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GWR GROUP LIMITED Capital/Financing Update 2017

Mar 14, 2017

65031_rns_2017-03-14_43ae9018-3943-42c4-a30b-d42aadc48041.pdf

Capital/Financing Update

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15 March 2017

ASX Announcements Office ASX Limited 20 Bridge Street Sydney NSW 2000

CORRECTION FOR TYPOGRAPHICAL ERROR IN ASX RELEASE: “ EXCEPTIONAL RESULTS FROM MAIDEN RC DRILLING PROGRAM AT HATCHES CREEK

Dear Sir/Madam

The Company’s ASX announcement dated 14 March 2017 and titled “ Exceptional Results from Maiden RC Drilling Program at Hatches Creek” contained a minor typographical error. Drill hole prefix references of “WWRC” should have read “HCRC”.

This has been corrected in the accompanying release attached hereto.

Sincerely,

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Craig Ferrier Chief Executive Officer

E [email protected] W www.gwrgroup.com.au

GWR Group Ltd 97 Outram Street ABN 54 102 622 051 West Perth WA 6005

PO Box 517 T +61 8 9322 6666 West Perth WA 6872 F +61 8 9322 2370

14 March 2017

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ASX Announcement

EXCEPTIONAL RESULTS FROM MAIDEN RC DRILLING PROGRAM AT HATCHES CREEK

Highlights

  • RC drilling at four prospects confirms polymetallic mineralisation.

  • Several prospects intersected wide zones of mineralisation in areas where narrow high grades were expected.

  • Intersections include:

  • HCRC013, 44m at 0.21% WO3 and 0.12% Cu, from 55m

  • HCRC014, 53m at 0.26% WO3 and 0.13% Cu, from 63m

  • HCRC016, 7m @ 0.73% WO3, and 0.01% Cu, from 81m

  • HCRC010, 2m @ 3.05% WO3 and 0.02% Cu, from 3m

  • HCRC004, 1m @ 2.85% WO3, 1.76g/t Au and 0.29% Cu, from 43m

  • HCRC004, 1m @ 1.96% WO3, 1.58g/t Au and 0.28% Cu, from 80m

  • Follow up drilling planned along strike as well as at next set of targets.

  • Metallurgical test work undertaken as part of the original dumps project in 2015 produced a concentrate of 66% WO3. In addition, a sulphide pre-float produced a concentrate assaying 16.4% Cu and 7.9g/t Au, demonstrating the ability to recover both tungsten and other valuable by-products.

  • Recent test work undertaken on dump samples from Pioneer showed that 97% of the WO3 could be recovered, with 34% mass reduction by simply crushing. At Hit or Miss, a combination of screening and X-ray ore sorting test work has resulted in a 98% WO3 yield and a mass rejection of 24%.

GWR Group Limited (ASX: GWR) (“GWR” or “the Company”) is pleased to announce that Reverse Circulation (RC) drilling at the Hatches Creek Project in the Northern Territory has successfully intersected tungsten mineralisation (WO3) as well as copper (Cu) and gold (Au) at some of the prospects.

GWR tested four prospects in this initial drilling campaign, with targets assessed based on previous dump sampling, mapping and accessibility.

At Treasure , broad zones of tungsten and copper mineralisation were intersected. Where the initial target was narrow high grade zones, the drilling returned 53m at 0.26% WO3 and 0.13% Cu, from 63m in HCRC014 and 44m at 0.21% WO3 and 0.12% Cu, from 55m in HCRC013.

Intersections at Hit or Miss included wide zones such as 36m at 0.18% WO3 and 0.24% Cu in HCRC011 from 52m and narrow high grade intersections including 2m at 3.05% WO3 from 3m in HCRC010.

At Pioneer , the Company intersected multiple stacked zones of mineralisation that correspond with historical mining zones. Several of the holes intersected at least three stacked mineralised zones. Better results included 2m at 1.60% WO3, 0.96g/t Au and 0.36% Cu from 43m in HCRC004, also in HCRC004, 1m @ 1.96% WO3, 1.58g/t Au and 0.28% Cu, from 80m and 3m at 0.63% WO3 from 81m in HCRC002. Eight of the mineralised tungsten zones also had coincident gold grades of greater than 0.8g/t Au.

PO Box 517 T +61 8 9322 6666 E [email protected] West Perth WA 6872 F +61 8 9322 2370 W www.gwrgroup.com.au

GWR Group Ltd 97 Outram Street ABN 54 102 622 051 West Perth WA 6005

At Copper Show , tungsten and copper mineralisation were of a similar tenor in the intersected holes. Results included 1m at 0.58% WO3 and 0.54% Cu from 3m and 1m at 0.49% WO3 and 0.12% Cu, both in HCRC006.

GWR’s Chief Executive Officer, Craig Ferrier, said “ These are excellent results from what was the first modern drilling program ever completed at Hatches Creek.

“While further drilling is required before we can confidently say that we have made a new polymetallic discovery, the success rate that we have had in this first program coupled with the grades and widths encountered, offers significant upside potential for shareholders.”

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Figure 1: Hatches Creek Location Plan

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Hatches Creek Drilling Program

GWR has completed an 18 hole, 1,739m maiden RC drilling program at its 100% owned Hatches Creek project located in the Northern Territory (Figure 1). Four prospect areas were targeted; Pioneer, Hit or Miss, Treasure and Copper Show (Table 1), while an additional 11 prospects remain to be drilled.

The drilling has intersected significant tungsten and copper mineralisation in all four areas targeted and at Treasure and Hit or Miss over much larger widths than expected. At Pioneer, the tungsten and copper mineralisation is also accompanied by gold mineralisation confirming the polymetallic nature of the mineralised structures.

Table 1

Drill Hole Collar Summary

Prospect Tenement Hole # Depth
(M)
East
(MGA)
North
(MGA)
RL Azimuth
/ Dip
Pioneer EL23463 HCRC001 29 518740 7692154 403 360/‐60
Pioneer EL23463 HCRC002 96 518744 7692114 401 360/‐60
Pioneer EL23463 HCRC003 130 518750 7692074 399 360/‐60
Pioneer EL23463 HCRC004 100 518630 7692080 400 360/‐60
Pioneer EL23463 HCRC005 84 518626 7692117 402 360/‐60
Copper
Show
EL22912 HCRC006 40 516950 7685380 450 180 /‐60
Copper
Show
EL22912 HCRC007 50 516950 7685400 450 180 /‐60
Copper
Show
EL22912 HCRC008 100 516950 7685425 450 180 /‐60
Hit or
Miss
EL22912 HCRC009 100 519590 7685740 431 090/‐60
Hit or
Miss
EL22912 HCRC010 100 519550 7685740 430 090/‐60
Hit or
Miss
EL22912 HCRC011 100 519510 7685740 430 090/‐60
Hit or
Miss
EL22912 HCRC012 100 519470 7685750 432 090/‐60
Treasure EL22912 HCRC013 120 519840 7686860 425 090/‐60
Treasure EL22912 HCRC014 120 519925 7686850 432 270/‐60
Treasure EL22912 HCRC015 120 519845 7687050 443 090/‐60
Treasure EL22912 HCRC016 150 519800 7687070 438 090/‐60
Hit or
Miss
EL22912 HCRC017 100 519460 7685750 432 090/‐60
Hit or
Miss
EL22912 HCRC018 100 519620 7685745 435 090/‐60

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Figure 2: Hatches Creek Prospect Locations

Pioneer

The Pioneer mine is the largest historical mine in the Hatches Creek region. Records show that the mine was developed to a vertical depth of 63m (206’) and consisted of up to 5 parallel lodes. The dumps and historical tailings contain a total Inferred Resource of 85,600 tonnes @ 0.66% WO3 (upper cut of 1.5% WO3 applied), refer to Arunta Resources Limited ASX release 23[rd] September 2014. Recent dump sampling by GWR also showed that the historical dumps contained anomalous to significant Au and Cu mineralisation (ASX release dated 27[th] October 2016).

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Figure 3: Pioneer Mine

A total of 5 RC holes (HCRC001 to HCRC005) were drilled on two east-west orientated lines (Figure 4), with historical mine plans used to assist with targeting the previously recognised lodes.

HCRC001 to HCRC003 (Figure 5) were drilled on a line adjacent to the Macarthur Shaft (headframe in Figure 2) and HCRC004 and HCRC005 (Figure 6) were drilled adjacent to Cambells shaft.

Significant results are listed in Table 2 and all results are provided in Appendix 1. Intercepts include:

  • HCRC002, 1m @ 1.31% WO3, 0.26g/t Au and 0.04% Cu, from 81m

  • HCRC003, 1m @ 1.20% WO3, 0.81g/t Au and 0.93% Cu, from 121m

  • HCRC004, 1m @ 2.85% WO3, 1.76g/t Au and 0.29% Cu, from 44m

The drilling results confirm the polymetallic nature of the mineralisation with significant and at times coincident WO3, Au and Cu intercepts having been achieved.

As Figure 5 shows (518745E Cross Section), the drilling intersected four mineralised structures, which correspond to the previously recognised, #1, #2 and #12 lodes, plus an additional unnamed possibly unknown structure. Interestingly, the significant / anomalous Au and Cu mineralisation appears to be confined to the Pedlar Gabbro and absent in the quartzite. Importantly, all the targeted lodes contained significant WO3 mineralisation.

Cross Section 518630E (Figure 6), shows that five mineralised structures were intersected, which appear to correspond with the previously recognised; #1 Lode, #5 Lode, Della Lode, #12 Lode and possibly Pink Lode. All significant WO3 intercepts also contained anomalous or significant Au mineralisation. On this section, all of the targeted lodes contained significant WO3 mineralisation.

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Figure 4: Pioneer Mine Drill Hole Collars

6

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Figure 5: Pioneer Cross Section 518745E

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Figure 6: Pioneer Cross Section 518630E

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Hit or Miss

The Hit or Miss Group historically contains the largest and most complex concentration of tungsten bearing veins at Hatches Creek. Historical mining activities have exposed multiple mineralised structures of varying orientations but dominantly north striking over an area of approximately 10 hectares (Figure 7). More than 30 individual mineralised structures have been identified by previous mining activities, which dominantly strike in a north to north-north east direction. However, there several east trending mineralised structures, suggesting significant potential for a quartz stockwork or sheeted vein style of mineralisation.

A total of 6 RC holes were completed on a single east-west orientated line with holes generally spaced at 40m intervals. The area drilled was selected because of topography and the presence of an existing track and not because of the density of potential mineralisation. The drilling was highly successful and identified 14 individual mineralised structures containing significant WO3 mineralisation. Anomalous and significant Cu mineralisation was also identified and interestingly, this was sometimes independent of the WO3 mineralisation. Lithology in this area strikes in an easterly direction and is subparallel to the drill traverse and all holes were dominantly within quartzites and some with minor shale. Historical accounts suggest that mineralisation is stronger within the felsic volcanics and these are the preferred host.

Significant results are listed in Table 2 and all results are provided in Appendix 1. Intercepts include:

  • HCRC010, 1m @ 8.68% WO3, and 0.04% Cu, from 4m

  • HCRC011, 36m @ 0.18% WO3, and 0.24% Cu, from 52m

  • HCRC012, 4m @ 0.06% WO3 and 1.65% Cu, from 43m

  • HCRC012, 5m @ 0.17% WO3 and 0.76% Cu, from 71m

As Figure 8 shows (Cross Section 70685740N), the RC drilling intersected 14 mineralised structures containing greater than 1m @ 0.1% WO3. Importantly, five of these were nestled between the previously recognised # 1 Lode and # 2 Lode over an estimated true width of 20m. As shown in Figure 7, there is evidence to the north of the drill traverse that this mineralised zone between #1 and 2 Lodes persists along strike. The significant and anomalous Cu mineralisation intersected in most holes, sometimes independent of the WO3, was unexpected and suggests that a powerful mineralising event has occurred. As Figure 7 also shows, the drilling to date has only tested approximately 50% of the potential width of the mineralised area.

