0050.0050.0050.005

0.0025


Depth(m)








GL-17-023 1 of 2 1

0.750.

5

0.25

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

140

130

120

110

100

and QC veins throughout. Localized boudinage of QC veins. Rare localized fold noses. Weak-moderately magnetic. Trace dis pyfine grained; grey granodiorite. Rare massive Q; QC; QCCHL veins with trace py mineralization. Localized fold nose with quartz-Kspar-sericite pressure shadow.

0.00250.011

0.00250.0510.0050.0050.0050.0050.030.01

0.0050.0050.01

0.0050.01

0.0050.0050.0050.005

0.005

F00008747F00008748F00008749F00008751F00008752F00008753F00008754F00008756F00008757F00008758F00008761F00008762F00008763F00008764F00008765F00008766F00008767F00008768F00008769F00008771

Depth(m)


GL-17-023 2 of 2 1

0.750.

5

0.25

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

fine to locally medium grained; dark; strongly chloritic gabbro (no gabbro in picklist so it's being labelled a ""diorite"") with fine grained primarily white feldspars and very rare fine grained quartz in a dark chloritic groundmass 1-3% fine grained magnetite common. Unit is weakly to moderately foliated and crosscut by hairline quartz-carbonate veins; some of which are folded.

green fine grained weakly to locally strongly foliated basalt(andesite).

fine grained; green; weakly to moderate pervasively chloritic blue quartz eye containing granodiorite. Trace to local 5%

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.012

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.0050.0050.0050.0050.0050.0050.0050.0050.0050.005


Depth(m)








GL-17-026 1 of 3 3210

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

190

180

170

160

150

140

130

120

110

100

pyrite. Rare vfg ccp. Fine grained mt throughout trace to 3%.

moderately foliated; moderately chloritic green andesite. Numerous crosscutting hairline calcite-quartz stringers. Trace to local 2% disseminated pyritegreen; fine grained weakly foliated blue quartz eye bearing granodiorite. Weak pervasive chlorite alteration; local minor k alt. Crosscut by calcite-quartz veins. Trace fg to vcg pyrite up to 5% local. Contact is in a quartz-calcite vein zone and is not clean.

fine grained; green; weakly to moderately chloritic foliated quartz-calcite vein bearing basalt (andesite). Rare flow contacts discernable (pillows).

fine grained unexpected blue quartz bearing granodiorite. pervasively weakly chloritized with trace to locally 1-2% fine grained disseminated and fracture fill pyrite. Sharp but undulating upper contact

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.03

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.010.060.01

2.0680.0950.0070.0080.005

0.00250.00250.00250.00250.006

0.00250.00250.00250.00250.00250.00250.00250.0150.0230.0090.009

0.0025

F00005113F00005114F00005115F00005117F00005118F00005119F00005120F00005121F00005122F00005123F00005124F00005125F00005126F00005127F00005128F00005129F00005131F00005132F00005133F00005134F00005136F00005137F00005138F00005139F00005140F00005141F00005142F00005143F00005145F00005146F00005147F00005148F00005149F00005150F00005151F00005152F00005153F00005155F00005157F00005158F00005160F00005161F00005162F00005163F00005164F00005166F00005167F00005168F00005169

Depth(m)


GL-17-026 2 of 3 3210

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

200

Depth(m)


GL-17-026 3 of 3 3210

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

fine grained pervasively weakly silicified with pervasive weak chlorite alteration of the groundmass. Trace to locally 2-5% fine grained and local coarse grained pyrite. Weakly foliated.

feldspar quartz porphyry. Coarse grained white feldspars with medium grained to coarse grained quartz in a chloritic groundmass. 1-2% disseminated fg pyrite. sharp upper and lower contacts.green fine grained blue quartz eye bearing granodiorite. Pervasively weak silicification and chlorite alteration. Trace to up to 2% local pyrite mainly fg disseminated. Weakly to locally well foliated.

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.260.07

0.0050.18

0.0050.0050.09

0.0050.0050.080.020.060.048.630.891.280.030.310.04

0.0050.0050.010.02

0.0050.0050.0050.0050.0050.02


F00005193AF00005194AF00005195AF00005196AF00005197AF00005199AF00005200AF00005201AF00005202AF00005204AF00005205F00005206F00005207F00005208F00005209F00005210F00005211F00005212F00005213F00005215

Depth(m)








GL-17-027 1 of 3 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100 very fine grained; green; weakly to moderately chlorite basalt. Top of unit is pillowed; going to a mix of pyroclastics (tuff and small fragments) and mafic flows. Very fine grained uniform flows with local amygdules with a lighter coloured; chaotic and softer interflow tuff. Unit is very weakly foliated and mineralized with pyrite and pyrrhotite

Very fine grained; weakly to moderately chloritic mafic flows with local small amygdules filled with calcite. Unit has flow contacts with epidote alteration. Mineralized by pyrite pyrrhotite and chalcopyrite. Very weakly foliated.

feldspar porphyry. Coarse euhedral to anhedral white feldspars in a dark chloritic matrixas above mafic flow unit.

0.020.0050.0050.0050.0050.0150.0130.01

0.0090.0050.0090.0090.01

0.0150.00250.0070.0190.0110.02

0.0110.019

0.00250.006

0.00250.0025

0.010.01

0.0070.011


Depth(m)


GL-17-027 2 of 3 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

220

200

Depth(m)


GL-17-027 3 of 3 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

fine grained; pervasive weak chloritic and silica alteration. Few xcutting quartz-tourm stringers. Trace to 1% f-cg dis and ff pyrite.

feldspar phenocrysts in a dark chloritic matrix. Upper and lower contacts are quartz veins with variable core anglesfine grained pervasive weak chloritic weakly to locally strongly sheared granodiorite. Local patchy k alteration. Few xcutting quartz veins with associated ankerite; tourmaline. Trace to local 1% fine grained disseminated pyrite and rare pyrrhotite.

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.03

0.0050.0050.32

0.0050.0050.0050.0050.24

0.0050.06

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.01


Depth(m)








GL-17-028 1 of 4 1

0.750.

5

0.250

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.050.24

0.0050.0050.0050.0050.05

0.0050.060.11

0.0050.0050.020.010.350.010.06

0.0050.072.1

0.482.130.050.021.110.020.020.090.140.380.530.530.020.030.040.130.040.014.650.17


Depth(m)


GL-17-028 2 of 4 1

0.750.

5

0.250

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

0.080.070.030.03120.2

0.220.880.020.020.070.240.230.460.050.870.03

14.640.040.020.242.73

0.0050.0050.030.530.11

0.0050.0050.032.48

0.0050.01

0.0050.340.040.68

0.0050.0051.370.310.190.260.021.14

0.0050.29

0.0050.320.050.13


Depth(m)


GL-17-028 3 of 4 1

0.750.

5

0.250

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

300

0.150.030.2

F00005423F00005424F00005425

Depth(m)


GL-17-028 4 of 4 1

0.750.

5

0.250

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

dark green; fine to medium grained; chloritic metamorphosed gabbro. Fine grained white feldspars with rare fine grained quartz in a dark chloritic groundmass. Weak-moderately magnetic. Weakly-moderately foliated and crosscut by hairline QC veins; localized folding and boudinage. Po replacing py throughout unit. locally visible fine grained dis magnetite crystals. Localized epidote within QC veins

0.0110.00250.00250.00250.005

0.00250.006

0.00250.0090.009

0.00250.006

0.00250.00250.00250.00250.014

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.007

0.00250.005

0.00250.00250.00250.00250.00250.00250.0025


Depth(m)








GL-17-029 1 of 4 2

1.751.

5

1.251 3

2.52

% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

180

160

140

120

100

dark greenish grey; fine grained; chloritized; amygdular; pillowed basalt (andesite). 1-2% py; 1-2% po mineralization. Crosscutting/boudinage/folding of QC stringers/veinlets. localized tuff beds

0.00250.00250.005

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.005

0.00250.00250.00250.00250.00250.0060.011

0.00250.009

0.00250.0070.0070.01

0.00250.00250.00250.00250.006

0.00250.00250.00250.00250.00250.00250.00250.016

0.00250.00250.00250.00250.00250.0110.01

0.00250.00250.00250.00250.0025


Depth(m)


GL-17-029 2 of 4 2

1.751.

5

1.251 3

2.52

% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

280

260

240

220

200

dark blueish grey; fine-medium grained; silica/Kspar/chlorite altered. Blue quartz eyes throughout. QA veins with localized offset and crosscutting. 1-2% dis py; py being replaced by po locally.

0.00250.00250.005

0.00250.00250.0090.0050.0050.0050.0050.00510.660.040.050.039.760.030.040.06

0.0050.07

0.0050.130.010.040.780.032.661.640.04

0.0050.21

0.0050.51

0.0050.5

0.160.28

0.0050.010.180.130.18

0.0050.0050.0050.0050.0050.050.330.05

0.005


Depth(m)


GL-17-029 3 of 4 2

1.751.

5

1.251 3

2.52

% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

320

300

0.020.0050.210.060.030.010.633.720.030.030.010.02

0.005

F00008670F00008671F00008672F00008673F00008674F00008676F00008678F00008679F00008681F00008682F00008683F00008684F00008686

Depth(m)


GL-17-029 4 of 4 2

1.751.

5

1.251 3

2.52

% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

irregular lower contact

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005

0.00250.00250.00250.0080.009

0.00250.00250.007

0.00250.0050.0090.0060.0090.0080.007

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.0025


Depth(m)








GL-17-030 1 of 2 1

0.750.

5

0.250

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

150

140

130

120

110

100

0.00250.00250.006

0.00250.00250.00250.00250.00250.00250.007

0.00250.006

0.00250.00250.018

0.00250.005

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.0025

F00004548F00004549F00004551F00004552F00004553F00004554F00004556F00004557F00004559F00004561F00004562F00004563F00004564F00004565F00004566F00004567F00004568F00004569F00004570F00004571F00004573F00004574F00004575F00004576F00004577F00004578F00004579

Depth(m)


GL-17-030 2 of 2 1

0.750.

5

0.250

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

increase in blue quartz over previous interval

0.0050.0050.0050.0050.0050.0050.0050.0051.840.030.230.13

0.0050.810.640.14

0.0050.0050.420.04

0.0051.340.718.770.430.270.130.220.130.120.090.1

0.0050.040.010.010.32

0.0050.0050.01


F00004614AF00004615AF00004616AF00004618AF00004619AF00004621AF00004622AF00004623AF00004624AF00004625AF00004626

Depth(m)








GL-17-031 1 of 2 2

1.51

0.50 20

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

130

120

110

100

increase in amygdales from 2% in first 6m to 7-10% overall

0.0050.0050.0050.0050.005

0.00250.00250.00250.00250.00250.00250.00250.005

0.00250.00250.00250.00250.0025

F00004627F00004628F00004629F00004631F00004632F00004633F00004634F00004636F00004637F00004639F00004641F00004642F00004643F00004644F00004645F00004646F00004647F00004648

Depth(m)


GL-17-031 2 of 2 2

1.51

0.50 20

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

Coarse grained in 20-30cm alteration halos surrounding veins; then fine grained between halos

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.03

0.0050.0050.0050.08

0.0050.02

0.0050.68

0.0050.040.172.53

0.0050.11.8

0.0050.04

0.0051.34

0.0051

0.030.120.040.040.120.170.07


Depth(m)








GL-17-032 1 of 3 2

1.51

0.50 100

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

190

180

170

160

150

140

130

120

110

100

pillows evident starting at 180m to EOH with qtz carb chlorite selvages

335.760.060.072.590.130.591.420.7

1.221.581.612.540.140.370.130.250.080.080.040.040.1

0.140.010.05

0.0050.060.120.030.050.050.110.01

0.0050.0050.0050.0050.0050.0050.005

0.00250.00250.00250.0070.006

F00004694F00004695F00004696F00004697F00004699F00004700

F00004701AF00004702AF00004704AF00004705AF00004707AF00004709AF00004710AF00004711AF00004712AF00004713AF00004714AF00004715AF00004716AF00004717AF00004718AF00004719AF00004720AF00004721AF00004722AF00004723AF00004724AF00004725AF00004727AF00004729AF00004730AF00004731AF00004734AF00004735AF00004736AF00004737AF00004738AF00004739AF00004740AF00004741F00004742F00004743F00004744F00004745

Depth(m)


GL-17-032 2 of 3 2

1.51

0.50 100

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

200

Depth(m)


GL-17-032 3 of 3 2

1.51

0.50 100

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

80

60

40

20

0

lower contact traces along vuggy QTZ-ANK vein but is not completely constrained by it

lower contact trends 45deg but is irregular; GRD xenolith in POR

0.0050.0050.0050.005

0.20.0050.020.031.99

0.0050.0050.0050.970.02

0.0050.0050.0050.0050.12

0.0050.0050.0050.0050.0050.0050.040.16

0.0050.0050.0050.0050.03

0.0050.0050.0050.0050.0050.0050.005


Depth(m)



Casing Depth: mEOH: 299 m





GL-17-033 1 of 4 3210 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

0.0050.010.03

0.0050.090.190.010.010.040.022.5

0.080.0050.020.030.05

0.0050.005

1.10.0050.110.020.140.070.070.2

0.090.060.220.140.3

0.121.090.5

0.030.060.050.120.020.040.120.1

0.070.110.120.030.420.2

0.730.040.02


Depth(m)


GL-17-033 2 of 4 3210 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

0.080.0050.040.010.160.020.560.020.070.2

0.170.050.350.120.020.010.040.360.090.3

0.090.020.120.220.030.19

0.0050.01

0.0050.010.03

0.0050.1

0.0050.040.01

0.0050.0050.030.02

0.0050.070.01

0.0050.070.050.130.040.02

0.0050.02


Depth(m)


GL-17-033 3 of 4 3210 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

300

0.010.020.02

F00004920F00004921F00004923

Depth(m)


GL-17-033 4 of 4 3210 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

Blue Quartz Eyes; amygdaloidal from 7.5m to 9m and from 17m to 18m.

contact with POR trends 40deg but is irregular

0.0050.0050.0050.0050.01

0.0050.0050.0050.03

0.0050.01

0.0050.0050.0050.0050.01

0.0050.0050.0050.0050.0050.0050.15

0.0050.0050.01

0.0050.0050.450.030.2

1.430.1

0.250.0050.040.06

0.0050.7

0.0050.005


Depth(m)








GL-17-034 1 of 3 3210

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100 30cm gradational contact. Blue quartz eyes starting at 200m

0.0050.08

0.0050.06

0.0050.0050.0051.311.948.750.06

0.0050.080.930.260.070.58

0.0050.1

0.180.050.390.080.070.02

0.0050.010.1

0.140.020.090.090.070.02

0.0050.01

0.0050.110.060.050.040.140.110.070.190.360.070.130.06

0.0050.02


Depth(m)


GL-17-034 2 of 3 3210

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

240

220

200

lineations of carbonate vesicles. blue quartz eyes

blue quartz eyes

0.110.090.140.220.02

0.0050.0050.0050.0050.02

0.0050.030.030.680.238.580.040.39


Depth(m)


GL-17-034 3 of 3 3210

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

Chl alteration present as wisps

AND xenolith at 29m; chill margins in GRD; xenolith is 10cm long by 20cm.

smaller grain size at top of unit; within 10cm becomes regular medium grainedlower contact near perpendicular to core axis with some irregularities

0.0050.0050.0050.0050.0050.0050.0050.010.02

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.03


Depth(m)




Start Date: February-26-17End Date: March-03-17Drill Contractor: Rodren Drilling



Project: GoldlundLogged by: Andrew WiebeLog Completed: March-03-17Core Location: TENT

GL-17-035 1 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

GRD xenolith in POR at lower contact

0.0050.0050.02

0.0050.01

0.0050.42

0.0050.0050.0050.0050.050.010.08

0.0050.030.231.160.790.33

10.790.6

0.820.03

0.0050.17

0.0050.160.770.93

0.0051.510.460.020.1

0.330.630.050.12

0.0050.0050.270.01

0.0050.0050.050.030.030.020.19


Depth(m)


GL-17-035 2 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

Blue Quartz Eyes alteration

0.420.130.150.04

0.0050.550.050.2

0.090.230.080.01

0.0050.070.290.020.050.260.080.48

0.0050.080.020.3

0.020.470.01

0.0050.380.080.080.920.370.310.070.1

0.060.050.270.11

0.0050.070.360.7

0.020.020.2

0.070.030.030.22


Depth(m)


GL-17-035 3 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

320

300

Blue Quartz Eyes from 294 to 302m. 0.0050.00250.00250.0025

F00005922F00005923F00005924F00005925

Depth(m)


GL-17-035 4 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

40

0

carbonate amygdules in sections alternating with lineations indicative of flows. lower contact trends 60deg and then veers of to 10deg. 24-32m were brought in soaked with fuel from drillers obscuring core; scrubbed with dish soap; water and wire brush but fuel still affects appearance of core.

35-38m were brought in covered in fuel from drillers obscuring core; scrubbed with dish soap; water and wire brush which improved appearance but still colour is still affected by fuel. Lower contact trends 50deg but highly irregular.

K-spar plag POR. Varying K-spar alteration along with hematite staining; hairline fracturing w/ calcite cement parallel to regional foliation 30deg. Xenolith's of GRD within POR. lower contact near perpendicular then veers off to 10deg.

0.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.04

0.0050.0050.010.03

0.0050.0050.0050.0050.005

0.005

0.005

0.0050.0050.005

F00005951F00005952F00005953F00005954F00005955F00005956F00005957F00005958F00005959F00005960F00005961F00005962F00005963F00005964F00005965F00005967F00005968F00005969F00005971F00005972F00005974F00005976F00005977F00005978F00005979F00005980F00005981F00005983F00005984F00005985F00005986F00005987F00005988F00005989F00005991F00005992F00005993

F00005995F00005996F00005997F00005998

Depth(m)








GL-17-036 1 of 6 3210 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

160

120

fine gradational to medium grained over +/- 5m

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.02

0.0050.0050.028.550.01

0.0050.020.010.031.450.01

0.0050.020.020.020.05

0.0050.0050.0050.070.02

0.0050.020.070.030.120.020.010.030.340.05


Depth(m)


GL-17-036 2 of 6 3210 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

280

240

200

Lamprophyre dike; fine grained; weak to moderate foliated; biotite and carbonate-rich

GD sliver sub //'l TCA with irregular contacts 261.8-262.4; LC of Porphyry is irregular

irregular LC

0.020.020.320.441.040.110.290.032.66

0.0051.931.080.010.130.13

0.0050.050.350.091.290.210.020.21

0.0050.020.020.15

0.0050.48

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.09

0.0050.390.08

0.0050.050.020.180.48

0.0050.005


Depth(m)


GL-17-036 3 of 6 3210 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

360

320

; LC with FP irregular

with fine grained intervals; LC with Porphyry irregular

includes interval of GD host with irregular contacts 394.7-395.05

0.0050.0050.020.020.190.1

0.070.0050.0050.01

0.0050.0050.020.090.04

0.0050.0050.02

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.020.120.210.220.03

0.0050.0050.240.04

0.0050.020.03

0.0050.162.480.810.030.010.070.02

0.005


Depth(m)


GL-17-036 4 of 6 3210 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

480

440

400

Mafic Dike; non -magnetic; strong albite alteration of fspars with weak ank; moderate chlorite alteration of ferro-magnetic; sheared UC

0.030.0050.0050.0050.32

0.0050.01

0.0050.0050.0050.0050.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.01

0.0050.0050.070.210.020.110.040.02

0.0050.030.11

0.0050.04

0.0050.0050.06

0.0050.02

0.0050.0050.06

0.0050.020.02

0.0050.03


Depth(m)


GL-17-036 5 of 6 3210 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

560

520

Mafic flow; scattered patches with 5-10 amygdales stretched 1: 4 ratio. Irregular Qtz -carb stringers and veinlets more frequent 534.8-540.0m; becoming occasional to EOH

0.180.010.080.4

0.020.0050.0050.03

0.0050.010.02

0.0050.030.02

0.0050.0050.0050.010.02

0.0050.0050.0090.0060.0050.008

F00008043F00008044F00008045F00008046F00008047F00008048F00008049F00008051F00008053F00008054F00008056F00008057F00008058F00008059F00008060F00008061F00008062F00008063F00008065F00008066F00008067F00008068F00008069F00008071F00008072

Depth(m)


GL-17-036 6 of 6 3210 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

80

60

40

20

0

Gabbro; medium grained massive to locally weakly foliated; weakly magnetic; intensely chloritized; a few irregular discontinuous qtz carbonate epidote veins/patches; LC shearedfine to medium grained Andesite; moderately magnetic; rare amygdales; irregular qtz carb stringers and veinlets; strong chlorite alterationfine grained 'GD' (Qtz Diorite?); strongly chloritic; moderate carbonate alteration; massive; weak to locally moderate foliated; 10-15% quartz and blue Qtz

fine to medium grained; strongly foliated; scattered altered amygdales stretched 1:5 up to 2X10mm; numerous qtz - carbonate continuous and discontinuous stringers and 5-10mm tension gashed QV with carbonate infilling

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005


Depth(m)







Project: GoldlundLogged by: Richard KowalskiLog Completed: March-20-17Core Location: TENT

GL-17-037 1 of 4 3210 20% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

180

160

140

120

100

GD host

local gradational finer grained sections

0.0050.0050.0050.0050.0050.0050.0050.0050.02

0.0050.0050.0050.0050.0050.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.01

0.0050.0050.04

0.0050.0050.03

0.0050.0050.08

0.0050.0050.0050.06

0.0050.020.010.030.02

0.0050.0050.0050.0050.230.050.3

0.15


Depth(m)


GL-17-037 2 of 4 3210 20% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

280

260

240

220

200

fine grained mafic volcanic; amygdales stretched 2:1; 0.5-1.5mm; could be large xenolith

Intense k altered; moderate silica; weak ank altered to 248.5m

0.080.060.281.86

0.0050.210.07

0.0050.66

0.0051.84

0.0050.0050.41

0.0050.01

0.0050.020.090.160.021.380.2

0.0050.030.1

0.0050.0050.0050.0050.06

0.0050.1

0.030.6

0.010.0050.040.020.01

0.0050.2

0.020.06

0.0050.490.050.020.010.040.870.23


Depth(m)


GL-17-037 3 of 4 3210 20% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

380

360

340

320

300

intensely broken blocky core; strongly altered Andesite with carb amygdales

0.0050.005

0.10.0050.0050.05

0.0050.010.08

0.0050.040.01

0.0050.0050.0050.0050.0050.0050.0050.0050.320.1

0.0050.0050.0050.02

0.0050.030.020.01

0.0050.0050.0050.0050.0050.02

F00008273F00008274F00008276F00008277F00008279F00008281F00008282F00008283F00008284F00008285F00008286F00008287F00008288F00008289F00008290F00008292F00008293

F00008294AF00008295AF00008296AF00008297AF00008298AF00008299AF00008301AF00008302AF00008304AF00008306AF00008307AF00008308F00008309F00008311F00008312F00008313F00008314F00008315F00008316

Depth(m)


GL-17-037 4 of 4 3210 20% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

80

60

40

20

0

moderately foliated; UC slightly irregular; LC sharpfine to medium grained

0.010.0050.0050.02

0.0050.76

0.0050.040.01

0.0050.0050.020.020.04

0.0050.02

0.0050.020.130.020.090.110.050.020.060.02

0.0050.02

0.0050.0050.0050.030.49

0.0050.0050.0050.0050.03

0.0050.0050.0050.005


Depth(m)



Casing Depth: 5.74 mEOH: 327.6 m




Project: GoldlundLogged by: Richard KowalskiLog Completed: April-24-17Core Location: TENT

GL-17-039 1 of 4 151050 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

Good QTZ Vein mineralization begins at 273m 0.0050.0050.02

0.0050.0050.0050.0050.0050.030.010.09

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.050.030.021.2

0.560.760.092.050.030.080.050.050.060.59

0.0053.06

0.005


Depth(m)


GL-17-039 2 of 4 151050 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

0.060.02

0.0050.0050.850.030.01

0.0050.08

0.0050.040.10.5

1.610.040.030.150.110.360.020.05

0.0050.290.1

0.0050.3

0.020.79

12.540.130.390.040.990.360.020.110.08

0.0050.030.040.220.450.134.460.181.740.040.6

0.140.330.66


Depth(m)


GL-17-039 3 of 4 151050 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

340

320

300

0.050.08

0.0050.550.090.050.010.030.020.030.11

0.0050.0050.020.190.020.26

F00005722F00005723F00005724F00005726F00005727F00005729F00005731F00005732F00005733F00005735F00005736F00005737F00005738F00005739F00005740F00005741F00005742

Depth(m)


GL-17-039 4 of 4 151050 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

irregular fingered lower contact

0.0050.2

0.0050.0050.690.140.140.030.010.01

0.0050.060.040.110.07

0.0050.0050.0050.26

0.0050.0050.0050.0050.0050.0050.0050.01

0.0050.06

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005


Depth(m)








GL-17-040 1 of 2 3210 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

170

160

150

140

130

120

110

100

numerous carb stringers and veinlets; and occasional primary boudinaged qtz-carb veinlets to164m

0.0050.0050.030.020.01

0.0050.020.01

0.0050.0050.01

0.0050.0050.0050.0050.02

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005

0.00250.0025

F00007055F00007056F00007058F00007059F00007060F00007062F00007063F00007064F00007065F00007067F00007069F00007070F00007071F00007072F00007073F00007074F00007075F00007077F00007078F00007079F00007080F00007081F00007082F00007083F00007084F00007085F00007087F00007088F00007090F00007092F00007093F00007094F00007095F00007096

Depth(m)


GL-17-040 2 of 2 3210 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

contact with porphyry irregular 0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.01


Depth(m)








GL-17-041 1 of 4 151050 20% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

180

160

140

120

100

0.0050.0050.0050.0050.0050.0050.05

0.0050.110.120.040.1

0.130.0050.040.020.170.080.640.011.210.031.730.080.030.110.120.830.1

0.250.05

0.0050.0050.0050.0050.0050.0050.070.020.17

0.0050.140.030.290.080.050.050.43

0.0050.110.39


Depth(m)


GL-17-041 2 of 4 151050 20% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

280

260

240

220

200

0.030.01

0.00511.50.010.120.040.090.4

0.050.290.040.150.110.140.030.3

2.237.470.091.491.831.131.293.471.340.020.580.560.2

0.210.020.050.2

0.010.650.210.091.680.6

3.280.510.020.110.180.690.530.190.210.02

0.005


Depth(m)


GL-17-041 3 of 4 151050 20% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

360

340

320

300

well foliated; LC intensely shearedfine grained becoming medium grained by end of interval in contact with andesitemedium grained massive; blue qtz eyes to 5-7%

FELSIC TUFF; fine grained; small spherical qtz; locally slightly larger fspar (up to 0.5mm) clasts stretched 2:1; fine grained groundmass. Irregular andesite remnant 333.1-331.5fine to medium grained; massive; local sections with amygdales .25-7mm

0.090.0050.03

0.0050.0050.020.060.310.170.1

0.040.030.220.130.310.19

0.0050.00250.00250.00250.00250.00250.00250.00250.00250.00250.0025


Depth(m)


GL-17-041 4 of 4 151050 20% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

80

40

0

weakly magnetic

no amygdules; flow lineations @45deg. moderately magnetic

at 50m grain size beings to gradually increase to medium grained at 51.3m. No observable contact angle as next lithology interval is medium grained gabbro. weakly magnetic

from 82m to lower contact grain size decreases from medium grained to coarse grained. weakly magnetic

carbonate amygdules. moderately magnetic

Depth(m)







Project: GoldlundLogged by: Andrew WiebeLog Completed: April-10-17Core Location: TENT

GL-17-042 1 of 5 3210 100% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

160

120

0.00250.00250.00250.00250.0050.005

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.01

0.0050.0050.0050.0050.0050.140.260.090.110.090.21

0.0050.0050.005

0.20.040.140.250.02

0.0050.0050.190.160.02

0.0050.0050.05

0.005

F00006551F00006552F00006553F00006554F00006555F00006556F00006557F00006558F00006559F00006560F00006561F00006562F00006563F00006564F00006565F00006566F00006568F00006569F00006571F00006572F00006573F00006576F00006577F00006578F00006579F00006580F00006581F00006582F00006583F00006584F00006585F00006586F00006588F00006589F00006591F00006592F00006593F00006594F00006595F00006596F00006597F00006598F00006599F00006601F00006602F00006603F00006604

Depth(m)


GL-17-042 2 of 5 3210 100% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

280

240

200

0.0050.0050.260.530.09

0.0050.0050.0050.051.620.060.110.020.580.090.030.060.460.320.060.120.340.240.060.060.130.15

0.0050.110.04

0.0050.230.330.2

0.0050.020.190.030.010.16

0.0050.030.01

16.380.030.090.120.170.920.450.15


Depth(m)


GL-17-042 3 of 5 3210 100% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

360

320

0.020.190.220.31

0.0050.820.060.460.050.620.420.03

0.0050.03

0.0050.030.6

0.070.0052.110.010.131.220.07

0.0050.080.070.370.460.070.030.070.040.050.120.130.191.370.030.1

0.340.030.080.860.021.850.590.030.020.04

0.005


Depth(m)


GL-17-042 4 of 5 3210 100% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

480

440

400

strongly chloritic and weak carbonate alteration; 5-10% blue qtz eyesstrong to intense chlorite alteration of ferro-magnesian minerals; 5% blue qtz eyes; scattered irregular qtz carb stringers

0.020.0050.28

0.0050.0050.020.049.66

0.0050.02

0.0050.06

0.0050.052.280.160.370.560.06

0.0050.00250.00250.00250.00250.00250.0025

F00006731F00006732F00006733F00006734F00006735F00006736F00006737F00006738F00006740F00006741F00006742F00006743F00006744F00006745F00006746F00006747F00006748F00006749F00006751F00006752F00006753F00006756F00006757F00006758F00006759F00006760

Depth(m)


GL-17-042 5 of 5 3210 100% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

from 74.2 m appearance of blue quartz eyes 0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.02

0.0050.020.130.06

0.0050.14

0.0050.3

0.050.040.040.950.290.010.07

0.0050.020.111.29

0.0050.0050.0050.005

0.00250.00250.00250.0025


Depth(m)







Project: GoldlundLogged by: Nikolay BashaevLog Completed: January-28-17Core Location: TENT

GL-17-043 1 of 2 151050 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

110

100

0.00250.00250.00250.00250.178

0.00250.00250.00250.0025

F00007248F00007249F00007250F00007251F00007252F00007253F00007254F00007256F00007258

Depth(m)


GL-17-043 2 of 2 151050 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

approx. from 20.3 m appearance of quartz blue eyes

sharp upper contact at 30 degrees TCA; sharp lower contact at 50 degrees TCA

0.060.0050.0050.0050.0050.02

0.0050.230.020.070.04

0.0050.0050.0050.03

0.0050.0050.0050.0050.03

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.110.05

0.0050.17

0.0050.230.950.970.4

18.43


Depth(m)




Start Date: January-28-17End Date: February-01-17Drill Contractor: Rodren Drilling



Project: GoldlundLogged by: Nikolay BashaevLog Completed: February-01-17Core Location: TENT

GL-17-044 1 of 3 3210

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

190

180

170

160

150

140

130

120

110

100

from 117.45 appearance of quartz bull eyes

sharp upper contact at 35 degrees TCA; vugs at 191.0 m

3.490.260.441.140.980.170.160.260.06

0.0050.040.01

0.0050.28

0.0050.0050.0050.0050.007

0.00250.00250.00250.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005


Depth(m)


GL-17-044 2 of 3 3210

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

200

0.0050.0050.005

F00007408F00007409F00007410

Depth(m)


GL-17-044 3 of 3 3210

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

moderately silicified; lots of interstitial CHL alteration along fluid pathways of faults (?; abundant vein offsets; fluid pathways near parallel core axis; frequent breccia)

Massive QTZ vein crosscuts both POR and GRD at upper contact

0.190.010.080.070.110.180.970.030.15

0.0050.0050.170.18

61.370.290.390.6

0.0052.190.160.020.160.01

0.0050.0050.0050.47

0.0051.440.590.060.091.4

0.0050.020.02

0.0050.190.01


Depth(m)








GL-17-045 1 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

0.0054.440.09

0.0050.050.810.040.2

0.290.460.230.050.020.020.05

0.0050.0050.020.03

0.0050.0050.0050.150.01

0.0050.0050.02

0.0050.113.940.020.040.040.03

0.0050.1

0.790.080.030.020.070.15

0.0050.0050.030.050.020.030.020.020.03


Depth(m)


GL-17-045 2 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

blue quartz eyes

0.150.005

0.20.010.180.330.350.090.060.040.05

0.0050.020.060.05

0.0050.090.120.080.080.320.120.040.020.060.070.070.020.060.050.070.380.470.190.550.270.170.06

0.0050.010.080.090.720.190.630.480.140.110.2

0.270.34


Depth(m)


GL-17-045 3 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

320

300

0.120.150.15

0.005

F00007619F00007620F00007621F00007622

Depth(m)


GL-17-045 4 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

0.0050.0050.0050.01

0.0050.0050.02

0.0050.0050.210.020.010.010.02

0.0051.71

0.0050.150.141.070.680.4

0.661.930.140.870.074.711.9

0.540.381.690.080.010.02

0.0050.130.28

0.0050.005

F00007651F00007652F00007653F00007654F00007655F00007656F00007657F00007658

F00007659AF00007660AF00007661AF00007662AF00007663AF00007664AF00007665AF00007667AF00007668AF00007669AF00007671AF00007673AF00007674AF00007676AF00007677AF00007678AF00007679AF00007680AF00007681AF00007682AF00007683AF00007684AF00007685AF00007686AF00007687AF00007688AF00007689AF00007691AF00007692AF00007693AF00007694AF00007695A

Depth(m)







Project: GoldlundLogged by: Nikolay BashaevLog Completed: February-05-17Core Location: TENT

GL-17-046 1 of 3 3210

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

190

180

170

160

150

140

130

120

110

100

0.0050.03

0.0050.02

0.0050.0051.530.020.480.180.260.01

0.0050.0050.0050.05

0.0050.0050.0052.38

0.0050.02

0.0050.211.5

0.040.030.62

0.0050.17

10.670.030.150.010.030.030.03

0.0050.060.020.110.050.1

0.0050.120.070.01

0.0050.0050.0050.005

F00007696AF00007697AF00007698AF00007699AF00007700AF00007701F00007702F00007703F00007704F00007706F00007707F00007708F00007709F00007711F00007712F00007713F00007714F00007715F00007716F00007717F00007718F00007719F00007720F00007721F00007722F00007723F00007724F00007725F00007726F00007727F00007728F00007729F00007731F00007732F00007733F00007734F00007736F00007737F00007738F00007739F00007740F00007741F00007742F00007743F00007744F00007745F00007746F00007747F00007748F00007749F00007751

Depth(m)


GL-17-046 2 of 3 3210

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

210

200

0.0050.0050.0050.0050.0050.0050.0050.0050.005

F00007752F00007753F00007754F00007755F00007756F00007757F00007758F00007759F00007760

Depth(m)


GL-17-046 3 of 3 3210

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

Datamine crashed and log from 7.7 to 140m was lost. Relog when time permits

0.0050.0050.0050.0050.01

0.0050.0050.0050.0050.0050.01

0.0050.020.040.04

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.040.01

0.0050.01

0.0050.0050.010.02

0.0050.0050.0050.0050.005


Depth(m)







Project: GoldlundLogged by: Adam RichardsonLog Completed: February-10-17Core Location: TENT

GL-17-047 1 of 3 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

0.0050.0050.0050.240.03

0.0050.17

0.0050.005

0.10.520.760.060.030.1

0.030.01

0.0050.03

16.950.040.04

0.0050.0050.0050.0050.005

0.50.0050.030.03

0.0050.032.430.020.430.040.350.030.060.160.720.030.280.350.020.020.120.020.030.14

F00007895F00007896F00007897F00007898F00007899F00007900F00007901

F00007902AF00007903AF00007904AF00007906AF00007907AF00007908AF00007909AF00007911AF00007912F00007913F00007914F00007915F00007916F00007917F00007918F00007919F00007920F00007921F00007922F00007923F00007924F00007925F00007926F00007927F00007928F00007929F00007931F00007932F00007933F00007934F00007936F00007937F00007938F00007939F00007940F00007941F00007942F00007943F00007944F00007945F00007946F00007947F00007948F00007949

Depth(m)


GL-17-047 2 of 3 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

0.110.040.080.02

0.0050.320.070.080.1

0.030.010.02

0.0050.080.020.060.020.020.03

0.0050.050.040.030.040.020.15

0.0050.0050.484.070.01

0.0050.0050.0050.020.02

0.0050.005

0.00250.00250.00250.00250.0025


F00007980AF00007981AF00007982AF00007983AF00007984AF00007985AF00007986AF00007987AF00007988AF00007989AF00007991F00007992F00007993F00007994F00007996F00007997

Depth(m)


GL-17-047 3 of 3 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

greenish fine to medium grained granodiorite. Trace local fine to medium grained pyrite with rare pyrrhotite. Crosscutting quartz and quartz-carbonate veins. Patchy albite alteration? associated with quartz carbonate veining. Pervasively chloritic.