The RC drilling program has demonstrated significant potential for a substantial WO3 / Cu deposit and further drilling is planned to evaluate the 10 hectare area of potential mineralisation, especially within the felsic volcanic rocks that are considered even more prospective.

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Figure 7; Hit or Miss Drill Hole Collars

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Figure 8; Hit or Miss Cross Section 7,685,750N

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Treasure

The Treasure area contains substantial underground workings that rival the Pioneer in their length but not in depth. Treasure was the 3[rd] largest producer at Hatches Creek behind Pioneer and Hit or Miss (Figure 9).

A total of four RC holes were completed on two east–west orientated lines (768650N and 7687060N) as shown in Figure 9. As with Hit or Miss, the drill sites were selected partly because of accessibility and not necessarily prospectivity. The drilling was however highly successful and intersected broad zones of significant WO3 mineralisation, which was often accompanied by significant to anomalous Cu mineralisation. All holes were within felsic volcanics and the mineralisation, based upon historical data, suggests that this is the preferred host in this location

Significant results are listed in Table 2 and all results are provided in Appendix 1. Intercepts include:

  • HCRC013, 44m @ 0.21% WO3, and 0.12% Cu, from 55m

  • HCRC013, 2m @ 1.27% WO3, and 0.58% Cu, from 114m

  • HCRC014, 53m @ 0.26% WO3, and 0.13% Cu, from 63m

  • HCRC014, 2m @ 1.72% WO3, and 0.07% Cu, from 112m

  • HCRC015, 11m @ 0.30% WO3, and 0.02% Cu, from 21m

  • HCRC016, 7m @ 0.73% WO3, and 0.01% Cu, from 81m

  • HCRC016, 3m @ 1.22% WO3, and 0.05% Cu, from 126m

On Cross Section 7686850N (Figure 10), multiple mineralised structures were intersected in HCRC013 and HCRC014, between the previously identified #2 and #3 lodes, containing unexpected significant and anomalous Cu mineralisation. The estimated true width of the mineralised zone is 25m, which is markedly different to the expected narrow high grade mineralisation. Outside of the above zone, two other mineralised structures were identified, meaning a total of six structures were intersected containing significant WO3 mineralisation with grades of up to 2.87% WO3 and up to 0.90% Cu.

On Cross Section 7687060N, HCRC015 and HCRC 016 intersected the targeted Main and #2 Lodes, with a combined estimated true width of 5 to 7m and grades of up to 3.54% WO3, plus an additional three mineralised structures. Interestingly, the mineralisation contained no anomalous Cu.

The RC drilling at Treasure, especially on line 7686850, has intersected broad widths of significant mineralisation over estimated true widths of up to 25m. Based upon historical records and mine workings, the potential strike length is 400 to 500m. As such, the potential for this area to host a significant WO3 / Cu deposit is considered to be high.

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Figure 9; Treasure Drill Hole Collars

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Figure 10; Treasure Cross Section 7,686,850N

Copper Show

Copper Show is located in the south west corner of the project area approximately 2.6km west south west of Hit or Miss (Figure 2). Historical mine workings exist over a strike length of approximately 120m and strike in an east-north east direction. According to historical records, the ore in this location is complex and contains wolframite, scheelite, and as the name suggests, substantial copper. Recent dump sampling by GWR (ASX release 27[th] October 2016) confirms WO3 grades of between 1% and 3.5% with Cu ranging from 1 to 3.7%.

A total of three RC holes (HCRC006 to 8) were drilled on a single north–south orientated line on 516950E. The results compared to the other areas were disappointing, with only 4 significant intercepts achieved, the best being HCRC006, 1m at 0.58% WO3 and 0.54% Cu. Based upon the substantial mineralisation evident from the historical mine workings and dumps, it is possible that the recent drilling has missed the target. Further work is planned to investigate this.

Metallurgical Test work and Recent Crushing and Ore Sorting Test work

Substantial metallurgical test work as part of the dumps project has already been undertaken over the project area with positive results (refer to announcement 19[th] January 2015, March 2015 Quarterly Report and June 2015 Quarterly Report).

Crushing and ore sorting testwork was recently undertaken on bulk samples previously collected from Pioneer and Hit or Miss. A 203kg sample of Hit or Miss (0.3% WO3) and 213kg sample of Pioneer (0.4% WO3) were chosen, crushed to p100 -40mm and screened at 20mm. The -40mm+20mm material was bagged and shipped to Tomra Ore Sorting Technology in NSW and the -20mm material remained at Nagrom.

For the Pioneer waste dump composite, 52% of the mass deported to the +20mm portion and for the Hit or Miss dump composite, 44% of the mass deported to the +20mm portion. In both samples, there is a significant %WO3 grade differential between the +20 and -20mm fraction, in particular for the Pioneer dump where the +20mm size fraction assayed 0.04% WO3 vs the -20mm size fraction that assayed 0.60% WO3.

For the Pioneer sample, 97% of the contained WO3 and 66% of the feed mass deports to the -20mm size fraction. The grade of the -20mm fraction has increased from 0.41 to 0.60% WO3. Although only 3% of the contained WO3 deported to the ore sorter feed, the ore sorter was effective in increasing the grade from 0.04% in the feed to 0.11% WO3 in the “accepts” portion whilst recovering 95% of the WO3. Overall WO3 recovery in the circuit was 99.9% with 22% of the mass removed as waste.

For the Hit or Miss sample, 81% of the contained WO3 and 69% of the feed mass deports to the -20mm size fraction and 19% of the contained WO3 has deported to the ore sorter feed. The ore sorter has been effective in increasing the WO3 grade from 0.17% in the feed to 0.68% in the “accepts” portion whilst recovering 89% of the WO3. Overall WO3 recovery in the circuit was 98% with 24% of the mass removed as waste.

Planned Work Future Program

The recent RC program tested four target areas and a further 11 targets remain. GWR has an approved Environmental Management and Monitoring Plan (EMMP) from both the NT Mines Department and Work Program from Central Land Council (CLC) to also drill at the Black Diamond, Copper Show, Bonanza, Hens and Chicken, Masters Gully and Kangaroo Group target areas. Based upon the highly

15

successful results to date, testing these targets is more than justified and GWR plans to undertake this as soon as practicably possible.

It is planned to also submit an EMMP to the NT Mines Department and CLC to test possible strike extensions to the mineralisation already identified and to also test additional target areas.

For further information: Craig Ferrier Chief Executive Officer Ph: +61 8 9322 6666 E: [email protected]

For Broker and Media Enquiries: Andrew Rowell Cannings Purple Ph: +61 400 466 226 E: [email protected]

Competent Persons Statement

The information in this report which relates to Exploration Targets, Exploration Results and Mineral Resources or Ore Reserves is based on information compiled by Mr Allen Maynard, who is a Member of the Australian Institute of Geosciences (“AIG”), a Corporate Member of the Australasian Institute of Mining & Metallurgy (“AusIMM”) and independent consultant to the Company. Mr Maynard is the Director and principal geologist of Al Maynard & Associates Pty Ltd and has over 35 continuous years of exploration and mining experience in a variety of mineral deposit styles. Mr Maynard has sufficient experience which is relevant to the style of mineralisation and type of deposit under consideration and to the activity which he is undertaking to qualify as a Competent Person as defined in the 2012 Edition of the “Australasian Code for reporting of Exploration Results, Exploration Targets, Mineral Resources and Ore Reserves”.(JORC Code). Mr Maynard consents to inclusion in the report of the matters based on this information in the form and context in which it appears.

Details concerning the JORC-2012 Resource Estimate for the Hatches Creek Tungsten Project (including table 1 report) and referred to in this announcement are set out in the ASX announcement of Arunta Resources Ltd dated 23 September 2014

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Table 2

Significant RC Drill Hole Intercepts

Prospect Hole# East
(MGA 94)
North
(MGA 94)
**Dip/Azi ** From
(m)
To
(m)
Interval
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Pioneer HCRC001 518740 7692154 ‐60 / 360 8 9 1 0.1 0.06 0.01
12 13 1 0.41 0.01 0.08
Pioneer HCRC002 518744 7692114 ‐60 / 360 44 45 1 0.45 0.01 0.01
68 69 1 0.73 0.11 0.10
76 77 1 0.16 0.50 0.26
81 84 3 0.63 0.10 0.05
INCL 81 82 1 1.31 0.26 0.04
EOH 95 96 1 0.25 0.02 0.04
Pioneer HCRC003 518750 7692074 ‐60 / 360 38 39 1 0.11 0.05 0.21
54 55 1 0.30 0.42 0.43
92 93 1 0.68 0.08 0.74
97 98 1 0.00 2.26 0.01
107 108 1 0.19 0.02 0.08
118 119 1 0.16 0.01 0.01
121 122 1 1.20 0.81 0.93
128 129 1 0.11 0.03 0.25
Pioneer HCRC004 518630 7692080 ‐60 / 360 0 1 1 0.14 0.10 0.06
2 4 2 0.14 0.80 0.31
INCL 3 4 1 0.14 1.33 0.29
35 36 1 0.31 0.07 0.03
43 45 2 1.60 0.96 0.36
INCL 44 45 1 2.85 1.76 0.29
48 49 1 0.44 0.19 0.02
52 54 2 0.39 0.99 0.03
INCL 53 54 1 0.42 1.96 0.04
70 71 1 0.23 0.06 0.28
72 74 2 0.16 0.01 0.31
80 81 1 1.96 1.58 0.28
93 94 1 0.12 0.01 0.01
95 96 1 0.12 0.01 0.03
Pioneer HCRC005 518626 7692117 ‐60 / 360 4 5 1 0.74 0.60 0.10
12 13 1 0.20 0.84 0.03
37 38 1 0.15 0.05 0.05
Copper Show HCRC006 516950 7685380 ‐60 / 180 0 1 1 0.49 0.12
3 4 1 0.58 0.54
Copper Show HCRC007 516950 7685400 ‐60 / 180 20 21 1 0.17 0.07
26 27 1 0.17 0.13
Hit or Miss HCRC009 519590 7685740 ‐60 / 090 55 56 1 0.20 0.01
73 75 2 0.66 0.03
INCL 73 74 1 1.19 0.00
0.05% LOWER CUT OFF 84 93 9 0.39 0.02
Prospect Hole# East
(MGA 94)
North
(MGA 94)
**Dip/Azi ** From
(m)
To
(m)
Interval
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
84 87 3 0.67 0.01
INCL 84 85 1 1.71 0.01
91 93 2 0.63 0.03
97 98 1 0.26 0.00
Hit or Miss HCRC010 518550 7685740 ‐60 / 090 0 1 1 0.12 0.01
3 5 2 3.05 0.02
INCL 4 5 1 8.68 0.04
16 17 1 0.11 0.04
41 42 1 0.15 0.04
49 51 2 0.41 0.01
61 63 2 0.24 0.01
Hit or Miss HCRC011 519510 7685740 ‐60 / 090 1 2 1 0.54 0.01
37 38 1 0.11 0.03
43 44 1 0.19 0.01
MINERALISED ZONE 52 88 36 0.18 0.24
52 56 4 0.67 0.02
INCL 55 56 1 1.39 0.02
62 65 3 0.39 0.20
67 68 1 0.12 0.08
69 71 2 0.20 0.15
71 72 1 0.09 0.73
73 74 1 0.07 3.30
76 77 1 0.24 0.03
78 79 1 0.20 0.02
86 87 1 0.04 1.62
87 88 1 0.69 1.09
99 100 1 0.04 0.53
Hit or Miss HCRC012 519470 7685750 ‐60 / 090 22 23 1 0.35 0.08
27 28 1 0.43 0.02
41 42 1 0.11 0.09
43 47 4 0.06 1.65
59 60 1 0.02 1.66
62 63 1 0.44 0.01
71 76 5 0.17 0.76
72 73 1 0.22 0.92
74 76 2 0.29 0.54
96 98 2 0.49 0.12
Treasure HCRC013 519840 7686860 ‐60 / 090 8 9 1 0.12 0.03
12 16 4 0.20 0.05
MINERALISED ZONE 55 99 44 0.21 0.12
55 64 9 0.22 0.03
INCL 58 59 1 2.87 0.08
68 71 3 0.16 0.05
76 80 4 0.48 0.04
84 90 6 0.15 0.12
Prospect Hole# East
(MGA 94)
North
(MGA 94)
**Dip/Azi ** From
(m)
To
(m)
Interval
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
94 96 2 0.11 0.16
98 99 1 0.24 0.27
104 106 2 0.13 0.01
111 112 1 0.15 0.01
114 116 2 1.27 0.58
INCL 114 115 1 1.98 0.38
Treasure HCRC014 519925 7686850 ‐60 / 270 1 4 3 0.13 0.03
29 30 1 0.13 0.05
36 37 1 0.50 0.11
41 42 1 0.14 0.01
MINERALISED ZONE 63 116 53 0.26 0.13
63 66 3 0.42 0.14
69 74 5 0.14 0.37
INCL 69 70 1 0.15 0.90
INCL 92 93 1 1.51 0.08
105 116 11 0.53 0.17
INCL 112 114 2 1.72 0.07
Treasure HCRC015 519845 7687050 ‐60 / 090 21 27 6 0.14 0.02
29 32 3 0.81 0.01
INCL 30 31 1 1.35 0.01
21 32 11 0.30 0.02
Treasure HCRC016 519800 7687070 ‐60 / 090 70 71 1 0.31 0.01
81 88 7 0.73 0.01
INCL 82 83 1 1.26 0.01
INCL 86 87 1 3.54 0.01
126 129 3 1.22 0.05
INCL 127 128 1 3.15 0.05
131 132 1 0.22 0.01
139 140 1 0.35 0.08
143 144 1 0.39 0.00
Hit or Miss HCRC017 519460 7685750 ‐80 / 090 6 7 1 0.74 0.25
54 59 5 0.33 0.18
60 64 4 0.04 0.87
61 62 1 0.04 1.41
73 74 1 0.14 0.05
86 87 1 0.14 0.01
92 93 1 0.45 0.07
Hit or Miss HCRC018 519620 7685745 ‐60 / 090 65 67 2 0.57 0.08
76 77 1 0.11 0.01
78 79 1 0.12 0.05

APPENDIX 1 JORC 2012 TABLE 1

JORC 2012 TABLE 1

SECTION 1: SAMPLING TECHNIQUES AND DATA

Criteria JORC Code explanation
Commentary
Sampling techniques Nature and quality of sampling (e.g. cut channels, random chips, or specific
specialised industry standard measurement tools appropriate to the minerals
under investigation, such as down hole gamma sondes, or handheld XRF
instruments, etc.). These examples should not be taken as limiting the broad
meaning of sampling.
The Pioneer, Copper Show, Hit or Miss and Treasure prospect areas at the Hatches Creek project
were sampled using Reverse Circulation (“RC”) drilling. A total of 18 holes for an aggregate of
1739m was completed.
Include reference to measures taken to ensure sample representivity and the
appropriate calibration of any measurement tools or systems used
The drill holes were located to intersect the mineralisation at representative points to help with
the overall understanding of the geology and distribution of the mineralisation.
All the sample recoveries were visually estimated and logged as they were collected and all the
samples were consistently logged as approximately 100%.
All the drill samples as well as QAQC samples including duplicates and Certified Standards were
submitted to an independent, ISO certified laboratory for chemical analysis.
No measurement tools or systems were used that required calibration.
Aspects of the determination of mineralisation that are Material to the Public
Report. In cases where ‘industry standard’ work has been done this would be
relatively simple (e.g. ‘reverse circulation drilling was used to obtain 1 m
samples from which 3 kg was pulverised to produce a 30 g charge for fire
assay’). In other cases more explanation may be required, such as where there
is coarse gold that has inherent sampling problems. Unusual commodities or
mineralisation types (e.g. submarine nodules) may warrant disclosure of
detailed information
Samples were collected at 1m intervals using cyclone and passed through a cone splitter. Duplicate
(A and B sample) sub samples were collected of approximately 2 to 4kg in pre‐numbered and
barcoded calico sample bags and the residue stored in a plastic bag. The A calico bag sample was
submitted to Nagrom Laboratories in Perth where the following was carried out;

Dried and pulverized

WO3, Sn, Fe2O3, MnO, SiO2, Al2O3, TiO2, CaO, MgO, As, P, S, Mo, Cu, Bi and Sb were all
analysed using the Nagrom XRF008 technique with a lower detection limit of 0.001%

At the Pioneer prospect Au was also analysed by fire assay with a lower detection limit
of 0.01 ppm
Drilling techniques Drill type (e.g. core, reverse circulation, open‐hole hammer, rotary air blast,
auger, Bangka, sonic, etc) and details (e.g. core diameter, triple or standard
tube, depth of diamond tails, face‐sampling bit or other type, whether core is
oriented and if so, by what method, etc).
A total of 18 RC holes for an aggregate of 1739m was completed at depths ranging from 29 to
150m, averaging 97m. All of the drilling was undertaken using a 146mm face sampling RC hammer
Drill sample recovery Method of recording and assessing core and chip sample recoveries and results
assessed
The sample recovery was visually assessed and recorded on drill logs and is considered to be
acceptable.
Criteria JORC Code explanation
Commentary
Measures taken to maximise sample recovery and ensure representative nature
of the samples
The samples were visually checked for recovery, moisture and contamination. A cyclone and cone
splitter were utilised to provide a representative sample and were regularly cleaned. The drilling
contractor blew out the hole at the beginning of each rod to remove any water.
Whether a relationship exists between sample recovery and grade and whether
sample bias may have occurred due to preferential loss/gain of fine/coarse
material.
The ground conditions were good and the drilling returned consistent sized dry samples and the
possibility of sample bias through selective recoveries is considered negligible.
Logging Whether core and chip samples have been geologically and geotechnically
logged to a level of detail to support appropriate Mineral Resource estimation,
mining studies and metallurgical studies.
All samples were geologically logged with lithology and mineralisation recorded. This logging was
of sufficient detail to support the findings of this report and, after further drilling is completed,
included in later Mineral Resource estimation.
Whether logging is qualitative or quantitative in nature. Core (or costean,
channel, etc) photography.
The drill sample logging was qualitative.
The total length and percentage of the relevant intersections logged
All the drill samples were logged.
Sub‐sampling techniques and
sample preparation
If core, whether cut or sawn and whether quarter, half or all core taken.
This section is not applicable as there were no core samples collected.
If non‐core, whether riffled, tube sampled, rotary split, etc and whether
sampled wet or dry.
The RC drilling chip samples were collected using a cyclone and then duplicate sub samples of 2kg
to 4kg in size collected using a cone splitter attached to the cyclone. All samples were dry.
For all sample types, the nature, quality and appropriateness of the sample
preparation technique.
Samples were submitted to Nagrom Laboratories in Perth where the following sample preparation
procedures were carried out;

The sample was dried and crushed to ‐6.3mm using a jaw crusher

Samples in excess of 2kg are riffle split

The crushed sample is pulverized to 95% passing 75 micron
These sample preparation procedures followed by the laboratory meet industry standards and are
appropriate for the sample type and mineralisation being analysed.
Quality control procedures adopted for all sub‐sampling stages to maximise
representivity of samples.
Certified Standards and duplicate samples were routinely inserted into the sample sequences
submitted for chemical analysis according to GWR Group Limited (“GWR”) QAQC procedures.
Results from the QAQC were found to be acceptable. Nagrom Laboratories also carried out internal
QAQC as per their operating procedures
Measures taken to ensure that the sampling is representative of the in situ
material collected, including for instance results for field duplicate/second‐half
sampling.
Field duplicates of the drilling samples were routinely collected and these were all found to agree
within acceptable limits with the original samples.
Whether sample sizes are appropriate to the grain size of the material being
sampled.
The sample size is considered appropriate to the grain size of the material being sampled.
Criteria JORC Code explanation
Commentary
Quality of assay data and
laboratory tests
The nature, quality and appropriateness of the assaying and laboratory
procedures used and whether the technique is considered partial or total.
XRF has proven to be a very accurate analytical technique for a wide range of base metals, trace
elements and major constituents found in rocks and mineral materials. Glass fusion XRF is utilised
for assaying, since it provides good accuracy and precision; it is suitable for analysis from very low
levels up to very high levels.
ICP and Fire Assay techniques are also considered appropriate and industry standard for the
elements analysed using this technique and the detection limits as stated.
The assaying techniques used are total analyses.
For geophysical tools, spectrometers, handheld XRF instruments, etc, the
parameters used in determining the analysis including instrument make and
model, reading times, calibrations factors applied and their derivation, etc.
Since this equipment was not used, this section is not applicable.
Nature of quality control procedures adopted (e.g. standards, blanks,
duplicates, external laboratory checks) and whether acceptable levels of
accuracy (i.e. lack of bias) and precision have been established.
Certified Standards and duplicate samples were routinely inserted into the sample sequences
submitted for chemical analysis according to GWR Group Limited (“GWR”) QAQC procedures. Results
from the QAQC indicate that the assays met acceptable levels of accuracy without significant bias.
Nagrom Laboratories also carried out internal QAQC as per their operating procedures.
No blanks were used for QAQC checking. The risk of contamination during sample preparation was
considered minimal because of the mineralogy of the samples being tested.
At this early stage of the exploration program no external laboratory checks have been undertaken.
Verification of sampling and
assaying
The verification of significant intersections by either independent or alternative
company personnel.
Brian Varndell of Al Maynard and Associates, who are consultants to GWR, has checked and
verified the data pertaining to the significant intercepts against original field logs, laboratory
certificates and by checking cross sections.
The use of twinned holes.
At this early stage of the exploration program no twin holes have been drilled.
Documentation of primary data, data entry procedures, data verification, data
storage (physical and electronic) protocols.
All field data is recorded on log sheets as per GWR operating procedures. Drill data is entered into a
digital database and is also stored in hard copy in Perth office. The digital data was checked against
the field logs by the geologist after the data entry was completed and also checked visually on cross
sections.
Discuss any adjustment to assay data.
No adjustments to the assay data were made.
Location of data points Accuracy and quality of surveys used to locate drillholes (collar and down‐hole
surveys), trenches, mine workings and other locations used in Mineral Resource
estimation.
The RC drill hole collar northings and eastings were surveyed using a hand held GPS while the RLs
were determined from contours generated by high quality photogrammetry.
A down hole survey measurement was taken at the bottom of each hole.
Specification of the grid system used.
The grid system is MGA GDA94 Zone 53.
Criteria JORC Code explanation
Commentary
Quality and adequacy of topographic control.
High resolution aerial photogrammetry was collected using an unmanned aerial vehicle (UAV)
survey undertaken in August 2015 with an accuracy of +‐40mm in all 3 dimensions.
Data spacing and distribution Data spacing for reporting of Exploration Results.
The drilling is of a first pass nature to test the overall geology and indicative style and extent of the
mineralisation only.
Whether the data spacing and distribution is sufficient to establish the degree
of geological and grade continuity appropriate for the Mineral Resource and
Ore Reserve estimation procedure(s) and classifications applied.
No resource estimation was undertaken using the drilling data so this section is not applicable
Whether sample compositing has been applied.
Only 1m RC drill samples were collected and no sample compositing was undertaken.
Orientation of data in relation to
geological structure
Whether the orientation of sampling achieves unbiased sampling of possible
structures and the extent to which this is known, considering the deposit type.
The drilling was designed to intersect mineralisation approximately perpendicular to the
mineralisation and not biased towards any special grade areas. However since the orientation of
the mineralisation has not been determined accurately at this early stage, the intersection widths
may be appreciably longer than the true width of the mineralisation intersected and some
mineralised structures intersected at sub‐optimal angles.
If the relationship between the drilling orientation and the orientation of key
mineralised structures is considered to have introduced a sampling bias, this
should be assessed and reported if material.
Since the drilling to date has been exploratory and not at a sufficient density to properly determine
the orientation and grade of the mineralisation, it cannot be determined at this early stage if the
orientation of the drilling has introduced a sampling bias. But the knowledge of the mineralisation
gained so far from surface mapping and drilling indicates that the drilling has been properly
oriented to test the mineralisation without undue bias.
Sample security The measures taken to ensure sample security.
Samples were collected in calico sample bags, then placed in a polyweave bag and the bag sealed
with a cable tie. The individual bags were then placed in a Bulka Bag and this bag was sealed with
rope. The bulka bags were transported by trucking contractors to Nagrom Laboratories in Perth.
Audits or reviews The results of any audits or reviews of sampling techniques and data.
Since the exploration program is only at an early stage there have been no audits or reviews of the
sampling techniques. It is believed by GWR that the sampling procedures and techniques followed
meet current international standards of quality.
Independent geological consultants, Al Maynard & Associates, have audited all the drilling data
collected to date.