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.09

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.21

0.0050.0050.01

0.0050.0050.020.05

0.0050.0050.0050.080.491.071.28

0.0050.31

0.0050.020.01


Depth(m)








GL-17-048 1 of 4 151050 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

0.090.27

0.0050.030.110.02

0.0050.12

0.0050.490.160.040.03

0.0050.2

0.030.050.060.050.140.1

0.083.920.050.080.010.1

0.240.571.1

0.160.180.150.211.230.060.020.030.160.010.04

0.0050.020.080.060.010.030.130.420.040.01


Depth(m)


GL-17-048 2 of 4 151050 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

0.040.090.070.28

0.0050.040.030.020.050.020.040.030.29

0.0050.0050.0050.03

0.0050.090.110.080.030.020.030.110.060.040.070.230.090.060.090.17

0.0050.020.070.06

0.0050.0050.0050.020.01

0.0050.05

0.0050.0050.0050.010.030.03

0.005


Depth(m)


GL-17-048 3 of 4 151050 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

320

300

0.0050.0050.0050.005

F00004169F00004170F00004171F00004173

Depth(m)


GL-17-048 4 of 4 151050 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

amygdules being stretched and rotated;lower contact obscure in rubble; angle is in 10-30deg range. Blue Quartz Eyes and mottled quartz appearance

amygdules being stretchedflow lineationsBlue Quartz Eyes and mottled quartz alteration decreasing in frequency downhole

0.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.07

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0051.45

0.0050.0050.024.960.020.01

0.0050.020.03


Depth(m)








GL-17-049 1 of 4 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

0.670.161.13

0.0050.0050.080.110.020.1

0.050.02

0.0050.010.070.030.010.271.1

0.011.040.13

0.0050.810.15

0.0050.020.120.210.07

0.0050.0050.0050.08

0.0050.020.060.080.480.120.211.430.1

0.0050.260.040.030.020.040.2

0.030.03


Depth(m)


GL-17-049 2 of 4 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

0.0050.03

0.0050.0050.02

0.0050.0050.0050.0050.050.030.020.11

0.0050.0050.030.08

0.0050.051.210.090.410.260.110.311.490.3

1.380.050.080.02

0.0050.0050.020.020.03

0.0050.0050.08

0.0050.0050.0050.07

0.0050.0050.02

0.0050.0050.0050.0050.005


Depth(m)


GL-17-049 3 of 4 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

340

320

300

0.0052.19

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005

F00006523F00006524F00006526F00006527F00006528F00006531F00006532F00006533F00006534F00006535F00006536F00006537F00006538F00006539F00006541F00006542

Depth(m)


GL-17-049 4 of 4 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

light gray fg-mg grd with 10-15% blue qtz eyes supported in a bluish translucent vfg qtzo-feldspathic groundmass separating fg felty intergrowths of chl and accicular act/trem supporting subhedral to euhedral grains and aggregates of mt +/- ilmenite; and trace vfg-fg py +/- po

strongly to intensely hydrothermally altered granodiorite (presence of 10-15% blue qtz eyes) forming a fg-mg weakly translucent light to pale greenish white coloured rock that is soft; easily scratched exhibiting a strong carbonate and sericitic alteration replacing the qtz-feldspathic groundmass; strongly resembles platy phyillic alteration with vfg silver white sericite

0.990.0050.020.270.73

0.0050.170.020.04

0.0050.01

0.0050.0050.0050.02

0.0050.050.030.02

0.0050.260.071.3

0.040.080.430.080.090.140.340.02

0.0050.03

0.0050.0050.0050.0050.030.02

0.0050.0050.0050.02


Depth(m)








GL-17-050 1 of 2 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

150

140

130

120

110

100

andesitic rock (possible tuffaceous units or meta-volcanic sediments) crosscut by numerous qtz-carb boudinaged veins/veinlets; groundmass of the olive green andesitic rock supports numerous fg amygdules comprised of qtz-carb + carb and fg blackish brown biotite clots; possible xenolith sloughed off along grd-mafic contactas above between 71.88 and 77.50m: strongly to intensely hydrothermally altered granodiorite (presence of 10-15% blue qtz eyes) forming a fg-mg weakly translucent light to pale greenish white coloured rock that is soft; easily scratched exhibiting a strong carbonate and sericitic alteration replacing the qtz-feldspathic groundmass; strongly resembles platy phyillic alteration with vfg silver white sericitevfg-fg intensely chloritic massive andesitic schist of meta-mafic volcanic rock with elongated amygdules filled with qtz-car; unit appears to be weakly silicifiedlight whitish greenish gray fg-mg granodiorite; unit appears to be a breccia; possible contact breccia; with vfg olive green wispy vein-like chloritic matrix separating angular to sub-angular grd fragmentsdark olive green vfg meta-mafic volcanic rock comprised of alternating flows and pillows separated by hyaloclastite fragmentals; flows and pillows exhibit rounded to subrounded to irregular shaped amygdules of qtz-carb filling; numerous veins/veinlets of qtz-carb material crosscuts the greenschist; lower section below 131m appears to transition into upper greenschist to lower amphibolite facies exhibited by hard black shiny glassy fracture surfaces - possible dehydration or amphibole-hornfels

0.0050.005

0.00250.00250.00250.00250.0025

F00002501F00002502F00002503F00002504F00002506F00002507F00002508

Depth(m)


GL-17-050 2 of 2 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

40

0

Fine to mostly medium-grained granodiorite generally with a little veining but having short sections with mineralized veining; moderately magnetic; flow banding near bottom of hole with strong silica-potassic alteration extending into hydrothermal alteration zone from 411.18 to 458.0m with Au particles associated with cg pyrite

0.20.0050.030.020.040.020.05

0.0050.0050.0050.0050.01

0.0050.0050.090.040.02

0.0050.0050.0050.0050.04

0.0050.16

0.0050.090.090.020.11

0.0050.0050.0050.0050.050.040.2

0.110.180.020.052.940.04


Depth(m)




Start Date: May-14-17End Date: May-18-17Drill Contractor: Rodren Drilling



Project: GoldlundLogged by: Harvey BuckLog Completed: May-18-17Core Location: TENT

GL-17-051 1 of 7 3020100 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

160

120

0.060.280.110.45

0.0050.0050.0050.0050.17

0.0050.0050.0050.050.59

0.0050.030.040.07

0.01

0.005

0.020.0050.0050.0050.0050.0050.01

0.0050.0050.0050.0050.040.080.030.01

0.0050.0050.0050.0050.0050.0050.0050.0050.060.010.060.380.010.190.25

F00000244F00000245F00000246F00000247F00000248F00000250F00001401F00001403F00001405F00001406F00001407F00001408F00001409F00001410F00001411F00001412F00001413F00001414F00001416


Depth(m)


GL-17-051 2 of 7 3020100 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

240

200

1.030.020.01

0.0050.020.130.01

0.0050.023.460.511.14

0.0050.150.012.130.1

0.211.320.120.19

0.0050.0050.050.24

0.0050.0050.03

0.0050.0050.120.19

0.0050.0050.0052.31

0.0050.06

0.0050.04

0.0050.210.160.240.010.03

0.0051.280.310.050.01


Depth(m)


GL-17-051 3 of 7 3020100 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

360

320

0.020.0050.0050.010.050.051.010.411.610.210.340.045.9

0.254.110.16

0.0050.03

0.0050.0050.0050.0050.0050.005

F00001513F00001514F00001515F00001516F00001517F00001518F00001520F00001521F00001522F00001523F00001525F00001526F00001527F00001528F00001529F00001530F00001531F00001533F00001534F00001535F00001536F00001537F00001538F00001539

Depth(m)


GL-17-051 4 of 7 3020100 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

480

440

400

Depth(m)


GL-17-051 5 of 7 3020100 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

600

560

520

Depth(m)


GL-17-051 6 of 7 3020100 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

640

possible andesitic tuff; unit is well banded and segregated into mafic and felsic bands; felsic bands have fg plagioclase microlites in a light grayish white glassy granular siliceous groundmass; the mafic bands are vfg to fg biotite amph qtz magnetite dark gray to blackFine to mostly medium-grained granodiorite

greenish-gray massive fg to mg; strongly chloritized gabbro with whitish-green strongly chloritized plagioclase grainsfg massive dark greenish-gray strongly chloritized and sericitized andesite

Depth(m)


GL-17-051 7 of 7 3020100 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

Fine to mostly medium-grained granodiorite with a little veining; moderately magnetic; the lower contact is sharp; slightly undulating

0.222.640.09

0.0050.070.050.560.060.04

0.0050.0050.0050.0050.0050.150.080.150.010.040.170.050.140.030.04

0.0050.77

0.0050.2

0.0050.040.050.010.12

0.0051.060.240.01

0.0050.0050.0050.0050.95


Depth(m)







Project: GoldlundLogged by: John CamierLog Completed: May-14-17Core Location: TENT

GL-17-052 1 of 3 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

180

160

140

120

100

Fine-grained weakly amygdaloidal andesite that is weakly magnetic; top 3 m has a decreasing number of blue quartz eyes; between 177.15 and 177.7 m is a tuff?? that is very fine-grained and massive and lacks quartz eyes; between approximately 200.5 and 212 core is fine-grained to aphanitic then rest of unit; has good amygdules; lower contact was not drilled

0.050.72

0.0050.040.090.140.360.090.030.010.03

0.0050.0050.01

0.0050.0050.02

0.0050.06

0.0050.060.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.010.02

0.0050.0050.0050.0050.0050.0050.0050.005

0.00250.00250.00250.00250.00250.00250.00250.0025


Depth(m)


GL-17-052 2 of 3 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

260

240

220

200

0.00250.00250.00250.0025

0.010.00250.00250.00250.00250.00250.0025

0.00250.00250.0025

F00001548F00001549F00001550F00000183F00000184F00000185F00000186F00000188F00000189F00000190F00000191

F00000192F00000193F00000194

Depth(m)


GL-17-052 3 of 3 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

80

60

40

20

0

Two mafic dykes; the first at 47.6 to 47.7 has a sharp straight upper contact at 36 degrees TC; the lower contact is irregular and is approx. 45 degrees TCA; the second at 63.8 to 64.15 m has a sharp straight upper contact at 22 degrees TCA and a more indistinct lower contact at 31 degrees that has been disrupted by quartz-ankerite veining; Gabbro is magnetic and appears to be porphyritic

Massive aphanitic to fine-grained andesite with stretched amygdules; moderately magnetic; numerous small blue quartz eyes in bottom half but still associated with amygdules so still mafic rock; lower contact is sharp; partly offset

0.00250.00250.0025

0.00250.006

0.00250.00250.00250.00250.00250.0025

0.00250.00250.011

0.0025

0.00250.0025

F00000531F00000532F00000533

F00000534F00000535F00000536F00000537F00000538F00000539F00000540F00000542

F00000543F00000544F00000545F00000546

F00000547F00000548

Depth(m)








GL-17-053 1 of 4 2

1.51

0.50 210

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

180

160

140

120

100

Fine to mostly medium-grained granodiorite; moderately magnetic; the lower contact is indistinct over a few cm due to veining but the contact angle is reasonable

0.0080.00250.00250.00250.00250.005

8.70.010.01

0.0050.0050.0050.31

0.0050.020.120.17

0.0050.021.690.01

0.0050.0050.0050.0050.01

0.0050.640.4

0.0312.070.050.03

0.0050.0050.04

0.0050.0050.0050.0050.0050.030.060.1

0.033.441.820.060.010.040.3

F00000549F00000551F00000552F00000554F00000556F00000557F00000558F00000559F00000560F00000561F00000562F00000563F00000564

F00000565AF00000567AF00000568AF00000569AF00000571AF00000572AF00000573AF00000574AF00000575AF00000576F00000577F00000578F00000580F00000581F00000582F00000583F00000584F00000586F00000587F00000588F00000591F00000592F00000593F00000594F00000595F00000596F00000597F00000598F00000599F00000601F00000602F00000603F00000604F00000605F00000606F00000607F00000608F00000609

Depth(m)


GL-17-053 2 of 4 2

1.51

0.50 210

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

280

260

240

220

200

Fine-grained weakly amygdaloidal andesite that is weakly magnetic; has a fair number of

0.0050.0051.270.05

0.0050.0050.0050.0050.020.160.532.87

0.0050.320.060.260.530.2

0.020.180.420.510.140.4

9.215.360.810.236.33

11.677.763.123.477.9

4.831.388.141.180.741.690.551.615.791.390.650.182.660.310.341.360.160.170.1

0.0050.0050.005

F00000611F00000612F00000614F00000616F00000617F00000618F00000619F00000620F00000621F00000622F00000623F00000624F00000625F00000627F00000628F00000629F00000631F00000632F00000633F00000634F00000635F00000636F00000637F00000638F00000640F00000641F00000642F00000643F00000644F00000646F00000647F00000649F00000051F00000052F00000053F00000054F00000055F00000056F00000057F00000058F00000059F00000061F00000062F00000063F00000064F00000065F00000066F00000067F00000068F00000069F00000071F00000073F00000074F00000076F00000077F00000078

Depth(m)


GL-17-053 3 of 4 2

1.51

0.50 210

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

300

undulating very distinct lower contactFine to mostly medium-grained granodiorite; moderately magnetic; the lower contact is sharp; moderately undulatingFine-grained weakly amygdaloidal andesite that is weakly magnetic; has a few blue quartz eyes; the lower contact was not drilled

0.0050.0050.005

F00000079F00000080F00000081

Depth(m)


GL-17-053 4 of 4 2

1.51

0.50 210

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

light greyish greenish medium grained granodiorite. locally mineralized by coarse to fine grained disseminated pyrite with rare pyrrhotite. Local regularly spaced alteration zones (albite?) associated with quartz-carbonate veins. Veins typically 45tca and not more than a few centimeters in size.

green; fine to medium grained weakly to locally strongly foliated mafic (andesite) volcanics. Pervasive weak to moderate chlorite alteration. Disseminated fine to medium grained pyrite throughout unit with local pyrrhotite. Usually trace to up to 1% local py; trace local po. Unit crosscut by regularly spaced hairline to p to 20cm wide (rare) quartz veins with trace carbonate. Local epidote alteration.

0.0050.0050.02

0.0050.0050.041.270.330.040.05

0.0050.005

0.10.020.080.090.1

0.070.040.090.280.030.07

0.0050.0050.03

0.0050.005

0.00250.008

0.00250.00250.00250.00250.007

0.00250.00250.00250.00250.0025


F00004204AF00004205AF00004206F00004207F00004208F00004209F00004211F00004212F00004214F00004215F00004216F00004217F00004218F00004219

Depth(m)








GL-17-055 1 of 2 1

0.750.

5

0.250 210

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

140

130

120

110

100

dark greyish greenish feldspar porphyry. Equant 1-5mm feldspar phenocrysts (40%) in a dark green aphanitic chloritic matrix. sharp upper and lower contacts.fine to medium grained weakly pervasively chlorite altered. few crosscutting qc veins and veinlets. pervasive fg dis py throughout.

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.006

0.00250.00250.007

0.00250.006

0.00250.0025


Depth(m)


GL-17-055 2 of 2 1

0.750.

5

0.250 210

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

60

56

52

48

44

40

36

32

28

24

20

16

12

8

40

Greyish greenish medium grained granodiorite. Patchy albite alteration associated with quartz-carbonate veins. Pyrite common; fine to locally coarse grained disseminated and blebby trace to locally 10-15% (over 30cm); usually higher pyrite is associated with the qc veins and the alteration zones.

0.120.611.720.560.071.2

0.271.342.060.380.180.360.76

0.0050.2

2.270.310.030.12

0.0050.030.02

0.0050.010.141.38


Depth(m)








GL-17-056 1 of 1 3210 1

0.50

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

dark; medium grained; weakly pervasive chlorite altered granodiorite; locally silica and ankerite alteration with pyrite and rare tourmaline. Blue quartz eyes start at around 82m

0.111.2

0.081.410.431.30.7

0.810.570.780.280.050.260.171.810.160.091.420.02

0.0050.2

0.0050.0050.06

0.0050.0050.040.750.86

0.0050.0050.0050.120.2

0.040.04

0.0050.0050.0050.0050.005


Depth(m)








GL-17-057 1 of 3 151050 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

dark; coarse-medium grained QFP. weakly pervasive sil+kspar alteration with biotite reaction rims around phenocrystsUPDATE DEPTH TO**dark; medium grained; weakly pervasive chlorite altered granodiorite; locally silica and ankerite alteration with pyrite and rare tourmaline; blue quartz eyes. Evidence of shearing locally (vein offset; minor brecciation)

0.0050.0050.010.01

0.0050.04

0.0050.010.010.110.060.1

0.0050.050.010.030.070.081.470.060.250.020.010.090.16

0.0050.07

0.0050.040.010.01

0.0050.35

0.0050.0050.09

0.0050.030.04

0.0050.0050.020.29

0.0050.05

0.0050.0050.0050.55

0.0050.005


Depth(m)


GL-17-057 2 of 3 151050 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

240

220

200

green; fine-medium grained mafic volcanic (andesite); pervasive chlorite altered. Localized shearing and crosscutting veins.

dark; medium grained; weak pervasive chl and sil alteration. Blue quartz eyes throughout.

green; fine-medium grained andesite; pervasive chl alt; also biotite and carbonate altered. Amygdules + pillows at the top of unit

0.0050.0050.0050.0050.0050.0050.140.020.01

0.0050.010.010.040.15

0.0050.0050.006

0.0025


Depth(m)


GL-17-057 3 of 3 151050 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

dark; medium grained granodiorite (tonalite); weak-mod pervasive sil and chl alteration. Coarse cubic py within alt haloes around vein sets; medium-coarse in between vein sets. Very fine grained dis py throughout. Po replacing py locally

0.153.2

0.0050.080.040.010.010.06

0.0050.0050.030.15

0.0050.120.190.14

0.0050.0050.35

0.0050.1

0.0050.0050.061.030.040.280.080.02

0.0050.170.120.2

0.070.04

0.0050.0050.47

0.0050.0050.06


Depth(m)







Project: GoldlundLogged by: Joseph WiebeLog Completed: February-24-17Core Location: TENT

GL-17-058 1 of 3 161161 32% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

190

180

170

160

150

140

130

120

110

100

dark grey; medium-coarse grained QFP. Pervasive Sil Alt with weak chl alt. Trace fine grained dis pydark; medium grained granodiorite (tonalite); weak-mod pervasive sil and chl alteration. Coarse cubic py within alt haloes around vein sets; medium-coarse in between vein sets. Very fine grained dis py throughout. BQE's begin around 140m

green; fine to medium grained locally weakly foliated mafic (andesite) volcanics(Gabbroic? presence of amphiboles). Pervasive weak to moderate chlorite alteration. Disseminated fine to medium grained pyrite throughout unit. Usually trace to up to 1% local py. Unit crosscut by regularly spaced hairline up to 20cm wide (rare) quartz veins with carbonate/chl. Rare BQE's

0.10.03

0.0050.02

0.0050.0050.01

0.0050.05

0.0050.09

0.0050.070.020.320.10.4

2.180.970.690.210.120.091.76

0.0050.290.110.040.020.170.020.020.060.020.020.030.062.41

0.0050.00250.0025


Depth(m)


GL-17-058 2 of 3 161161 32% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

200

Depth(m)


GL-17-058 3 of 3 161161 32% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

dark grey/blue. Medium grained. Pervasive; weak-moderate sil alteration; pervasive weak chl alteration. Silica/Kspar alteration haloes around quartz ankerite veins. Mineralized by py and trace po. BQE's begin at around 34m. Localized brecciation and shearing; along with vein/veinlet offset and vein/veinlet/stringer crosscutting

0.0050.0050.050.01

0.0050.0050.0050.0050.06

0.0050.0050.0050.080.080.02

0.0050.0050.0050.04

0.0050.59

0.0050.0050.13

0.0050.120.3

0.170.12

0.0050.0050.0050.240.890.240.140.293.860.110.280.13


Depth(m)








GL-17-059 1 of 4 7550250 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

180

160

140

120

100

dark grey feldspar porphyry. 1-5mm feldspar phenocrysts (40%) in a dark aphanitic weakly biotite/chlorite altered matrix. Localized Sil/Kspar alt haloes around massive Q veins. trace-1% dis pydark grey/blue. Medium grained. Pervasive; weak-moderate sil alteration; pervasive weak chl alteration. Silica/Kspar alteration haloes around quartz ankerite veins. Mineralized by py and trace Po; Mag; and Altaite. BQE's begin at around 34m. Localized vein/veinlet offset and vein/veinlet/stringer crosscutting

0.110.050.020.050.843.960.150.220.5

0.0623.62

0.10.310.060.13

0.0050.7

0.961.24

0.0052.340.370.020.030.120.060.020.280.120.480.17

186.490.210.110.060.020.040.620.420.010.07

0.0050.0050.030.010.020.030.130.021.090.120.16


Depth(m)


GL-17-059 2 of 4 7550250 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

280

260

240

220

200

dark greyish green; fine grained-aphanitic; amygdular pillowed basalt (andesite) xenolith. Moderate pervasive chl-carb alteration; moderate-strongly magnetic. Interval contains a 1-1.5m long crosscutting aphanitic ultramafic (gabbro?)dyke. The lower contact of the basalt (andesite) runs parallel to the core axis for around 1m. Unit contains abundance of crosscutting carb and chl-carb FF stringers; some displaying ptygmatic folds. Trace dis and FF pydark grey/blue. Medium grained. Pervasive; weak-moderate sil alteration; pervasive weak chl alteration. Mineralized by py and trace PO. BQE's present throughout interval. Localized vein/veinlet offset and vein/veinlet/stringer crosscutting

UPDATE DEPTH TO*** dark greyish green; fine grained-aphanitic; amygdular pillowed basalt (andesite). Moderate-strong pervasive chl-carb alteration; moderate-strongly magnetic. . Unit contains abundance of crosscutting carb and chl-carb FF stringers; some displaying ptygmatic folds. BQE's present within first 2-3m. Trace dis py. Possible ultramafic (Gabbro?) dyke crosscutting unit

0.040.0050.0050.010.010.030.010.39

0.0050.0050.0050.0050.0050.0050.0050.0050.04

0.0050.0050.0050.0050.230.02

0.0050.04

0.0050.0050.005

0.00250.00250.0025


Depth(m)


GL-17-059 3 of 4 7550250 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

320

300

Depth(m)


GL-17-059 4 of 4 7550250 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

80

60

40

20

0

dark greyish blue; medium grained granodiorite; mod pervasive sil alt; weak chl alt. Strong sil/kspar alt haloes around massive Q-QA veins. Crosscutting carbonate stringers. 1% dis py within groundmass; coarse cubic py within sil/kspar alt haloes. BQE's begin at around 51.5m

0.0050.0050.0050.0050.0050.0050.0050.0050.530.06

0.0050.0050.0050.0050.0050.11

0.0050.05338.540.110.490.330.021.341.550.080.04

0.0050.020.28

0.0050.040.26

0.0050.06

0.0050.730.06

0.0054.07


Depth(m)








GL-17-060 1 of 3 3210 20% % %

Angle toCore Axis3210

%

10.

750.5

0.250

180

160

140

120

100

dark grey feldspar porphyry. 1-5mm feldspar phenocrysts (40%) in a dark aphanitic weakly biotite/chlorite altered matrix. Localized Sil/Kspar alt haloes around massive Q veins. 1% dis py. Irregular lower contact angledark greyish blue; medium grained granodiorite; mod pervasive sil alt; weak-mod chl alt. Strong sil/kspar alt haloes around massive Q-QA veins. Localized hydrostatic fracture zones with strong sil/kspar alt. Crosscutting Q; QA veins/veinlets. 2% dis py within groundmass; 2-5% coarse cubic py within sil/kspar alt haloes; along with FF py. Gradational Lower contact; several meters long

0.281.450.240.370.3

0.560.540.520.770.250.390.21

0.0051.510.2

0.650.180.680.420.150.430.460.090.070.310.2

0.050.490.180.420.110.46

0.0050.010.03

0.0050.020.12

0.0050.010.020.030.2

0.470.2

0.0050.020.17

0.0050.050.150.08


Depth(m)


GL-17-060 2 of 3 3210 20% % %


%

10.

750.5

0.250

280

260

240

220

200

dark greyish green; fine grained-aphanitic; amygdular pillowed basalt (andesite). Moderate-strong pervasive chl-carb alteration; moderate-strongly magnetic. Unit contains abundance of crosscutting carb and chl-carb FF stringers; some displaying ptygmatic folds and boudinage. BQE's present within first 2-3m. Trace dis py.

0.040.0050.04

0.0050.14

0.0050.04

0.0050.0050.0050.01

0.0050.0050.0050.0050.040.04

0.0050.0050.0050.005

0.00250.00250.0025


Depth(m)


GL-17-060 3 of 3 3210 20% % %


%

10.

750.5

0.250

80

60

40

20

0

carbonate amygdules; weak chloritization; strong silification. amygdules w/ 30deg lineation.sharp contact w/ silica bleeding out from And along edges of unit. AND xenoliths following 30deg lineations at lower contact.carbonate amygdules; weak chloritization; strong silification. amygdules w/ 30deg lineations. flow lines trending 30deg.

0.0050.0050.0050.02

0.0050.0050.0050.0050.0050.02

0.0050.02

0.0050.0050.0050.0050.0050.0051.32

0.0050.0050.0050.02

0.0050.31

0.0050.0050.02

0.0050.0050.0050.010.180.09

0.0050.020.360.02

0.0050.020.030.030.210.29

F00006151F00006152F00006153F00006154F00006155F00006156F00006157F00006158F00006159F00006160F00006161F00006163F00006164F00006165F00006166F00006167F00006168F00006169F00006171F00006173F00006174F00006176F00006177F00006178F00006179F00006180F00006181F00006182F00006183F00006184F00006185F00006186F00006187F00006188F00006191F00006192F00006193F00006194F00006195F00006196F00006197F00006198F00006199F00006200

Depth(m)








GL-17-061 1 of 3 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

Kspar alteration in first 15cm of unit. Bound by upper contact and Qtz Massive vein. GRD xenolith in POR at lower contact.

0.10.02

0.0050.0050.020.01

0.0050.090.120.260.1

0.360.32

0.0050.040.080.060.190.080.020.060.920.150.220.030.080.310.020.070.060.02

0.0050.032.540.14

0.0050.030.01

0.0050.1

0.050.090.070.020.231.640.440.160.160.010.21

0.005


Depth(m)


GL-17-061 2 of 3 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

alternating between amygdules (carbonate filled) and flows approx. every 2m;

0.0050.02

0.0050.060.01

0.0050.0050.07

0.0050.0050.0050.020.02

0.0050.020.030.03

0.0050.010.06

0.0050.12

0.0050.020.010.01

0.0050.0050.040.020.01

0.0050.0050.0120.012


Depth(m)


GL-17-061 3 of 3 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

76

72

68

64

60

56

52

48

44

40

36

32

28

24

20

16

12

8

40 2.9-4.0m is cored GD - probable boulder;

some fracturing but no gossanous fractures as in bedrock; casing block marked @ 4.5m

increase in blue qtz to 15-20% from 42.0m - 51.04

FELSIC TUFF; small qtz 0.25-0.5mm

scattered patches of carb rich amygdules up to +/- 1cm; often stretched 1:4

0.0050.0050.0050.0052.080.285.240.03

0.0050.98

0.0050.250.250.120.03

0.0050.150.050.20.10.2

0.0050.0050.0050.010.38

0.00250.00250.00250.00250.0025


Depth(m)







Project: GoldlundLogged by: Richard KowalskiLog Completed: May-07-17Core Location: TENT

GL-17-062 1 of 1 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

carbonate amygdules

0.0530.0630.3050.0060.2470.370.010.010.250.41

0.0050.330.740.05

0.0050.130.140.490.470.020.016.493.070.474.271.060.30.2

0.910.171.386.650.050.030.050.030.070.020.050.040.050.010.140.030.03

F00008951F00008952F00008953F00008954F00008955F00008956F00008957F00008958F00008959F00008960F00008961F00008962F00008963F00008965F00008966F00008967F00008968F00008969F00008971F00008973F00008974F00008976F00008977F00008978F00008979F00008980F00008981F00008982F00008984F00008985F00008986F00008987F00008988F00008989F00008991F00008992F00008993F00008994F00008995F00008996F00008997F00008998F00008999F00009000F00009002

Depth(m)







Project: GoldlundLogged by: Andrew WiebeLog Completed: May-06-17Core Location: TENT

GL-17-063 1 of 3 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

190

180

170

160

150

140

130

120

110

100

FELSIC TUFF; fine grained matrix; 5-10% 0.25-1.0mm qtz

fine to locally medium grained; scattered patches of qtz carb amygdules stretched 1:4 up to 5mm; and rare to 1cm; irregular qtz carbonate stringers

0.040.190.020.241.820.290.270.120.030.070.1

0.120.020.060.260.11

0.0050.550.022.4

0.0050.020.020.070.110.420.340.140.570.02

0.0050.160.32

0.0050.0050.160.760.01

0.0050.00250.00250.00250.00250.0025

F00009003F00009004F00009006F00009007F00009008F00009011F00009012F00009013F00009014F00009015F00009016F00009017F00009018F00009020F00009021F00009022F00009023F00009024F00009025F00009026F00009027F00009028F00009029F00009031F00009032F00009034F00009036F00009037F00009038F00009039F00009040F00009041F00009042F00009043F00009045F00009046F00009047F00009048F00009049F00009051F00009052F00009053F00009054F00009055

Depth(m)


GL-17-063 2 of 3 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

200

Depth(m)


GL-17-063 3 of 3 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0moderately magnetic; grain size varies between fine and medium; 20deg; no observed lower contact angle due to gradational boundary

carbonate amygdules; moderately magnetic; flow lineations 25deg

0.00250.00250.006

0.00250.00250.0052.780.040.010.01

0.0050.0050.0050.030.020.01

0.0050.040.01

0.0050.190.033.64

0.0050.0050.0050.0050.005

F00008351F00008352F00008353F00008354F00008355F00008356F00008357F00008358F00008359F00008360F00008361F00008362F00008363F00008364F00008366F00008367F00008368F00008369F00008371F00008372F00008373F00008376F00008377F00008378F00008379F00008380F00008381F00008382

Depth(m)




Start Date: April-29-17End Date: May-03-17Drill Contractor: Rodren Drilling



Project: GoldlundLogged by: Andrew WiebeLog Completed: May-03-17Core Location: TENT

GL-17-064 1 of 3 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

0.0050.190.02

0.0050.050.020.020.030.020.76

0.0050.0050.0050.0050.02

0.0054.64

0.0050.005

0.10.140.290.470.290.010.010.180.230.13

0.0051.170.060.25

0.0050.0050.020.510.13

0.0050.060.332.990.02

0.0050.0050.0050.0050.0050.0050.0050.005


Depth(m)


GL-17-064 2 of 3 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

strong sericitization and silicification of GRD unit; fine grained QTZ eyes.

carbonate amygdules; flow lineations 25deg

0.0050.02

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.016

0.00250.011

0.0025


Depth(m)


GL-17-064 3 of 3 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

lower contact has no clear angle; gradational change in grain size; medium muscovite grains at 53.4m.