$

SECTION 2: REPORTING OF EXPLORATION RESULTS

Criteria JORC Code explanation
Commentary
Mineral tenement and land
tenure status
Type, reference name/number, location and ownership including agreements
or material issues with third parties such as joint ventures, partnerships,
overriding royalties, native title interests, historical sites, wilderness or national
park and environmental settings.
The Hatches Creek project is located in the Northern Territory of Australia upon EL22912 and
EL23463 covering a total area of approximately 31.8 km2
The registered holder of the tenements is NT Tungsten Pty Ltd, which is a 100% owned subsidiary of
GWR Group Limited.
The tenements are located upon Aboriginal Freehold Land, which is owned by the Anurrete
Aboriginal Trust and administered by the Central Land Council (CLC), with whom a Deed of
Exploration has been executed
NT Tungsten holds a 100% interest in the tenements and a 1.5% net smelter royalty is payable to
Davenport Resources Limited.
The security of the tenure held at the time of reporting along with any known
impediments to obtaining a licence to operate in the area.
The tenements are in good standing.
Exploration done by other
parties
Acknowledgment and appraisal of exploration by other parties.
Previous mining activities up to 1960 are well documented and are summarised in Bulletin No 6 “The
Geology and Mineral Resources of the Hatches Creek Wolfram Field, Northern Territory”, G. R Ryan
1961.
Between 2008 and 2015 the ground was held by numerous companies associated with Davenport
Resources Limited and Arunta Resources Limited. Their ~~a~~ctivities focused on sampling and mapping
of the historical mine workings.
Geology Deposit type, geological setting and style of mineralisation.
Tungsten mineralisation at Hatches Creek is associated with quartz veins in shear zones within a
variety of Proterozoic host rocks forming part of the Davenport Province. Wolframite and Scheelite
are the dominant tungsten minerals present
Drill hole Information A summary of all information material to the understanding of the exploration
results including a tabulation of the following information for all Material drill
holes:

easting and northing of the drill hole collar

elevation or RL (Reduced Level – elevation above sea level in
metres) of the drill hole collar

dip and azimuth of the hole

down hole length and interception depth

hole length.
All relevant data for GWR’s RC drilling is summarised in Tables 1 and 2 in the body of the report
and all assay data in Appendix 2
Criteria JORC Code explanation
Commentary
Data aggregation methods In reporting Exploration Results, weighting averaging techniques, maximum
and/or minimum grade truncations (e.g. cutting of high grades) and cut‐off
grades are usually Material and should be stated.
Significant Intercept
Significant WO3 intersections are reported for all intervals greater than 1m at 0.1% WO3 or greater
than 2m at 0.1% WO3and up to 2m of internal waste.
Significant Cu intersections are reported for all intervals greater than 1m at 0.5% Cu.
Significant Au intercepts are reported for all intervals greater than 1m at 0.5g/t Au.
All composited intercept assays were weighted by sample length. No upper cut‐off grades were
applied.
Mineralised Zone
At the Hit or Miss and Treasure prospects mineralised zones have been reported which encompass
the significant intercepts within defined structures that do contain multiple mineralised structures
and these with the internal waste intervals are shown on the accompanying Figures 8 and 10
Where aggregate intercepts incorporate short lengths of high grade results and
longer lengths of low grade results, the procedure used for such aggregation
should be stated and some typical examples of such aggregations should be
shown in detail.
All the drill samples are collected over consistent 1 m intervals and composited assays weighted by
sample lengths.
The assumptions used for any reporting of metal equivalent values should be
clearly stated.
Metal equivalent values have not been reported
Relationship between
mineralisation widths and
intercept lengths
These relationships are particularly important in the reporting of Exploration
Results.
If the geometry of the mineralisation with respect to the drill hole angle is
known, its nature should be reported.
If it is not known and only the down hole lengths are reported, there should be
a clear statement to this effect (e.g. ‘down hole length, true width not known’).
Based upon historical mine reports and surface observations; the geometry of the mineralisation is
reasonably well understood. In most cases the drilling is close to perpendicular to the strike and as
the mineralisation is steeply dipping, true widths of the mineralisation are considered to be greater
than 60% of the intercept width. Plans and cross sections are provided in the body of the report
that show the relationship between the drill holes and he mineralisation.
Diagrams Appropriate maps and sections (with scales) and tabulations of intercepts
should be included for any significant discovery being reported These should
include, but not be limited to a plan view of drill hole collar locations and
appropriate sectional views.
Refer to diagrams provided in the body of the report
Balanced reporting Where comprehensive reporting of all Exploration Results is not practicable,
representative reporting of both low and high grades and/or widths should be
practiced to avoid misleading reporting of Exploration Results.
All drilling results are provided in Appendix 2 of the report.
Criteria JORC Code explanation Commentary
Other substantive exploration The area was the subject of detailed study by the Bureau of Mineral Resources and this was
data Other exploration data, if meaningful and material, should be reported published in Bulletin No 6 (1961). The geology of all the areas drilled are described in detail in this
including (but not limited to): geological observations; geophysical survey report.
results; geochemical survey results; bulk samples – size and method of
treatment; metallurgical test results; bulk density, groundwater, geotechnical GWR has undertaken significant metallurgical test work on representative mineralised samples
and rock characteristics; potential deleterious or contaminating substances. with the results of these tests reported in previous ASX announcements.
Further work The nature and scale of planned further work (e.g. tests for lateral extensions
or depth extensions or large‐scale step‐out drilling). Further RC drilling and possibly diamond drilling is planned to follow up on the results described in
Diagrams clearly highlighting the areas of possible extensions, including the this report and also to evaluate the remaining prospect areas not tested in the current program.
main geological interpretations and future drilling areas, provided this
information is not commercially sensitive

APPENDIX 2 DRILL HOLE ASSAY RESULTS

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC001 0 1 0.035 **0.116 ** 0.078 0.003 0.014 0.004 <0.001 0.336
HCRC001 1 2 0.029 0.073 0.010 0.001 0.021 0.003 0.002 0.004
HCRC001 2 3 0.007 0.014 0.020 <0.001 <0.001 <0.001 <0.001 0.006
HCRC001 3 4 0.008 0.025 0.021 <0.001 0.008 <0.001 <0.001 0.002
HCRC001 4 5 0.002 0.003 0.004 <0.001 <0.001 <0.001 0.004 0.001
HCRC001 5 6 0.005 0.005 0.006 <0.001 0.002 <0.001 <0.001 0.002
HCRC001 6 7 0.019 0.024 0.047 <0.001 0.002 <0.001 <0.001 <0.001
HCRC001 7 8 0.004 0.004 0.025 <0.001 0.002 <0.001 0.007 0.002
HCRC001 8 9 **0.102 ** **0.056 ** 0.140 <0.001 0.020 0.003 <0.001 0.005
HCRC001 9 10 0.071 0.046 0.324 <0.001 0.003 <0.001 0.007 0.009
HCRC001 10 11 0.013 0.021 0.147 <0.001 0.002 0.002 0.008 0.002
HCRC001 11 12 0.013 0.004 0.043 <0.001 <0.001 0.007 0.007 0.004
HCRC001 12 13 0.411 0.013 0.075 <0.001 0.003 <0.001 0.004 0.002
HCRC001 13 14 0.019 0.016 0.098 <0.001 <0.001 <0.001 0.005 0.003
HCRC001 14 15 0.007 0.008 0.028 <0.001 0.007 0.008 <0.001 <0.001
HCRC001 15 16 0.006 0.010 0.030 <0.001 0.010 <0.001 <0.001 <0.001
HCRC001 16 17 0.004 0.006 0.035 <0.001 0.004 <0.001 0.002 0.003
HCRC001 17 18 0.004 0.005 0.020 <0.001 0.003 0.006 0.003 0.001
HCRC001 18 19 0.005 0.007 0.028 <0.001 <0.001 0.003 0.003 0.002
HCRC001 19 20 0.004 0.004 0.012 <0.001 <0.001 0.010 0.002 0.003
HCRC001 20 21 0.005 0.016 0.009 <0.001 0.015 <0.001 <0.001 0.002
HCRC001 21 22 0.008 0.015 0.028 <0.001 0.007 <0.001 0.003 0.002
HCRC001 22 23 0.052 0.011 0.022 <0.001 0.010 0.005 0.002 0.002
HCRC001 23 24 0.005 0.001 0.004 <0.001 0.003 0.004 0.004 0.002
HCRC001 24 25 0.030 0.015 0.048 <0.001 0.016 0.003 0.004 0.004
HCRC001 25 26 0.020 0.017 0.034 <0.001 0.022 0.003 0.005 0.002
HCRC001 26 27 0.047 **0.103 ** 0.250 <0.001 0.008 0.002 0.002 0.008
HCRC001 27 28 0.025 0.030 0.218 <0.001 0.004 0.005 0.004 0.004
HCRC001 28 29 0.006 0.012 0.016 <0.001 0.009 0.004 0.005 0.003
HCRC002 0 1 No sample
HCRC002 1 2 0.036 0.045 0.052 <0.001 0.022 <0.001 0.004 0.016
HCRC002 2 3 0.002 0.009 0.004 <0.001 <0.001 <0.001 0.002 0.006
HCRC002 3 4 <0.001 0.005 0.002 <0.001 <0.001 <0.001 <0.001 0.001
HCRC002 4 5 0.008 0.004 0.044 <0.001 0.010 <0.001 <0.001 0.003
HCRC002 5 6 0.003 0.002 0.069 <0.001 <0.001 <0.001 0.002 0.002
HCRC002 6 7 0.004 0.001 0.058 <0.001 0.002 0.004 0.002 0.015
HCRC002 7 8 0.002 <0.001 0.018 <0.001 0.003 <0.001 <0.001 0.006
HCRC002 8 9 0.003 <0.001 0.010 <0.001 0.003 <0.001 0.002 0.002
HCRC002 9 10 0.004 0.002 0.017 <0.001 0.005 0.002 <0.001 0.001
HCRC002 10 11 0.002 0.001 0.011 <0.001 <0.001 0.005 0.002 0.002
HCRC002 11 12 0.002 <0.001 0.007 <0.001 0.002 0.001 <0.001 <0.001
HCRC002 12 13 0.003 0.001 0.014 <0.001 0.002 0.001 0.002 0.001
HCRC002 13 14 0.021 0.005 0.034 <0.001 0.007 0.002 <0.001 <0.001
HCRC002 14 15 0.005 0.005 0.007 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC002 15 16 0.016 0.004 0.031 <0.001 <0.001 0.002 0.002 0.004
HCRC002 16 17 0.021 0.004 0.045 <0.001 <0.001 <0.001 0.006 0.003
HCRC002 17 18 0.006 0.002 0.024 <0.001 0.004 <0.001 0.005 <0.001
HCRC002 18 19 0.004 0.001 0.013 <0.001 <0.001 0.010 <0.001 0.002
HCRC002 19 20 0.009 0.001 0.029 <0.001 <0.001 <0.001 0.006 0.002
HCRC002 20 21 0.007 0.003 0.030 <0.001 <0.001 <0.001 0.008 0.003
HCRC002 21 22 0.010 0.010 0.091 <0.001 <0.001 0.002 0.013 0.003
HCRC002 22 23 0.026 0.013 0.090 <0.001 <0.001 0.006 0.005 0.015
HCRC002 23 24 0.008 0.038 0.037 <0.001 <0.001 <0.001 0.008 0.008