Depth(m)








GL-17-065 1 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

1000.005

0.00250.0060.0080.0070.0050.0050.0050.0050.0050.0050.0050.0050.07

0.0050.0050.0050.0050.0050.0050.0050.0050.15

0.0050.0050.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.030.050.01

0.005

F00008801F00008802F00008803F00008804F00008805F00008806F00008807F00008808F00008809F00008810F00008811F00008812F00008813F00008814F00008815F00008817F00008818F00008819F00008821F00008822F00008823F00008826F00008827F00008828F00008829F00008830F00008831F00008832F00008833F00008834F00008835F00008836F00008837F00008839F00008841F00008842F00008843F00008844F00008845F00008846F00008847F00008848F00008849F00008850F00008852

Depth(m)


GL-17-065 2 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

moderately magnetic; flow lineations 15deg

0.180.020.130.070.180.171.250.040.030.920.291.931.831.227.221.971.350.170.980.090.290.02

0.0050.110.01

0.0050.010.380.560.132.250.290.040.390.011.954.55

11.820.631.514.822.770.641.491.161.630.190.02

0.0050.041.62


Depth(m)


GL-17-065 3 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

360

340

320

300 weakly magnetic; flow lineations 20deg

flow lineations 25deg; no amygdules; frequent fluid alteration. GRD Dyke from 314.73 to 314.86m w/ sharp contact; 5cm true width; 18deg TCA; weak CARB and CHL INT alteration.

deuteric alteration; strong silicification and seritization

carbonate amygdules

0.110.16

0.0050.00250.009

0.00250.00250.0390.005

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.0025


Depth(m)


GL-17-065 4 of 4 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0light blueish-grey; fine grained; sil-chl altered granodiorite. Crosscut by Q;QA veins/veinlets at 30-40 degrees tca. Mineralized by fg dis; ff; and cx Py; Po; and Mag. Majority of mineralization occurs in sil alt haloes around QA veins. Unit is crosscut by Andesite xeno

light blueish-grey; fine grained; sil-chl altered granodiorite. Crosscut by Q;QA veins/veinlets at 30-40 degrees tca. Mineralized by fg dis; ff; and cx Py; Po; and Mag. Majority of mineralization occurs in sil alt haloes around QA veins. Strong localized Hem alt between 72-78m; localized foliation/banding; localized mod-strong hydrothermal ser alt between 119-135m

0.060.040.170.020.370.420.140.390.020.3

0.080.212.1

0.040.030.1

0.0050.0050.05

0.0050.140.020.04

11.070.030.050.03

0.0050.110.050.06

0.0050.080.140.130.060.030.570.280.1

3.440.1

0.03


Depth(m)








GL-17-066 1 of 2 3210 20% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

170

160

150

140

130

120

110

100

0.180.120.050.060.041.2

0.34

0.020.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.08

0.0050.0050.0050.005

0.00250.00250.0025


Depth(m)


GL-17-066 2 of 2 3210 20% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

Dark bluish grey; fine grained; granodiorite. Crosscut with QA; QC; and QCCHL veins/veinlets. Moderate sil; chlorite and carbonate alteration throughout; with sil-kspar haloes around vein sets. Most mineralization occurs within the alteration haloes as fg dis; cx cubic; and ff py and po. Unit is cross cut by 4m long portion of andesite; possibly sluffed off of main andesite body during intrusion. Sharp low angle lower contact

1.040.02

0.0050.0051.631.64

0.0050.01

0.0050.0050.040.060.050.080.160.020.481.920.130.1

0.0050.0050.570.110.790.070.020.040.080.060.030.1

0.080.130.120.130.080.090.450.020.060.02

0.005


Depth(m)








GL-17-067 1 of 3 3210 100% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

190

180

170

160

150

140

130

120

110

100

dark greenish grey; fine grained; amygdular andesite. Chlorite and carb altered. 0.9m grd xeno within unit. sharp upper and lower low angle contactsDark bluish grey; fine grained; granodiorite. Crosscut with QA; QC; and (predominantly) QCCHL veins/veinlets. Moderate sil; chlorite and carbonate alteration throughout; with sil haloes around vein sets. Trace mineralization occurs within the alteration haloes as fg dis; cx cubic; and ff py; along with fg dis mag . Unit contains several andesite xeno's under 0.5m long; possibly sluffed off of main andesite body during intrusion. Sharp low angle lower contact

dark greenish grey; fine grained; amygdular/pillowed andesite. Chlorite and carb altered.

0.130.011.39

0.0050.0050.140.3

1.430.08

0.0050.23

0.0050.0050.0050.0050.020.030.08

0.0050.0050.09

0.0050.0050.020.150.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005

0.00250.00250.005

0.00250.008

F00015051F00015052F00015053F00015054F00015056F00015057F00015058F00015061F00015062F00015063F00015064F00015065F00015066F00015067F00015068F00015069F00015070F00015071F00015073F00015074F00015075F00015076F00015077F00015078F00015079F00015081F00015082F00015084F00015086F00015087F00015088F00015089F00015090F00015091F00015092F00015094F00015095F00015096F00015097F00015098F00015099F00015101F00015103F00015104F00015105F00015106F00015107F00015108F00015109F00015110

Depth(m)


GL-17-067 2 of 3 3210 100% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

210

200

Depth(m)


GL-17-067 3 of 3 3210 100% % %

Angle toCore Axis3

2.752.

52.

252

%

10.

750.5

0.250

80

60

40

20

0Greyish-green; fine to locally medium grained chl/bt/carb altered Gabbro. Crosscut by QC veins and veinlets. Weak-moderately magnetic. Trace fg dis py/po within groundmass. Gradational lower contact between Gabbro and Andesite

dark greyish-green; fine grained andesite with localized amygdules and pillows. Localized foliation. Trace fg dis py. Sharp low angle contact between andesite and granodiorite

light blueish grey; fine grained; sil-chl altered (with local hem alt and a zone of strongly hydrothermal alt of ser) granodiorite. Crosscut by Q; QA; and QCCHL veins/veinlets. Locally mineralized with fg dis py; cx py; and ff py. Several fault/fracture zones. Highest amounts of mineralization occur around and within QA veins in a Sil/Sil-Kspar alt halo. Py altering to Po locally. Moderately magnetic throughout; BQE's throughout. Low angle sharp contact between grd and and

0.00250.00250.00250.00250.00250.0050.180.410.2

0.0050.010.020.010.1

0.010.160.05

0.0050.0050.06

0.0050.0050.0050.0050.04

0.005


Depth(m)








GL-17-068 1 of 3 3210 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

180

160

140

120

100

0.0050.38

0.0050.0050.0050.0050.0050.11

0.0050.01

0.0050.040.050.220.510.230.250.070.190.010.090.24

0.0050.040.280.090.661.863.790.090.510.270.030.65

0.0050.011.020.220.05

0.0050.0050.042.250.020.74

16.060.340.020.010.02

0.005


Depth(m)


GL-17-068 2 of 3 3210 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

260

240

220

200

0.0050.0050.010.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005

0.00250.00250.00250.00250.0025


Depth(m)


GL-17-068 3 of 3 3210 20% % %

Angle toCore Axis2

1.51

0.50

%

10.

750.5

0.250

80

60

40

20

0light greyish green; fine-coarse grained; chl-carb altered gabbro. Crosscut by QC veins; C stringers; and andesite xenoliths. Coarse grained amphiboles; locally dis leucoxene and minor ank alt. Fault with gouge at around 83-86. Trace dis and blebby py/po

Depth(m)







Project: GoldlundLogged by: Joseph WiebeLog Completed: May-04-17Core Location: TENT

GL-17-069 1 of 4 3210 20% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

180

160

140

120

100

light blueish grey; fine-locally medium grained; sil-chl altered granodiorite. Crosscut by an andesite xenolith and flow gneiss. Localized hem alt and sil-kspar alt around QA veins. Strong mineralization from 240-307m; very fine grained dis VG at 273.62 in a QA-T vein within a Sil/kspar alt halo. Localized crackle brecciation; especially in some of the more mineralized zones. localized weak foliation.

light blueish grey; fine-locally medium grained; sil-chl altered granodiorite. Crosscut by an andesite xenolith and flow gneiss. Localized hem alt and sil-kspar alt around QA veins. Strong mineralization from 240-307m; very fine grained dis VG at 273.62 in a QA-T vein within a Sil/kspar alt halo. Localized crackle brecciation; especially in some of the more mineralized zones. localized weak foliation.

0.00250.00250.00250.027

0.00250.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.01

0.0050.0050.01

0.0050.005

0.10.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.360.010.01


Depth(m)


GL-17-069 2 of 4 3210 20% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

280

260

240

220

200

0.020.0050.07

0.0050.0050.0050.01

0.0050.070.010.060.02

0.0050.0050.0050.0050.0050.0050.030.030.07

13.930.390.030.710.8

0.780.640.860.70.1

2.191.3

0.135.9

0.470.080.160.134.140.134.940.020.010.180.080.370.840.031.640.681.06


Depth(m)


GL-17-069 3 of 4 3210 20% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

320

300

0.613.7

4.670.1

0.150.190.11

0.0050.00250.00250.00250.00250.0025

F00015422F00015423F00015424F00015426F00015427F00015428F00015431F00015432F00015433F00015434F00015435F00015436F00015437

Depth(m)


GL-17-069 4 of 4 3210 20% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

68

64

60

56

52

48

44

40

36

32

28

24

20

16

12

8

40

Blue Qtz visible 0.0050.0050.005

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.006

0.00250.00250.00250.00250.006

0.00250.00250.00250.00250.00250.00250.00250.0025


Depth(m)


Claim ID: KRL23114Easting: 545449.97 mENorthing: 5527201.61 mNElevation: 386.83 mASL Core Size: HQ





Project: GoldlundLogged by: Aaron AnsteyLog Completed: February-16-17Core Location: TENT

GL-17-070 1 of 1 3210 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

85

80

75

70

65

60

55

50

45

40

35

30

25

20

15

10

5

0

0.330.190.410.440.250.322.320.2

0.370.740.722.440.151.130.370.810.580.720.915.531.880.590.630.060.160.23

0.0050.0050.0050.0050.0050.0050.005

0.00250.006


Depth(m)








GL-17-071 1 of 1 3210 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

1.161.710.030.230.10.2

0.030.161.120.281.592.160.320.520.771.420.390.320.290.380.010.271.150.490.140.130.030.182.230.550.120.732.9

1.550.170.4

0.460.330.11


Depth(m)








GL-17-072 1 of 3 2

1.51

0.50 20

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

190

180

170

160

150

140

130

120

110

100

blue Qtz still visible up until contact with andesite

0.030.0050.020.030.03

0.0050.0050.0050.0050.0050.0050.0050.01

0.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.010.02

0.0050.0050.0050.0050.0050.0270.0180.007


Depth(m)


GL-17-072 2 of 3 2

1.51

0.50 20

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

210

200

Depth(m)


GL-17-072 3 of 3 2

1.51

0.50 20

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

dark to medium greenish-gray; massive granodiorite; fg to locally mg; chlorite altered groundmass; mt-rich; crosscut by numerous qtz veins with sil-kspr-mt-haloes

0.040.005

0.56.910.020.070.020.06

0.0050.010.020.340.139.050.240.1

1.780.88

0.0050.830.2

0.010.0050.661.080.010.060.2

0.020.140.19

36.530.960.030.030.092.940.04


Depth(m)







Project: GoldlundLogged by: John CamierLog Completed: February-22-17Core Location: TENT

GL-17-073 1 of 2 7550250 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

170

160

150

140

130

120

110

100 pinkish gray porphyritic unit with 20-25% albitic plagioclase + lesser K-spr phenocrysts set within a fg crystalline groundmass of quartz-biotite with sharp upper and lower intrusive contactsContact aureole (zone) between GRD and And (basalts); large xenoliths of pillowed basalts supported within granodiorite intrusion; xenoliths display contact shear (induced foliation) edges at between 20 and 25 deg TCA

Cg feldspar porphyry intrusion crosscutting contact zone between GRD and And (pillowed basalts); contacts sharpContact aureole (zone) continuation between GRD and And (basalts); large xenoliths of pillowed basalts supported within granodiorite intrusion; xenoliths display contact shear (induced foliation) edgesAndesite; pillowed tholeiitic ocean floor basalts (high Fe-Mg) with well developed amygdules (qtz-carb) defining pillow edges and vfg selvages between pillows; unit is strongly chloritized (greenschist facies)

0.020.260.03

0.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.01

0.0050.040.01

0.0050.0050.0050.008

0.00250.0025

F00012295F00012296F00012297F00012298F00012299F00012301F00012302F00012303F00012304F00012306F00012307F00012308F00012309F00012311F00012312F00012313F00012314F00012316F00012317F00012318F00012319F00012320F00012321

Depth(m)


GL-17-073 2 of 2 7550250 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

pale greenish gray fg to mg; moderately to strongly silicified with weakly chloritized groundmass granodiorite; unit crosscut by numerous qtz and qtz-carb veins with kspr and minor albitization haloes; unit is variably sulphidized

0.0050.02

0.0050.420.090.680.040.031.150.090.050.010.910.150.020.11

0.0050.180.030.030.024.181.720.1

0.0050.29

0.0050.182.160.060.510.120.520.590.180.110.020.090.28

10.54


Depth(m)







Project: GoldlundLogged by: John CamierLog Completed: February-25-17Core Location: TENT

GL-17-074 1 of 3 151050 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

mg to cg fsp porphyry with fg groundmass of bio-mt; plag>ksprpale greenish gray fg to mg; moderately to strongly silicified with weakly chloritized groundmass granodiorite; unit crosscut by numerous qtz and qtz-carb veins with kspr and minor albitization haloes; unit is variably sulphidized

strongly to intensely chloritized mafic rocks; amygdaloidal basalt grading into finely laminated narrow tuffaceous units with ptygmatic folding of qtz-carb veins suggestive of shear lineations at 30 degTCAweakly chloritized light gray possible felsic (dacitic) tuffaceous units alternating with narrow mafic tuffaceous units; unit is finely laminated at 35 degTCA with individual thicker beds readily visible

strongly chloritized fg grading into mg gabbroic unit with readily visible bio-mt altered amph phenocrysts at 20-25%; strongly magnetic; amph 2-3mm dia.; 5-10% blue quartz eyes within the unit; weak foliation at 30degTCA

0.360.0050.0050.190.050.01

0.0050.08

0.0050.040.09

0.0050.0050.11

0.0050.030.090.010.040.040.130.1

0.030.005

0.10.250.070.03

0.0050.02

0.0050.01

0.0050.0050.007

0.0025


Depth(m)


GL-17-074 2 of 3 151050 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

240

220

200EOH; dark green strongly to intensely chloritized amygdaloidal basalt with well defined pillows and selvages; amygdule and vesicles are qtz-carb filled; unit foliated at 30 degTCA

Depth(m)


GL-17-074 3 of 3 151050 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

light greenish gray fg-mg granodiorite with mm sized blue qtz eyes interstitial to the groundmass; mt-biotite after amph; unit is weakly to moderately magnetic; weak ser alteration; silicified; unit is crosscut by qtz-carb veins with strong to weak kspr-alb alteration and cubic py

0.040.090.140.910.040.06

0.0050.131.160.16

0.0050.82

0.0050.02

0.0050.11

0.0050.030.080.01

0.0050.04

0.0050.020.370.050.06

0.0050.031.26

0.0050.030.020.1

0.020.02

0.0050.0050.0050.02


Depth(m)








GL-17-075 1 of 4 151050 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

mg-cg plag porphyry with plag>>kspr; 25-30%; 0.3-0.8cm diameter phenocrysts are set in a fg kspr-qtz-bio-mt groundmass with trace py grains and aggregates; some phenos exhibit zonation with plag coreslight greenish gray fg-mg granodiorite with mm sized blue qtz eyes interstitial to the groundmass; mt-biotite after amph; unit is weakly to moderately magnetic; weak ser alteration; silicified; unit is crosscut by qtz-carb veins with strong to weak kspr-alb alteration and cubic py

green strongly to intensely chloritized + carb altered vesicular andesite with fg groundmass

2.190.020.02

0.0050.010.080.03

0.0050.050.03

0.0050.11

0.0050.040.120.03

0.0050.030.09

0.0050.0050.01

0.0050.0050.03

0.0050.0050.0050.010.050.02

0.0050.02

0.0050.0050.0050.0050.020.020.030.020.090.03

0.0050.0050.030.03

0.0050.005

0.00250.0025


Depth(m)


GL-17-075 2 of 4 151050 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

5-10% blue qtz eyes supported in the groundmass

light greenish gray fg-mg granodiorite with mm sized blue qtz eyes interstitial to the groundmass; mt-biotite after amph; unit is weakly to moderately magnetic; weak ser alteration; silicified; unit is crosscut by qtz-carb veins with strong to weak kspr-alb alteration and cubic py

dark green intensely chloritized vesicular tholiietic basalt of alternating flows and pillows; unit is strongly chl-carb altered and crosscut by numerous qtz-carb and carb veins and veinlets

Depth(m)


GL-17-075 3 of 4 151050 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

300

Depth(m)


GL-17-075 4 of 4 151050 100% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

Light gray; massive; fg-mg; weakly to moderately foliated and jointed; strongly to narrow sections with local intense silicification + potassic +/- albite +/- carb-ankerite alteration associated with qtz veins/veinlets and localized qtz flooding; upper section of the grd unit displays near surface meteoric weathering with dissolution and hematization of py grains within the groundmass and qtz vein alteration halos; localized sections of bleaching due to hydrothermal alteration yielding a strongly to intensely silicified +/-sericitic alteration zone with wispy to feathery contact edges suggestive of fluid migration

0.010.470.020.040.01

0.0050.020.020.040.050.230.17

0.0050.12

0.0050.10.1

0.0050.2412.40.160.230.960.02

0.0050.0050.0050.0050.0050.010.01

0.0050.0050.010.030.010.06

0.0050.330.050.21


Depth(m)








GL-17-076 1 of 2 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

170

160

150

140

130

120

110

100

Moderate to dark olive green; strongly chloritized andesitic to basaltic greenschist; unit is strongly FeO-altered along the contact with the granodiorite with formation of contact thermal metamorphic magnetite (mt) yielding a strongly magnetic unit that weakens significantly with distance from the contact; upper section of the greenschist unit is comprised of massive andesitic flow(s) that transition into pillows outlined with amygdules and separated by selvages and hyaloclastites; unit is strongly foliated (schistose); weakly to moderately silicified and metamorphosed to lower- to mid-greenschist facies with the rock comprised predominately of chlorite-plagioclase microlites-act/trem-mt-carbonate + fg biotite

0.120.210.03

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.02

0.00250.00250.00250.00250.0025


Depth(m)


GL-17-076 2 of 2 151050

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

variably altered fg to mg; massive light gray chloritized-silicified and weakly to moderately to locally intense potassic alteration associated with crosscutting variably mineralized qtz-carb-albite-tourmaline veins; upper section of the borehole is fragmental with lim-goeth clays and hematite alteration coating fracture walls; some fractures display slickenfibres in the carb-chl wall coatings when not covered in lim-goeth clays; weak to locally strong foliation developed within the granodiorite; numerous narrow to wide crosscutting qtz +/- carb +/- albite +/- tourmaline generally display wide alteration halos with varying amounts of sulphides predominantly py as fg-cg cubic subhedral to euhedral grains from 1-15%; several intensely hydrothermally altered sections occur within the rock exhibiting near complete silicification + potassic alteration overprinting/replacing the grd textures; which supports py mineralization and several clouds of visible Au

0.140.010.03

0.0050.020.220.76

0.0050.02

0.0050.890.042.080.040.020.270.110.8

0.690.010.140.08

0.0050.240.061.75

0.0050.04

0.0051.990.040.390.030.030.180.010.030.590.050.01

0.005


Depth(m)








GL-17-077 1 of 3 3210 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

190

180

170

160

150

140

130

120

110

100intensely silicified-sericitized and potassic altd porcelain textured tannish gray rock from hydrothermal alteration (deuteric) with primary textures predominantly masked by the alteration; contacts are fairly sharp but wispy with strong silicification; almost cherty; along the edges of the alteration frontvariably altered fg to mg; massive light gray chloritized-silicified and weakly to moderately to locally intense potassic alteration associated with crosscutting variably mineralized qtz-carb-albite-tourmaline veins; upper section of the borehole is fragmental with lim-goeth clays and hematite alteration coating fracture walls; some fractures display slickenfibres in the carb-chl wall coatings when not covered in lim-goeth clays; weak to locally strong foliation developed within the granodiorite; numerous narrow to wide crosscutting qtz +/- carb +/- albite +/- tourmaline generally display wide alteration halos with varying amounts of sulphides predominantly py as fg-cg cubic subhedral to euhedral grains from 1-15%; several intensely hydrothermally altered sections occur within the rock exhibiting near complete silicification + potassic alteration overprinting/replacing the grd textures; which supports py mineralization and several clouds of visible Aubluish olive green strongly chloritized massive andesitic flow with mg subhedral sericitized feldspars intermixed with 10% blue qtz eyes and 10-15% fg mt grains in a fg mafic groundmassintensely silicified-sericitized and sericitized (potassic) altd porcelain textured tannish gray rock from hydrothermal alteration (deuteric) with primary textures predominantly masked by the alteration; contacts are fairly sharp but wispy with strong silicification; almost cherty; along the edges of the alteration front

bluish olive green strongly chloritized massive andesitic flow with mg subhedral sericitized feldspars intermixed with 10% blue qtz eyes and 10-15% fg mt grains in a fg mafic groundmass; unit appears to be overturned;

0.240.1

0.080.380.03

0.0050.0051.87

0.0050.030.08

0.0050.0050.01

0.0050.0050.081.82

0.0050.03

0.0050.0051.320.020.010.01

0.0050.013

0.00250.00250.00250.00250.0025


Depth(m)


GL-17-077 2 of 3 3210 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

210

200

eyes up hole in the section; grading into finer-grained material downhole towards lower contact with pillowsolive green strongly chloritized pillows outlined with white qtz-carb amygdules outlining the well developed pillows separated with selvages and hyaloclastite breccias in mafic pillowed meta-basalt

Depth(m)


GL-17-077 3 of 3 3210 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

massive; fg to mg; olive green; strongly chloritized gabbroic rock with 40-45% whitish green subhedral plagioclase phenocrysts set in a fg olive green chloritized amph-pyroxene groundmass; with decrease in plag content and increase in mg-cg amph-pyx phenocrysts downhole

olive green vfg to fg mafic volcanic flows; pillows and tuff beds; pillows are amygdaloidal; with variolitic texture of qtz-carb filled vesicles; unit is crosscut by numerous qtz-carb veins of varying thickness and are often boudinaged; tuff beds occur between 75.25 and 78.10m depth; meta-volcanics are strongly schistose

0.008 F00002509

Depth(m)








GL-17-078 1 of 3 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100 fg to mg; massive light to medium gray granodiorite apophysis/dyke off main grd intrusion; unit is weakly chloritized and displays interstitial carb alteration along grain boundaries and as joint cement; and contains 10-15% blue qtz eyes supported in a blue-gray glassy qtzo-feldspathic groundmass; ferromagnesian minerals of vfg-fg chl-mt-bio occur interstitial to the qtzo-feldspathic groundmassolive green chloritized metavolcanics unit displaying variolites; same as the unit between 40.75 and 98.11mfg to mg; massive; light gray to medium gray grd; unit is weakly to moderately chloritized and displays interstitial to grain boundaries carb alteration and as joint cement intermixed with qtz and chl; groundmass is comprised of grayish blue transparent qtzo-feldspathic groundmass intermixed with a vfg-fg grainy to felty and accicular interstitial ferromagnesian minerals (chl-biotite-act/trem) supporting 0.1-0.3cm diameter 10-15% blue qtz eyes; sulphides are generally disseminated or occur within hydrothermal vein alteration halos

0.00250.00250.0110.0080.0050.0050.0050.0050.0050.0050.0050.0050.05

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.03

0.0050.0050.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005


Depth(m)


GL-17-078 2 of 3 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

260

240

220

200

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.01

0.0050.02

0.0050.0050.0050.02

0.0050.050.02

0.0050.005

F00003871F00003872F00003873F00003874F00003875F00003876F00003878F00003879F00003880F00003881F00003882F00003883F00003884F00003885F00003886F00003887F00003889F00003890F00003892F00003894F00003895F00003896F00003897F00003898F00003900F00003901F00003902F00003903F00003904F00003905

Depth(m)


GL-17-078 3 of 3 151050 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

Alternating mafic meta-volcanic pillows; flows; lapilli and tuff beds; intensely chloritized; locally silicified; carb-altd; fg to mg; strongly foliated (schistose); and crosscut by numerous qtz-carb veins/veinlets some of which display boudinaged textures

Light greenish gray massive fg-mg strongly silicified to locally intensely silicified and potassic altd; unit is comprised of milky white blue qtzo-feldspathic groundmass with interstitial felty masses of chl intermixed with accicular to bladed act/trem + subhedral to euhedral grainy mt + variably sericitized subhedral plagioclase microlites and carb (cte); supporting anhedral rounded to subrounded grains of blue qtz eyes and finely disseminated py+/-po; the unit is crosscut by qtz + qtz-carb veinlets with occasional 1cm+ veins supporting ankerite clots and occasional albite that can display narrow to wide sil-potassic alteration halos supporting variable amounts of sulphides (py); the grd is metamorphosed to mid-greenschist facies

0.00250.00250.00250.00250.00250.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.020.02

0.005

F00001613F00001614F00001615F00001616F00001617F00001618F00001619F00001620F00001621F00001622F00001624F00001625F00001626F00001627F00001628F00001629F00001630F00001631F00001633F00001634F00001636F00001638

Depth(m)








GL-17-079 1 of 3 1

0.750.

5

0.250

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

190

180

170

160

150

140

130

120

110

100

and/or qtzo-feldspathic banding/segregations; sections within the unit exhibit moderate to strong to locally intense hydrothermal alteration (sil-potassic +/- ser) giving the rock a glassy siliceous wavy to feathery texture

0.0050.0050.0050.0050.0050.0050.0050.02

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.010.13

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005


Depth(m)


GL-17-079 2 of 3 1

0.750.

5

0.250

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

200

0.0050.0050.0050.0050.005

F00001700F00001701F00001703F00001704F00001705

Depth(m)


GL-17-079 3 of 3 1

0.750.

5

0.250

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

olive green fg-mg gabbro with gabbroic texture of white felspars supported in a moderately to strongly chloritized amph groundmass; unit is crosscut by numerous metamorphic qtz-carb veinlets and veins; weakly to strongly foliated

light olive green strongly chloritized and weakly silicified mafic flows and pillows; pillows outlined by amygdules and selvages; flows and pillows separated by mafic meta-volcanic tuffs

Depth(m)








GL-17-080 1 of 4 1

0.750.

5

0.25

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100 light greenish gray fg-mg; silicified and chloritized granodioritic unit with weak foliation and crosscut by narrow 1-2mm wide conjugate veinlets and joints; 1-2mm wide conjugate joints cemented by muscovite-qtz-carb and chl

0.0080.00250.0120.008

0.00250.0050.0050.0050.0050.0050.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.01

0.0050.0050.0050.0050.020.02

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005


Depth(m)


GL-17-080 2 of 4 1

0.750.

5

0.25

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

dark olive green fg-mg And with ~5-10% blue qtz eyes + 10-15% (up to 20%) clots of fg subhedral mt aggregates in a strongly chloritized dark greenish-black amph-plagioclase groundmass intermixed with felty chlorite-act-trem; unit displays weak sericitization as vfg whitish-silver grainy coating on feldspars within the groundmass; minor trace to 0.5% disseminated py-po-ccp

0.0050.0050.04

0.0050.0050.0050.0050.0050.0050.0050.0050.07

0.0050.0050.0050.0050.0050.22

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005

0.00250.00250.00250.00250.0025

F00001768F00001769F00001770F00001771F00001772F00001774F00001775F00001776F00001777F00001778F00001779F00001780F00001781F00001782F00001783F00001784F00001786F00001788F00001789F00001791F00001792F00001793F00001794F00001795F00001796F00001798F00001799F00001800F00001801F00001803F00001804F00001805F00001806F00001807

Depth(m)


GL-17-080 3 of 4 1

0.750.

5

0.25

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

Massive aphanitic to fine-grained andesite with small stretched amygdules that go in and out in places; moderately magnetic; lower contact is gradational over one to two cm approx. parallel to the foliation and undulating somewhat.

Massive fine to medium-grained gabbro that is less distinct at the top but obvious below about 73.5 m; weakly to occasionally moderately magnetic; lower contact is indistinct at the base of a 2 m long coarse-grained section of gabbro where the dark clots fade to nothing

0.00250.00250.00250.0025

F00001808F00001809F00001810F00001811

Depth(m)








GL-17-081 1 of 4 2

1.51

0.50

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

180

160

140

120

100

Aphanitic to fine-grained andesite with small stretched amygdules that go in and out very distinctly; moderately magnetic; from 113.0 to 113.5 m there is a well banded felsic tuff or sediment with sharp contacts at about 52 degrees TCA; bottom 70 cm have a mix of ghostly amygdules and blue quartz eyes; lower contact is disrupted by a 2 cm wide quartz-carbonate vein.Fine to mostly medium-grained granodiorite that has more massive sections along with more foliated sections that are in and out; moderately magnetic; lower contact is sharp and straight

0.00250.00250.0490.0190.0180.0050.12

0.0050.0050.0050.0050.0050.01

0.0050.0050.005

0.10.0050.0050.0050.0050.0050.01

0.0050.0050.0050.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.010.02

0.005


Depth(m)


GL-17-081 2 of 4 2

1.51

0.50

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

280

260

240

220

200

Felsic Tuff; fine-grained massive to banded; logged as dacite because there is no other choice; lower contact is sharp and straightFine to medium-grained granodiorite; moderately magnetic; Felsic Tuff in part of the core between 241.4 and 241.8 m with sharp; sometimes serrated highly irregular contacts; the lower contact is sharp; partly obscured by veining and highly irregular and convoluted

Massive to weakly banded on a cm scale FELSIC TUFF (logged as dacite) with a fine-grained matrix containing about 4-5% altered quartz eyes? to about 1 mm in size; nonmagnetic; from about 246.1 to 247.1 m is a section that probably is an intermediate flow (Dacite); this has about 5% blue quartz eyes and this is strongly magnetic; the lower contact is sharp but slightly undulatingIntermediate flow that is massive and medium grained; moderately to strongly magnetic; Tuff has about 2-3% blue to grey quartz eyes to 1.0 mm; from 251.9 to the base Felsic tuff is irregularity mixed with the Dacite; the lower contact is sharp and highly irregular but the base is at about 22 degrees TCAMassive to weakly banded on a cm scale FELSIC TUFF (logged as dacite) with a fine-grained matrix containing about 3% altered quartz eyes? to about 1 mm in size; nonmagnetic to weakly magnetic; the lower contact is sharp and straightAphanitic to fine-grained andesite with a few small stretched amygdules; moderately magnetic; from 258.8 m to the base; felsic tuff is irregularity intermixed with the andesite; lower contact is sharp and slightly undulating.