1

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC002 24 25 0.031 **0.073 ** 0.062 <0.001 0.003 <0.001 0.002 0.022
HCRC002 25 26 0.006 0.005 0.038 <0.001 <0.001 <0.001 0.002 0.003
HCRC002 26 27 No sample
HCRC002 27 28 **0.086 ** **0.080 ** 0.297 0.001 0.017 <0.001 0.005 0.016
HCRC002 28 29 0.031 0.026 0.152 <0.001 0.004 <0.001 0.004 0.121
HCRC002 29 30 0.074 0.028 0.123 0.003 0.006 <0.001 0.002 0.261
HCRC002 30 31 0.027 0.031 0.225 0.001 0.003 <0.001 0.002 0.143
HCRC002 31 32 0.010 0.016 0.146 <0.001 0.005 <0.001 0.003 0.250
HCRC002 32 33 0.005 <0.001 0.032 <0.001 0.002 <0.001 <0.001 0.158
HCRC002 33 34 0.006 0.004 0.043 <0.001 0.002 0.002 <0.001 0.078
HCRC002 34 35 0.006 0.006 0.049 0.005 0.002 0.004 0.002 0.579
HCRC002 35 36 0.013 0.006 0.028 0.004 0.004 0.001 0.005 0.481
HCRC002 36 37 0.012 0.009 0.069 0.011 0.006 0.004 0.003 1.407
HCRC002 37 38 0.004 0.003 0.032 0.003 0.002 <0.001 0.003 0.285
HCRC002 38 39 0.006 0.005 0.022 0.002 0.004 <0.001 0.004 0.273
HCRC002 39 40 0.014 0.004 0.025 0.001 0.002 <0.001 0.002 0.129
HCRC002 40 41 0.039 **0.063 ** 0.225 0.002 0.005 0.001 0.006 0.428
HCRC002 41 42 0.014 0.017 0.154 0.003 0.014 <0.001 <0.001 0.240
HCRC002 42 43 0.005 0.005 0.007 <0.001 <0.001 0.003 <0.001 0.011
HCRC002 43 44 0.003 <0.001 0.004 0.001 0.003 <0.001 0.002 0.005
HCRC002 44 45 0.454 0.013 0.005 0.012 0.009 <0.001 0.003 0.015
HCRC002 45 46 0.007 0.044 0.012 <0.001 0.007 0.004 <0.001 0.011
HCRC002 46 47 0.022 0.025 0.058 0.003 0.063 <0.001 <0.001 0.109
HCRC002 47 48 0.003 <0.001 0.009 <0.001 0.003 <0.001 0.002 0.009
HCRC002 48 49 0.004 <0.001 0.008 <0.001 0.002 <0.001 <0.001 0.002
HCRC002 49 50 0.003 0.013 0.014 <0.001 0.009 <0.001 0.002 0.061
HCRC002 50 51 0.008 0.013 0.043 0.004 0.010 0.002 <0.001 0.295
HCRC002 51 52 0.010 0.007 0.026 <0.001 0.005 <0.001 0.002 0.028
HCRC002 52 53 0.003 <0.001 0.002 <0.001 0.003 0.004 <0.001 0.006
HCRC002 53 54 0.003 0.040 0.145 0.001 0.020 0.001 0.002 0.258
HCRC002 54 55 0.004 0.020 0.045 0.001 0.009 <0.001 <0.001 0.207
HCRC002 55 56 0.002 0.020 0.043 0.003 0.011 0.003 0.002 0.184
HCRC002 56 57 0.001 0.004 0.002 <0.001 0.002 <0.001 0.002 0.030
HCRC002 57 58 0.002 0.007 0.034 <0.001 0.003 0.002 0.002 0.045
HCRC002 58 59 0.002 0.011 <0.001 <0.001 0.002 0.003 <0.001 0.005
HCRC002 59 60 0.007 **0.056 ** 0.080 0.007 0.055 0.003 <0.001 0.729
HCRC002 60 61 0.002 0.006 0.022 0.001 0.006 0.004 <0.001 0.064
HCRC002 61 62 0.092 0.020 0.010 0.008 0.043 <0.001 <0.001 0.053
HCRC002 62 63 0.002 0.002 0.002 <0.001 <0.001 <0.001 <0.001 0.051
HCRC002 63 64 0.003 0.006 <0.001 <0.001 0.006 <0.001 0.002 0.015
HCRC002 64 65 0.002 0.002 <0.001 <0.001 0.002 <0.001 0.002 0.007
HCRC002 65 66 0.001 0.001 <0.001 <0.001 0.002 <0.001 0.002 0.013
HCRC002 66 67 <0.001 <0.001 0.009 <0.001 <0.001 0.002 0.002 0.018
HCRC002 67 68 0.002 0.009 0.032 0.001 0.008 <0.001 <0.001 0.060
HCRC002 68 69 **0.727 ** **0.107 ** 0.100 0.004 0.076 0.003 0.002 0.223
HCRC002 69 70 0.014 0.087 0.043 0.003 0.050 <0.001 0.002 0.102
HCRC002 70 71 0.006 0.101 0.016 0.002 0.024 0.003 <0.001 0.200
HCRC002 71 72 0.004 0.012 0.005 0.001 0.007 <0.001 <0.001 0.079
HCRC002 72 73 0.003 0.018 0.009 0.001 0.004 0.006 <0.001 0.224
HCRC002 73 74 0.004 0.002 0.005 <0.001 0.003 <0.001 <0.001 0.145
HCRC002 74 75 0.002 0.002 0.008 <0.001 0.002 0.005 <0.001 0.126
HCRC002 75 76 0.014 0.005 0.020 0.002 0.002 <0.001 0.002 0.258
HCRC002 76 77 **0.158 ** **0.498 ** 0.258 0.009 0.149 0.004 0.002 0.559

2

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC002 77 78 0.062 0.031 0.010 <0.001 0.013 <0.001 <0.001 0.124
HCRC002 78 79 0.008 0.003 0.002 <0.001 0.003 <0.001 0.002 0.012
HCRC002 79 80 0.010 0.005 0.021 <0.001 0.003 <0.001 0.002 0.141
HCRC002 80 81 0.014 0.003 0.011 <0.001 0.004 0.003 <0.001 0.139
HCRC002 81 82 **1.313 ** 0.263 0.039 0.003 0.137 <0.001 0.002 0.192
HCRC002 82 83 0.242 0.021 0.039 0.003 0.021 <0.001 0.007 0.432
HCRC002 83 84 0.329 0.015 0.062 0.004 0.014 <0.001 0.002 0.287
HCRC002 84 85 0.026 0.012 0.040 0.005 0.015 <0.001 <0.001 0.202
HCRC002 85 86 0.026 0.031 0.064 0.004 0.010 <0.001 0.005 0.530
HCRC002 86 87 0.005 **0.057 ** 0.065 0.008 0.020 <0.001 <0.001 0.525
HCRC002 87 88 0.018 0.032 0.093 0.005 0.013 0.002 0.002 0.590
HCRC002 88 89 0.009 0.037 0.083 0.007 0.019 0.002 0.002 0.831
HCRC002 89 90 0.047 0.055 0.047 0.006 0.025 <0.001 0.002 0.539
HCRC002 90 91 0.019 0.010 0.020 0.003 0.009 <0.001 <0.001 0.246
HCRC002 91 92 0.003 0.010 0.037 0.004 0.004 <0.001 <0.001 0.529
HCRC002 92 93 0.002 0.011 0.046 0.009 <0.001 <0.001 0.004 1.393
HCRC002 93 94 0.004 0.012 0.066 0.012 0.003 <0.001 0.005 1.905
HCRC002 94 95 0.003 0.024 0.091 0.011 0.019 <0.001 0.003 1.204
HCRC002 95 96 0.246 0.022 0.039 0.011 0.023 <0.001 0.004 0.749
HCRC003 0 1 No sample
HCRC003 1 2 0.036 0.100 0.026 0.001 0.015 0.007 0.002 0.053
HCRC003 2 3 0.002 0.006 0.010 <0.001 <0.001 <0.001 <0.001 0.010
HCRC003 3 4 0.003 0.003 0.008 <0.001 <0.001 0.003 0.002 0.005
HCRC003 4 5 0.006 0.014 0.086 <0.001 0.004 <0.001 0.002 0.004
HCRC003 5 6 <0.001 0.002 0.011 <0.001 <0.001 0.004 <0.001 0.002
HCRC003 6 7 0.005 0.010 0.026 <0.001 <0.001 <0.001 0.002 0.005
HCRC003 7 8 0.003 0.004 0.015 <0.001 <0.001 0.004 0.002 0.002
HCRC003 8 9 0.005 0.002 0.019 <0.001 0.001 0.007 <0.001 0.003
HCRC003 9 10 0.001 0.003 0.016 <0.001 <0.001 <0.001 <0.001 0.003
HCRC003 10 11 0.003 0.001 0.016 <0.001 0.005 0.001 <0.001 0.003
HCRC003 11 12 0.008 0.013 0.097 <0.001 0.003 0.010 <0.001 0.003
HCRC003 12 13 0.006 0.003 0.019 <0.001 0.001 <0.001 <0.001 0.007
HCRC003 13 14 0.003 0.006 0.022 <0.001 0.002 0.003 0.002 0.003
HCRC003 14 15 0.005 0.004 0.022 <0.001 0.002 <0.001 0.002 0.002
HCRC003 15 16 0.011 0.006 0.019 <0.001 0.003 0.004 0.002 0.002
HCRC003 16 17 0.016 0.023 0.025 <0.001 0.004 <0.001 0.003 0.003
HCRC003 17 18 0.017 0.009 0.050 <0.001 0.004 <0.001 0.006 0.006
HCRC003 18 19 0.008 0.006 0.026 <0.001 0.002 0.006 0.003 0.005
HCRC003 19 20 0.006 0.006 0.026 <0.001 0.003 <0.001 0.004 0.002
HCRC003 20 21 0.012 0.007 0.051 <0.001 0.006 0.008 <0.001 0.002
HCRC003 21 22 0.004 0.005 0.039 <0.001 0.016 0.006 <0.001 0.007
HCRC003 22 23 0.004 0.009 0.016 <0.001 0.001 <0.001 <0.001 0.002
HCRC003 23 24 0.013 0.006 0.118 <0.001 0.016 <0.001 <0.001 0.008
HCRC003 24 25 0.004 0.001 0.036 <0.001 0.002 <0.001 0.002 0.003
HCRC003 25 26 0.010 0.010 0.115 <0.001 0.012 0.004 <0.001 0.004
HCRC003 26 27 0.007 0.033 0.096 <0.001 0.017 0.002 <0.001 0.003
HCRC003 27 28 0.007 0.007 0.065 <0.001 0.005 <0.001 <0.001 0.003
HCRC003 28 29 0.017 0.027 0.085 <0.001 0.005 <0.001 <0.001 0.009
HCRC003 29 30 0.002 <0.001 0.009 0.001 0.002 <0.001 <0.001 0.111
HCRC003 30 31 0.002 0.001 0.004 <0.001 0.002 0.006 <0.001 0.098
HCRC003 31 32 0.002 0.017 0.005 <0.001 0.002 <0.001 <0.001 0.067
HCRC003 32 33 0.004 0.001 0.011 0.001 0.002 <0.001 0.002 0.212
HCRC003 33 34 0.003 0.002 0.016 <0.001 0.006 0.005 <0.001 0.190