0.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005

0.00250.00250.00250.00250.00250.00250.0025


Depth(m)


GL-17-081 3 of 4 2

1.51

0.50

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

300

banded on a cm scale FELSIC TUFF (logged as dacite) with a fine-grained matrix containing about 8% altered quartz eyes? to about 1 mm in size; nonmagnetic to weakly magnetic; the lower contact is sharp and slightly undulating to slightly irregularFine-grained andesite with a few small stretched amygdules; moderately magnetic; top 60 cm has a about 5% blue quartz eyes; lower contact was not drilled

Depth(m)


GL-17-081 4 of 4 2

1.51

0.50

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

blue qtz eye's exist throughout grd up until contact with and

0.090.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005

0.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005


Depth(m)







Project: GoldlundLogged by: Joseph WiebeLog Completed: January-22-17Core Location: TENT

GL-17-082 1 of 2 3210 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

120

110

100

0.0050.0050.0050.005

0.00250.00250.00250.00250.00250.0025

0.0025

F00014146F00014148F00014149F00014150F00014151F00014152F00014153F00014154F00014156F00014158F00014159

Depth(m)


GL-17-082 2 of 2 3210 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

blue qtz eye grd begins around 59.36 0.010.0050.0050.250.080.11

0.0050.0050.74

0.0050.040.510.07

0.0050.040.010.130.010.150.090.350.190.46

0.0050.0050.0050.0050.0050.0050.0050.005

0.00250.00250.00250.00250.00250.0025

F00014201F00014202F00014203F00014204F00014205F00014206F00014207F00014208F00014209F00014210F00014211F00014212F00014214

F00014215AF00014216AF00014217AF00014218AF00014219AF00014221AF00014222AF00014223AF00014226AF00014227AF00014228F00014229F00014230F00014231F00014232F00014233F00014234F00014235F00014236F00014237F00014238F00014241F00014242F00014243

Depth(m)








GL-17-083 1 of 2 151050 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

110

100

0.00250.00250.00250.00250.00250.00250.0025

0.0025

F00014244F00014245F00014246F00014247F00014248F00014249F00014251F00014252

Depth(m)


GL-17-083 2 of 2 151050 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

blue qtz eye grd starts around 92m 1.870.050.030.220.040.02

0.0050.330.010.140.030.220.020.02

0.0050.25

0.00541.930.030.230.090.140.3

1.210.380.283.094.950.438.440.5

1.310.462.640.02

F00014351F00014352F00014353F00014354F00014355F00014356F00014357F00014358F00014360F00014361F00014362F00014363F00014364

F00014365AF00014366AF00014367AF00014368AF00014369AF00014371AF00014372AF00014373AF00014376AF00014377AF00014378F00014379F00014380F00014381F00014382F00014383F00014384F00014386F00014387F00014388F00014389F00014391

Depth(m)








GL-17-084 1 of 2 151050 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

170

160

150

140

130

120

110

100irregular lower contactirregular lower contact

0.220.0050.0050.0050.0050.0050.0050.0050.0050.560.040.04

0.0050.005

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.0070.006

0.00250.007

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.0025


Depth(m)


GL-17-084 2 of 2 151050 20% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

blue quartz eye's from 18.65-35.40 0.0050.0050.0050.020.13

0.0050.05

0.0050.03

0.0050.16

0.0050.05

0.0050.0050.0050.061.410.25

0.0050.0050.0050.0050.02

0.0050.1

0.060.0050.170.04

0.0050.0050.022.390.14

0.005

F00014551F00014552F00014553F00014554F00014555F00014556F00014557F00014559

F00014560AF00014561AF00014562AF00014563AF00014564AF00014565AF00014566AF00014567AF00014568AF00014569AF00014571AF00014573AF00014574AF00014576AF00014577AF00014578AF00014579AF00014580AF00014581AF00014582AF00014583AF00014584AF00014585AF00014586AF00014587AF00014588AF00014591AF00014592A

Depth(m)








GL-17-085 1 of 2 2

1.51

0.50 210

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

170

160

150

140

130

120

110

100

blue quartz eyes seen around 129m

0.030.03

0.0050.0050.0050.0050.02

0.0050.0050.0050.04

0.0050.0050.0050.0050.02

0.0050.0050.0050.0050.0050.005

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.0025

F00014593AF00014594AF00014595AF00014596AF00014597AF00014598AF00014599AF00014601AF00014602AF00014603AF00014604AF00014606AF00014607AF00014609AF00014611AF00014612AF00014613AF00014614AF00014615AF00014616AF00014617AF00014618AF00014620F00014621F00014622F00014623F00014624F00014625F00014626F00014627F00014628F00014629F00014631F00014632F00014634F00014636F00014637F00014638F00014639F00014640F00014642F00014643

Depth(m)


GL-17-085 2 of 2 2

1.51

0.50 210

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

85

80

75

70

65

60

55

50

45

40

35

30

25

20

15

10

5

0 Casing extended to 11m; core from 8.9m

medium to fine grained

well foliated 73.95-75m in contact with GD; moderate irregular qtz carb stringers and patches of epi alteration

0.010.02

0.0050.010.020.01

0.0050.020.02

0.0050.0050.040.02

0.0050.020.030.030.020.73

0.0050.020.05

0.0050.020.020.010.03

0.0050.110.050.010.07

0.0050.005

0.00250.00250.0025


Depth(m)








GL-17-086 1 of 2 2

1.51

0.50 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

100

95patches of amygdules and local primary qtz carb stringers and flow

Depth(m)


GL-17-086 2 of 2 2

1.51

0.50 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0 casing to 9.0m; core starts at 7.5m

massive medium to fine grained. 0.0050.0050.0050.0050.0050.0050.0050.02

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.02

0.0050.0050.0050.0050.01

0.0050.0050.0050.01


Depth(m)








GL-17-087 1 of 2 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

140

130

120

110

100

massive; numerous primary irregular QC stringers

0.0050.0050.02

0.0050.060.1

0.0050.0050.0050.02

0.0050.0050.0050.005

0.00250.00250.00250.0025


Depth(m)


GL-17-087 2 of 2 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

brecciated lower contact with Felsic Tuff

FELSIC TUFF; fine grained; variably sericite / potassic altered; fine magnetite and trace fine py generally throughout; small qtz 0.25-0.50mm

Granodiorite; fine to medium grained; with larger blue qtz up to 5mm. dark; matrix is weakly to moderately sheared; however blue qtz eyes fairly rounded and pristine. Appears locally dacitic? Lower contact with Andesite shallow with steepening along foliation @ 32 deg TCA. Fspar Porphyry 78m-78.4m: contacts 8-15 deg TCA

Massive; weak to moderately foliated; occasional 1-2m sections with amygdules up to 5mm; generally stretched 2or3:1. Several

0.0050.0050.0050.005

0.00250.00250.00250.009

0.00250.00250.00250.00250.00250.00250.00250.00250.0110.009

0.00250.00250.00250.021

0.00250.00250.00250.0050.0050.0050.0050.0050.0050.01

0.0050.0050.01

0.0050.0050.0050.005

0.00250.025


Depth(m)








GL-17-088 1 of 3 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

stringers and veinlets

Intermediate Tuff; moderately sheared; 15-20 qtz up to 6mm strained 1.5 to 2:1 with pressure shadowsFelsic Tuff; moderate thin intermediate banding first 10m. Strongly sheared to 129m; then moderate decreasing to weak by end of interval; pressure shadows of qtz well developed to 130m. Granodiorite intrusion with irregular contacts +/- 30 deg TCA from 137.95-138.35mGranodiorite; medium to fine grained; moderately sheared. Felsic tuff interflow 144.55m - 145.20m 10 deg TCA and 147.2m-147.75m 25-30deg TCAFelsic tuff; QFP 155.8-157.5m

Granodiorite; sheared; lower contact with tuff //'l TCAFelsic Tuff interbedded with granodiorite to contact with Andesitemoderately to strongly foliated; irregular thin primary qtz carbonate stringers and veinlets; Granodiorite 173.73-178.43m 25 deg TCAweakly sheared; phenos stretched and altered 5:1 in central coreFG And; scattered amygdules stretched generally 4:1; numerous irregular primary qtz-carbonate stringers and veinlets

0.00250.006

0.00250.006

0.00250.006

0.00250.00250.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.005

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.023

0.00250.00250.00250.00250.006

0.00250.01

0.00250.00250.009

0.00250.0140.0110.0120.0070.006

0.00250.00250.0025

F00009138F00009139F00009141F00009142F00009143F00009144F00009146F00009147F00009148F00009151F00009152F00009153F00009154F00009155F00009156F00009157F00009158F00009159F00009160F00009161F00009162F00009163F00009164F00009166F00009167F00009168F00009169F00009171F00009172F00009174F00009176F00009177F00009178F00009179F00009180F00009181F00009182F00009183F00009185F00009186F00009187F00009188F00009189F00009191F00009192F00009193F00009194F00009195F00009196F00009197

Depth(m)


GL-17-088 2 of 3 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

240

220

200

Depth(m)


GL-17-088 3 of 3 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

85

80

75

70

65

60

55

50

45

40

35

30

25

20

15

10

5

0

0.010.29

0.0050.0050.080.420.310.03

0.0050.0050.010.361.491.1

0.010.040.461.19

0.00250.0025


F00015767F00015769

Depth(m)







Project: GoldlundLogged by: Adam RichardsonLog Completed: May-13-17Core Location: TENT

GL-17-089 1 of 1 3210 1

0.50

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

0.0050.030.01

0.0050.0050.0050.020.010.060.020.030.010.030.010.030.020.02

0.0050.050.01

0.0050.0050.030.030.010.050.04

0.0050.0050.0050.0050.0050.29

0.0050.050.4

0.361.160.260.010.030.03


Depth(m)








GL-17-091 1 of 2 3210

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

170

160

150

140

130

120

110

100

quartz feldspar

pillowed basalt/andesite

0.020.070.080.3

0.130.530.780.240.620.370.040.030.110.570.260.04

0.0050.030.10.2

0.020.005

0.00250.00250.0025

F00015717F00015718F00015719F00015720F00015721F00015722F00015723F00015724F00015725F00015726F00015727F00015728F00015729F00015731F00015732F00015733F00015734F00015735F00015737F00015739F00015740F00015742F00015743F00015744F00015746

Depth(m)


GL-17-091 2 of 2 3210

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

light gray with greenish tinge from interstitial chl alteration to strongly silicified groundmass; groundmass comprised of fg bio-mt-fsp(plag>kspr)-chl supporting 5-10%; loc 15%; phaneritic blue qtz eyes between 1-2mm dia; fsp are weakly ser-altd

dark green mafic volcanic alternating units of flows; tuff beds and pillows with strong metamorphic foliation at 15-30 degTCA; intense chl alteration in the mafic greenschist; tuff beds are alternating mafic to felsic

0.0050.410.717.51

0.0050.591.150.260.771.740.790.02

0.0050.009

0.0025

F00013151F00013152F00013153F00013154F00013155F00013156F00013157F00013158F00013159F00013160F00013161F00013162F00013164F00013165F00013166

Depth(m)








GL-17-092 1 of 2 151050 18

17.517

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

110

100

Depth(m)


GL-17-092 2 of 2 151050 18

17.517

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

0.0050.16

0.0050.5

0.050.01

0.0050.130.030.110.021.080.540.29

0.0050.060.090.09

0.0050.0050.0050.02

0.0050.0050.0050.0050.0050.0050.0050.02

0.0050.0050.0050.0050.0050.005


Depth(m)








GL-17-093 1 of 3 1

0.750.

5

0.250 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

Contact changed from 130.20 to 111.5 on review

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005


Depth(m)


GL-17-093 2 of 3 1

0.750.

5

0.250 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

240

220

200

massive quartz vein with chl alteration

0.0050.0050.0050.0050.0050.0050.0050.0050.005

0.00250.00250.007

0.00250.00250.0025

0.010.00250.00250.00250.00250.0025


Depth(m)


GL-17-093 3 of 3 1

0.750.

5

0.250 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

0.020.020.040.023.360.06

0.0050.0050.0050.450.020.030.020.02

0.0050.0050.0050.05

0.0050.0050.0050.03

0.0050.0050.34

0.0050.02

0.0050.05

0.0050.0050.0050.02

0.0050.010.030.01


Depth(m)








GL-17-094 1 of 4 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

coarse grained andesite. seem to be drilling along contact zone

0.020.0050.18

0.0050.0050.0050.04

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005

0.00250.00250.008

0.00250.008

0.00250.007

0.00250.0080.01

0.0060.00250.0060.008

0.00250.01

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.0025


Depth(m)


GL-17-094 2 of 4 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

coarse to fine grained andesite; amygdaloidal

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.008

0.00250.007

0.00250.00250.00250.00250.00250.00250.005

0.00250.00250.00250.00250.00250.00250.00250.006

0.00250.00250.00250.00250.00250.00250.0060.005

0.00250.00250.00250.00250.00250.00250.00250.0025

F00016054F00016055F00016057F00016058F00016059F00016060F00016061F00016062F00016063F00016064F00016066F00016067F00016068F00016069F00016071F00016073F00016074F00016075F00016076F00016077F00016078F00016079F00016080F00016081F00016082F00016083F00016084F00016086F00016087F00016088F00016089F00016091F00016092F00016093F00016094F00016096F00016097F00016098F00016100F00016101F00016102F00016103F00016104F00016105F00016106F00016107F00016108F00016109

Depth(m)


GL-17-094 3 of 4 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

300

Depth(m)


GL-17-094 4 of 4 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

0.20.020.010.010.11

0.0050.480.010.04

0.0050.0050.0050.0050.0050.0050.0050.140.01

0.0050.0050.0050.0050.0050.0050.0050.02

0.0050.040.07

0.0050.010.030.37

0.0050.030.06

0.005


Depth(m)








GL-17-095 1 of 3 3210 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

blue qtz visible

coarse grained andesite. massive qtz veining with Ccp; Py and Po

0.0050.03

0.0050.010.010.030.040.051.850.150.02

0.0050.020.03

0.0050.0050.010.01

0.0050.0050.0050.0050.06

0.0050.0050.0050.0050.0050.02

0.0050.0050.01

0.0050.02

0.0050.0050.0050.0050.04

0.0050.0050.0050.02

0.0050.0050.0050.005

0.00250.00250.00250.0025


Depth(m)


GL-17-095 2 of 3 3210 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

260

240

220

200

0.00250.00250.00250.00250.00250.00250.00250.00250.00250.00250.007

0.00250.00250.00250.006

0.00250.0110.0090.007

0.00250.00250.00250.00250.00250.00250.00250.0190.0060.01

0.00250.0060.0120.0090.006

0.0025


Depth(m)


GL-17-095 3 of 3 3210 3

2.52

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

85

80

75

70

65

60

55

50

45

40

35

30

25

20

15

10

5

0

pillowed basalt

0.0050.050.212.050.36

0.0050.04

0.0050.05

0.0050.640.170.860.462.150.81.6

0.851.660.08

0.0050.00250.00250.00250.00250.0025


Depth(m)








GL-17-096 1 of 2 3210 1

0.50

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

105

100

95

Depth(m)


GL-17-096 2 of 2 3210 1

0.50

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

0.010.0050.020.090.020.040.02

0.0050.26

0.0050.06

0.0050.0050.080.280.03

0.0050.070.010.060.260.620.244.230.240.226.180.150.190.960.160.150.050.960.4

0.261.26

0.00250.00250.1380.076


Depth(m)








GL-17-097 1 of 2 3210 1

0.50

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

140

130

120

110

100

1.1850.032

F00015877F00015879

Depth(m)


GL-17-097 2 of 2 3210 1

0.50

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

0.0050.0050.0050.01

0.0050.01

0.0050.0050.0050.0050.020.040.040.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.222.220.080.010.120.02


Depth(m)








GL-17-098 1 of 2 3210

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

150

140

130

120

110

100

pillowed basalt

0.170.080.540.140.09

0.0050.005

0.00250.00250.0025

F00015817F00015818F00015820F00015821F00015822F00015823F00015824F00015825F00015826F00015828

Depth(m)


GL-17-098 2 of 2 3210

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

40

0Medium to fine-grained Andesite; weakly to mostly moderately magnetic; possibly a few amygdules around 57 m; lower contact is sharp and straight

Depth(m)








GL-17-103 1 of 6 151050 100% % %

Angle toCore Axis18

17.7

517

.517

.2517

%

10.

750.5

0.250

160

120

Massive bull white quartz vein with a sharp slightly undulating lower contactMedium to fine-grained Andesite; Abundant large qtz veining within; weakly to mostly moderately magnetic; lower contact is sharp and straight

Massive bull white quartz vein; with pyrrhotite and chalcopyrite; with a sharp slightly undulating lower contactMedium to rarely fine-grained Andesite; weakly to mostly moderately magnetic; lower contact is sharp and straight

Massive fine-grained Intermediate dyke (granodiorite??) with a sharp straight lower contactMassive fine to dominantly medium-grained gabbro; weakly to generally moderately to strongly magnetic; lower contact is sharp and undulating

Depth(m)


GL-17-103 2 of 6 151050 100% % %

Angle toCore Axis18

17.7

517

.517

.2517

%

10.

750.5

0.250

280

240

200

Fine to medium-grained very massive granodiorite; weakly magnetic; lower contact is sharp and undulatingMassive fine to dominantly medium-grained gabbro; weakly to generally moderately magnetic; lower contact is sharp and undulating

Fine to medium-grained very massive granodiorite; weakly magnetic; lower contact is sharp and straightMedium to fine-grained Andesite; weakly to mostly moderately magnetic; lower contact is sharp and slightly undulating

Fine- to medium-grained massive light gray granodiorite; moderately magnetic; lower contact is sharp and slightly undulatingMassive pillowed And; light greenish gray; strongly silicified; mid greenschist facies; foliated; amygdaloidal; fg groundmass; crosscut by parallel-to-foliation qtz and qtz-carb veins/veinlets some of which display muscovite plates and books

light gray fg-mg chloritized granodiorite with 15-20% blue qtz eyes; unit is strongly magnetic in the upper section over several metres decreasing to moderately magnetic

0.0050.0050.0050.0050.005

F00002201F00002202F00002203F00002204F00002205

Depth(m)


GL-17-103 3 of 6 151050 100% % %

Angle toCore Axis18

17.7

517

.517

.2517

%

10.

750.5

0.250

360

320

olive green fg to mg strongly chloritized and

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.03

0.0050.020.050.020.010.110.065.760.580.971.392.050.1

0.260.466.66

45.456.850.86

0.0058.230.090.120.920.140.140.040.020.040.030.090.710.210.530.330.240.450.15

0.0050.01

0.0025


Depth(m)


GL-17-103 4 of 6 151050 100% % %

Angle toCore Axis18

17.7

517

.517

.2517

%

10.

750.5

0.250

480

440

400disseminated fg mt grains

aphanitic to fg light gray strongly silicified granodiorite dykeolive green fg to mg strongly chloritized and silicified gabbro supporting 10-15% disseminated fg mt grainsolive green to light olive greenish gray pillowed mafic basalts alternating with strongly chloritized vfg selvages separating the pillows and occasional lapilli tuff and banded tuffaceous horizonslight gray very fine-grained granodiorite dyke with vfg-fg blue qtz eyes (</=1mm) supported in a dark gray vfg-fg glassy groundmassolive green to light olive greenish gray pillowed mafic basalts alternating with strongly chloritized vfg selvages separating the pillows and occasional lapilli tuff and banded tuffaceous horizons

light gray very fine-grained granodiorite dyke with vfg blue qtz eyes (<1mm) supported in a dark gray vfg-fg glassy groundmassolive green to light olive greenish gray pillowed mafic meta-volcanic basalts alternating with strongly chloritized vfg selvages separating the pillows with flows separated by lapilli tuff horizons

0.00250.015

0.00250.0025

F00002269F00002270F00002271F00002272

Depth(m)


GL-17-103 5 of 6 151050 100% % %

Angle toCore Axis18

17.7

517

.517

.2517

%

10.

750.5

0.250

80

40

0massive; medium to fine grained; weak to locally moderately foliated. Occasional qtz carbonate stringers. Mafic dyke in shear zone 63.05-63.6m 50 deg TCA

Depth(m)








GL-17-104 1 of 5 2

1.51

0.50 210

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

160

120

moderately foliated; carb altered larger fspars ; moderate irregular qtz carb stringers

coarse grained massive equigranular Andesite; possibly a medium grained diorite?; weakly foliated; occasional Qtz-carb stringer

weakly foliated

massive; weak to moderate foliated; strong qtz carb stringers and flooding; lower contact with GD gradational over 0.8m; sheared; with boudinaged qtz-carb; and 30% irregular GD patchesGD; fine grained; strongly altered with qtz carb stringers; patches of intensely qtz-carb-chlorite+/- biotite altered and strained intervals of andesite wall rock from 145.05-161.0m

weakly foliated; 1-3mm carb amygdales stretched 2:1

fine to medium grained; moderately foliated; LC with Andesite irregular and brecciated

Depth(m)


GL-17-104 2 of 5 2

1.51

0.50 210

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

240

200locally coarse grained; GD 232.60-232.8m 47 deg TCA; //'l to foliation

moderate to well foliated

fine grained GD 269.46-269.56mfine grained; weakly foliatedweak to moderately foliated

patchy chlorite; carbonatefine grained flow; numerous qtz-carb vein and stringers; larger (1-4cm) veins display tension gashes. Scattered 2-3% amygdules up to; 2X5mm; rarely to 10mm

Depth(m)


GL-17-104 3 of 5 2

1.51

0.50 210

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

360

320

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.06

0.0050.020.020.140.190.040.040.44

0.0050.060.020.030.06

0.0050.012.061.7

0.210.2

0.050.0050.010.010.08

0.0050.04

0.0050.04

0.0050.220.130.08


Depth(m)


GL-17-104 4 of 5 2

1.51

0.50 210

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

480

440

400

weakly foliated; feldspar porphyry dyke @422.56-422.59m; 422.66-422.68m; both 35deg and from 423.36-423.73m irregular trending 5deg 2cm true width. Feldspar Porphyry appears to be same as the unit starting at 427m.

medium grained feldspars phenocrysts in a quartz-feldspar ground mass. Irregular QC veining with a fault constrained to this unit. very fine grained pyrite; magnetite within ground mass; weakly magnetic.andesitic tuff; 5% carbonate amygdules. GRD dyke from 433.26 to 433.38; 45deg; two carbonate veins constrained to dyke and orthogonal to contacts but taper out before contacts with AND; possibly contraction veins.same as POR unit from 427-430.54 but more abundant sulphides in ground mass.

0.010.04

0.0050.060.03

0.0050.290.240.04

0.005

0.0050.0050.04

0.0050.0050.0050.0050.020.030.02

0.020.030.010.03


Depth(m)


GL-17-104 5 of 5 2

1.51

0.50 210

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

80

70

60

50

40

30

20

10

0

Blue quartz eye's between 31-66.23m 0.040.07

0.0050.05

0.0050.01

0.0059.140.03

0.0050.0050.330.08

0.0050.0050.090.03

0.0050.010.260.03

0.0050.050.020.1

0.060.050.090.02

0.0050.0050.0050.112.86

0.005


Depth(m)







Project: GoldlundLogged by: Joseph WiebeLog Completed: February-03-17Core Location: TENT

GL-17-105 1 of 3 3210 32% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

190

180

170

160

150

140

130

120

110

100

Blue quartz visible in small Grd section

0.170.150.080.240.650.490.04

0.0050.05

0.0050.270.8

0.020.070.270.060.010.150.6

0.020.1

0.090.180.070.040.070.130.010.01

0.0050.03

0.0050.010.020.02

0.0050.0050.0050.0050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.02


Depth(m)


GL-17-105 2 of 3 3210 32% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

200

0.0050.0050.0050.005

F00016802F00016804F00016805F00016806

Depth(m)


GL-17-105 3 of 3 3210 32% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

40

0

0.0050.0050.0050.0050.010.030.02

0.0050.0050.0050.0050.0050.0050.0050.0050.160.020.01

0.0050.0050.060.23

0.0050.080.080.150.250.34

0.0050.0050.620.171.982.520.230.761.470.37

0.005


Depth(m)








GL-17-106 1 of 5 3210 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

160

120

0.0050.0050.0050.08

0.0050.140.230.080.140.030.220.070.120.1

0.020.090.07

0.0050.090.240.050.040.020.230.250.670.020.730.050.280.060.040.020.050.350.180.090.860.140.030.110.210.010.291.480.010.040.85

0.00543.280.67


Depth(m)


GL-17-106 2 of 5 3210 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

280

240

200

Added by BB from core photos

6.910.190.470.160.430.010.110.040.220.380.430.110.081.530.130.290.121.2

4.974.210.1

2.190.461.393.92

13.518.351.423.291.410.864.660.050.190.28

13.880.021.070.380.110.170.050.1

0.160.050.020.150.060.020.060.21


Depth(m)


GL-17-106 3 of 5 3210 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

360

320

pale grey; mg grd; locally strong magnetism; strong silica halos; weak to strong kspar halos; strong pervasive silicification; moderate interstitial carbonate. fg interstitial chl-bt-mag-carb.

0.0050.060.030.05

F00014967F00014968F00014969F00014970

Depth(m)


GL-17-106 4 of 5 3210 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

480

440

400

Depth(m)


GL-17-106 5 of 5 3210 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

80

60

40

20

0

0.110.020.05

0.0050.240.03

0.0050.760.120.350.16

0.0050.050.4

0.0050.020.04

0.0050.240.01

0.0050.230.020.78

0.0050.0050.13

0.0050.030.020.74

0.0050.030.050.010.078.820.03

0.0050.45


Depth(m)








GL-17-107 1 of 3 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

0.470.170.4

0.680.09

0.0050.170.060.120.09

0.0050.070.920.48

13.921.530.030.530.590.1

0.160.990.08

0.0050.090.750.070.080.040.3

0.020.190.15

0.0050.030.080.470.110.020.530.850.320.2

4.040.7

2.460.41

0.0050.02

0.0050.27


Depth(m)


GL-17-107 2 of 3 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200

9.171.680.020.030.330.410.04

0.0050.16

0.0054.851.33

0.0050.00250.00250.00250.00250.00250.0025


Depth(m)


GL-17-107 3 of 3 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

40

0

0.170.22

0.0050.0050.0050.0050.010.030.81

0.0050.02

0.0050.211.02

0.0050.0050.0050.0050.0050.140.19

0.0050.55

0.0050.06

0.0050.040.040.090.140.090.030.220.140.190.230.080.510.44


Depth(m)








GL-17-108 1 of 6 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

160

120

0.0050.0050.090.13

0.0050.090.030.040.330.033.870.02

0.0050.070.050.410.14

0.0050.0050.0050.010.1

0.020.270.230.120.020.080.810.970.390.980.390.2

0.030.10.1

0.270.06

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005


Depth(m)


GL-17-108 2 of 6 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

240

200

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.030.02

0.0050.010.04

0.0050.030.020.03

0.0050.0050.0050.0050.0050.010.54

0.0050.150.19

0.0050.010.980.27

0.0050.010.011.03

0.0050.0050.270.140.1

0.0050.050.350.050.080.010.140.13


Depth(m)


GL-17-108 3 of 6 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

360

320

pale grey fine grained grd; strong local magnetism; strong alteration halos and pervasive sil; interstitial carb; interstitial fg chl-bt-mt. xenolith of mafic intrusives from 410 to 413.4m.

0.674.130.030.020.510.2

0.020.1

0.110.05

0.0050.4

0.0050.441.1

1.570.020.02


Depth(m)


GL-17-108 4 of 6 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

480

440

400

QFP; intense sericite and strong hematite alteration; alteration has extensively replaced and obscures original rock; chill margins along contactspale grey fg grd; strong local magnetism

blackish grey fg plag; quartz with vfg groundmass of bt-mt-chl; strong sericite alteration; may be transitioning to gabbro compositionsee grd descriptions above; QCCHL veins w/ associated low sulphide content

Depth(m)


GL-17-108 5 of 6 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

520

Depth(m)


GL-17-108 6 of 6 3210 210% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

Massive fine to medium-grained gabbro that is more distinct at the top then near the base; weakly to generally moderately to strongly magnetic; possible small sections of much finer grained Andesite between 24.95 and 25.7 m and between 28 and 28.7 m; Possible Felsic to Intermediate Dyke between 42.3 an 42.5 m with sharp; weakly undulating contacts at 30 and 18 degrees TCA going downhole; larger Intermediate to Felsic Dyke between 44.0 and 44.6 m with sharp well defined contacts; thee upper one is undulating at 17 degrees TCA; the lower one is sharp and straight at 26 degrees TCA; lower contact is indistinct and gradational over a few dm

Aphanitic to fine-grained andesite with small stretched amygdules that go in and out very distinctly; weakly to moderately magnetic; from 73.05 to 73.4 m there is a well banded section that is probably strained; lower contact is sharp; irregular and possibly partly displaced.

Fine to mostly medium-grained granodiorite;

0.00250.0025

0.0180.00250.00250.00250.00250.0025

0.00250.00250.00250.00250.00250.00250.00250.043

0.00250.0050.01

0.005

F00001902F00001903

F00001904F00001905F00001906F00001907F00001908F00001909

F00001910F00001911F00001912F00001914F00001915F00001916F00001917F00001918F00001919F00001920F00001922F00001923

Depth(m)








GL-17-109 1 of 3 2

1.51

0.50

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

180

160

140

120

100

and highly irregular

Felsic Tuff; fine-grained to aphanitic; massive; generally weakly to sometimes moderately magnetic; logged as dacite because there is no other choice; three submeter sections of granodiorite intrusions all with sharp undulating (base of first dyke at 26 degrees TCA) to mostly highly irregular contacts; dykes are between 131.15-132.05; 138.4-138.85; and 138.95-139.2 m; lower contact is sharp and straight

Fine to mostly medium-grained granodiorite; moderately magnetic; section between 161.1-161.4 has a sharply defined; irregular piece of felsic tuff xenolith; lower contact is sharp and irregular

Felsic (Lapilli?) Tuff; fine-grained to aphanitic; massive; generally weakly to rarely moderately magnetic; logged as dacite because there is no other choice; two possible lapilli at 161.6; 164.35 m; lower contact is sharp and highly irregularFine to mostly medium-grained granodiorite; moderately magnetic; lower contact is sharp and slightly undulatingAphanitic to fine-grained andesite; weakly to mostly moderately magnetic; from 174.15 to 174.4 m; there is a patch of granodiorite; possibly a few amygdules; lower contact is sharp; slightly undulating

Fine to mostly medium-grained granodiorite;

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.040.060.020.02

0.0050.0050.0050.0050.0050.0050.005


Depth(m)


GL-17-109 2 of 3 2

1.51

0.50

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

260

240

220

200

missing in broken core; but only a little core is missingAphanitic to fine-grained andesite with small stretched amygdules especially in the upper 2/3 of the zone; weakly to mostly moderately magnetic; lower contact is sharp; slightly undulatingFine to mostly medium-grained granodiorite; moderately magnetic; weakly mineralized; lower contact is sharp and slightly wavy

Generally fine-grained andesite with a few small stretched amygdules; but from the top to about 236 m the andesite has a fine to barely medium-grained gabbroic texture and may be the core of a flow; moderately magnetic; from 226.8 to 227.3 m is a very fine-grained section that may be a mafic dyke with sharp; slightly undulating contacts at 45 and 43 degrees TCA respectively; lower contact is was not drilled

0.0050.0050.0050.0050.0050.0050.11

0.0050.06

0.0050.0050.020.040.080.05

0.00250.009

0.00250.00250.0025


Depth(m)


GL-17-109 3 of 3 2

1.51

0.50

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

80

40

0

Massive fine to medium-grained gabbro that is more distinct in some sections than in other sections as the grain size varies; probably from alteration and strain; weakly to generally moderately to strongly magnetic; from 29.3 to 29.85 is a mafic dyke? or andesite? with sharp undulating contacts at 53 and 36 degrees TCA respectively downhole; lower contact is sharp and straight

Fine-grained Intermediate dyke; no code for it so I am using mafic dyke; moderately

0.00250.00250.00250.00250.0025

0.00250.00250.0025

0.00250.00250.0060.0080.005

0.00250.0050.0070.0090.006

0.00250.007

0.00250.0025

F00002010F00002011F00002012F00002013F00002014

F00002015F00002016F00002017

F00002018F00002019F00002021F00002022F00002023F00002024F00002025F00002026F00002027F00002028

F00002030F00002031F00002032F00002035

Depth(m)








GL-17-110 1 of 5 3210 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

160

120

veinlets; very massive otherwise; has some grey quartz eyes; lower contact is sharp and straightMassive fine to dominantly medium-grained gabbro; bottom 1.5 m fines downhole to the contact; weakly to generally moderately to strongly magnetic; lower contact is sharp and somewhat irregular

Fine-grained to bandy subordinate bandy medium-grained Andesite with a few possible amygdules; weakly to moderately magnetic; lower contact is distinct at a selvage.

Fine-grained pillow lava with selvages here and there; one at 145 m has varioles parallel to the selvage; amygdules in patches; weakly to moderately magnetic; the lower contact is slightly disrupted by a carbonate rich veinlet and is otherwise basically straight to slightly undulating

Medium-grained granodiorite; moderately magnetic; lower contact is sharp and straightFine-grained very massive Intermediate dyke; no code for it so I am using mafic dyke; weakly magnetic; lower contact is sharp and straightMedium-grained to rarely fine-grained (especially near the base) granodiorite; moderately magnetic; lower contact is gradational over a few cm as the exact contact was obscured by alteration

0.00250.00250.013

0.00250.006

0.00250.00250.00250.007

0.00250.00250.00250.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.03

0.0050.0050.0050.005


Depth(m)


GL-17-110 2 of 5 3210 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

280

240

200 Fine-grained to bandy subordinate medium-grained Andesite with a few possible amygdules; weakly to moderately magnetic; lower contact is disrupted by veining over about 1 cm widthMedium-grained to rarely fine-grained (especially near the base) granodiorite; moderately magnetic; lower contact is sharp and slightly undulatingMedium-grained to fine-grained feldspar porphyry that is massive; feldspars reach 8 mm long and are subhedral to euhedral; slightly to dominantly nonmagnetic; the lower contact is sharp and slightly undulatingFine to medium-grained granodiorite; moderately magnetic; between 227.4 and 227.95 m is an Intermediate Dyke with sharp contacts; the upper one is at 32 degrees and is slightly undulating; the lower on is at 35 degrees and is straight; lower contact is at 35 degrees and is slightly displacedFine-grained very massive Intermediate dyke; no code for it so I am using mafic dyke; weakly magnetic; lower contact is sharp and slightly undulatingFine to medium-grained to massive granodiorite; relatively unaltered to 276 m; then altered by mineralization; moderately magnetic; two Feldspar Porphyry dykes with 20% feldspar phenocrysts wit sharp irregular contacts; the first between 245.55 and 245.85 m has contacts at about 13 degrees; the second between 250.6 and 251.15 m has contacts at very approximately 10 degrees; four more feldspar porphyry dykes with a few % feldspar phenocrysts; have sharp slightly undulating contacts; the upper one between 254.4 and 254.6 m has contacts a 25 and 22 degrees TCA respectively; the second one between 267.7-268.1 m has contacts at 29 and 30 degrees TCA; the third one between 271.8-272.0 m has contacts at 48 and 42 degrees; the fourth one between 273.45 and 273.55 m has contacts at 60 and 56 degrees TCA; lower contact is sharp and straight

0.0050.0050.0050.0050.0050.0050.02

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.05

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.04

0.0050.0050.0050.0050.0050.0050.0050.0050.040.2

0.040.0050.040.240.030.130.020.03


Depth(m)


GL-17-110 3 of 5 3210 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

360

320

0.660.020.010.551.750.020.223.051.230.020.2

0.380.124.230.080.48

0.0050.310.40.1

0.650.0050.241.470.071.041.230.480.1

0.040.532.070.680.080.610.270.240.030.120.410.050.370.811.650.010.09

0.0050.060.01

0.0050.14


Depth(m)


GL-17-110 4 of 5 3210 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

440

400 Fine-grained to dominantly medium-grained Andesite; moderately to mostly strongly magnetic; lower contact is sharp and straight

Felsic Tuff; fine-grained to aphanitic; massive; nonmagnetic; logged as dacite because there is no other choice; 18 cm long andesite fragment (lapilli) centered at 418.2 m; lower contact is sharp and slightly undulatingFine-grained pillow lava with selvages here and there that almost always have varioles associated with them parallel to the selvage; amygdules in patches; weakly to moderately magnetic; the lower contact was not drilled

3.130.55

0.0070.0025

0.010.00250.0025

F00002193F00002194F00002195F00002196F00002197F00002198F00002200

Depth(m)


GL-17-110 5 of 5 3210 210% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

90

85

80

75

70

65

60

55

50

45

40

35

30

25

20

15

10

5

0

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005


Depth(m)








GL-17-111 1 of 2 1

0.750.