3

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC003 34 35 0.003 0.003 0.036 0.001 0.002 <0.001 0.005 0.376
HCRC003 35 36 0.007 0.015 0.071 0.003 0.004 0.004 0.005 0.651
HCRC003 36 37 0.005 0.016 0.106 0.003 0.002 <0.001 0.002 0.435
HCRC003 37 38 0.008 0.006 0.052 0.005 0.003 0.006 0.006 0.650
HCRC003 38 39 **0.112 ** **0.051 ** 0.205 0.041 0.023 0.009 0.006 6.403
HCRC003 39 40 0.008 0.003 0.021 0.002 0.004 <0.001 0.003 0.266
HCRC003 40 41 0.004 0.001 0.020 <0.001 0.003 <0.001 <0.001 0.190
HCRC003 41 42 0.020 0.031 0.063 0.002 0.004 0.004 0.002 0.559
HCRC003 42 43 0.003 0.002 0.009 0.001 0.002 0.007 <0.001 0.195
HCRC003 43 44 0.002 0.057 0.010 <0.001 0.003 <0.001 <0.001 0.163
HCRC003 44 45 0.006 0.005 0.033 0.003 0.006 0.001 <0.001 0.603
HCRC003 45 46 0.004 0.013 0.097 0.011 0.006 <0.001 0.002 1.420
HCRC003 46 47 0.002 0.005 0.010 0.002 0.001 0.003 <0.001 0.395
HCRC003 47 48 0.001 0.003 0.006 0.002 0.001 <0.001 <0.001 0.276
HCRC003 48 49 0.002 0.004 0.011 0.001 0.005 0.005 <0.001 0.232
HCRC003 49 50 0.003 0.002 0.019 0.001 0.003 0.003 <0.001 0.525
HCRC003 50 51 0.003 0.005 0.018 0.001 0.002 <0.001 <0.001 0.246
HCRC003 51 52 0.008 0.027 0.049 0.002 0.005 <0.001 0.003 0.422
HCRC003 52 53 0.090 0.022 0.104 0.005 0.004 0.004 0.002 0.722
HCRC003 53 54 0.018 **0.151 ** 0.269 0.006 0.002 <0.001 0.006 1.045
HCRC003 54 55 **0.295 ** **0.420 ** 0.426 0.010 0.048 <0.001 0.005 0.884
HCRC003 55 56 **0.090 ** **0.165 ** 0.489 0.015 0.031 0.004 0.002 2.314
HCRC003 56 57 **0.055 ** **0.062 ** 0.351 0.018 0.019 <0.001 0.006 2.557
HCRC003 57 58 0.067 0.037 0.134 0.003 0.007 <0.001 0.004 0.608
HCRC003 58 59 0.029 **0.066 ** 0.240 0.003 0.009 0.002 0.002 0.592
HCRC003 59 60 0.017 0.026 0.125 0.003 0.007 <0.001 <0.001 0.447
HCRC003 60 61 0.009 0.049 0.212 0.005 0.004 <0.001 <0.001 0.775
HCRC003 61 62 0.006 **0.051 ** 0.064 0.002 0.004 0.005 0.002 0.621
HCRC003 62 63 0.023 0.008 0.057 0.006 0.004 <0.001 0.005 1.235
HCRC003 63 64 0.010 0.025 0.081 0.007 0.004 0.003 0.004 1.224
HCRC003 64 65 0.016 0.022 0.124 0.008 0.003 <0.001 0.005 1.475
HCRC003 65 66 0.008 0.013 0.093 0.004 0.003 <0.001 0.009 0.854
HCRC003 66 67 0.062 0.031 0.161 0.007 0.008 <0.001 <0.001 1.062
HCRC003 67 68 0.014 0.017 0.085 0.003 0.006 0.003 <0.001 0.678
HCRC003 68 69 0.006 0.004 0.036 0.003 0.004 <0.001 0.003 0.356
HCRC003 69 70 0.004 0.005 0.023 0.002 0.004 0.004 <0.001 0.429
HCRC003 70 71 0.005 0.008 0.026 0.003 0.004 0.008 <0.001 0.469
HCRC003 71 72 0.008 0.005 0.024 0.001 0.002 0.008 <0.001 0.227
HCRC003 72 73 0.006 0.024 0.042 0.003 0.026 0.004 <0.001 0.314
HCRC003 73 74 0.063 0.026 0.058 <0.001 0.024 0.003 <0.001 0.373
HCRC003 74 75 0.025 0.020 0.029 0.001 0.010 <0.001 0.002 0.154
HCRC003 75 76 0.006 0.008 0.044 <0.001 0.004 0.004 <0.001 0.219
HCRC003 76 77 0.006 0.006 0.027 <0.001 0.004 0.002 <0.001 0.159
HCRC003 77 78 0.013 0.009 0.098 0.002 0.005 <0.001 0.002 0.222
HCRC003 78 79 0.058 0.022 0.108 <0.001 0.009 <0.001 0.006 0.309
HCRC003 79 80 0.056 0.026 0.212 0.014 0.002 0.001 0.006 2.189
HCRC003 80 81 0.014 0.026 0.183 0.009 0.006 <0.001 0.005 0.567
HCRC003 81 82 0.012 0.011 0.052 0.003 0.001 0.003 0.006 0.395
HCRC003 82 83 0.009 0.006 0.050 0.009 0.002 <0.001 0.002 1.238
HCRC003 83 84 0.012 0.010 0.031 0.003 0.002 <0.001 0.011 0.363
HCRC003 84 85 0.047 **0.081 ** 0.151 0.002 0.013 0.004 0.002 0.464
HCRC003 85 86 0.009 **0.094 ** 0.054 0.005 0.003 <0.001 0.010 0.478
HCRC003 86 87 0.012 0.006 0.035 0.002 0.003 <0.001 0.006 0.199

4

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC003 87 88 0.012 0.012 0.077 0.002 0.004 <0.001 0.002 0.323
HCRC003 88 89 0.019 0.022 0.029 <0.001 0.015 0.006 0.002 0.151
HCRC003 89 90 0.019 **0.074 ** 0.173 0.009 0.035 0.006 <0.001 1.020
HCRC003 90 91 0.017 0.034 0.076 0.002 0.011 0.005 <0.001 0.232
HCRC003 91 92 0.003 0.035 0.027 <0.001 0.004 <0.001 0.002 0.078
HCRC003 92 93 **0.678 ** **0.081 ** 0.742 0.011 0.018 0.006 <0.001 1.163
HCRC003 93 94 0.010 0.005 0.012 <0.001 <0.001 <0.001 0.002 0.047
HCRC003 94 95 0.004 0.019 0.009 0.005 0.020 0.004 <0.001 0.346
HCRC003 95 96 0.003 0.005 0.003 <0.001 0.003 0.002 <0.001 0.043
HCRC003 96 97 0.003 **0.061 ** 0.057 0.002 0.020 <0.001 <0.001 0.199
HCRC003 97 98 0.003 2.258 0.008 0.003 0.178 <0.001 <0.001 0.069
HCRC003 98 99 0.002 0.024 0.006 <0.001 0.003 <0.001 <0.001 0.028
HCRC003 99 100 0.001 0.005 0.001 <0.001 0.001 <0.001 <0.001 0.009
HCRC003 100 101 0.001 0.005 0.002 <0.001 <0.001 0.005 <0.001 0.019
HCRC003 101 102 0.001 0.001 0.001 <0.001 <0.001 0.001 0.002 0.019
HCRC003 102 103 0.037 0.038 0.030 0.004 0.009 0.001 <0.001 0.151
HCRC003 103 104 0.004 0.015 0.026 <0.001 0.007 0.008 0.002 0.100
HCRC003 104 105 0.003 0.535 0.030 0.004 0.082 <0.001 <0.001 0.152
HCRC003 105 106 0.005 0.027 0.040 0.004 0.010 <0.001 <0.001 0.552
HCRC003 106 107 0.078 0.004 0.021 <0.001 0.003 0.006 0.006 0.104
HCRC003 107 108 0.185 0.021 0.077 0.001 0.016 <0.001 0.004 0.217
HCRC003 108 109 0.013 0.043 0.068 <0.001 0.021 0.002 0.003 0.480
HCRC003 109 110 0.005 0.006 0.034 <0.001 0.007 0.004 0.005 0.424
HCRC003 110 111 0.031 0.004 0.019 <0.001 0.007 <0.001 <0.001 0.257
HCRC003 111 112 0.025 **0.080 ** 0.065 <0.001 0.007 <0.001 <0.001 0.357
HCRC003 112 113 **0.053 ** **0.107 ** 0.196 <0.001 0.101 <0.001 0.003 0.426
HCRC003 113 114 0.006 0.007 0.029 <0.001 0.005 0.009 0.004 0.298
HCRC003 114 115 0.013 0.020 0.016 <0.001 0.014 0.003 <0.001 0.229
HCRC003 115 116 0.002 0.005 0.009 <0.001 0.001 0.009 <0.001 0.143
HCRC003 116 117 0.004 0.004 0.029 <0.001 0.002 <0.001 0.002 0.446
HCRC003 117 118 0.006 0.004 0.014 0.001 0.003 0.010 <0.001 0.253
HCRC003 118 119 0.159 0.011 0.014 0.003 0.007 <0.001 <0.001 0.149
HCRC003 119 120 0.037 **0.122 ** 0.897 <0.001 0.031 0.002 0.002 1.373
HCRC003 120 121 0.014 0.009 0.031 <0.001 0.004 0.004 <0.001 0.210
HCRC003 121 122 **1.197 ** **0.814 ** 0.932 <0.001 0.191 0.003 <0.001 2.077
HCRC003 122 123 0.052 0.044 0.048 <0.001 0.030 0.007 <0.001 0.215
HCRC003 123 124 0.010 0.007 0.019 0.002 0.004 0.008 <0.001 0.443
HCRC003 124 125 0.008 0.008 0.019 0.003 0.005 0.002 0.002 0.597
HCRC003 125 126 0.028 0.012 0.042 <0.001 0.007 0.001 0.004 1.147
HCRC003 126 127 0.017 0.012 0.043 <0.001 0.002 <0.001 0.005 0.668
HCRC003 127 128 0.003 0.007 0.042 <0.001 0.002 0.002 <0.001 0.986
HCRC003 128 129 0.110 0.033 0.252 <0.001 0.019 <0.001 <0.001 1.193
HCRC003 129 130 0.040 0.015 0.162 <0.001 0.088 0.006 <0.001 0.802
HCRC004 0 1 **0.139 ** **0.104 ** 0.056 0.002 0.021 <0.001 0.003 0.064
HCRC004 1 2 0.010 0.019 0.124 <0.001 0.003 <0.001 <0.001 0.023
HCRC004 2 3 **0.152 ** **0.276 ** 0.324 0.002 0.055 <0.001 0.003 0.044
HCRC004 3 4 **0.136 ** **1.333 ** 0.291 0.002 0.082 0.003 0.006 0.039
HCRC004 4 5 0.005 **0.062 ** 0.130 <0.001 0.003 0.003 0.002 0.018
HCRC004 5 6 0.007 0.037 0.017 <0.001 0.010 0.009 <0.001 0.007
HCRC004 6 7 0.019 **0.058 ** 0.055 <0.001 0.014 <0.001 <0.001 0.017
HCRC004 7 8 0.005 0.010 0.024 <0.001 0.003 0.003 0.002 0.008
HCRC004 8 9 0.006 0.038 0.058 <0.001 0.002 0.002 <0.001 0.004
HCRC004 9 10 0.006 0.005 0.009 <0.001 0.004 0.002 0.002 0.029