5

0.25

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

105

100

95

0.0050.0050.0050.005

0.00250.00250.0025

F00015487F00015489F00015490F00015491F00015492F00015493F00015494

Depth(m)


GL-17-111 2 of 2 1

0.750.

5

0.25

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

80

60

40

20

0

light grey sheared quartz crystal tuff

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.01

0.0050.0050.0050.050.01

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005


Depth(m)








GL-17-112 1 of 4 3210 1

0.50

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

180

160

140

120

100

quartz feldspar porphyry

0.0050.01

0.0050.0050.0050.070.02

0.0050.01

0.0050.0050.0050.030.010.01

0.0050.06

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.020.03

0.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.0050.005


Depth(m)


GL-17-112 2 of 4 3210 1

0.50

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

280

260

240

220

200quartz feldspar

qfp

qfp

0.0050.0050.0050.020.040.03

0.0050.0050.040.02

0.0050.0050.0050.0050.0050.0050.0050.010.010.010.03

0.0050.0050.0050.0050.01

0.0050.0050.01

0.0050.01

0.0050.0050.0050.0050.040.02

0.0050.150.3

0.020.241.2

0.150.253.170.36

0.0050.005

0.00250.0025


Depth(m)


GL-17-112 3 of 4 3210 1

0.50

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

300

rhyolite/very fine grained silica rich volcanic rock

0.0025 F00015666

Depth(m)


GL-17-112 4 of 4 3210 1

0.50

% % %

Angle toCore Axis1

0.750.

50.

250

%

10.

750.5

0.250

90

85

80

75

70

65

60

55

50

45

40

35

30

25

20

15

10

5

0

0.430.01

0.0050.050.01

0.0050.150.04

0.0050.0050.0050.0050.0050.0050.0050.005

0.00250.00250.006

0.0025


Depth(m)








GL-17-113 1 of 1 1

0.750.

5

0.25

0.75

0.25

% % %

Angle toCore Axis1

0.750.

50.

25

%

10.

750.5

0.250

38 | P a g e

Appendix D: Cross Sections

Section Holes Page 545350 mE GL-17-092, GL-17-093, GL-17-094, and GL-17-095 1 545400 mE GL-17-082, GL-17-083, GL-17-084, GL-17-085, and GL-17-105 2 545450 mE GL-17-070, GL-17-071, GL-17-072, GL-17-073, GL-17-074, and GL-17-075 3 545500 mE GL-17-055, GL-17-056, GL-17-057, GL-17-058, GL-17-059, GL-17-060,

and GL-17-061 4

545550 mE GL-17-043, GL-17-044, GL-17-045, GL-17-046, GL-17-047, GL-17-048, and GL-17-049

5

545600 mE GL-17-030, GL-17-031, GL-17-032, GL-17-033, GL-17-034, GL-17-035, GL-17-036, and GL-17-037

6

545650 mE GL-17-016, GL-17-017, GL-17-018, GL-17-019, and GL-17-021 7 545700 mE GL-17-002, GL-17-003, GL-17-004, GL-17-005, GL-17-006, GL-17-007,

and GL-17-008 8

545750 mE GL-17-010, GL-17-011, GL-17-012, GL-17-013, and GL-17-014 9 545800 mE GL-17-023, GL-17-026, GL-17-027, GL-17-028, and GL-17-029 10 545850 mE GL-17-039, GL-17-040, GL-17-041, and GL-17-042 11 545900 mE GL-17-106, GL-17-107, GL-17-108, and GL-17 113 12 545950 mE GL-17-050, GL-17-051, GL-17-052, GL-17-053, and GL-17-054 13 546000 mE GL-17-062, GL-17-063, GL-17-064, and GL-17-065 14 546050 mE GL-17-066, GL-17-067, GL-17-068, GL-17-069 and GL-17-103 15 546100 mE GL-17-076, GL-17-077, and GL-17-078 16 546150 mE GL-17-079, GL-17-080, GL-17-081, and GL-17-104 17 546200 mE GL-17-109 and GL-17-110 18 546250 mE GL-17-111 and GL-17-112 19 546300 mE GL-17-086, GL-17-087, and GL-17-088 20 546350 mE GL-17-089 and GL-17-091 21 546400 mE GL-17-096, GL-17-097, and GL-17-098 22

5,527,000mN

5,527,000mN

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5,527,100mN

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Projection: UTM NAD 83 Zone 15

Goldlund Project, OntarioCross Section: E545350Looking East50 m Section Window

Scale: 1:1250

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GL-17-074239 m

GL-17-075284 m

GL-17-07065 m

GL-17-072206 m

GL-17-073164 m

GL-17-07186 m

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GL-17-059317 m

GL-17-060278 m

GL-17-061269 m

GL-17-057233 m

GL-17-058200 m

GL-17-055131 m

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GL-17-05659 m

GL-17-048302 m

GL-17-049326 m

GL-17-045302 m

GL-17-044200 m

GL-17-043107 m

GL-17-047278 m

GL-17-046209 m

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GL-17-036548 m

GL-17-037365 m

GL-17-034228 m

GL-17-035314 m

GL-17-030143 m

GL-17-031125 m

GL-17-032200 m

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5,527,200mN

5,527,200mN

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5,527,100mN

5,527,100mN

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GL-17-033 299 m

GL-17-017302 m

GL-17-021383 m

GL-17-016152 m

GL-17-019374 m

GL-17-018149 m

5,527,200mN

5,527,200mN

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GL-17-008300 m

GL-17-005656 m

GL-17-004257 m

GL-17-002158 m

GL-17-006326 m

GL-17-007293 m

GL-17-003302 m

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5,527,100mN

5,527,100mN

5,527,200mN

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GL-17-010629 m

GL-17-012299 m

GL-17-014371 m

GL-17-011152 m

GL-17-013275 m

5,527,100 mN

5,527,100 mN

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GL-17-028299 m

GL-17-029320 m

GL-17-027218 m

GL-17-026188 m

GL-17-023131 m

5,527,200mN5,527,300mN

5,527,300mN

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GL-17-042Exit Section370.82 m

GL-17-040173 m

GL-17-041347.26 m

GL-17-039327.6 m

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5,527,200mN

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GL-17-108500 m

GL-17-11389 m

GL-17-107269 m

GL-17-042Enter Section

370.77 m

GL-17-042450 m

GL-17-106455 m

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GL-17-052257 m

GL-17-050144 m

GL-17-053300 m

GL-17-054302 m


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GL-17-051Enter Section405.07 m

GL-17-065341 m

GL-17-051629 m

GL-17-06274 m

GL-17-063200 m

GL-17-064269 m

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GL-17-069320 m

GL-17-066164 m

GL-17-067206 m

GL-17-068248 m

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5,527,300mN

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5,527,200mN

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GL-17-078251 m

GL-17-103Enter Section418.69 m

GL-17-103491 m

GL-17-077206 m

GL-17-076176 m

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5,527,200mN

5,527,200mN

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GL-17-104443 m

GL-17-080284 m

GL-17-079200 m

GL-17-081275 m

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5,527,200mN

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GL-17-110431 m

GL-17-109251 m

5,527,100mN

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39 | P a g e

Appendix E: Assay Certificates

A full suite of assays can be found in the accompanying folder \Appendices\Appendix E . The sub folders have the assays certificates sorted by method.

40 | P a g e

Appendix F: SGS Analytical Guide

ANALYTICAL SERVICES

1

When you need:

• UNPARALLELED network of commercial and mine-site labs

• Uniform ANALYTICAL methods

• Unequalled analytical TECHNOLOGY to detect deeply buried deposits

• Secure Internet data access at https://qlab.sgs.com

Contact SGS to be sure

INDEXWELCOME TO SGS 2

QUALITY POLICY STATEMENT 4

CODE OF ETHICS 6

YOUR PARTNERSHIP WITH SGS 6

ON-SITE TESTING SERVICES 9

On-Site Labs 9Mobile Sample Preparation Units 10Core Logging Services 11

Portable XRF 12

COMMERCIAL TESTING SERVICES 13

Sample Administration 13 Sample Preparation 15Precious Metals 21Exploration-Grade Analysis 31Ore-Grade Analysis 48Control-Grade Analysis 53Commercial Trade Analysis 58Select Methods 60Ores and Commodities 64

ELEMENTS AND PACKAGES 70

MINERALOGY SERVICES 72

METALLURGY SERVICES 73

APPENDICES 75

Conversion Factors 75SGS Minerals Locations (Geochemistry) 78SGS Minerals Locations (Metallurgy) 84SGS Minerals Locations (Engineering Services) 86

www.sgs.com/geochemwww.sgs.com/metallurgy

Geochemical sampling and analysis is the basis for many decisions in exploration.WHEN YOU NEED TO BE SURE of procedures, protocols or lab practice, we hope that you will turn to our free publication.

Rocks to Results - A practical guide to laboratory operations.

Order yours online at www.sgs.com/geochem

2017

2 3

WELCOME TO SGSSGS was founded in 1878 and is recognized as the global leader in inspection, testing, verification and monitoring services for international trade in the minerals, agricultural, petroleum and consumer products sectors.

SGS operates a global network of over 2,000 offices and laboratories around the world and employees over 90,000 employees in 300+ countries.

SGS provides support to you as a strategic partner and a technical advisor. Through our unequalled global network of operations and laboratories, we deliver a broad spectrum of independent geochemical and metallurgical testing, process engineering and quality and quantification services for minerals, coal and coke, bio-fuels, non-ferrous metals, steel and steel- making raw materials, fertilizers, cement and industrial minerals.

The SGS Group has a unique depth and breadth of expertise and experience that can be accessed by clients from our global network.

USING THIS GUIDEThis guide details SGS’ core competencies in analytical services and is designed to help you choose the analytical methodology that most appropriately fits your needs. It will direct you to the right methodology for the type of sample, element and species of that element you need. It also helps you select the smallest number of methods you need so you can maximize your analytical dollar.

• This guide is divided into sections based on sample grade, analysis techniques and analyte offerings. The purpose of this guide is to provide the best SGS analytical services available in our core competencies.

• This guide includes an elements and packages table on page 70 with determinative procedures highlighted. This table groups elements into analytical schemes which you can use to pick the best analytical method for your needs.

This guide outlines the most common procedures required by the geological community. Regional capabilities can differ throughout the SGS network based on available equipment and expertise. Contact your regional client services representative for details and pricing. Samples can be submitted to any analytical laboratory in the SGS network for forwarding to the most appropriate SGS testing laboratory for that sample type, element and test method. If samples have to be shipped out you will be notified prior to shipping via our quotation and then our final data reports will note where the samples were processed.

This guide represents only a small selection of the methods available at SGS. Please contact us to obtain a quote for your particular program. We can help you and supply you with an individually tailored quotation and analysis program that meets all of your needs.

DEFINITIONSSGS’ analytical services are used by a broad spectrum of clients in the mining sector - from those needing analysis for property assessment during exploration to those needing analysis of metallurgical products, to those requiring commercial analysis for trade transactions. To support these various needs, we have organized our services into categories and have included short explanations concerning the purpose of a test, its advantages and limitations. The categories carry over into our method-coding nomenclature so you can be sure to get the method that is fit for your specific purpose.

Types of analyses offered by SGS include:

• Exploration-grade analysis – This class of analysis is intended for large scale reconnaissance exploration programs. Typically, such programs generate rock or soil samples with low metal contents. In general, the frequency of inserted quality control materials is a minimum of 11% and methods with upper measurement limits of about 1% are used.

• Ore-grade analysis – This group of tests is used when analysing medium to high grade mineralized rock or core samples containing percent levels of target elements. The data from these analyses are often used for resource/reserve estimation. In general, the frequency of inserted quality control materials is a minimum of 12% and select methods with upper limits of about 30% are used.

• Control-grade analysis – Also known as process control, metallurgical support or metal accounting, the data from control-grade analyses are used to monitor or control a metallurgical or mining process. The frequency of inserted quality control materials is a minimum of 18% to a maximum of 120%. Control-grade methods can analyse samples that contain up to 100% of the target element in some cases. High precision and accuracy is achieved using control-grade methodology and can be increased with the number of assays per sample.

4 5

• Commercial-grade analysis – Commercial-grade analyses provide high precision and accuracy data that can be used to finalise commercial transactions. This data is used for commercial contract settlement or assay exchange (party analysis) and to settle disputes between buyers and sellers of traded commodities (umpire analysis). The frequency of inserted quality control materials is a minimum of 125%. Commercial- grade methods can analyse samples that contain up to 100% of the target element.

ROCKS TO RESULTSFor more information and a background to the topics in this guide, please refer to our publication, Rocks to Results. This book provides geoscientists with an introduction to geoanalysis and is available at www.sgs.com/geochem.

QUALITY POLICY STATEMENTSGS is committed to customer satisfaction and providing a consistent level of quality service that sets the industry benchmark. The quality objectives that we measure and assess are:

• The delivery of high quality geochemical and mineralogical analyses of rocks, minerals, ores, and other materials in a timely manner.

• The use of methods which are suitably validated, fit-for-purpose and based on internationally recognized methods when possible.

• The use of a Quality Management System that strives to provide customer satisfaction by ensuring, through its documented policies and procedures, that all quality-related activity is clearly demonstrated, assessable and followed.

We will achieve this by:

• Being innovative and providing added-value to your product or service.

• Giving a committed team effort.

• Standardizing our processes.

• Using a Quality Management System that meets, as a minimum requirement, ISO 9001 and ISO/IEC 17025.

• Employing a detailed quality audit program that ensures corporate and customer feedback.

• Utilizing a continuous improvement system.

• The clever and extensive use of quality control and quality assurance to ensure delivery that exceeds the industry benchmark.

• Providing appropriate staff training.

• Reviewing our Quality System annually.

SGS management and staff are appropriately empowered to ensure these requirements are met. All employees and contractors are familiar with the requirements of the Quality Management System, the above objectives and process outcomes. We welcome your feedback on this program.

QUALITY AND RESPONSIVENESSSGS has an on-going intensive program to monitor quality. Supervised by dedicated quality management personnel, the program is proactively and continuously monitored. It enables us to react promptly to fluctuations in performance.

SGS labs follow a global procedure to select appropriate quality control materials. We define the specified frequency with appropriate acceptance and rejection data criteria for each of our methods. Data are monitored both short term and long term on a continuous basis. Client specific reports are generated with our SLIM (SGS Laboratory Information Management) system and are readily available. Please see our Laboratory Quality Control Summary at www.sgs.com/geochem for more details on these procedures.

This concern for quality extends to SGS’ market attitude. SGS recognises that not all analytical problems can be solved with routine methodology. We value close communication with you, not only to address individual sample situations, but also to address issues confronted by the minerals industry as a whole.

The backbone of the “local” service you receive at SGS laboratories is a global quality protocol used by over 300 SGS minerals analytical laboratories. It controls procedures and methodology, data management and reporting, quality control and governing activities, service attitudes and response. Thus you are assured of a uniform, standardized response from any SGS laboratory worldwide. You can trust us and rely upon us.

6 7

CODE OF ETHICSIntegrity is the core of SGS; it is the common thread through all our activities. Our ethical compliance program is based on our Code of Integrity and Professional Conduct, and ensures that the highest standards of integrity are applied to all of our activities worldwide in accordance with international best practice. It has been approved by the SGS Board of Directors and our Operations Council and all SGS employees are trained in it yearly.

The purpose of this code is to document rules of behavior and to provide guidance in our day-to-day business. These rules apply to all employees of SGS. Our joint venture partners, agents, intermediaries, consultants and subcontractors are also required to comply with them. It is the responsibility of all of us at SGS, at all levels of our organization, to live by our code.

Our code is explained in detail on our website and can be summarized by the following common sense principles:

• Do not do anything which you know or believe to be illegal or unethical.

• Do not use any company property for your own benefit.

• Do not engage in any transaction which does not have a genuine, legitimate business purpose.

• Ask yourself whether any contemplated transaction or business practice would withstand the scrutiny of the public eye if exposed.

• Do not do anything which could require you to be untruthful.

• Seek advice when in doubt.

YOUR PARTNERSHIP WITH SGSSGS’ Centres of Excellence conform to the ISO/IEC 17025 standard and most of our major regional facilities are ISO 9001 certified. SGS provides analytical services for every stage of your project.

• exploration

• developmental studies

• mine production

• shipment

• trade

• mine closure

ANALYTICAL METHODS AND LIMITSThere are several distinct stages in the evaluation of a project – from a grassroots exploration (early stage) to the final stages of process/grade control at mine development and operation. At each stage, the analytical technique should be carefully considered with respect to the needs of the program. For example, grassroots exploration generally requires methods based on a partial or weak extraction followed by multi-element analysis. In contrast, analyses for a feasibility stage program generally involve a complete digestion followed by the analysis of a specific elemental suite focused on pay and penalty elements.

In the early stages of exploration, precision at low concentrations, sensitivity and cost effectiveness are usually key when defining an anomaly. Accuracy might not be as important as the ability of the method to reproduce and detect subtle anomalies above background or threshold levels. A partial or weak extraction method that is followed by multi-element scans could be acceptable at this stage.

In process or grade control situations, both accuracy and precision are critical. A total dissolution of the sample followed by the analysis of specific elements is more appropriate.

Commercial transaction assays require highly precise and accurate assays involving classical methodology. Please see page 58 for details.

In mineral analysis, the concept and application of detection limit is not defined universally nor is it governed by a regulated policy. The terminology used to describe this concept is varied, misused and often confusing. The lower limit in SGS laboratories is frequently used to market method ranges and capabilities but depending upon how this limit is defined, developed and tested, these ranges and capabilities can be misleading. It is important when selecting a method, that all factors are considered.

• What are the elements of interest and their concentration range?

• What is the required precision at or near the concentration of the analyte of interest?

• What is the mineral composition or source of my samples and will this affect the detection limit for the elements of interest?

Method choice should not be exclusively selected based on the lower limit or without consideration of the points above. Limits must be well defined and established using rigorous studies that involve matrix equivalent samples taken through the entire method process and not simply by using a reagent or water blank. Statistical analysis must be used both to estimate

8 9

and test the lower limit at a suitable confidence level. At SGS, our labora-tories take pride in our determination of method/analyte specific limits to ensure that this limit can be confidently projected across a wide range of samples and is fit for purpose.

There are many different analytical methods available in the industry. More detailed descriptions of the common analytes, grades and methods follow in this guide and can help you with method selection. A more exhaustive list of methods is available at your local laboratory. An SGS professional is also always available to assist you with analytical technique selection.

ELECTRONIC DATA AVAILABILITYMany clients use our web-based data access tool “QLab” (https://qlab.sgs.com) for immediate and secure retrieval of their analytical data over the internet. QLab allows you to track the progress of samples and view information such as job status, turn-around-time, scheme/method, client-specific quality control data and the results of your analyses. To maintain the integrity of our sophisticated LIMS (Laboratory Information Management System), QLab does not access the database directly, but instead receives data transmissions on a regular basis.

REPORTINGAll results are reported electronically immediately upon completion. Fax and/or hardcopy can be sent - a fee may apply. Copies of all certificates and invoices are sent via PDF email to the address you specify. Our QLab data portal, located at https://qlab.sgs.com, is accessible over the internet. Reporting units can be specified as ppb, ppm, g/t, % or oz/tonne (as applicable).

DATA TURNAROUNDSamples are processed at each SGS laboratory as promptly as possible. Sample batches requiring turnaround commitments outside contracted arrangements should be discussed with the appropriate laboratory client services personnel.

FEES AND PAYMENT METHODSThis List of Services outlines the range of analytical services and methods offered by SGS. Please contact us for a quote. Payment terms are strictly 30 days for approved clients. Interest at 1.5% per month will be levied on overdue accounts. If credit has not been established, advance payment is required. SGS accepts payment by Visa or MasterCard in many locations. Please inquire.

ON-SITE TESTING SERVICESON-SITE LABSSGS offers design, construction and management services for on-site laboratories. No matter how remote your operation, SGS services can be brought to your site and tailored to your specific needs. SGS’s on-site laboratory expertise is unparalleled in the industry, with more than 80 on-site analytical laboratories currently in operation. We apply the same principles, procedures and quality standards to our outsourced laboratories that we do to our commercial labs.

Allowing SGS to design, staff and operate your lab will ensure that you have at your disposal a full scope of capabilities for the fast turn-around of accurate, reliable data needed to run and optimize your plant operations and confirm the value produced by your operations. Outsourcing of mine-site laboratories allows you to allocate capital and staff more efficiently, concentrate on your core competencies and ensure that the data you base important decisions upon is accurate and consistent. The impartiality of a third party outsourcing partner ensures your results are transparent and meet regulatory reporting requirements.

The SGS Build, Own, Operate, and Maintain (BOOM) initiative is available globally to the minerals industry. This program provides clients the opportunity to outsource capital requirements, engineering, construction, commissioning, maintenance and operation of non-core facilities.

10 11

MOBILE SAMPLE PREPARATION UNITS

SGS offers sample preparation services globally and we have many Mobile Sample Preparation Units (MSPU) in some of the most remote locations in the world. Our MSPUs allow you to access our trusted third party sample preparation services in locations that might not otherwise support laboratory facilities. An SGS-designed, staffed and operated MSPU is safe, efficient, well staffed and operationally stable, thus giving you better speed to market and a competitive edge. By choosing our mobile laboratory services, you will:

• Take advantage of SGS’s globally recognized technical expertise and laboratory quality management program.

• Reduce shipping delays.

• Benefit from fast turnaround and accurate, reliable geochemical and/or assay data.

• Gain flexibility by choosing the sample preparation protocol that best suits your needs.

• Gain NI 43-101/JORC defensible data with minimal operational demands on your project team.

• Allocate your financial and staff resources more effectively by focusing on the core aspects of your program.

CORE LOGGING SERVICESTo maximize the return of the considerable investment in obtaining core, SGS provides expert and innovative geological exploration services for comprehensive core characterization in gold and precious metals, base metals, iron ore, coal, uranium and industrial minerals. At the most basic level it may include manual logging by an experienced team of SGS geologists. Chemical and mineralogical data can be obtained by hand held XRF, hyperspectral infrared spectrometers, or portable XRD at the drill site or in an SGS facility, at a sampling frequency suitable to the project requirements.

Should a more comprehensive service be required, automated core logging is available via high resolution VNIR-SWIR hyperspectral scanning that generates objective and consistent digital mineralogy, core photographs and textural data that is easily exported into standard modeling databases. This capability can be installed in exploration camps, mine-sites, or any SGS lab facility. The processed data can be accessed digitally anywhere in the world in a cloud based system, or reviewed on a customized, interactive viewing table that allows actual-size visualization with mineralogical overlays. Archived core can also be scanned to provide security against potential future core loss.

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PORTABLE XRF Portable XRF spectrometers allow you to take the instrument to the sample, rather than the sample to the instrument. This is advantageous for use in the field at mobile sample preparation laboratories or in on-site laboratories where rapid semi-quantitative multi-element data can improve exploration and metallurgical process decision making. Qualitative base metal and mineralization pathfinder multi-element scan packages are available. This technique is significantly influenced by sample mineralogy, particle size and sample matrix. It is best used on pulverized samples. Precious metals, Au, Ag, Pt, Pd and Rh are not available using this technique.

SGS has reviewed and compared all of the portable XRF units currently on the market. This extensive development work with a wide range of mineralogical assemblages has allowed SGS to offer the following element suites:

HH XRF

MAJOR ELEMENTS BASE METALS OTHERS

Al Co As

Ca Cu Bi

Fe Mo Cr

K Ni Nb

Mg Pb Rb

Mn Zn Sb

S Se

Si Sr

Ti V

W

Zr

Elemental suites and reporting limits are established on a project basis. The precision and accuracy of this technique is suitable for identifying anomalous samples to aid in exploration target definition, but is not appropriate for use in resource calculations. This technique can also be used for relative metallurgical plant process control but is not appropriate for metal accounting or final product characterizations. Please inquire.

COMMERCIAL TESTING SERVICES Most SGS laboratories provide exploration clients with dedicated sample preparation areas. Our Centres of Excellence dedicated to geochemical analysis are located strategically around the globe in Belo Horizonte, Chita, Johannesburg, Lakefield, Lima, Perth and Vancouver. Refer to the directory at the end of this guide for location details.

SGS analysts perform quality, multi-element analyses that target a wide variety of elements in many types of sample matrices. We are firmly committed to advancing the technologies for ICP-AES and ICP-MS. This commitment ensures we deliver on our promise to provide benchmark-setting quality service. Your needs are unique; therefore we have both tailored analytical packages and high-level custom service offerings.

SAMPLE ADMINISTRATION

SAMPLE SUBMITTAL, COLLECTION AND PICK UPSamples can be submitted to the nearest SGS laboratory or sample preparation facility. When your samples are transported to SGS by a third party, please send notice of shipment dispatch directly to the SGS receiving laboratory. Please record the name of the freight company, date of dispatch, waybill numbers, number of pieces and number of samples. This ensures that we can help track overdue or missing shipments.

We recommend that all sample submissions be clearly labeled. Sample submissions that are poorly labeled or packaged can incur additional sorting charges. Please ensure that your sample documents have full details of the analytical tests you request and reporting details.

All sample shipments require a sample submittal form or letter with clear instructions to avoid delays. Sample submission forms can be found on our website at www.sgs.com/geochem. Samples will not be analyzed until we have complete instructions. The minimum information required to proceed is:

• Company name and complete address.

• Contact name.

• Details for distribution of reports and invoices.

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• Method codes.

• Instructions on sample preparation.

• List or range of sample numbers.

• Sample disposal / return requirements.

• Unusual sample characteristics.

• Warning if any samples are potentially hazardous.

To eliminate customs delays, please include the following information:

• Description of goods, such as “Geological sample for testing purposes only”.

• The receiving SGS laboratory will have the needed customs or quarantine certification to receive your submission promptly. Please contact the laboratory so we can provide the permit details that must be included with the transport documents prior to dispatch.

• Some national authorities require prior notification before samples can be received by certified laboratories. This includes NORM samples and International Soil Samples. SGS will facilitate this to avoid unnecessary delays in sample receipt. Please contact your local SGS representative.

Together, we can eliminate unnecessary delays and costs by using these sample submission protocols.

PKP01 Sample collection / pick up

LOG02 Pre-preparation processing, sorting, logging, boxing etc.

WGH79 Weighing of samples and reporting of weights

SAMPLE TRACKINGAll SGS laboratories run sophisticated LIMS systems, the SGS SLIM, which facilitates complete tracking of analyses throughout the laboratory. SLIM directly tracks all samples from the time they are received at the preparation facility until they are sent to an SGS Centre of Excellence, analyzed and reported. For more information about this process, please ask your local SGS laboratory for the SGS Chain of Custody document.

SAMPLE RETURN, RETENTION, STORAGE AND DISPOSALSample pulps will be stored for three months free of charge. Samples will be discarded after three months unless you specifically request their return. Disposal, storage and shipping costs may apply.

While SGS will take all reasonable care to protect your samples during analysis and storage, the samples shall at all times be at your risk.

RTN95 Return of rejects samples, per kg

RTN96 Return of pulp samples to client, per kg

RTR01 Retrieval of samples for re-analysis

STO97 Handling/retrieval of samples per hour rate

STO98 Storage of pulps, 30 day rate

STO99 Storage of rejects, 30 day rate

DIS93 Disposal of international soil samples, incineration, per kg rate

DIS94 Disposal of samples, per kg rate

SAMPLE PREPARATION (SIZE REDUCTION)

Sample preparation (also referred to as sample reduction) is the process by which a sample is crushed and pulverized for analysis. This will almost always involve sub-sampling. The right sampling method will produce a sub-sample that is representative of the total sample. Good sample reduction practice is essential to obtaining meaningful and reliable analytical data. More information is available in Rocks to Results, Chapter 4.

SGS is committed to providing dedicated sample preparation procedures at each of our locations. This involves technologically advanced equipment and, in most cases, physically separated sample processing areas for each sample type.

The crushing and pulverizing options available are varied. Your choice can depend on the sample type and the mineral that hosts the element of interest within the sample matrix. Please consult with our staff for the best possible option for your samples before starting an analytical program.

SAM

PLE

PREP

ARA

TIO

N

16 17

During sample reduction, there are many critical points where sample contamination can occur. One such area arises from the type of equipment used. Unfortunately, during sample reduction, contamination can never be avoided but processes are utilised to keep the level of contamination to a minimum. The levels are dependent on sample hardness, crushing and pulverizing time as well as crushing / grinding media used. Contamination levels can be measured and the table below indicates the type of levels of possible contamination from a variety of grinding media. More information is available in Rocks to Results, Chapter 4.1.

BOWL SELECTIONBOWL TYPE SAMPLE MAIN MINOR CAPACITY CONTAMINANT CONTAMINANT

Standard mild To 3.5 kg Fe, Cr Mo steel bowl

Cr-free steel 500 g to 1.5 kg Fe Mn

Zirconia 100 g Zr, Hf Al

Tungsten carbide 150 g W, Co Ta

Agate 100 g Si

Note: Not all pulverizing bowl types are available at all locations. Please inquire.

SAMPLE PREPARATION PROCEDURESDRYING

DRY10 Dry samples <3.0 kg, 105ºC

DRY11 Dry samples >3.0 kg, 105ºC, per kg rate

DRY12 Dry samples <3.0 kg, 60ºC

DRY13 Dry samples >3.0 kg, 60ºC, per kg rate

DRY14 Ambient temperature drying

DRY15 Dry excessively wet samples, per kg rate

DRY16 Dry and macerate vegetation

ASH01 Ashing of samples prior to analysis

CRUSHING

CRU20 Coarse crush to 6mm

CRU21 Crush <3.0 kg, 75% passing 2 mm

CRU22 Crush >3.0 kg, 75% passing 2 mm, per kg rate

CRU23 Crush <3.0 kg, 75% passing various mm

CRU24 Crush >3.0 kg, 75% passing various mm, per kg rate

CRU26 Crush <3.0 kg, 90% passing 2 mm

CRU27 Crush >3.0 kg, 90% passing 2 mm, per kg rate

SPLITTING

SPL25 Split into representative sub-samples by cone and quartering

SPL26 Split into representative sub-samples using riffle splitter, per kg

SPL27 Split into representative sub-samples using rotary splitter, per kg

SPL28 Split additional representative sub-samples

SCREENING - Applicable to soils and sediments

SCR30 Dry screening to -180 microns, <1 kg

SCR31 Dry screening to -180 microns, >1 kg, per kg rate

SCR32 Dry screening, various microns, <1 kg

SCR33 Dry screening, various microns, >1 kg, per kg rate

Note: Wet screening options are available. Please contact your local lab for details.

PULVERIZING

PUL45 Pulverize 250 g, Cr steel, 85% passing 75 microns

PUL46 Pulverize 500 g, Cr steel, 85% passing 75 microns

PUL47 Pulverize 1000-1500 g, Cr steel, 85% passing 75 microns

PUL48 Pulverize 1500-3000 g, Cr steel, 85% passing 75 microns

PUL49 Pulverize >3000 g, Cr steel, 85% passing 75 microns

PUL51 Pulverize 500-1500 g, mild steel, 85% passing 75 microns

Note: Samples can be pulverized in bowls made of other specialized materials if non-metallic preparation is required (e.g. tungsten carbide, zirconia, agate, etc.). Samples can also be pulverized at customer specified grain sizes (i.e. 106 or 120 microns) and % passing requirements. Please inquire.

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SAMPLE REDUCTION PACKAGES

PRP85 Dry, pulverize, 75 microns, <1.5 kg

PRP86 Dry, pulverize, 75 microns, <3.0 kg

PRP87 Weigh, dry, (<1.5 kg), crush to 75% passing 2 mm, split, pulverize to 85% pass at 75 microns

PRP89 Weigh, dry, (<3.0 kg), crush to 75% passing 2 mm, split 250 g, pulverize to 85% passing 75 microns






PRP104 Weigh, dry @ 60°, (<1 kg), screen -80mesh (180µm), for soil samples

AUTOMATED SAMPLE PREPARATIONAutomated sample preparation is the process by which a sample is crushed, split and pulverised mechanically in a closed system, with no human intervention. Such a system can be connected to an automated fused glass bead machine which produces a sample that is ready for analysis by XRF.

Automated sample preparation has several advantages. First, samples are prepared in a consistent reproducible fashion independent of any human habits or variability. Second, such preparation distances the operator from any hazardous materials that could be present, thus providing a much improved working environment. Third, an automated sample preparation system is much more reproducible. Finally, because the system is computer controlled, preparation parameters are traceable. Thus every sample can be tracked and all parameters pertaining to the sample preparation are recorded.

PRP72 Robotic Prep, 1 kg., reverse circulation, pulverize 106 microns

PRP73 Robotic Prep, 1 kg., drill core, pulverize 75 microns

PRP74 Robotic Prep, 3 kg., reverse circulation, pulverize 106 microns




Note: This option is available only at certain locations. Samples can be prepared to a variety of mesh sizes. Please contact your local lab.

MISCELLANEOUS PROCEDURESWSH78 Barren wash between each sample - pulverizing stage

WSH79 Barren wash between each sample - crushing stage

COM77 Compositing samples - gravimetric

COM78 Compositing samples - volumetric

RAD01T Radiation monitoring using scintillation counter

PRP70 Dedicated preparation environment (required for NORM or asbestos-bearing samples)

QRT03 Sample quarantine and handling

WST01 Waste disposal fee

MOISTURE AND LOSS ON IGNITION (LOI)Many materials contain volatile components or moisture. SGS has a variety of tests, including moisture (H2O), loss on ignition (LOI) (at various tempera-tures) and thermogravimetric analysis (TGA), that provide reliable, qualitative and quantitative analyses of these components.