5

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC004 10 11 0.002 0.003 0.006 <0.001 0.001 0.001 <0.001 0.005
HCRC004 11 12 <0.001 0.003 0.003 <0.001 <0.001 0.005 <0.001 0.003
HCRC004 12 13 0.002 0.002 <0.001 <0.001 <0.001 0.003 <0.001 0.005
HCRC004 13 14 0.002 0.003 0.121 <0.001 0.001 <0.001 0.002 0.003
HCRC004 14 15 0.002 0.036 0.351 0.001 0.019 0.003 0.002 0.004
HCRC004 15 16 0.003 0.003 0.018 <0.001 0.007 0.002 <0.001 0.003
HCRC004 16 17 0.002 0.007 0.006 <0.001 <0.001 <0.001 0.003 0.002
HCRC004 17 18 0.003 0.016 0.023 <0.001 0.003 0.007 0.002 0.007
HCRC004 18 19 0.003 0.005 0.062 <0.001 0.002 0.005 0.002 0.002
HCRC004 19 20 0.017 0.005 0.098 <0.001 0.002 0.007 <0.001 0.036
HCRC004 20 21 0.005 0.030 0.084 <0.001 0.011 <0.001 <0.001 0.075
HCRC004 21 22 0.004 0.001 0.017 <0.001 0.002 0.006 <0.001 0.007
HCRC004 22 23 0.004 <0.001 0.008 <0.001 0.002 <0.001 <0.001 0.002
HCRC004 23 24 0.003 0.008 0.011 <0.001 0.003 0.006 <0.001 0.003
HCRC004 24 25 0.001 0.009 0.027 <0.001 <0.001 <0.001 <0.001 0.002
HCRC004 25 26 0.002 0.025 0.045 0.003 0.003 0.003 0.002 0.046
HCRC004 26 27 0.005 0.030 0.024 0.001 0.002 <0.001 0.002 0.015
HCRC004 27 28 0.007 0.010 0.057 <0.001 0.002 <0.001 0.003 0.006
HCRC004 28 29 0.003 0.175 0.017 <0.001 0.070 <0.001 <0.001 0.011
HCRC004 29 30 0.003 0.009 0.026 <0.001 0.005 <0.001 0.002 0.036
HCRC004 30 31 0.060 0.024 0.298 <0.001 0.005 0.003 0.005 0.014
HCRC004 31 32 0.093 0.022 0.106 <0.001 0.003 0.008 0.004 0.350
HCRC004 32 33 0.008 0.004 0.027 <0.001 0.002 <0.001 0.003 0.062
HCRC004 33 34 0.005 0.004 0.013 <0.001 0.002 <0.001 <0.001 0.059
HCRC004 34 35 0.017 0.001 0.010 <0.001 0.003 <0.001 0.005 0.026
HCRC004 35 36 **0.313 ** 0.070 0.030 0.041 0.108 0.003 0.003 0.310
HCRC004 36 37 0.016 0.002 0.005 <0.001 0.008 0.004 0.002 0.019
HCRC004 37 38 0.004 0.004 0.004 <0.001 0.002 0.003 <0.001 0.011
HCRC004 38 39 0.010 0.011 0.011 0.004 0.005 0.003 0.003 0.077
HCRC004 39 40 0.006 0.047 0.004 0.023 0.008 0.006 0.003 0.038
HCRC004 40 41 0.005 <0.001 <0.001 <0.001 0.004 0.002 <0.001 0.009
HCRC004 41 42 0.003 0.002 0.014 <0.001 <0.001 0.006 0.004 0.028
HCRC004 42 43 0.006 0.004 0.010 <0.001 0.002 0.004 0.002 0.029
HCRC004 43 44 **0.341 ** **0.155 ** 0.436 <0.001 0.033 0.002 0.003 3.609
HCRC004 44 45 **2.854 ** **1.758 ** 0.285 0.004 0.270 <0.001 0.004 0.842
HCRC004 45 46 0.068 0.026 0.016 <0.001 0.007 <0.001 <0.001 0.203
HCRC004 46 47 0.049 0.034 0.073 <0.001 0.009 0.003 <0.001 0.432
HCRC004 47 48 0.021 0.015 0.012 <0.001 0.004 0.003 <0.001 0.208
HCRC004 48 49 **0.437 ** 0.188 0.018 <0.001 0.034 <0.001 0.002 0.283
HCRC004 49 50 0.018 0.016 0.013 <0.001 0.007 0.005 0.002 0.222
HCRC004 50 51 0.008 0.016 0.014 <0.001 0.004 <0.001 <0.001 0.272
HCRC004 51 52 0.006 0.005 0.014 <0.001 0.003 <0.001 0.002 0.391
HCRC004 52 53 0.355 0.019 0.027 <0.001 0.005 <0.001 <0.001 0.556
HCRC004 53 54 **0.418 ** 1.962 0.039 <0.001 0.243 <0.001 0.003 0.920
HCRC004 54 55 0.016 0.041 0.016 <0.001 0.008 <0.001 <0.001 0.425
HCRC004 55 56 0.007 0.020 0.049 <0.001 0.005 <0.001 0.006 0.654
HCRC004 56 57 0.012 0.013 0.030 <0.001 0.004 <0.001 0.003 0.875
HCRC004 57 58 0.013 0.034 0.013 <0.001 0.001 <0.001 <0.001 0.442
HCRC004 58 59 0.006 0.016 0.048 <0.001 0.003 <0.001 <0.001 1.223
HCRC004 59 60 0.008 0.076 0.041 <0.001 0.027 0.002 <0.001 0.723
HCRC004 60 61 0.011 0.004 0.030 <0.001 0.003 0.006 <0.001 0.341
HCRC004 61 62 0.007 0.003 0.009 <0.001 0.001 0.003 <0.001 0.066
HCRC004 62 63 0.009 0.004 0.004 <0.001 0.005 <0.001 0.002 0.025

6

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC004 63 64 0.008 0.091 <0.001 <0.001 0.006 0.002 0.002 0.008
HCRC004 64 65 0.006 0.006 <0.001 <0.001 0.002 0.001 0.002 0.005
HCRC004 65 66 0.006 0.002 0.002 <0.001 0.002 0.005 0.002 0.005
HCRC004 66 67 0.033 0.054 0.001 0.002 0.004 0.004 0.002 0.013
HCRC004 67 68 0.026 0.011 0.007 <0.001 0.007 0.006 0.003 0.020
HCRC004 68 69 0.013 0.034 0.007 <0.001 0.015 0.004 <0.001 0.029
HCRC004 69 70 0.004 0.004 0.011 <0.001 0.002 <0.001 <0.001 0.046
HCRC004 70 71 **0.234 ** **0.057 ** 0.276 0.004 0.031 0.004 0.002 1.045
HCRC004 71 72 0.030 0.013 0.047 <0.001 0.006 <0.001 0.005 0.152
HCRC004 72 73 0.145 0.017 0.038 <0.001 0.005 <0.001 <0.001 0.393
HCRC004 73 74 0.167 0.007 0.031 0.005 0.003 <0.001 <0.001 0.343
HCRC004 74 75 0.046 0.039 0.045 <0.001 0.040 0.007 0.002 0.340
HCRC004 75 76 0.005 0.024 0.023 <0.001 0.003 <0.001 <0.001 0.347
HCRC004 76 77 0.016 0.004 0.028 <0.001 0.003 <0.001 <0.001 0.343
HCRC004 77 78 0.005 0.007 0.039 0.014 0.013 <0.001 0.002 0.678
HCRC004 78 79 0.031 0.011 0.099 <0.001 0.004 0.006 0.006 1.203
HCRC004 79 80 0.005 0.008 0.030 <0.001 0.002 <0.001 0.002 0.530
HCRC004 80 81 **1.956 ** **1.579 ** 0.278 0.011 0.297 <0.001 <0.001 0.442
HCRC004 81 82 0.004 0.009 0.026 <0.001 0.003 <0.001 <0.001 0.242
HCRC004 82 83 0.051 0.026 0.058 0.009 0.016 <0.001 0.003 0.465
HCRC004 83 84 0.009 0.007 0.026 <0.001 0.003 <0.001 <0.001 0.339
HCRC004 84 85 0.004 0.002 0.015 <0.001 0.003 <0.001 <0.001 0.180
HCRC004 85 86 0.006 0.029 0.153 <0.001 0.035 0.004 <0.001 0.689
HCRC004 86 87 0.005 0.332 0.027 <0.001 0.142 0.004 <0.001 0.449
HCRC004 87 88 0.003 0.006 0.008 <0.001 0.005 <0.001 <0.001 0.159
HCRC004 88 89 0.005 0.006 0.008 <0.001 0.002 0.002 0.002 0.100
HCRC004 89 90 0.002 0.001 0.010 <0.001 0.003 0.003 0.002 0.104
HCRC004 90 91 0.009 0.006 0.021 <0.001 0.010 0.002 0.002 0.770
HCRC004 91 92 0.018 0.040 0.066 <0.001 0.092 0.003 <0.001 0.447
HCRC004 92 93 0.007 <0.001 0.011 <0.001 0.004 0.003 <0.001 0.074
HCRC004 93 94 0.119 0.005 0.010 <0.001 0.004 <0.001 0.005 0.098
HCRC004 94 95 0.005 <0.001 0.011 0.001 0.003 <0.001 <0.001 0.242
HCRC004 95 96 0.119 0.012 0.033 <0.001 0.021 <0.001 0.003 0.238
HCRC004 96 97 0.024 0.003 0.011 <0.001 0.010 0.001 <0.001 0.079
HCRC004 97 98 0.007 0.001 0.017 <0.001 0.003 <0.001 <0.001 0.326
HCRC004 98 99 0.005 0.004 0.009 <0.001 0.004 0.007 0.002 0.176
HCRC004 99 100 0.006 0.003 0.012 <0.001 0.002 0.001 0.003 0.157
HCRC005 0 1 **0.078 ** 0.123 0.030 0.001 0.030 <0.001 0.002 0.130
HCRC005 1 2 **0.084 ** 0.066 0.026 <0.001 0.015 <0.001 <0.001 0.029
HCRC005 2 3 0.007 0.012 0.010 <0.001 0.003 <0.001 <0.001 0.007
HCRC005 3 4 0.013 0.028 0.097 <0.001 0.006 0.004 0.002 0.008
HCRC005 4 5 **0.739 ** **0.601 ** 0.095 0.003 0.188 0.010 0.002 0.005
HCRC005 5 6 0.008 0.009 0.016 <0.001 0.001 <0.001 <0.001 0.002
HCRC005 6 7 0.037 0.033 0.130 <0.001 0.002 0.002 0.002 0.002
HCRC005 7 8 0.028 0.017 0.063 <0.001 <0.001 <0.001 0.004 0.003
HCRC005 8 9 0.005 0.005 0.005 <0.001 <0.001 0.002 0.002 <0.001
HCRC005 9 10 0.011 0.004 0.010 <0.001 0.001 0.007 0.003 <0.001
HCRC005 10 11 0.014 0.014 0.037 <0.001 0.002 0.002 0.002 0.003
HCRC005 11 12 0.013 0.009 0.049 <0.001 0.016 <0.001 <0.001 0.004
HCRC005 12 13 **0.199 ** 0.840 0.027 <0.001 0.121 0.003 <0.001 0.003
HCRC005 13 14 0.027 0.078 0.012 <0.001 0.010 0.009 <0.001 0.002
HCRC005 14 15 0.009 0.014 0.013 <0.001 0.004 0.004 <0.001 0.002
HCRC005 15 16 0.007 0.010 0.007 <0.001 0.003 0.005 0.002 0.003