MOISTURE (H2O)

CODE ELEMENT LIMIT(S) DESCRIPTION

G PHY08D H2O- 0.1 - 100% Gravimetric determination at 105ºC

G PHY09B H2O+ 0.1 - 100% Penfield tube

20 21

LOSS ON IGNITION (LOI)


G PHY01K LOI -10 - 100% Gravimetric determination at 1000ºC

G PHY02V LOI -10 - 100% Multi-point TGA at client- specified temperatures

Note: Moisture and LOI can be determined at other temperatures. Please inquire.

SPECIFIC GRAVITY AND BULK DENSITYSpecific gravity is the density of a material relative to water or air. Since rocks are comprised of several distinct mineral phases, they do not have a fixed specific gravity. Instead, a rock’s “bulk density” arises as a result of the percentage of each mineral phase in a sample multiplied by the specific gravity of each phase. SGS has extensive experience determining specific gravity and bulk density and we can identify the mineral phases using QEMSCAN®. Specific gravity and bulk density provide key information needed to design your processing flowsheet.

SGS can determine the specific gravity (SG) and bulk density (BD) of rocks, ores and aggregates. International standards are used to control the analysis whether the determination is done using the pycnometer, water and air measurements or the wax method. Such data can yield:

• Precise and accurate identification of mineral composition, including pay, penalty and detrimental metals.

• The most effective processing method.

• Appropriate sizing parameters for processing equipment.

• The exact weight of an ore (often required to calculate shipping and storage costs).

G PHY03V Specific gravity - pycnometer

G PHY05V Specific gravity - volumetric

G PHY14V Specific Gravity - pycnometer bottle

G PHY04V Bulk density - immersion

Note: If samples are porous, PHY04V will require a pre-preparation charge if it is necessary to coat samples with a sealant or wax coating.

PARTICLE SIZE ANALYSISParticle size analysis is used to determine the size classification and structural properties of an ore sample or to produce sized fractions for additional testing/analyses. SGS offers particle size analysis by wet screening, dry screening, a combination of both, or laser diffraction.

Wet screening is preferable to dry screening for materials containing a high percentage of clays which tend to agglomerate and thus give erroneous dry screening results. Dry screen tests can be performed on a variety of materials, but the sample must be free flowing and the particles separate (e.g. unagglomerated).

Often wet and dry methods are combined. Wet screening is performed to remove excessive fines then dry screening is performed to remove the oversize. Depending upon the nature of the material, dry screening, wet screening or a combination of both can be used.

Laser diffraction is recommended for very fine grained samples, as it is capable of measuring particle sizes at very low limits (0.02 microns). Laser diffraction is suitable for use with both wet and dry flows.

G PHY06V Particle size, sieve analysis (dry or wet)

G PHY07V Particle size, laser diffraction

PRECIOUS METALS

Precious metals (gold, silver and platinum group elements) can be analyzed by many techniques. Procedures for gold determination must take into account the sample type, sample concentration, purpose of the analysis, sample mineralogy and form of the gold (if known). Lead collection fire assay is considered the most definitive technique while acid digests and accelerated cyanide leaches can be effective for specific purposes. Similarly, silver can be determined by fire assay or acid digest techniques.

Please discuss your particular circumstance with an SGS chemist so you can choose the most appropriate technique. For more details, see our publication, Rocks to Results, Chapter 4.3.

PREC

IOU

S M

ETA

LS

22 23

Some platinum group elements (PGE) can also be determined by lead collection fire assay but this is not recommended. The six element PGE suite is best determined by nickel sulphide collection fire assay and neutron activation or ICP-MS. Sulphide-rich samples can require a reduction in sample weight to fuse properly.

Note: Lower and upper reporting limits of a given method can vary slightly among SGS laboratories due to reagent quality, access to consumables and instrument availability. Please inquire.

GOLDEXPLORATION-GRADE ANALYSIS

FIRE ASSAY GOLD


GE FAA313 Au 5 - 10,000 ppb 30 g, Fire assay, AAS finish

GE FAA515 Au 5 - 10,000 ppb 50 g, Fire assay, AAS finish

GE FAI313* Au** 1 - 10,000 ppb 30 g, Fire assay, ICP-AES finish

GE FAI515* Au** 1 - 10,000 ppb 50 g, Fire assay, ICP-AES finish

GE FAI323 Au** 5 - 10,000 ppb 30 g, Fire assay, ICP-AES finish

GE FAI525 Au** 5 - 10,000 ppb 50 g, Fire assay, ICP-AES finish

GE FAM313 Au** 1 - 2,000 ppb 30 g, Fire assay, ICP-MS finish

GE FAM515 Au** 1 - 2,000 ppb 50 g, Fire assay, ICP-MS finish

Note: *GE FAI313/515 methods use new fire assay pots to achieve lower limits. ** Pt and Pd can be included, refer to page 29.

Gold in soils and/or sediments can be determined by aqua regia digest and DIBK extraction. This is a partial leach and can require a pre-treatment such as roasting if samples contain significant sulphur bearing phases. This gold analytical method has the following advantages:

• Use of large sample sizes (25 g - 50 g) which ensures representative results for materials exhibiting nugget effect.

• The digest used for gold can also be used for a large suite of additional elements.

GOLD BY ACID DIGESTION (AQUA REGIA)


GE ARE145 Au 2 - 200 ppb 50 g, Aqua regia digest, DIBK extraction, AAS finish

GE ARE133 Au 0.02 - 200 ppm 25 g, Aqua regia digest, DIBK extraction, AAS finish

GE ARE155 Au 0.01 - 100 ppm 50 g, Aqua regia digest, DIBK extraction, AAS finish

GE ARM133 Au* 1 - 500 ppb 25 g, Aqua regia digest, ICP-MS finish

GE ARM155 Au* 1 - 500 ppb 50 g, Aqua regia digest, ICP-MS finish

* Note: Refer to page 36 for additional elements that can be determined by this method.

Cyanide leach procedures are used to enhance small gold anomalies during exploration and to monitor gold extraction efficiencies in metallurgical applications.

Bulk Leach Extractable Gold (BLEG) is a cyanide-based partial leach procedure that uses a large sample size (0.5 kg to 5 kg). It is used to enhance small gold anomalies during exploration. The cyanide leachate solution is extracted into an organic solvent and measured by flame AAS or ICP-MS. Our active cyanide leach packages are available with a variety of sample sizes, detection limits and finishing methods. The mini cyanide leach package is available for smaller sample sizes, allowing for faster TAT than active cyanide leach.

Other elements are also partially extracted with the cyanide leach and can be measured on request.

CYANIDE EXTRACTABLE GOLD


GE BLE643 Au 0.1 - 1000 ppm Hot, 30 g, Mini cyanide leach, ICP-AES or AAS finish

GE BLE61K Au 0.02 - 100 ppm 500 g, Active cyanide leach, 24 hr solvent extraction, AAS finish

GE BLE61N Au 1 ppb - 100 ppm 2000 g, Active cyanide leach, 24 hr solvent extraction, AAS finish

24 25

GE BLL61K Au 0.05 ppb - 100 ppm 500 g, Active cyanide leach, 24 hr ICP-MS finish

GE BLL61N Au 0.05 ppb - 100 ppm 2000 g, Active cyanide leach, 24 hr ICP-MS finish

The Leachwell™ tab is a proprietary product and Leachwell™ is a patented process. Accelerated cyanide leach techniques are used to determine bulk leachable gold in exploration samples using modified cyanide leach (Leachwell™). The large sample is mixed with water and Leachwell™ tabs and tumbled. The gold is extracted into DIBK and analyzed by flame AAS or ICP-MS. Other elements (Cu, Ag, Pb and Zn) are also partially extracted by the cyanide leach and can be measured on request.

ACCELERATED CYANIDE LEACH FOR GOLD


GE LWL69J Au 0.01 - 1,000 ppm 200 g, Accelerated cyanide leach, AAS

GE LWL69K Au 0.01 - 1,000 ppm 500 g, Accelerated cyanide leach, AAS

GE LWL69L Au 0.01 - 1,000 ppm 800 g, Accelerated cyanide leach, AAS

GE LWL69M Au 0.01 - 1,000 ppm 1000 g, Accelerated cyanide leach, AAS

GE LWL69N Au 0.01 - 1,000 ppm 2000 g, Accelerated cyanide leach, AAS

ORE-GRADE ANALYSIS

INSTRUMENTAL AND GRAVIMETRIC ANALYSIS


GO FAA303 Au 0.01 - 100 ppm 30 g, Fire assay, AAS finish

GO FAA505 Au 0.01 - 100 ppm 50 g, Fire assay, AAS finish

GO FAI303 Au 0.01 - 100 ppm 30 g, Fire assay, ICP-AES finish


GO FAG303 Au 0.5 - 3000 ppm 30 g, Fire assay, gravimetric finish

GO FAG505 Au 0.5 - 3000 ppm 50 g, Fire assay, gravimetric finish

GO FAG323 Au 0.01 - 100 ppm 30 g, Fire assay, AAS finish (Au) gravimetric finish (Ag)

Ag 10 - 5000 ppm


Ag 10 - 5000 ppm

GO FAG333 Au 0.5 - 3000 ppm 30 g, Fire assay, gravimetric finish (Au, Ag)

Ag 10 - 5000 ppm

SCREEN METALLIC GOLD ANALYSIS

Analytical results can be difficult to reproduce using typical sample reduction and fire assay procedures when coarse grained metallic gold is present. To address this, the sample can be analyzed using the screened metallics sample preparation and assaying procedure. This consists of:

• Screening 500g of the sample to a defined grain size, usually 75 or 106 microns.

• Weighing the various fractions.

• Assaying the entire plus fraction.

• Weighing and analysing the undersize (usually in duplicate).

• Calculating and reporting of size-fraction weights, coarse and fine fraction gold content and total gold content.

• The finish technique may involve AAS, ICP-AES or gravimetric, depending upon concentration. Limits shown are based on gravimetric analysis. AAS and ICP-AES limits are lower, please contact us for more information.

Note: This technique requires a minimum sample of 500g. This technique can also be used for coarse grained native metals such as platinum, palladium, silver and copper.

26 27

SCREENED METALLICS


GO FAS30K Au 0.5 ppm(grav) 500 g, Screen to 75 micron, fire assay




Note: A reporting limit of 0.01 ppm for Au can be achieved using AAS Finish when applicable to the sample concentration.

CONTROL AND CONCENTRATE-GRADE ANALYSIS



GC FAA35V Au 0.02 ppm Variable wt, Fire assay, AAS finish

GC FAI34V Au 0.02 ppm Variable wt, Fire assay, ICP-AES finish

GC FAG323 Au 0.02 ppm 30 g, Fire assay, AAS finish (Au)

Ag 10 ppm 30 g, Fire assay, gravimetric finish (Ag)

GC FAG333 Au 5 ppm 30 g, Fire assay, gravimetric finish (Au, Ag)

Ag 10 ppm

GOLD IN PROCESS SOLUTIONS


GC FSA84T Au >0.01 mg/L Solution (non CN), fire assay, AAS finish

GC FSI84T Au >0.01 mg/L Solution (non-CN), Fire assay, ICP-AES finish

GOLD IN CYANIDE LIQUORS


GC SOL81T Au >0.1 mg/L CN solution, AAS finish

GC SOL81X Au 0.01 - 50 mg/L Solvent extraction, DIBK, AAS finish

GOLD IN CARBON


GC FAA01V Au 5 - 50,000 ppm 1-2 g, Fire assay, AAS finish

GC ARS12D Au 5 - 250,000 ppm 1 g, Ash, acid digest, AAS finish

GC FAG01V Au 5 - 100,000 ppm 1-5 g, Fire assay, gravimetric finish

GOLD BULLION


GC BUL36V Au >10% 250-500 mg, Fire assay, gravimetric finish

Ag >0.1% 250-500 mg, Fire assay, gravimetric finish

SILVER

EXPLORATION-GRADE ANALYSIS

ACID DIGESTION - INSTRUMENTATION


GE AAS12E Ag 0.3 - 100 ppm 2 g, 2-Acid digest, AAS finish



Note: It is recommended that mineralized samples with Ag >30g/t are analyzed using the GO_AAS10D method below. Silver (Ag) can also be analyzed in many multi-element packages. Refer to page 32.

ORE-GRADE ANALYSIS

ACID DIGESTION - INSTRUMENTATION


GO AAS10D Ag 1 - 300 ppm 0.5 g, 2-Acid digest, AAS finish

28 29

GRAVIMETRIC ANALYSIS


GO FAG313 Ag 10 - 5000 ppm 30 g, Fire assay, gravimetric finish

GO FAG515 Ag 10 - 5000 ppm 50 g, Fire assay, gravimetric finish


Ag 10 - 5000 ppm

GO FAG333 Au 0.5 - 3000 ppm 30 g, Fire assay, gravimetric finish (Au, Ag)

Ag 10 - 5000 ppm

GO FAG525 Au 0.01 - 100 ppm 50 g, Fire assay, AAS finish (Au), gravimetric finish (Ag)

Ag 10 - 5000 ppm

CONTROL AND CONCENTRATE-GRADE ANALYSIS



GC AAS42V Ag 1 - 1000 ppm Variable wt, 4-acid digest, AAS finish

GC FAG323 Au 0.02 ppm 30 g, Fire assay, AAS finish (Au) gravimetric finish (Ag)

Ag 10 ppm

GC FAG333 Au 5 ppm 30 g, Fire assay, gravimetric finish (Au, Ag)

Ag 10 ppm

GC ARS12D Ag 2 - 2,000 ppm Carbon, 1 g, ash, acid digest, extract, AAS finish

GC BUL37V Ag 0.1 - 30% 100 mg, Fire assay, gravimetric finish

GOLD, PLATINUM, PALLADIUM AND OTHER PRECIOUS METALS


GOLD, PLATINUM AND PALLADIUM


GE FAI313* Au 1 - 10,000 ppb 30 g, Fire assay, ICP-AES finish

Pt 10 - 10,000 ppb

Pd 1 - 10,000 ppb

GE FAI515* Au 1 - 10,000 ppb 50 g, Fire assay, ICP-AES finish

Pt 10 - 10,000 ppb

Pd 1 - 10,000 ppb

GE FAM313 Au 1 - 2,000 ppb 30 g, Fire assay, ICP-MS finish

Pt 0.5 - 2,000 ppb

Pd 0.5 - 2,000 ppb

GE FAM515 Au 1 - 2,000 ppb 50 g, Fire assay, ICP-MS finish

Pt 0.5 - 2,000 ppb

Pd 0.5 - 2,000 ppb

GE FAI323 Au 5 - 10,000 ppb 30 g, Fire assay, ICP-AES finish

Pt 10 - 10,000 ppb

Pd 5 - 10,000 ppb

GE FAI525 Au 5 - 10,000 ppb 50 g, Fire assay, ICP-AES finish

Pt 10 - 10,000 ppb

Pd 5 - 10,000 ppb

Note: *GE FAI313/515 methods use new fire assay pots to achieve lower limits.

30 31

PLATINUM GROUP ELEMENTS


GE NAA363 Pt 0.02 - 10 ppm 30 g, Fire assay nickel sulphide collection, NAA (neutron activation) finish

Pd 0.02 - 10 ppm

Rh 0.005 - 10 ppm

Ru 0.05 - 10 ppm

Ir 0.001 - 10 ppm

Os 0.01 - 10 ppm

Note: This method is not available in all SGS laboratories; please contact us for more information.

ORE-GRADE ANALYSIS




Pt 0.01 - 100 ppm

Pd 0.01 - 100 ppm


Pt 0.01 - 100 ppm

Pd 0.01 - 100 ppm



GO FAM363 Pt 0.02 ppm 30 g, Fire assay nickel sulphide and/or collection, ICP-MS or NAA finish GO NAA363

Pd 0.02 ppm

Rh 0.02 ppm

Ru 0.05 ppm

Ir 0.04 ppm

Os 0.05 ppm

Note: Samples can be analyzed by ICP-MS or sent for neutron activation. This method is not available in all SGS laboratories; please contact us for more information.

CONTROL-GRADE ANALYSIS



GC FAI34V Au 0.02 ppm Variable wt, Fire assay, ICP-AES finish

Pt 0.02 ppm

Pd 0.02 ppm



GC FAM363 Pt 0.02 ppm 30 g, Fire assay nickel sulphide and/or collection, ICP-MS or NAA finish GC NAA363

Pd 0.02 ppm

Rh 0.02 ppm

Ru 0.05 ppm

Ir 0.04 ppm

Os 0.05 ppm

Note: Samples can be analyzed by ICP-MS or sent for neutron activation. This method is not available in all SGS laboratories; please contact us for more information.


MULTI-ELEMENT, TRACE ICP-AES AND ICP-MS PACKAGESA variety of approaches can be used for exploration analysis depending on your needs. In every case, each approach consists of a digestion technique and an instrumentation technique or “finish”. Each combination provides a unique suite of elements and specific upper and lower reporting limits.

EXPL

ORA

TIO

N-G

RAD

E A

NA

LYSI

S

32 33

SAMPLE DECOMPOSITION / DIGESTIONSample digestion is the most important parameter to consider when choosing an analytical method. There are several types of digestion available, including:

• Aqua regia digestion.

• Multi-acid (two, three or four acid) digestion.

• Sodium peroxide fusion.

• Lithium metaborate fusion.

Rocks to Results also provides more details in Chapter 4.2.

Typically, reconnaissance exploration-grade samples (including regional soil samples) are analyzed by aqua regia digestion followed by a multi-element ICP-AES or ICP-MS scan for base metals, trace and lithological elements.

Drill-core and rock samples are generally analyzed by multi-acid or fusion digestion, with a multi-element finish. Where metal contents are high (or ore-grade), samples can require further testing or other methods to ensure data is precise and accurate enough for regulatory reporting. Refer to the Ore-Grade Analysis section in this guide.

INSTRUMENTATIONICP-AES and ICP-MS are the most widely used geoanalytical instrumentation techniques because they yield many elements concurrently. These instruments are widely accepted in the mineral exploration industry as rapid and cost-effective means of analysis. Other instruments that can be used are AAS (Atomic Absorption Spectrophotometer) and Hydride AAS.

TWO-ACID / AQUA REGIA DIGESTION PACKAGESThe following packages are based on a two-acid digest (a combination of HNO3 and HCI). After the digestion, the solution is analyzed by either ICP-AES or ICP-MS or both. We can also analyze these digestions by Hydride AAS to determine the hydride forming elements (Hg, Sb, As, Bi, Se, Te). Two-acid digests are the weakest of the digestions and will not attack silicate minerals. As such, the leach provides partial results for most elements.

The methods listed below with the designation “12” are based on a combination of 2:1 HNO3 : HCl. This digest is recommended for samples with organic or high sulphide mineral content*.

The methods listed below with the designation “14” are based on a combination of 3:1 HCl : HNO3. This is an aqua regia digest and is recommended for all samples which contain no organic material and are low in sulphide mineral content.

All elements and limits are identical in the “12” and “14” digests.

NOTE: Requires a minimum sample weight of 0.5g. Detection and upper limits can vary slightly among SGS laboratories because some laboratories may not have access to high purity reagents and consumables and/or they have slight differences in instrumentation. Please talk with your local lab manager to make sure you get the reporting limits you need.

*High sulphide mineral content is defined as over 10%.

TWO ACID / AQUA REGIA DIGESTION / ICP-AES PACKAGE (34 ELEMENTS)

GE ICP12B or GE ICP14B

ELEMENTS AND LIMIT(S)

Ag 2 - 100 ppm* Hg 1 - 10000 ppm Sb 5 - 10000 ppm

Al 0.01 - 15% K 0.01 - 15% Sc 0.5 - 10000 ppm

As 3 - 10000 ppm La 0.5 - 10000 ppm Sn 10 - 10000 ppm

Ba 5 - 10000 ppm Li 1 - 10000 ppm Sr 5 - 10000 ppm

Be 0.5 - 2500 ppm Mg 0.01 - 15% Ti 0.01 - 15%

Bi 5 - 10000 ppm Mn 2 - 10000 ppm V 1 - 10000 ppm

Ca 0.01 - 15% Mo 1 - 10000 ppm W 10 - 10000 ppm

Cd 1 - 10000 ppm Na 0.01 - 15% Y 0.5 - 10000 ppm

Co 1 - 10000 ppm Ni 1 - 10000 ppm Zn 1 - 10000 ppm

Cr 1 - 10000 ppm P 0.01 - 15% Zr 0.5 - 10000 ppm

Cu 0.5 - 10000 ppm Pb 2 - 10000 ppm

Fe 0.01 - 15% S 0.01 - 5%

*Note: The upper limit of 100ppm for Ag is achieved with the GE_ICP14B package only. GE_ICP12B will not fully recover Ag in high concentrations. Refer to the Ag specific methods on page 28.

34 35

TWO ACID / AQUA REGIA DIGESTION / ICP-MS PACKAGE (36 ELEMENTS)

GE IMS12B or GE IMS14B


Ag 0.01 - 10 ppm Ga 0.1 - 10000 ppm Sb 0.05 - 10000 ppm

Al 0.01 - 10% Hg 0.01 - 100 ppm Sc 0.1 - 10000 ppm

As 1 - 10000 ppm K 0.01 - 10% Sn 0.3 - 1000 ppm

Ba 5 - 10000 ppm La 0.1 - 10000 ppm Sr 0.5 - 10000 ppm

Bi 0.02 - 10000 ppm Mg 0.01 - 15% Th 0.1 - 10000 ppm

Ca 0.01 - 15% Mn 2 - 10000 ppm Ti 0.01 - 10%

Cd 0.01 - 10000 ppm Mo 0.05 - 10000 ppm Tl 0.02 - 10000 ppm

Ce 0.05 - 1000 ppm Na 0.01 - 10% U 0.05 - 10000 ppm

Co 0.1 - 10000 ppm Ni 0.5 - 10000 ppm V 1 - 10000 ppm

Cr 1 - 10000 ppm P 0.01 - 1% W 0.1 - 10000 ppm

Cu 0.5 - 10000 ppm Pb 0.2 - 10000 ppm Y 0.05 - 10000 ppm

Fe 0.01 - 15% Rb 0.2 - 10000 ppm Zn 1 - 10000 ppm

TWO ACID / AQUA REGIA DIGESTION / COMBINED ICP-AES AND ICP-MS PACKAGE (51 ELEMENTS)

GE ICM12B or GE ICM14B


Ag 0.01 - 100* ppm Hg 0.01 - 10000 ppm Sc 0.1 - 10000 ppm

Al 0.01 - 15% In 0.02 - 500 ppm Se 1 - 1000 ppm

As 1 - 10000 ppm K 0.01 - 15% Sn 0.3 - 1000 ppm

Ba 5 - 10000 ppm La 0.1 - 10000 ppm Sr 0.5 - 10000 ppm

Be 0.1 - 100 ppm Li 1 - 10000 ppm Ta 0.05 - 10000 ppm

Bi 0.02 - 10000 ppm Lu 0.01 - 1000 ppm Tb 0.02 - 10000 ppm

Ca 0.01 - 15% Mg 0.01 - 15% Te 0.05 - 1000 ppm

Cd 0.01 - 10000 ppm Mn 2 - 10000 ppm Th 0.1 - 10000 ppm

Ce 0.05 - 1000 ppm Mo 0.05 - 10000 ppm Ti 0.01 - 15%

Co 0.1 - 10000 ppm Na 0.01 - 15% Tl 0.02 - 10000 ppm

Cr 1 - 10000 ppm Nb 0.05 - 1000 ppm U 0.05 - 10000 ppm

Cs 0.05 - 1000 ppm Ni 0.5 - 10000 ppm V 1 - 10000 ppm

Cu 0.5 - 10000 ppm P 0.01 - 15% W 0.1 - 10000 ppm

Fe 0.01 - 15% Pb 0.2 - 10000 ppm Y 0.05 - 10000 ppm

Ga 0.1 - 10000 ppm Rb 0.2 - 10000 ppm Yb 0.1 - 100 ppm

Ge 0.1 - 10000 ppm S 0.01 - 5% Zn 1 - 10000 ppm

Hf 0.05 - 500 ppm Sb 0.05 - 10000 ppm Zr 0.5 - 10000 ppm

*Note: The upper limit of 100ppm for Ag is achieved with the GE_ICP14B package only. GE_ICP12B will not fully recover Ag in high concentrations. Refer to the Ag specific methods on page 28.

TWO ACID / AQUA REGIA DIGESTION / HYDRIDE AAS PACKAGE

GE HAS12B or GE HAS14B


As 0.1 - 500 ppm Sb 0.1 - 500 ppm Te 0.1 - 500 ppm

Bi 0.1 - 500 ppm Se 0.1 - 500 ppm

Very low detection limits can be obtained by aqua regia digest and ICP-MS finish. This technique is applicable to exploration work as it yields rapid and accurate data.

Note: GE ARM133 and GE ARM155 are not available in all SGS laboratories. Please inquire.

AQUA REGIA DIGESTION ICP-MS PACKAGE (49 ELEMENTS)

GE ARM133 (25g) or GE ARM155 (50g)


Ag 0.02 - 100 ppm Hg 0.02 - 1000 ppm Se 0.5 - 2500 ppm

As 0.5 - 2000 ppm Ho 0.01 - 2000 ppm Sm 0.02 - 1000 ppm

Au 1 - 500 ppb In 0.01 - 2000 ppm Sn 0.05 - 1000 ppm

Ba 0.5 - 5000 ppm La 0.05 - 2000 ppm Sr 0.1 - 1000 ppm

Be 0.02 - 1000 ppm Li 0.01 - 2000 ppm Ta 0.01 - 1000 ppm

Bi 0.01 - 2000 ppm Lu 0.02 - 1000 ppm Tb 0.005 - 1000 ppm

Cd 0.02 - 1000 ppm Mn 0.5 - 5000 ppm Te 0.05 - 1000 ppm

Ce 0.05 - 2000 ppm Mo 0.02 - 2000 ppm Th 0.01 - 1000 ppm

Co 0.1 - 1000 ppm Nb 0.02 - 2000 ppm Tl 0.01 - 1000 ppm

Cs 0.01 - 1000 ppm Nd 0.05 - 2000 ppm U 0.01 - 1000 ppm

Cu 1 - 5000 ppm Ni 0.5 - 5000 ppm W 1 - 1000 ppm

Dy 0.01 - 2000 ppm Pb 0.2 - 1000 ppm Y 0.02 - 1000 ppm

Er 0.01 - 2000 ppm Pr 0.01 - 1000 ppm Yb 0.01 - 1000 ppm

36 37

Eu 0.01 - 2000 ppm Rb 0.05 - 1000 ppm Zn 1 - 5000 ppm

Ga 0.05 - 1000 ppm Re 0.01 - 100 ppm Zr 0.1 - 2000 ppm

Gd 0.01 - 2000 ppm Sb 0.02 - 1000 ppm

Hf 0.01 - 2000 ppm Sc 0.1 - 1000 ppm

MULTI-ACID (4-ACID) DIGESTION PACKAGES

NITRIC, HYDROFLUORIC, PERCHLORIC AND HYDROCHLORIC ACID DIGEST

Multi-acid (4-acid) digestion is a very effective dissolution procedure for a large number of mineral species and is suitable for a wide range of elements. Multi-acid digestion uses a combination of HNO3 (nitric acid), HF (hydrofluoric acid), HClO4 (perchloric acid) and HCl (hydrochloric acid). Because hydrofluoric acid dissolves silicate minerals, these digestions are often referred to as “near-total digestions”. For more details, see our publication, Rocks to Results, Chapter 4.

NOTE: Requires a minimum sample weight of 0.5g. Detection and upper limit can vary slightly among SGS laboratories because some laboratories may not have access to high purity reagents and consumables and/or they can have slight differences in instrumentation. Please talk with your local lab manager to make sure you get the reporting limits you need.

NOTE: Refractory minerals such as oxides have limited solubility in multi-acid (4-acid) digestions. Often elements can precipitate or volatize during digestion. These factors can compromise analytical results for Al, Ba, Cr, Hf, Mo, Mn, Nb, Pb, Si, Sn, Ti, Ta, W, Zr, As, Sb, Se and Te in some sample types.

MULTI-ACID (4-ACID) DIGESTION / ICP-AES PACKAGE (33 ELEMENTS)

GE ICP40B


Ag 2 - 100 ppm Fe 0.01 - 15% S 0.01 - 5%

Al 0.01 - 15% K 0.01 - 15% Sb 5 - 10000 ppm

As 3 - 10000 ppm La 0.5 - 10000 ppm Sc 0.5 - 10000 ppm

Ba 1 - 10000 ppm Li 1 - 10000 ppm Sn 10 - 10000 ppm

Be 0.5 - 2500 ppm Mg 0.01 - 15% Sr 0.5 - 10000 ppm

Bi 5 - 10000 ppm Mn 2 - 10000 ppm Ti 0.01 - 15%

Ca 0.01 - 15% Mo 1 - 10000 ppm V 2 - 10000 ppm

Cd 1 - 10000 ppm Na 0.01 - 15% W 10 - 10000 ppm

Co 1 - 10000 ppm Ni 1 - 10000 ppm Y 0.5 - 10000 ppm

Cr 1 - 10000 ppm P 0.01 - 15% Zn 1 - 10000 ppm

Cu 0.5 - 10000 ppm Pb 2 - 10000 ppm Zr 0.5 - 10000 ppm

Note: Additional elements can be added. Please inquire.

MULTI-ACID (4-ACID) DIGESTION / COMBINED ICP-AES AND ICP-MS PACKAGE (49 ELEMENTS)

GE ICM40B


Ag 0.02 - 100 ppm K 0.01 - 15% Sn 0.3 - 1000 ppm

Al 0.01 - 15% La 0.1 - 10000 ppm Sr 0.5 - 10000 ppm

As 1 - 10000 ppm Li 1 - 10000 ppm Ta 0.05 - 10000 ppm

Ba 1 - 10000 ppm Lu 0.01 - 1000 ppm Tb 0.05 - 10000 ppm

Be 0.1 - 2500 ppm Mg 0.01 - 15% Te 0.05 - 1000 ppm

Bi 0.04 - 10000 ppm Mn 2 - 10000 ppm Th 0.2 - 10000 ppm

Ca 0.01 - 15% Mo 0.05 - 10000 ppm Ti 0.01 - 15%

Cd 0.02 - 10000 ppm Na 0.01 - 15% Tl 0.02 - 10000 ppm

Ce 0.05 - 1000 ppm Nb 0.1 - 1000 ppm U 0.05 - 10000 ppm

Cs 1 - 1000 ppm Ni 0.5 - 10000 ppm V 2 - 10000 ppm

Co 0.1 - 10000 ppm P 0.005 - 15% W 0.1 - 10000 ppm

Cr 1 - 10000 ppm Pb 0.5 - 10000 ppm Y 0.1 - 10000 ppm

Cu 0.5 - 10000 ppm Rb 0.2 - 10000 ppm Yb 0.1 - 1000 ppm

Fe 0.01 - 15% S 0.01 - 5% Zn 1 - 10000 ppm

Ga 0.1 - 500 ppm Sb 0.05 - 10000 ppm Zr 0.5 - 10000 ppm

Hf 0.02 - 500 ppm Sc 0.5 - 10000 ppm

In 0.02 - 500 ppm Se 2 - 1000 ppm

Note: Select packages for rare earth elements can be found on pg 59.

38 39

FUSION PACKAGESFusion involves the complete digestion of the sample in molten flux. Fusions are generally more aggressive than acid digestion methods and are suitable for many refractory, difficult-to-dissolve minerals such as chromite, ilmenite, spinel, cassiterite and minerals of the tantalum-tungsten solid solution series. Fusion analyses are presumed to provide a complete chemical analysis and are referred to as a “total” analysis.

For more details, see our publication, Rocks to Results, Chapter 4.

NOTE: Detection and upper limit can vary slightly among SGS laboratories because some laboratories may not have access to high purity reagents and consumables and/or they can have slight differences in instrumentation. Please talk with your local lab manager to make sure you get the reporting limits you need.

SODIUM PEROXIDE FUSION

Sodium peroxide is a strongly oxidizing flux that is basic, not acidic in nature. It renders most refractory minerals soluble. Because the fusion temperature is lower than that of lithium metaborate fusions, the hydride elements are not volatilized. This technique requires a minimum sample weight of 0.2 g.

SODIUM PEROXIDE FUSION / ICP-AES PACKAGE (29 ELEMENTS)

GE ICP90A


Al 0.01 - 25% K 0.1 - 25% Sc 0.0005 - 5%

As 0.003 - 10% La 0.001 - 5% Si 0.1 - 30%

Ba 0.001 - 5% Li 0.001 - 5% Sn 0.005 - 5%

Be 0.0005 - 2.5% Mg 0.01 - 25% Sr 0.001 - 0.5%

Ca 0.1 - 25% Mn 0.001 - 10% Ti 0.01 - 25%

Cd 0.001 - 5% Mo 0.001 - 5% V 0.001 - 5%

Co 0.001 - 5% Ni 0.001 - 10% W 0.005 - 4%

Cr 0.001 - 5% P 0.01 - 25% Y 0.0005 - 2.5%

Cu 0.001 - 5% Pb 0.002 - 10% Zn 0.001 - 5%

Fe 0.01 - 25% Sb 0.005 - 10%

SODIUM PEROXIDE FUSION / COMBINED ICP-AES AND ICP-MS PACKAGE (56 ELEMENTS)

GE ICM90A


Ag 1 - 1000 ppm Ge 1 - 1000 ppm Sb 0.1 - 10000 ppm

Al 0.01 - 25% Hf 1 - 10000 ppm Si 0.1 - 30%

As 0.0005 - 10% Ho 0.05 - 1000 ppm Sm 0.1 - 1000 ppm

Ba 10 - 10000 ppm In 0.2 - 1000 ppm Sn 1 - 10000 ppm

Be 5 - 2500 ppm K 0.1 - 25% Sr 10 - 5000 ppm

Bi 0.1 - 1000 ppm La 0.1 - 10000 ppm Ta 0.5 - 10000 ppm

Ca 0.1 - 25% Li 0.001 - 5% Tb 0.05 - 1000 ppm

Cd 0.2 - 10000 ppm Lu 0.05 - 1000 ppm Th 0.1 - 1000 ppm

Ce 0.1 - 10000 ppm Mg 0.01 - 25% Ti 0.01 - 25%

Co 0.5 - 10000 ppm Mn 0.001 - 10% Tl 0.5 - 1000 ppm

Cr 0.001 - 5% Mo 2 - 10000 ppm Tm 0.05 - 1000 ppm

Cs 0.1 - 10000 ppm Nb 1 - 10000 ppm U 0.05 - 1000 ppm

Cu 10 - 10000 ppm Nd 0.1 - 10000 ppm V 5 - 10000 ppm

Dy 0.05 - 1000 ppm Ni 5 - 10000 ppm W 1 - 10000 ppm

Er 0.05 - 1000 ppm P 0.01 - 25% Y 0.5 - 1000 ppm

Eu 0.05 - 1000 ppm Pb 5 - 10000 ppm Yb 0.1 - 1000 ppm

Fe 0.01 - 25% Pr 0.05 - 1000 ppm Zn 5 - 10000 ppm

Ga 1 - 1000 ppm Rb 0.2 - 10000 ppm Zr 0.5 - 10000 ppm

Gd 0.05 - 1000 ppm Sc 0.0005 - 5%

SGS now offers an innovative, low cost, multi-element, analytical fusion package (GE_IMS90A). This package offers the best recoveries, fastest analysis time with the widest range of limits and elements offered in a single pass.

40 41

SODIUM PEROXIDE FUSION / ICP-MS PACKAGE (33 ELEMENTS)

GE IMS90A


Al 0.01 - 25% Fe 0.01 - 25% Sb 1 - 10000 ppm

As 3 - 10000 ppm K 0.1 - 30% Si 0.1 - 40%

Ba 10 - 10000 ppm La 0.1 - 10000 ppm Sn 1 - 10000 ppm

Be 1 - 2500 ppm Li 5 - 10000 ppm Sr 10 - 10000 ppm

Bi 0.1 - 1000 ppm Mg 0.01 - 30% Te 1 - 1000 ppm

Ca 0.1 - 25% Mn 10 - 10000 ppm Ti 0.01 - 30%

Cd 0.2 - 10000 ppm Mo 2 - 10000 ppm V 5 - 10000 ppm

Co 0.5 - 10000 ppm Ni 5 - 50000 ppm W 5 - 10000 ppm

Cr 5 - 10000 ppm P 0.01 - 25% Y 0.5 - 10000 ppm

Cs 0.1 - 10000 ppm Pb 2 - 50000 ppm Yb 0.1 - 1000 ppm

Cu 2 - 50000 ppm S 1 - 25% Zn 5 - 50000 ppm

Note: This package is currently only available at our Burnaby, Canada location. An additional 22 elements (Ce, Dy, Er, Eu, Ga, Gd, Ge, Ho, In, Lu, Nb, Nd, Pr, Rb, Re, Sm, Ta, Tb, Th, Tl, Tm, U) can be added. Please inquire.

SODIUM PEROXIDE FUSION / HYDRIDE AAS PACKAGE

GE HAS90A


As 0.5 - 1000 ppm Bi 0.5 - 1000 ppm Sb 0.5 - 1000 ppm

LITHIUM METABORATE FUSION

Lithium metaborate fusion is a high temperature procedure that dissolves rock forming minerals, trace minerals and refractory minerals. Lithium metaborate fusion solutions can be analyzed by ICP-AES, ICP-MS or both ICP-AES and ICP-MS. This technique requires a minimum sample weight of 0.2 g.

LITHIUM METABORATE FUSION / ICP-MS PACKAGE (33 ELEMENTS)

GE IMS95A


Ag 1 - 1000 ppm Ho 0.05 - 1000 ppm Ta 0.5 - 10000 ppm

Ce 0.1 - 10000 ppm La 0.1 - 10000 ppm Tb 0.05 - 1000 ppm

Co 0.5 - 10000 ppm Lu 0.05 - 1000 ppm Th 0.1 - 1000 ppm

Cs 0.1 - 10000 ppm Mo 2 - 10000 ppm Tl 0.5 - 1000 ppm

Cu 5 - 10000 ppm Nb 1 - 10000 ppm Tm 0.05 - 1000 ppm

Dy 0.05 - 1000 ppm Nd 0.1 - 10000 ppm U 0.05 - 10000 ppm

Er 0.05 - 1000 ppm Ni 5 - 10000 ppm V 5 - 10000 ppm

Eu 0.05 - 1000 ppm Pr 0.05 - 1000 ppm W 1 - 10000 ppm

Ga 1 - 1000 ppm Rb 0.2 - 10000 ppm Y 0.5 - 1000ppm

Gd 0.05 - 1000 ppm Sm 0.1 - 1000 ppm Yb 0.1 - 1000 ppm

Hf 1 - 10000 ppm Sn 1 - 10000 ppm Zr 0.5 – 1000 ppm

Note: Additional packages containing rare earth elements (REEs) are found on pg 59.

XRF ANALYSISX-ray fluorescence (XRF) spectroscopy has been available to the geochemical industry for over 50 years. It is the preferred method for the determination of the major oxides as well as some trace elements. The advantages of XRF include its:

• Accurate analyses, arising from the fact that inter-element corrections are well known and highly predictable.

• Precise determinations, due to inherent instrumental factors.

• Rapid analysis time.

• Ability to use a solid sample as opposed to a liquid digest.

• Wide analytical range which extends from the parts-per-million to tens of percent range.

42 43

Fusion and pressed pellet are the two industry-standard sample preparation techniques for XRF analysis. In pressed pellet XRF, samples are compressed into a pellet and analyzed instrumentally. Only lower levels of metals can be done accurately by this method. Fusion involves melting the sample with flux and casting it into a glass disc. Trace element and sulphide samples require specialized fusions or the pressed pellet technique. Please talk to us to determine the right method for your samples.

For information about fusion-XRF packages for whole rock samples, base metals, iron ores, REEs, and other minerals, please refer to the Ore-Grade Analysis section in this guide.

PRESSED PELLET / XRF PACKAGE (26 ELEMENTS)

GE XRF75V


As 3 - 10000 ppm Mn 50 - 10000 ppm Th 5 - 10000 ppm

Ba 10 - 4000 ppm Mo 3 - 10000 ppm Ti 4 - 10000 ppm

Ca 0.01 - 20% Nb 2 - 4000 ppm U 5 - 4000 ppm

Co 2 - 4000 ppm Ni 2 - 4000 ppm V 5 - 10000 ppm

Cr 5 - 4000 ppm Pb 5 - 10000 ppm W 5 - 4000 ppm

Cu 2 - 4000 ppm Rb 2 - 4000 ppm Y 2 - 4000 ppm

Ga 3 - 4000 ppm Sb 3 - 4000 ppm Zn 2 - 4000 ppm

Ge 5 - 10000 ppm Sn 3 - 4000 ppm Zr 3 - 4000 ppm

K 0.01 - 20% Sr 2 - 4000 ppm

Note: This method is not available at all SGS laboratories, please inquire. This technique requires a minimum sample weight of 12g.

MOBILE METAL ION – MMI™SGS is the owner and sole provider of MMI™ Technology. We have over 15 years of experience with this technology, and we are the market leaders in providing a weak extraction of the mobile form of the ions residing in near surface soils. MMI™ is a world-renowned exploration tool repeatedly proven to find buried mineral deposits.

MMI™ Technology is an innovative analytical process that uses a unique approach to the semi-quantitative analysis of metals in soils and weathered materials. Target elements are extracted using weak solutions of organic

and inorganic compounds rather than conventional aggressive acid or cyanide-based digests. MMI™ solutions contain strong ligands, which detach and hold the metal ions that were loosely bound to soil particles by weak atomic forces. The extraction does not dissolve the bound forms of the metal ions. Thus, the metal ions in MMI solutions are the chemically active or ‘mobile’ component of the sample. Because these mobile, loosely bound complexes are in very low concentrations, elemental determinations are made by conventional ICP-MS and the latest evolution of this technology, ICP-MS Dynamic Reaction Cell™ (DRC II™).

There are many benefits to using MMI™ Technology for soil geochemistry.

• Few false anomalies

• Focused anomalies

• Minimal nugget effects

SAMPLE COLLECTION

Sample collection is the most critical part of a soil geochemistry program. The MMI™ Technology has specific sampling protocol based on years of experience and research. In the absence of an orientation survey, samples must be taken at a constant depth (10-25 cm) below the organic-inorganic soil interface. There is no sample preparation or drying. The analysis is done on a 50 gram sample and the extracted solution is analyzed via ICP-MS or ICP-MS DRCII™, providing determinations in the part per billion range. For detailed instructions for the MMI™ sampling protocols and orientation surveys, please visit www.sgs.com/mining/mmi or contact us at [email protected].

ICP-MS DRC II™

SGS is committed to the MMI™ Technology. With the development of the ICP-MS DRC II™, we have been able to further enhance this analytical approach. The lower detection limits provided by ICP-MS DRC II™ mean that we can better define anomalous targets. For instance, for the exploration of nickel deposits, kimberlites and layered intrusions, low level chrome (1 ppb) is an important geological trace element. For uranium exploration, low level vanadium (1 ppb) is also important. If either or both of these elements are required for your program, we can analyze your samples for low chrome and/or vanadium values using our MMI-ME package.

44 45

Sulfur, bromine, iodine and lead isotopes can be added to the MMI packages. For these additional elements, please contact us at [email protected].

MOBILE METAL ION STANDARD PACKAGE / ICP-MS (53 ELEMENTS)

GE MMI-M


Ag 0.5 ppb Er 0.2 ppb Nd 1 ppb Tb 0.1 ppb

Al 1 ppm Eu 0.2 ppb Ni 5 ppb Te 10 ppb

As 10 ppb Fe 1 ppm P 0.1 ppm Th 0.5 ppb

Au 0.1 ppb Ga 0.5 ppb Pb 5 ppb Ti 10 ppb

Ba 10 ppb Gd 0.5 ppb Pd 1 ppb Tl 0.1 ppb

Bi 0.5 ppb Hg 1 ppb Pr 0.5 ppb U 0.5 ppb

Ca 2 ppm In 0.1 ppb Pt 0.1 ppb W 0.5 ppb

Cd 1 ppb K 0.5 ppm Rb 1 ppb Y 1 ppb

Ce 2 ppb La 1 ppb Sb 0.5 ppb Yb 0.2 ppb

Co 1 ppb Li 1 ppb Sc 5 ppb Zn 10 ppb

Cr 100 ppb Mg 0.5 ppm Sm 1 ppb Zr 2 ppb

Cs 0.2 ppb Mn 100 ppb Sn 1 ppb

Cu 10 ppb Mo 2 ppb Sr 10 ppb

Dy 0.5 ppb Nb 0.5 ppb Ta 1 ppb

MOBILE METAL ION ENHANCED PACKAGE / ICP-MS (55 ELEMENTS)

GE MMI-ME


Ag 0.5 ppb Er 0.2 ppb Nd 1 ppb Ta 1 ppb

Al 1 ppm Eu 0.2 ppb Ni 5 ppb Tb 0.1 ppb

As 10 ppb Fe 1 ppm P 0.1 ppm Te 10 ppb

Au 0.1 ppb Ga 0.5 ppb Pb 5 ppb Th 0.5 ppb

Ba 10 ppb Gd 0.5 ppb Pd 1 ppb Ti 10 ppb

Bi 0.5 ppb Hg 1 ppb Pr 0.5 ppb Tl 0.1 ppb

Ca 2 ppm In 0.1 ppb Pt 0.1 ppb U 0.5 ppb

Cd 1 ppb K 0.5 ppm Rb 1 ppb V 1 ppb

Ce 2 ppb La 1 ppb Sb 0.5 ppb W 0.5 ppb

Co 1 ppb Li 1 ppb Sc 5 ppb Y 1 ppb

Cr 1 ppb Mg 0.5 ppm Se 2 ppb Yb 0.2 ppb

Cs 0.2 ppb Mn 100 ppb Sm 1 ppb Zn 10 ppb

Cu 10 ppb Mo 2 ppb Sn 1 ppb Zr 2 ppb

Dy 0.5 ppb Nb 0.5 ppb Sr 10 ppb

Note: S, Br, I and lead isotopes can be added to the MMI-ME package by special request.

MOBILE METAL ION PRECIOUS METAL PLUS PACKAGE / ICP-MS (11 ELEMENTS)

GE MMI-MP


Au 0.05 ppb Ag 0.1 ppb Cu 10 ppb Zn 10 ppb

Pd 0.1 ppb Cd 0.5 ppb Ni 5 ppb U 0.5 ppb

Pt 0.02 ppb Co 1 ppb Pb 5 ppb

BIOGEOCHEMISTRY SGS has considerable experience in the preparation and analysis of a wide range of vegetation samples. Such samples may be dried and macerated or ashed prior to acid digestion and analysis by ICP-MS. Please consult your local lab for more information.

HYDROGEOCHEMISTRYThe analyses offered in this section are suitable for groundwater samples used in mineral exploration, but NOT for salt water, brines, effluent solutions and metal-carrying solutions generated in processing circuits or environmental applications. Samples such as salt water, effluents or metal-carrying solutions will incur an extra charge and element detection limits can increase. Requests for environmental services will be forwarded to an SGS Environmental Services Laboratory.

46 47

GROUND WATER ANALYSIS / ICP-AES PACKAGE (31 ELEMENTS)

GE ICP80T


Ag 1 ppb Co 10 ppb Mo 10 ppb Sr 1 ppb

Al 50 ppb Cr 10 ppb Na 50 ppb Ti 10 ppb

As 30 ppb Cu 5 ppb Ni 10 ppb V 10 ppb

Ba 10 ppb Fe 50 ppb P 50 ppb W 50 ppb

Be 5 ppb K 100 ppb Pb 30 ppb Y 5 ppb

Bi 50 ppb La 10 ppb Sb 50 ppb Zn 5 ppb

Ca 50 ppb Mg 50 ppb Sc 1 ppb Zr 10 ppb

Cd 10 ppb Mn 5 ppb Sn 50 ppb

GROUND WATER ANALYSIS / ICP-MS PACKAGE (49 ELEMENTS)

GE IMS80T


Ag 0.01 ppb Eu 0.01 ppb Ni 0.1 ppb Th 0.01 ppb

As 1 ppb Ga 0.01 ppb Pb 0.01 ppb Tl 0.01 ppb

Ba 0.01 ppb Gd 0.01 ppb Pr 0.01 ppb Tm 0.01 ppb

Be 0.1 ppb Hf 0.01 ppb Rb 0.1 ppb U 0.01 ppb

Bi 0.01 ppb Hg 0.2 ppb Sb 0.1 ppb V 1 ppb

Cd 0.01 ppb Ho 0.01 ppb Sc 0.1 ppb W 0.01 ppb

Ce 0.01 ppb In 0.01 ppb Se 1 ppb Y 0.01 ppb

Cs 0.01 ppb La 0.01 ppb Sm 0.01 ppb Yb 0.01 ppb

Cr 1 ppb Lu 0.05 ppb Sn 0.01 ppb Zn 1 ppb

Co 0.1 ppb Mn 0.1 ppb Sr 0.01 ppb Zr 0.1 ppb

Cu 0.1 ppb Mo 1 ppb Ta 0.01 ppb

Dy 0.1 ppb Nb 0.01 ppb Tb 0.01 ppb

Er 0.01 ppb Nd 0.01 ppb Te 0.1 ppb

Note: Au, Pt, Pd, Rh, Ru, Ir and Re can be added upon request.

ADDITIONAL GROUND WATER ANALYSIS

CODE(S) ELEMENT DESCRIPTION

GE PHY22V Total dissolved solids (TDS) Gravimetric

GE ISE06T pH Ion selective electrode (ISE)

GE ISE07T Fluoride F_ Ion selective electrode (ISE)

GE ISE08T Chloride Cl_ Ion selective electrode (ISE)

INDIVIDUAL METHODS FOR EXPLORATION-GRADE ANALYSISSULPHUR AND CARBON

CODE(S) ELEMENT LIMIT(S) DESCRIPTION MIN. SAMPLE WT.(g)

GE CSA06V S 0.005 - 30% IR Combustion 0.2

C 0.005 - 30% 0.2

GE CSA07V SO42- 0.01% Leach/ 1.0

IR combustion

GE CSA08V S2- 0.01% Leach/Digest/ 1.0 IR combustion

GE CSA09V S (elemental) 0.01% Leach/Gravimetry 1.0

GE CSA02V CO2 (Carbonate) 0.05% IR combustion 1.0

GE CSB02V CO2 (Carbonate) 0.05% Coulometry 1.0

GE CSA03V C (organic, 0.01% IR combustion 1.0 inorganic)

GE CSB03V C (organic, 0.05% Coulometry 1.0 inorganic)

GE CSA05V C (graphitic) 0.05% IR combustion 1.0

GE CSB05V C (graphitic) 0.05% Coulometry 1.0

48 49

ADDITIONAL SINGLE ELEMENTS


GE CVA20A Hg 0.005 - 100 ppm Cold vapour AAS 0.2

GE ISE07A F 0.0025 - 10% Ion specific 0.2 electrode

GE ISE08B Cl 50 - 5000 ppm Ion specific 0.5 electrode

GE CLA02V Cl 0.005 - 1% Titration 0.5

SGS offers a wide variety of specific element analyses. Please contact your local site.

ORE-GRADE ANALYSIS

Ore-grade packages are used to analyse samples that have high concentrations of pay metals. They can be used in prefeasibility, feasibility or production circumstances. As well, these methods can be used to provide over range analysis when an upper limit of an element in an exploration package is exceeded. Typically, ore-grade analyses are accomplished by adjusting the sample weight and final solution volume ratio, thus expanding the linear range of the analysis.

ORE-GRADE / OVER RANGE METHODS

CODE(S) ELEMENTS LIMIT(S) DESCRIPTION

GO ICP13B Refer to GE ICP14B Minors (0.01 - 30%) Aqua regia digest / ICP-AES

Majors (0.1 - 30%)

GO ICP41Q Refer to GE ICP40B Minors (0.01 - 30%) 4-Acid digest / ICP-AES

Majors (0.1 - 30%)

Note: For details on the above digestion techniques, refer to the Exploration-Grade Analysis section of this guide.

MULTI-ACID (4-ACID) DIGESTION PACKAGES4-ACID DIGESTION / AAS PACKAGE (16 ELEMENTS)

GO AAS42S


Ag 5 - 500 ppm Cr 0.005 – 5% Pb 0.002 - 2.5%

As 0.025 - 5% Cu 0.001 - 50% Sb 0.01 - 2%

Bi 50 - 5000 ppm Fe 0.01 - 40% V 0.005 - 5%

Ca 0.01 - 40% Mn 0.001 - 5% Zn 0.001 - 5%

Cd 5 - 5000 ppm Mo 0.002 - 5%

Co 0.002 - 2.5% Ni 0.001 - 5%

4-ACID DIGESTION / ICP-AES PACKAGE (26 ELEMENTS)

GO ICP42S


Ag 5 - 250 ppm Fe 0.025 - 100% Pb 0.0025 - 2.5%

Al 0.025 - 40% K 0.1 - 40% Sb 0.001 - 2%

As 0.002 - 2.5% Li 5 - 2500 ppm Sn 0.002 - 2%

Bi 0.005 - 2.5% Mg 0.005 - 40% Ta 0.005 - 2.5%

Ca 0.01 - 40% Mn 0.002 - 2.5% Ti 0.002 - 5%

Cd 0.0005 - 2% Mo 0.002 - 2.5% V 0.0005 - 2.5%

Co 0.001 - 2.5% Na 0.01 - 40% Zn 0.001 - 5%

Cr 0.002 - 5% Ni 0.002 - 2.5% Zr 0.001 - 5%

Cu 0.001 - 2.5% P 0.01 - 25%

Note: Requires a minimum sample weight of 0.5 g.

ORE

-GRA

DE

AN

ALY

SIS

50 51

FUSION-ICP PACKAGESSODIUM PEROXIDE FUSION / ICP-AES PACKAGE

GO ICP90Q


Co 0.01 - 30% Mo 0.01 - 30% Pb 0.01 - 30%

Cu 0.01 - 30% Ni 0.01 - 30% Zn 0.01 - 30%

Fe 0.05 - 50%

Note: Additional elements can be added to this method upon request. Elements greater than 30% can require analysis by another technique for full recovery. Requires a minimum sample weight of 0.5 g.

SODIUM PEROXIDE FUSION / ICP-AES NICKEL LATERITE PACKAGE (SAMPLES DRIED AT 105ºC / 8 HOURS)

GO ICP90B


Al2O3 0.01 - 25% Cu 0.01 - 10% Ni 0.01 - 10%

CaO 0.1 - 35% Fe2O3 0.01 - 30% P2O5 0.01 - 25%

Cr 0.01 - 10% K2O 0.1 - 25% SiO2 0.01 - 25%

Co 0.01 - 10% MgO 0.01 - 30% TiO2 0.01 - 25%

Requires a minimum sample weight of 0.5 g.

LITHIUM METABORATE FUSION / ICP-AES (LITHOLOGIC) PACKAGE (18 ELEMENTS)

GO ICP95A


Al2O3 0.01 - 75% MgO 0.01 - 30% Sr 0.001 - 10%

Ba 0.001 - 10% MnO 0.01 - 10% TiO2 0.01 - 25%

CaO 0.01 - 60% Na2O 0.01 - 30% Y 0.001 - 10%

Cr2O3 0.01 - 10% Nb 0.001 - 10% Zn 5 - 10000 ppm

Fe2O3 0.01 - 75% P2O5 0.01 - 25% Zr 0.001 - 10%

K2O 0.01 - 25% SiO2 0.01 - 90% LOI 0.01 - 50%

Requires a minimum sample weight of 0.2 g.

FUSION-XRF PACKAGESWhole rock analysis is the determination of major elements (reported as “oxides”). This analysis will approximate 100% in non-mineralized samples. SGS offers whole rock analysis using both ICP-AES or XRF below. Whole rock analysis by XRF is particularly suitable for the analysis of bulk commodities such as iron ore, silicate, feldspar, gypsum and limestone. This method is not suitable for samples with a sulphide mineral content > 1%.

BORATE FUSION / XRF WHOLE ROCK PACKAGE (13 ELEMENTS)

GO XRF76V


Al2O3 0.01 - 100% MnO 0.01 - 100% TiO2 0.01 - 100%

CaO 0.01 - 100% Na2O 0.01 - 100% V2O5 0.01 - 100%

Cr2O3 0.01 - 100% P2O5 0.01 - 100% LOI -10 - 100%

K2O 0.01 - 100% Fe2O3 0.01 - 100% SUM %

MgO 0.01 - 100% SiO2 0.01 - 100%

Additional major and minor elements can be added to the borate fusion / XRF method. Requires a minimum sample weight of 5.0 g. Please contact your local lab. Rare earth elements can also be analyzed by this technique. Refer to page 61. For iron ore samples (GO XRF78S), refer to page 65.

PYROSULPHATE FUSION / XRF BASE METAL PACKAGE (10 ELEMENTS)

GO XRF77B


Co 0.01 - 100% Mn 0.01 - 100% W 0.01 - 100%

Cr 0.01 - 100% Mo 0.01 - 100% Zn 0.01 - 100%

Cu 0.01 - 100% Ni 0.01 - 100%

Fe 0.01 - 100% Pb 0.01 - 100%

Note: Requires a minimum sample weight of 1.0 g.

52 53

INDIVIDUAL METHODS FOR ORE-GRADE ANALYSISINTERNAL STANDARD / RESISTIVE MINERALS / XRF

GO XRF75F


As >0.001% Sn >0.002% ThO2 >0.005% WO3 >0.002%

Sb >0.002% Ta >0.002% U3O8 >0.002%

Note: Requires a minimum sample weight of 25 g. depending on the elements of interest. This method is not available at all SGS laboratories. Please inquire.

SULPHUR AND CARBON


GO CSA06V S 0.01 - 75% IR combustion

C 0.01 - 75%

Note: Requires a minimum sample weight of 0.2 g. Carbon and sulphur can be speciated using a variety of methods. Please inquire.

ADDITIONAL SINGLE ELEMENTS


GO CVA20B Hg 0.3ppm - 100% Cold vapour 0.4 AAS

GO CLA10E Insolubles 0.1% Gravimetric 5 (acid)

GO CLA07C CaO 0.01% Available lime 2

GO CLA01V FeO 0.1 - 30% Ferric/Ferrous 0.5 iron titration

SGS can analyse a number of individual ore-grade elements. Please inquire.

CONTROL-GRADE ANALYSISMetallurgical processes are monitored and controlled by the chemical analysis of feed and head samples, middlings, concentrates, metals, tails, slags, residues or pregnant solutions. A wide range of analytical techniques are needed to accommodate the varying matrices and complex nature of such samples. Several of the techniques are listed here, but this list is not meant to be comprehensive. We have extensive experience supporting metallurgical facilities and would be happy to speak with you regarding your specific project requirements.

CUSTOMIZED SPECTROSCOPIC ANALYSISThe analytical approach for control analysis differs from the standard geochemistry “package” methodology. Instead, we provide both multi-element packages and customized spectroscopic determinations that can include multiple dilutions and spectral analyses on an element-by-element basis to ensure that the interferences common in complex samples are identified and resolved.

These control assay methods are only a small selection of the methods and capabilities available at SGS. A wide variety of other methods are available including fire assay, manual and automated titrations, CVAA mercury analysis, AAS, carbon, sulphur and chromatography. Fire assay methods often require customized fluxes and finishes. Please contact us if you have any needs in this area – we have lots of expertise to share.

CON

TRO

L-G

RAD

E A

NA

LYSI

S

54 55

TWO ACID/AQUA REGIA DIGESTION PACKAGESAQUA REGIA DIGESTION PACKAGE / ICP-AES (30 ELEMENTS)

GC ICP14C

ELEMENTS AND REPORTING LIMIT(S)

Ag 0.8 ppm Co 3 ppm Mo 6 ppm Sr 0.02 ppm

Al 2 ppm Cr 1 ppm Na 20 ppm Ti 0.2 ppm

As 30 ppm Cu 1 ppm Ni 6 ppm Tl 30 ppm

Ba 0.07 ppm Fe 2 ppm P 50 ppm V 2 ppm

Be 0.02 ppm K 10 ppm Pb 20 ppm Y 0.2 ppm

Bi 10 ppm Li 20 ppm Sb 10 ppm Zn 7 ppm

Ca 9 ppm Mg 0.7 ppm Se 30 ppm

Cd 0.9 ppm Mn 0.4 ppm Sn 20 ppm

Additional elements can be added. An ICP-MS option is available. Concentrate samples containing greater than 50% of the target element can require alternative analytical methods if full recovery is required. Requires a minimum sample weight of 1.0 g.

MULTI-ACID (4-ACID) DIGESTION PACKAGESMULTI-ACID DIGESTION PACKAGE / ICP-AES (30 ELEMENTS)

GC ICP42C


Ag 2 ppm Co 4 ppm Mo 5 ppm Sr 0.03 ppm

Al* 2 ppm Cr* 4 ppm Na 10 ppm Ti* 0.4 ppm

As* 30 ppm Cu 0.5 ppm Ni 20 ppm Tl 30 ppm

Ba* 0.2 ppm Fe 4 ppm P 30 ppm V 2 ppm

Be 0.03 ppm K* 20 ppm Pb 20 ppm Y 0.2 ppm

Bi 20 ppm Li 5 ppm Sb* 10 ppm Zn 2 ppm

Ca* 20 ppm Mg* 1 ppm Se 30 ppm

Cd 2 ppm Mn 0.3 ppm Sn* 20 ppm

Additional elements can be added. An ICP-MS option is available. Requires a minimum sample weight of 1.0 g. Concentrate samples containing greater than 50% of the target element can require alternative analytical methods if full recovery is required.

*Recovery can be incomplete so analysis can be biased low.

MULTI-ACID DIGESTION PACKAGE / FUSION / ICP-AES (30 ELEMENTS)

GC ICP46C


Ag 2 ppm Co 4 ppm Mo 5 ppm Sr 0.03 ppm

Al 2 ppm Cr 4 ppm Na 10 ppm Ti 0.4 ppm

As 30 ppm Cu 0.5 ppm Ni 20 ppm Tl 30 ppm

Ba 0.2 ppm Fe 4 ppm P 30 ppm V 2 ppm


Bi 20 ppm Li 5 ppm Sb 10 ppm Zn 2 ppm

Ca 20 ppm Mg 1 ppm Se 30 ppm

Cd 2 ppm Mn 0.3 ppm Sn 20 ppm

Additional elements can be added. An ICP-MS option is available. Requires a minimum sample weight of 1.0 g. Concentrate samples containing greater than 50% of the target element can require alternative analytical methods if full recovery is required. Data for volatiles (As, Sb) and/or precipitants (Pb) may be incomplete.

FUSION PACKAGESFUSION / ICP-AES PACKAGE (28 ELEMENTS)

GC ICP93A


Ag 200 ppm Co 200 ppm Mo 300 ppm Tl 2000 ppm

Al 400 ppm Cr 40 ppm Ni 300 ppm V 80 ppm

As 1200 ppm Cu 40 ppm Pb 800 ppm Y 8 ppm

Ba 3 ppm Fe 500 ppm Sb 400 ppm Zn 300 ppm

Be 0.8 ppm K 400 ppm Se 2000 ppm

56 57

Bi 400 ppm Li 800 ppm Sn 800 ppm

Ca 800 ppm Mg 30 ppm Sr 10 ppm

Cd 40 ppm Mn 20 ppm Ti 8 ppm


FUSION / AAS PACKAGE (11 ELEMENTS)

GC AAS93A


Al 0.02% Fe 0.01% Si 0.07% V 0.1%

Ca 0.06% Mg 0.005% Sn 0.05% Zn 0.001%

Cr 0.005% Mn 0.005% Ti 0.05%


FUSION / XRF CONTROL-GRADE PACKAGES

CODE(S) ELEMENTS / LIMIT(S) DESCRIPTION

GC XRF76V Refer to Ore-Grade Analysis section Borate fusion / XRF for elements and ranges

GC XRF77B Refer to Ore-Grade Analysis section Pyrosulphate fusion / XRF for elements and ranges

GC XRF75F Refer to Ore-Grade Analysis section Internal standard / XRF for elements and ranges

PROCESS SOLUTION PACKAGESPROCESS SOLUTION PACKAGE / ICP-AES / NON-CYANIDE BASED (30 ELEMENTS)

GC SOL91T


Ag 0.08 ppm Co 0.3 ppm Mo 0.6 ppm Sr 0.002 ppm

Al 0.2 ppm Cr 0.1 ppm Na 2 ppm Ti 0.02 ppm

As 3 ppm Cu 0.1 ppm Ni 0.6 ppm Tl 3 ppm

Ba 0.007 ppm Fe 0.2 ppm P 5 ppm V 0.2 ppm


Bi 1 ppm Li 2 ppm Sb 1 ppm Zn 0.7 ppm

Ca 0.9 ppm Mg 0.07 ppm Se 3 ppm


Additional elements can be added. Requires a minimum sample volume of 5 mL. ICP-MS option may be available locally. Please inquire.

PROCESS SOLUTION PACKAGE / ICP-AES / CYANIDE BASED (30 ELEMENTS)

GC SOL92T


Ag 0.08 ppm Co 0.3 ppm Mo 0.6 ppm Sr 0.002 ppm

Al 0.2 ppm Cr 0.1 ppm Na 2 ppm Ti 0.02 ppm

As 3 ppm Cu 0.1 ppm Ni 0.6 ppm Tl 3 ppm

Ba 0.007 ppm Fe 0.2 ppm P 5 ppm V 0.2 ppm


Bi 1 ppm Li 2 ppm Sb 1 ppm Zn 0.7 ppm

Ca 0.9 ppm Mg 0.07 ppm Se 3 ppm


Additional elements can be added. Requires a minimum sample volume of 10 mL. ICP-MS option may be available locally. Please inquire.

58 59

INDIVIDUAL METHODS FOR CONTROL-GRADE ANALYSISSULPHUR AND CARBON


GC CSA06V S 0.01 - 100% IR combustion 0.2

C 0.01 - 100% 0.2

GC CSA08V S2- 0.01 - 100% Leach/Digest/IR 1.0

GC CSA09V S (elemental) 0.01 - 100% Leach/Gravimetry 1.0

Single elements can be determined by numerous decomposition techniques and finishes. Please contact your local lab for options.

VOLUMETRIC AND GRAVIMETRIC METHODS FOR CONCENTRATES


GC CON13V Cu 5 - 60% Titration 2.0

GC CON03V Cu 5 - 100% Electroplating 5.0

GC CON07V Ni 10 - 100% Electroplating 5.0

GC CON11V Pb 10 - 70% Titration 2.0

GC CON12V Zn 5 - 65% Titration 2.0

GC CON08V Fe 10 - 75% Titration 0.5

GC CLA01V FeO >0.2 Titration 0.5

Note: these elements can be analyzed to party or umpire quality standards (GT) and can be reported up to 100%. Refer to the Commercial Trade Analysis section in this guide. Additional elements can be determined on concentrate samples in some SGS laboratories. Please inquire. Trade sample analyses typically require moisture analysis and may require a larger minimum sample weight.

COMMERCIAL TRADE ANALYSISSGS is the global leader and innovator in inspection, verification, testing and certification services. Our Minerals Services group, with its global network of laboratories and offices, provides customers with weighing, inspection, sampling and analytical services that are highly respected throughout the industry.

When possible, we follow published, accredited procedures and test methods. As well, SGS can accept your speciality methods and jointly ensure that your analytical results meet your needs and are suitably in control. The SGS Centre of Excellence laboratories that perform these commercial assays conform to the requirements of the ISO/IEC 17025:2005 standard for specific registered tests. SGS recognizes that your reputation and financial position can be at stake during commercial transactions and so we strive to continually improve our services and processes.

SGS’ commercial analysis offerings consist of:

• ‘Load-port‘ or ‘pre-shipment’ assays used by underwriters to quickly confirm product quality and determine approximate value of the shipment. These assays can also be used to calculate partial payment while the parcel or cargo is en-route to the customer. Assay techniques are chosen based on the quality required and turn-around requirements that are demanded during some loading operations.

• Party analyses (also known as settlement or assay exchange analysis) are used to determine the quality of a commodity or product and thus its value and the payment due. The major or payable elements and all minor or penalty parameters are measured and reported. Party assays use commodity-specific methodology and require rigorous quality control steps. SGS employs rugged and reliable procedures, including traditional fire assay, classical gravimetric analysis, electroplating and volumetric titrimetry as well as AAS, ICP-AES and ICP-MS in this type of work.

• Umpire assays are used to resolve a dispute between a buyer and a seller. Samples of the cargo or product are analyzed in triplicate (at minimum) using approved, accredited methods and quality control protocols are set to provide the highest level of accuracy and precision.

• Product verification analysis for validation. SGS has the experience, ability and international approvals to test all types of products against published specifications, such as minimum or maximum limits, weights, quantities or other physical parameters.

SGS Minerals Services works for you to protect your interests and reduce your risk. Please contact us for the services and pricing specific to your commodity, cargo, product shipment and testing needs.

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SELECT METHODS

SGS offers a wide variety of select methods to analyze specific elements, species and/or groups of elements. These methods address specific circumstances that arise due to mineralogy, chemistry or commercial requirements. A selection of commonly requested methods are listed below and others are available. Please inquire.

RARE EARTH ELEMENT ANALYSISRare earth element (REE) samples can be analyzed using a variety of techniques depending on the concentration levels in the samples. The following packages are available for trace to percent level concentrations. Please inquire to ensure we meet your requirements.

The following REE packages can be combined with the multi-trace packages for low grade mineralized samples, as listed in the Exploration-Grade Analysis section of this guide.

RARE EARTH ELEMENT TRACE PACKAGES

CODE(S) ELEMENTS DESCRIPTION

GE IMS12B / GE IMS14B Pr, Nd, Sm, Eu, Gd, 2-Acid / AR digest / ICP-MS Dy, Ho, Er, Tm

GE ICM12B / GE ICM14B Pr, Nd, Sm, Eu, Gd, 2-Acid / AR digest / ICP-AES / Dy, Ho, Er, Tm ICP-MS

GE ICM40B Pr, Nd, Sm, Eu, Gd, 4-Acid digest / ICP-AES / ICP-MS Dy, Ho, Er, Tm

GE ICM90A La, Ce, Pr, Nd, Sm, Eu Sodium peroxide fusion / Gd, Tb, Dy, Ho, Er, Yb, ICP-AES / ICP-MS Lu, Tm, Th, U

GE IMS95A La, Ce, Pr, Nd, Sm, Lithium metaborate fusion / Eu, Gd, Tb, Dy, Ho, ICP-MS Er, Yb, Lu, Th, U, Y

Note: For details on the above digestion techniques, refer to the Exploration-Grade Analysis section of this guide or contact your local SGS lab.

SODIUM PEROXIDE FUSION / ICP-MS REE PACKAGE (17 ELEMENTS)

GO IMS91B


La 50 ppm Eu 1 ppm Er 0.5 ppm Y 5 ppm

Ce 50 ppm Gd 5 ppm Tm 0.1 ppm U 1 ppm

Pr 10 ppm Tb 1 ppm Yb 1 ppm

Nd 50 ppm Dy 1 ppm Lu 0.2 ppm

Sm 10 ppm Ho 0.1 ppm Th 5 ppm

Note: Other elements are available, please inquire. This technique requires a minimum sample weight of 0.5 g.

BORATE FUSION / XRF REE PACKAGE

GO XRF76R


La2O3 0.01 - 100% Nd2O3 0.02 - 100% Y2O3 0.02 - 100%

Ce2O3 0.02 - 100% Sm2O3 0.05 - 100% U3O8 0.01 - 100%

Pr2O3 0.03 - 100% ThO2 0.01 - 100%

Note: Other elements are available, please inquire. This technique requires a minimum sample weight of 5.0 g.

SELECT COPPER METHODSCopper can occur as oxide, sulphide and metallic forms in mineral deposits and metallurgical products so there are a variety of different analytical techniques available.

Note: Refer to the Exploration-Grade Analysis section for descriptions of the 12B, 14B, 40B and 90A digestion techniques. For descriptions of the 13B, 41Q, 42S and 90Q techniques, please see the Ore-Grade Analysis section, and for 13V and 03V refer to the Control-Grade Analysis section.

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EXPLORATION-GRADE COPPER METHODS

CODE(S) LIMIT(S) DESCRIPTION

GE ICP12B / GE ICP14B 0.5 ppm - 1% 2-Acid digest / Aqua regia – ICP-AES

GE IMS12B / GE IMS14B 0.5 ppm - 1% 2-Acid digest / Aqua regia – ICP-MS

GE ICM12B /GE ICM14B 0.5 ppm - 1% 2-Acid digest / Aqua regia – ICP-AES / ICP-MS

GE ICP40B 0.5 ppm - 1% 4-Acid digest – ICP-AES

GE ICM40B 0.5 ppm - 1% 4-Acid digest – ICP-AES / ICP-MS

GE ICP90A 10 ppm - 5% Fusion – ICP-AES

GE ICM90A 10 ppm - 1% Fusion – ICP-AES / ICP-MS

GE IMS90A 2 ppm - 5% Fusion – ICP-MS

ORE-GRADE COPPER METHODS


GO ICP13B 0.01 - 30% Aqua regia digest – ICP-AES

GO ICP41Q 0.01 - 30% 4-Acid digest – ICP-AES

GO AAS42S 0.001 - 50% 4-Acid digest – AAS

GO ICP90Q 0.01 - 30% Fusion – ICP-AES

CONCENTRATE-GRADE COPPER METHODS


GC CON13V* 5 - 60%* Short iodide titration

GC CON03V* 5 - 100%* Electrogravimetry

* These methods can be done at party or umpire quality (GT). In these cases, the upper end of the reporting range will be 100%.

MINERAL SELECTIVE COPPER METHODS


GO AAS71D >0.002% Cu oxide method, citric acid leach, AAS

GO AAS72B >0.002% Cu (non-sulphide method), H2SO4 leach, AAS

GO AAS77C >0.002% Cu acetic acid soluble, AAS finish

GO CSC67D >0.002% CN soluble Cu, AAS finish

GO AAS01D >0.001% Metallic Cu, AgNO3 digest, AAS

GO SQL01/02/03D >0.002% Sequential Cu leach (H2SO4 soluble Cu, Cyanide soluble Cu, residual Cu), AAS finish

Note: Slight method and coding variations can occur in different regions.

SELECT NICKEL METHODSNickel is used in stainless steels, metal alloys, plating, electric batteries and chemicals. It is found in either sulphide or laterite type ores so analytical methods are needed to ensure complete digestion.

Note: Refer to the Exploration-Grade Analysis section in this guide for descriptions of the 12B,14B, 40B and 90A digestion techniques. For descriptions of the 13B, 41Q, 42S and 90Q techniques, please see the Ore-Grade Analysis section, and for 06V and 07V refer to the Control-Grade Analysis section.

EXPLORATION-GRADE NICKEL METHODS


GE ICP12B / GE ICP14B 1 ppm - 1% 2-Acid digest / Aqua regia – ICP-AES

GE IMS12B / GE IMS14B 0.5 ppm - 1% 2-Acid digest / Aqua regia – ICP-MS

GE ICM12B / GE ICM14B 0.5 ppm - 1% 2-Acid digest / Aqua regia – ICP-AES / ICP-MS

GE ICP40B 1 ppm - 1% 4-Acid digest – ICP-AES

GE ICM40B 0.5 ppm - 1% 4-Acid digest – ICP-AES / ICP-MS

GE ICP90A 10 ppm - 10% Fusion – ICP-AES

GE ICM90A 5 ppm - 1% Fusion – ICP-AES / ICP-MS

GE IMS90A 5 ppm - 5% Fusion – ICP-MS

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ORE-GRADE NICKEL METHODS


GO ICP13B 0.01 - 30% Aqua regia digest – ICP-AES

GO ICP41Q 0.01 - 30% 4-Acid digest – ICP-AES

GO AAS42S 0.001 - 5% 4-Acid digest – AAS

GO ICP90Q 0.01 - 30% Fusion – ICP-AES

CONCENTRATE-GRADE NICKEL METHODS


GC CON06V 5 - 65% DMG separation / EDTA titration

GC CON07V 10 - 100% DMG separation / electroplating

* These methods can be done at party or umpire quality (GT). In these cases, the upper end of the reporting range will be 100%.

MINERAL SELECTIVE NICKEL METHODS

CODE LIMIT(S) DESCRIPTION

GO AAS03D >0.002% Metallic & sulphide nickel by bromine-methanol leach, AAS finish

Note: Additional selective methods for nickel may be available. Please inquire.

ORES AND COMMODITIES IRON ORESGS has unmatched XRF expertise at many of our laboratories. Iron ore is common in many mineral forms (hematite, magnetite, goethite, limonite or siderite) and analytical methods must be carefully chosen as iron minerals respond differently to various analytical methods. Borate fusion/XRF analysis is an extremely robust technique for major and minor element analysis in complex ores and offers highly precise and accurate results for iron ore samples. This method is not suitable for materials in which sulphide minerals exceed 1%.

BORATE FUSION / XRF IRON ORE PACKAGE (14 ELEMENTS)

GO XRF78S


Al2O3 0.01 - 100% MnO 0.01 - 100% TiO2 0.01 - 100%

CaO 0.01 - 100% Na2O 0.01 - 100% V2O5 0.01 - 100%

Cr2O3 0.01 - 100% P2O5 0.01 - 100% SO3 0.01 - 100%

K2O 0.01 - 100% Fe2O3 0.01 - 100% LOI 0.01 - 100%

MgO 0.01 - 100% SiO2 0.01 - 100% SUM %

Note: Additional minor elements can be added (As, Ba, Cl, Co, Cu, Ni, Pb, Sn, Sr, Ta, Zn and Zr). This method is available using robotic sample preparation as XRF78R in some SGS laboratories. This method is not suitable for samples with sulphide mineral contents > 1%. Please inquire.

VOLUMETRIC METHOD FOR IRON ORE

CODE ELEMENT LIMIT(S) DESCRIPTION MIN. SAMPLE WT.(g)

GC CON08V Fe 10 - 75% Titration 0.5

Note: these elements can be analyzed to party or umpire quality standards (GT) and can be reported up to 100%.

Magnetically susceptible minerals can be extracted from samples. Magnetic materials can be separated from nonmagnetic materials and materials with strong magnetic fields can be separated from materials with low magnetic fields. This property can be used to separate crushed iron ore at various stages of mineral processing.

The Satmagan test provides a measure of magnetic susceptibility, with results expressed as magnetic iron. The Davis Tube test also measures magnetic susceptibility, and can also separate various magnetic mineral phases. This allows for mass and elemental balancing.

SGS offers various magnetic separation techniques.

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CODE(S) TECHNIQUE DESCRIPTION

GO PHY29V Satmagan Measures the total magnetic moment in a saturated magnetic field to determine the percentage of magnetic material present

GO PHY28V Davis Tube Separates and gravimetrically determines strongly magnetic particles from weak and non-magnetic particles

URANIUMSGS complies with all national licensing requirements associated with the safe handling and analysis of naturally occurring radioactive materials samples for transportation, workplace safety and environmental protection. The following analytical packages are specifically designed for uranium exploration and are offered at designated SGS laboratories.

Multi-element packages are listed in the Exploration-Grade Analysis section of this guide for low grade uranium analysis.

URANIUM PACKAGES FOR LOW GRADE MINERALIZATION

CODE(S) ELEMENTS/ LIMIT(S) DESCRIPTION

GE IMS12B / GE IMS14B U (0.05 - 10000 ppm) 2-Acid / aqua regia digest / ICP-MS

GE ICM12B / GE ICM14B U (0.05 - 10000 ppm) 2-Acid / aqua regia digest / ICP-AES / ICP-MS

GE ICM40B U (0.05 - 10000 ppm) 4-Acid digest / ICP-AES / ICP-MS

GE ICM90A U (0.05 - 1000 ppm) Sodium peroxide fusion / ICP-AES / ICP-MS

GE IMS95A U (0.05 - 1000 ppm) Lithium metaborate fusion / ICP-MS

GE MMI-ME U (1 ppb) Mobile Metal Ion Technology™ for soils

Multi-element packages are listed in the Ore-Grade Analysis section of this guide. These methods are for medium to highly mineralized samples that include uranium analysis.

URANIUM PACKAGES FOR HIGHER GRADE MINERALIZATION


GO IMS91B 0.0001 - 1% Sodium peroxide fusion / ICP-MS

GO XRF75F 0.002 - 3% Internal standard / XRF

GO XRF76B 0.01 - 100% Borate fusion with internal standard / XRF

LITHIUMSGS has the methodology to support exploration and production analysis of lithium. Multi-element packages are listed in the Exploration-Grade Analysis section of this guide for low grade lithium samples.

LITHIUM PACKAGES FOR LOW GRADE MINERALIZATION


GE ICP12B / GE ICP14B Li (1 - 10000 ppm) 2-Acid / aqua regia digest / ICP-AES

GE ICM12B / GE ICM14B Li (1 - 10000 ppm) 2-Acid / aqua regia digest / ICP-AES / ICP-MS

GE ICP40B Li (1 - 10000 ppm) 4-Acid digest / ICP-AES

GE ICM40B Li (1 - 10000 ppm) 4-Acid digest / ICP-AES / ICP-MS

Multi-element packages are listed in the Exploration-Grade Analysis and Ore-Grade Analysis sections of this guide for medium to highly mineralized samples for lithium analysis.

LITHIUM PACKAGES FOR HIGHER GRADE MINERALIZATION


GE ICP90A Li (0.001 - 5%) Sodium peroxide fusion / ICP-AES

GE ICM90A Li (0.001 - 5%) Sodium peroxide fusion / ICP-AES / ICP-MS

GE IMS90A Li (0.0005 - 1%) Sodium peroxide fusion / ICP-MS

GO AAS93B Li (>0.001%) Sodium peroxide fusion / AAS

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FLUORSPARSGS has the methodology to support testing of fluorspar material. Due to the nature of the test this scheme is only applicable to acid grade or other soluble fluorspar products.

SOLUBLE FLUORSPAR PACKAGE


GC_CLA37V Ca (1-50%) EDTA Titration

CaCO3 (0.1-10%) EDTA Titration

CaF2 (10-100%) calculation

Note: For F results under 10%, CaF2 can be determined by calculation from GC_ISE05V. Samples with Ca content greater than 25% may not be suitable for GC_ISE05V.

GRAPHITIC CARBONSGS has the methodology to support testing of graphitic carbon.

GRAPHITIC CARBON PACKAGES

CODE(S) ELEMENTS/ LIMIT(S) DESCRIPTION MIN. SAMPLE WT. (g)

GE_CSB05V C graphitic (0.05%) Coulometry 0.2

GC_CSA05V C graphitic (0.05%) Roast; HCl leach; 0.4 IR Combustion

C graphitic (>30%) Roast; HCl leach; 0.4 high temp IR combustion (*SC632)

GC_CSA06V Total Carbon (<30%) IR Combustion 0.2

Total Carbon (>30%) High temp 0.2 IR Combustion (*SC632)

G_ASH01 **Ash content Gravimetric 20 (0.01-10%)

Note: *SC632 high temperature IR combustion furnace provides greater precision for carbon >30%.

**Ash content is not a suitable measurement of graphite purity for samples containing carbonates or other non-graphitic carbon species and is only recommended for samples >90% graphite.

IMPURITIES FOR GRAPHITIC CARBON (12 ELEMENTS)

GC ICP95A


Al 10 ppm K 8 ppm P 20 ppm

Ba 0.3 ppm Mg 3 ppm Si 30 ppm

Ca 10 ppm Mn 0.4 ppm Ti 0.8 ppm

Fe 20 ppm Na 5 ppm Zr 0.3 ppm

Requires a minimum sample weight of 20 g.

Note: Trace impurities are determined by lithium metaborate fusion with ICP-AES analysis on residue obtained by ashing (G_ASH01). Additional impurity elements are available upon request.

Graphitic carbon and impurity analysis is not available at all SGS locations, please inquire.

SGS offers a wide selection of analyses for ores, commodities and concentrates specific to your needs. The following list additional selections, and others are available. Please inquire.

• Manganese ores

• Aluminium ores (bauxite, including extractable SiO2, Al2O3, reactive Si, available Al)

• Tantalum ores

• Industrial minerals (limestone, chromite, borate)

• Fertilizers products (phosphate, sulphur, potash)

• Concentrates and metals

• Mineral sands

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ELEMENTS AND PACKAGES

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MINERALOGY SERVICESHigh Definition Mineralogy is the expert quantitative study of minerals using automated techniques. SGS is the world leader in providing comprehensive automated High Definition Mineralogy to the global minerals industry and other market sectors that need detailed material, product or residue characterizations.

SGS’ world-class team of mineralogical professionals provides a significant interpretive value to the High Definition Mineralogy product at every stage of your project. Our expertise, years of experience and comprehensive capabilities allow us to provide crucial input into your strategic decisions, giving you the competitive advantage you need.

While we can support investigations and interpretations of mineralogical data in many industries, we specialize in applications rooted in the exploration and mining industry. High Definition Mineralogy can provide important insights at the acquisition, exploration, prefeasibility, feasibility and operational levels:

SUPPORT FOR MINERAL EXPLORATION AND RESOURCE DELINEATION

Our EXPLOMIN™ products can help map the bulk mineralogy and ore textures with property development. Automated trace mineral searches are also available to identify precious or rare minerals including gold. We can also provide mineralogical, liberation and deportment data and interpretation in support of geometallurgical programs.

SUPPORT FOR METALLURGICAL OPERATIONS AND PLANTS

Our ore characterization and process mineralogy offerings provide detailed snapshots of the factors that influence grindability and metallurgical recovery. Such data is used to support flowsheet development for grassroots start-ups, metallurgical accounting for on-going operations and to benchmark plants during audits and troubleshooting programs.

SUPPORT FOR ENVIRONMENTAL CONSIDERATIONS

SGS provides the identification and deportment (texture) of minerals or phases in natural or industrial environments to:

• Support environmental programs (composition of waste rock, tailings and soils).

• Map deleterious mineral assemblages (As, Pb, Se).

• Establish sources of contaminants using forensic determinations.

• Analyze environments for industrial hygiene purposes (respirable silica and asbestos determinations).

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SGS’ team of applied and process mineralogists are experienced in the evaluation of ore samples and metallurgical products from a wide variety of commodities. Our Advanced Mineralogy Facilities are equipped with a wide variety of mineralogical equipment and techniques including:

• QEMSCAN®.

• X-ray diffraction (XRD).

• Scanning electron microscopy (SEM).

• Electronic microprobe.

• Optical mineralogy.

Refer to Rocks to Results, Section 5, and www.sgs.com/mining/mineralogy for additional information.

METALLURGY SERVICES

SGS’s demonstrated success in metallurgical and process design has provided thousands of companies with effective flowsheets and practical technical solutions to processing problems. From that core of capability, we continue to provide the processing industry with innovative approaches to geometallurgy, process modeling, production forecasting and advanced control systems.

The major activities of SGS’s mineral processing, metallurgy and process design experts include:

• Integrated analytical and mineralogical analysis.

• Risk mitigation using geometallurgical solutions.

• Development of environmentally sustainable processes and flowsheets for recovery and purification of pay metals.

• Confirmation of flowsheets via pilot plant testing programs.

• Development of new and innovative technologies for complex ore processing.

• Generation of engineering data for plant design purposes.

• Chemical engineering and process design for production facilities.

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CONVERSION FACTORS

US STANDARD TEST SIEVE SERIES

AMERICAN ASTM TYLER STANDARD SCREEN INTERNATIONAL

INCH OR SIEVE INCH OR SIEVE MILLIMETERS OR MICRONS

1.06 inch 1.05 inch 26.50mm

1 - 25.00

7/8 0.883 22.40

3/4 0.742 19.00

5/8 0.624 16.00

0.53 0.525 13.20

1/2 - 12.50

7/16 0.441 11.20

3/8 0.371 9.50

5/16 2 1/2 mesh 8.00

0.265 3 6.70

1/4 - 6.30

3 1/2 sieve 3.5 5.60

4 4 4.75

5 5 4.00

6 6 3.35

7 7 2.80

8 8 2.36

10 9 2.00

12 10 1.70

14 12 1.40

16 14 1.18

18 16 1.00

20 20 850µm

25 24 710

30 28 600

35 32 500

40 35 425

45 42 355

50 48 300

60 60 250

70 65 212

80 80 180

100 100 150

120 115 125

140 150 106

170 170 90

200 200 75

230 250 63

270 270 53

325 325 45

400 400 38

450 - 32

500 - 25

635 - 20

• On-site technical evaluations and audits.

• Evaluation and installation of advanced process control using expert systems.

• Evaluation and stabilization of discharge streams and waste products.

SGS provides solid, reliable, reputable, independent solutions for:

• Scoping studies.

• High Definition Mineralogy.

• Flowsheet development.

• Cyanidation technologies.

• Sustainable process development.

• Geometallurgy.

• Pilot plants.

• Bulk sample processing and market sample creation.

• Engineering data generation and modeling.

• Particulate testing.

For more information on the extensive range of bankable metallurgical services offered by SGS, please visit www.sgs.com/metallurgy.

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FREQUENTLY REQUESTED EQUIVALENTS

% G/T (GRAMS / MG/KG µG/KG PPM PPB METRIC TONNE)

1 10,000 10,000 10,000,000 10,000 10,000,000

0.1 1000 1000 1,000,000 1000 1,000,000

0.01 100 100 100,000 100 100,000

0.001 10 10 10,000 10 10,000

0.0001 1 1 1000 1 1000

CHEMICAL CONVERSION FACTORS

FORMULA RESULT FORMULA RESULT

Al x 1.889 AI2O3 Mn x 1.291 MnO

Ba x 1.699 BaSO4 MnO x 1.2255 MnO2

Ba x 1.116 BaO Mo x 1.668 MoS2

Be x 2.775 BeO Na x 1.348 Na2O

Ca x 1.399 CaO Nb x 1.431 Nb2O5

Ca x 2.497 CaCO3 P x 2.291 P2O5

CaO x 1.78479 CaCO3 Pb x 1.15474 PbS

Cr x 1.461 Cr2O3 Rb x 1.094 Rb2O

Cu x 1.25228 Cu2S Si x 2.139 SiO2

F x 2.055 CaF2 Sn x 1.27 SnO2

Fe x 1.286 FeO Sr x 1.185 SrO

Fe x 1.43 Fe2O3 Ta x 1.221 Ta2O5

Fe x 1.57414 FeS Th x 1.138 ThO2

Fe2O3 x 0.69943 Fe Ti x 1.668 TiO2

Fe2O3 x 0.89981 FeO U x 1.179 U3O8

Fe2O3 x 1.10101 FeS V x 1.785 V2O5

K x 1.205 K2O W x 1.261 WO3

Mg x 1.658 MgO Y x 1.27 Y2O3

Mg x 3.46908 MgCO3 Zr x 1.351 ZrO2

MgO x 2.09176 MgCO3 Zn x 1.49044 ZnS

DRILL CORE SPECIFICATION

DIAMETER VOLUME LENGTH

(MM) (INCH) M3X10-3 / M INCH3 / FOOT

AQ 27.0 1.062 0.57 10.6

TT 35.0 1.378 0.96 17.8

BQ 36.4 1.433 1.04 19.3

NQ 47.6 1.875 1.78 33.1

HQ 63.5 2.500 3.17 58.9

BQ3 33.5 1.320 0.88 16.4

NQ3 45.1 1.775 1.60 29.7

HQ3 61.1 2.406 2.93 54.6

PQ3 83.1 3.270 5.43 100.8

PQ 85.0 3.345 5.67 105.5

CONVERSION FACTORS

TROY OUNCES PER

PARTS PER PARTS PER METRIC SHORT LONG MILLION (ppm) BILLION (ppb) TONNE TON TON

1 Gram / MT 1 1000 0.03215 0.02917 0.0327

1 Troy oz / short ton 34.286 34286 1.1023 1 1.12

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SGS MINERALS LOCATIONSGEOCHEMISTRY CONTACTSAUSTRALIA

KALGOORLIE

17 Stockyard Way, Broadwood, WA, 6430Tel: + 61 (08) 9021 2911 Jared Olsen, [email protected]

PERTH

28 Reid Rd., Perth Airport, WA, 6105Tel: + 61 (0)8 9373 3500 Graeme Farrant, [email protected]

TOWNSVILLE

50 Leyland St., Garbutt, QLD, 4814Tel: + 61 (0)7 4725 2311 Anthony Wilson, [email protected]

WEST WYALONG

Lot 9, Gelling St., West Wyalong, NSW, 2671Tel: + 61 (0)2 6972 1211 Robert Moses, [email protected]

BRAZIL

BELO HORIZONTE

SGS Geosol Laboratorios Ltda, Rodovia MG 010, Km 24, 5 Bairro Angicos 33200-000 - Vespasiano - MG Tel: + 55 31 30450200 Alberto Faria, [email protected]

BURKINA FASO

OUAGADOUGOU

Zone Industrielle de Kossodo 11 BP: 565 Ouagadougou 11Mob: + 226 70 21 21 02 Helena Bouda, [email protected]

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CANADA

COCHRANE

1 First Ave., Cochrane, ON P0L 1C0Tel: + 1 705 272 2559 Ken Williams, [email protected]

LAKEFIELD

185 Concession St., Lakefield, ON K0L 2H0Tel: + 1 705 652 2000 Shelley Meyers, [email protected]

RED LAKE

16A Young St., Red Lake, ON P0V 2M0Tel: + 1 807 727 2939 Susan Isaac, [email protected]

VANCOUVER

3260 Production Way, Burnaby, BC V5A 4W4Tel: + 1 604 638 2349 Andrew Lai, [email protected]

CHILE

ANTOFAGASTA

Av. El Cobre #400 Parque Industrial, La Negra, Antofagasta Mob: + 56 99 8680857Enrique Bravo, [email protected]

CALAMA

Camino a Antofagasta S/N, Sitio 34, Parque Industrial APIAC Mob: + 56 99 8680857Enrique Bravo, [email protected]

COPIAPO

Calle 4, N° 718, Barrio Industrial Paipote, Copiapo Mob: + 56 99 8680857Enrique Bravo, [email protected]

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INDONESIA

JAKARTA

Sentra Industri Terpadu, Pantai Indah KapukBlok E2 No. 28, 29, 37, 38, Jalan Kamal Muara VII, Jakarta UtaraMob: + 62 21 5698 2898Nopi Mujiyanto, [email protected]

MALAYSIA

PORT KLANG (NEAR KUALA LUMPUR)

Wisma SGS, Lot 603, Leboh Raja Lumu Kawasan Perindustrian PKNS, Pandamaran Port Klang, Selangor, 42000Tel: + 60 3 3165 2320Gopi Dass Sivanandan, [email protected]

MALI

BAMAKO

Zone Industrielle Sotuba, Rue 947, Porte 213, BPE 2514 BamakoMob: + 223 66 74 62 39Firmin Bado, [email protected]

BAMAKO

c/o Morila Gold Mine, BPE 1194, BamakoMob: + 223 6558 9955E. Ohene Darko, [email protected]

MEXICO

DURANGO

Antimonio #121 Cd. Industrial, Durango, CP 34208Mob: + 52 1 618 125 1819 Marco Barragan, [email protected]

MONGOLIA

ULAANBAATAR

Uildveriin toirgiin 101 toot, Bayangol district 20th khoroo, Ulaanbaatar 36Tel: + 976 7014 4415Ankhbayar L., [email protected]

SANTIAGO

Puerto Madero 9600, Parque Industrial Puerto Santiago Pudahuel – SantiagoMob: + 56 99 8680857 Enrique Bravo, [email protected]

CHINA

TIANJIN

SGS Mansion, No. 41, The 5th Ave., TEDA, Tianjin, 300457Tel: + 86 (0) 22 6528 8209 Freeman Bu, [email protected]

URUMQI

No. 82, Nanyixiang, Huangshan St.2nd Development Area, Urumqi, XJ, 830026Tel: + 86 (0) 991 3775351 Jenny Ma, [email protected]

COLOMBIA

MEDELLIN

Carrera 52 No 14 Sur 26, Medellin Mob: + 57 4 3201080 William Joleane, [email protected]

DEMOCRATIC REPUBLIC OF THE CONGOLUBUMBASHI

No. 006838, Route Likasi, Quartier Jolie SiteCommune Annexe, Ville de LubumbashiLubumbashi, Haut Katanga Mob: + 243 8130 77538 Alex Adom, [email protected]

GHANA

TARKWA

Jerusalem Junction, Bankyim, Tarkwa Western Region, P.O. Box 38, Tarkwa Mob: + 233 (0) 24 432 3404 Thelma Botes, [email protected]

82 83

NEW ZEALAND

WAIHI

43 Victoria St., Waihi, 3610, P.O. Box 135, Waihi, 3641Tel: + 64 7 863 8969 Chris Morgan, [email protected]

WESTPORT

5 Lyttelton St., Westport, P.O. Box 240, 7866Mob: + 64 3 788 9003Nick Lees, [email protected]

PAKISTAN

KARACHI

H3/3 Sector #5, Korangi Industrial Area, Karachi, 74900Tel: + 92 21 3512 1388Tasneem Ilyas, [email protected]

PERU

LIMA (CALLAO)

Ave. Elmer Faucett, 3348, Callao 1 (Lima)Tel: + 51 1 517 1900 Maria Elena Napanga, [email protected]

RUSSIA

CHITA

5 Malaya St., 672014, ChitaTel: + 7 (3022) 31 46 44Anton Shatskikh, [email protected]

SOUTH AFRICA

ALLANRIDGE (NEXT TO TARGET MINE)

2 Buffalo St., Allanridge, Free State, 9490Tel: + 27 (57) 451 3412 Dwyne Van Zyl, [email protected]

BARBERTON

Rusplaas, Noordkaap, Barberton, Mpumalanga, 1300Tel: + 27 (13) 719 9775 Wimpie Geldenhuys, [email protected]

RANDFONTEIN

Zuurbekom Rd., Next to Cooke Recovery Plant Randfontein, Gauteng, 1760Tel: + 27 (0) 79 841 5877 Stephan Botha, [email protected]

RUSTENBURG

1 Ferro Street, Industrial Area, Rustenburg, 0299Tel: + 27 (0) 14 592 1654/8273 Wilford Tapudzai, [email protected]

TANZANIA

MWANZA

Nyanza Glass Works, Shinyanga Rd., MwanzaTel: + 255 28 2550861 Siegmond Laryea, [email protected]

TURKEY

ANKARA

Ankara 1. Organize Sanayi Bölgesi Orhan Isik Cad No:11 Sincan Ankara, 06935Mob: + 90 533 020 2149Z. Nazli Hatipoglu, [email protected]

ZAMBIA

KALULUSHI

SGS Kalulushi Chibuluma Business Park, KalulushiTel: + 260 (212) 730045 / 46 Joseph Chibesa, [email protected]

ZIMBABWE

HARARE

603 Shumba Rd., Ruwa, HarareTel: + 263 273 3058 / 3069 Masimera Mangana, [email protected]

84 85

METALLURGY CONTACTS

AUSTRALIA

PERTH

431 Victoria Rd., Malaga, WA, 6090 Tel: + 61 (0)8 9209 8700 Dwight Van Der Meulen, [email protected]

BRAZIL

BELO HORIZONTE

SGS Geosol Laboratorios Ltda, Rodovia MG 010, Km 24, 5Bairro Angicos 33200-000, Vespasiano, MG Tel: + 55 31 30450200 Fernanda Santos, [email protected]

CANADA

LAKEFIELD

185 Concession St., Lakefield, ON K0L 2H0 Tel: + 1 705 652 2000 Richard Wagner, [email protected]

QUEBEC

125 rue Fortin, Suite 100, Québec, QC G1M 3M2Tel: + 1 418 661 6624 Francois Verret, [email protected]

TORONTO

1140 Sheppard Ave. West, Unit #6, Toronto, ON M3K 2A2Tel: + 1 416 633 9400 Alan Gomez, [email protected]

BURNABY (VANCOUVER)

3260 Production Way, Burnaby, BC V5A 4W4Tel: + 1 604 638 2349 Sarah Prout, [email protected]

CHILE

SANTIAGO

Puerto Madero 9600, Parque Industrial Puerto Santiago, Pudahuel – Santiago Tel: + 56 2 898 9100 Reinaldo Barrera, [email protected]

PERU

LIMA (CALLAO)

Ave. Elmer Faucett, 3348, Callao 1 (Lima)Tel: + 51 1 517 1900Edmundo Alfaro, [email protected]

RUSSIA

CHITA

5 Malaya St., 672014, ChitaTel: + 7 (3022) 31 46 44Eugenia Glotova, [email protected]

SOUTH AFRICA

BOOYSENS-JOHANNESBURG

259 Kent Ave., Ferndale, Randburg Mob: + 27 (0) 82 894 4165Gavin Martin, [email protected]

UNITED KINGDOM

CORNWALL

Wheal Jane, Truro, Cornwall, TR3 6EE Tel: + 44 0 1872 561577 Nigel MacDonald, [email protected]

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ENGINEERING SERVICES CONTACTS

SOUTH AFRICA

JOHANNESBURG

SGS Bateman (Pty) LtdWoodmead North Office Park 54 Maxwell Drive, Waterfall 2191Tel: + 27 11 100 9100Bert van Hege, [email protected] Ken Richardson, [email protected]

UNITED STATES

TUCSON

3845 N. Business Center Dr., Suite 111, Tucson, AZ, 85705 Tel: + 1 520 579 8315 John Holley, [email protected]

WWW.SGS.COM

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Appendix G: DGI Report

Phase 1 Diamond Drilling Program - Goldlund Property 2017

Documents

Transcript of Phase 1 Diamond Drilling Program - Goldlund Property 2017