7

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC005 16 17 0.017 0.004 0.010 <0.001 0.001 <0.001 0.002 0.002
HCRC005 17 18 0.011 0.019 0.009 0.002 0.004 <0.001 0.002 0.005
HCRC005 18 19 0.007 0.004 0.012 <0.001 0.001 <0.001 <0.001 0.001
HCRC005 19 20 0.018 0.010 0.044 <0.001 0.011 0.005 <0.001 0.005
HCRC005 20 21 0.006 0.003 0.010 <0.001 0.002 <0.001 0.005 0.002
HCRC005 21 22 0.005 0.009 0.010 <0.001 0.001 <0.001 0.005 0.002
HCRC005 22 23 0.029 0.022 0.018 <0.001 0.006 <0.001 0.002 0.005
HCRC005 23 24 0.024 0.007 0.087 <0.001 0.008 <0.001 <0.001 0.040
HCRC005 24 25 0.035 **0.114 ** 0.372 0.001 0.042 0.006 0.003 0.022
HCRC005 25 26 0.017 0.008 0.079 <0.001 0.002 0.004 <0.001 0.025
HCRC005 26 27 0.006 0.003 0.012 <0.001 0.003 0.002 0.002 0.003
HCRC005 27 28 0.006 0.003 0.010 <0.001 0.002 <0.001 <0.001 0.002
HCRC005 28 29 0.015 0.003 0.010 <0.001 0.002 0.004 <0.001 0.003
HCRC005 29 30 0.011 0.008 0.032 <0.001 0.007 0.008 <0.001 0.006
HCRC005 30 31 0.007 0.003 0.009 <0.001 0.003 0.002 0.002 0.005
HCRC005 31 32 0.006 0.006 0.009 <0.001 0.003 <0.001 0.002 0.004
HCRC005 32 33 0.009 0.071 0.020 <0.001 0.091 0.002 0.002 0.005
HCRC005 33 34 0.005 0.006 0.013 <0.001 0.004 <0.001 <0.001 0.065
HCRC005 34 35 0.015 0.038 0.032 0.001 0.002 0.003 0.005 0.215
HCRC005 35 36 0.005 0.014 0.016 <0.001 0.002 <0.001 0.002 0.161
HCRC005 36 37 0.005 0.055 0.009 0.003 0.004 0.006 <0.001 0.218
HCRC005 37 38 0.145 0.048 0.046 0.003 0.042 <0.001 0.002 0.379
HCRC005 38 39 0.008 0.016 0.046 0.002 0.004 <0.001 <0.001 0.271
HCRC005 39 40 0.015 0.030 0.150 0.014 0.073 0.002 0.005 1.335
HCRC005 40 41 0.011 0.015 0.024 0.001 0.023 <0.001 0.002 0.284
HCRC005 41 42 0.004 0.001 0.016 <0.001 0.007 <0.001 0.003 0.194
HCRC005 42 43 0.006 **0.353 ** 0.055 0.008 0.139 <0.001 0.002 0.563
HCRC005 43 44 0.012 0.012 0.020 <0.001 0.005 <0.001 <0.001 0.240
HCRC005 44 45 0.010 0.012 0.038 0.003 0.013 0.003 <0.001 0.417
HCRC005 45 46 0.005 0.009 0.113 0.004 0.011 0.006 0.002 0.725
HCRC005 46 47 0.003 0.006 0.031 0.002 0.031 <0.001 <0.001 0.414
HCRC005 47 48 0.040 0.033 0.134 0.004 0.013 0.005 0.003 0.400
HCRC005 48 49 0.060 0.040 0.036 0.002 0.028 <0.001 <0.001 0.255
HCRC005 49 50 0.013 0.037 0.186 0.003 0.059 <0.001 0.002 0.467
HCRC005 50 51 0.008 0.007 0.046 <0.001 0.009 <0.001 0.002 0.207
HCRC005 51 52 0.030 0.005 0.025 <0.001 0.003 <0.001 0.002 0.189
HCRC005 52 53 0.045 0.012 0.349 0.007 0.012 <0.001 <0.001 1.006
HCRC005 53 54 0.022 0.006 0.043 <0.001 0.001 0.007 0.002 0.336
HCRC005 54 55 0.003 0.190 0.023 <0.001 0.004 0.004 0.002 0.350
HCRC005 55 56 0.002 0.005 0.010 <0.001 0.001 0.002 <0.001 0.037
HCRC005 56 57 0.065 0.011 0.028 0.003 0.011 <0.001 0.003 0.118
HCRC005 57 58 0.004 0.006 0.030 <0.001 0.003 <0.001 <0.001 0.142
HCRC005 58 59 0.008 0.001 0.008 0.001 0.002 <0.001 <0.001 0.177
HCRC005 59 60 0.003 0.003 0.016 <0.001 0.004 <0.001 <0.001 0.083
HCRC005 60 61 0.013 0.001 0.021 0.001 0.002 <0.001 0.002 0.236
HCRC005 61 62 0.004 0.040 0.027 <0.001 0.007 <0.001 <0.001 0.147
HCRC005 62 63 0.005 **0.560 ** 0.158 <0.001 0.019 <0.001 <0.001 0.237
HCRC005 63 64 0.025 0.010 0.034 <0.001 0.002 <0.001 <0.001 0.158
HCRC005 64 65 0.005 0.016 0.022 <0.001 0.002 <0.001 <0.001 0.051
HCRC005 65 66 0.002 0.001 0.009 <0.001 0.002 <0.001 <0.001 0.034
HCRC005 66 67 0.004 <0.001 0.008 <0.001 0.002 <0.001 0.003 0.048
HCRC005 67 68 0.014 0.005 0.018 0.002 0.004 <0.001 0.002 0.327
HCRC005 68 69 0.002 0.003 0.015 <0.001 0.001 0.001 0.002 0.062

8

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC005 69 70 0.001 <0.001 0.010 <0.001 0.001 0.004 0.002 0.114
HCRC005 70 71 0.011 <0.001 0.008 <0.001 0.002 <0.001 <0.001 0.111
HCRC005 71 72 0.013 0.009 0.044 0.001 0.002 <0.001 0.006 0.446
HCRC005 72 73 0.003 0.007 0.008 <0.001 0.003 0.003 <0.001 0.120
HCRC005 73 74 0.001 0.002 0.009 <0.001 0.001 <0.001 <0.001 0.158
HCRC005 74 75 0.003 <0.001 0.014 <0.001 0.001 <0.001 0.002 0.132
HCRC005 75 76 0.006 <0.001 0.014 <0.001 0.002 <0.001 <0.001 0.162
HCRC005 76 77 0.003 0.001 0.010 <0.001 0.002 <0.001 <0.001 0.152
HCRC005 77 78 0.008 0.004 0.012 <0.001 0.002 <0.001 <0.001 0.127
HCRC005 78 79 0.004 0.001 0.012 <0.001 0.001 <0.001 <0.001 0.082
HCRC005 79 80 0.003 <0.001 0.010 <0.001 0.002 <0.001 <0.001 0.076
HCRC005 80 81 0.004 0.001 0.028 <0.001 0.003 <0.001 0.002 0.063
HCRC005 81 82 0.008 0.004 0.058 <0.001 <0.001 <0.001 0.010 0.156
HCRC005 82 83 0.014 0.008 0.032 <0.001 0.002 0.002 0.013 0.117
HCRC005 83 84 0.016 0.014 0.027 <0.001 <0.001 <0.001 0.005 0.164
HCRC006 0 1 0.493 0.122 <0.001 <0.001 <0.001 <0.001 0.013
HCRC006 1 2 0.020 0.096 0.003 0.002 <0.001 0.005 0.006
HCRC006 2 3 0.007 0.074 <0.001 0.001 <0.001 0.007 <0.001
HCRC006 3 4 0.579 0.535 0.002 0.001 <0.001 0.008 0.006
HCRC006 4 5 0.091 0.301 <0.001 <0.001 0.006 0.014 0.001
HCRC006 5 6 0.028 0.286 <0.001 0.002 0.001 0.015 0.002
HCRC006 6 7 0.017 0.140 <0.001 <0.001 <0.001 0.012 0.002
HCRC006 7 8 0.010 0.096 <0.001 0.002 <0.001 0.015 <0.001
HCRC006 8 9 0.016 0.133 <0.001 0.002 <0.001 0.020 0.002
HCRC006 9 10 0.017 0.136 <0.001 <0.001 <0.001 0.021 0.001
HCRC006 10 11 0.022 0.088 <0.001 <0.001 <0.001 0.011 <0.001
HCRC006 11 12 0.029 0.106 <0.001 <0.001 0.002 0.008 <0.001
HCRC006 12 13 0.014 0.040 <0.001 0.001 <0.001 0.006 <0.001
HCRC006 13 14 0.019 0.054 <0.001 <0.001 0.004 0.007 <0.001
HCRC006 14 15 0.019 0.200 <0.001 <0.001 <0.001 0.008 <0.001
HCRC006 15 16 0.047 0.386 <0.001 0.003 0.003 0.014 0.012
HCRC006 16 17 0.048 0.160 0.003 0.001 0.005 0.006 0.003
HCRC006 17 18 0.013 0.136 <0.001 0.002 <0.001 0.009 <0.001
HCRC006 18 19 0.035 0.443 <0.001 <0.001 <0.001 0.011 <0.001
HCRC006 19 20 0.014 0.092 <0.001 0.001 <0.001 0.010 <0.001
HCRC006 20 21 0.016 0.020 <0.001 <0.001 <0.001 0.006 <0.001
HCRC006 21 22 0.012 0.009 <0.001 <0.001 <0.001 0.004 <0.001
HCRC006 22 23 0.016 0.016 <0.001 0.001 0.003 0.004 <0.001
HCRC006 23 24 0.021 0.008 <0.001 <0.001 <0.001 0.002 <0.001
HCRC006 24 25 0.023 0.004 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC006 25 26 0.006 0.002 <0.001 <0.001 0.004 0.002 <0.001
HCRC006 26 27 0.054 0.004 <0.001 <0.001 <0.001 0.004 <0.001
HCRC006 27 28 0.013 0.016 <0.001 <0.001 <0.001 0.003 0.010
HCRC006 28 29 0.020 0.040 <0.001 <0.001 <0.001 0.003 <0.001
HCRC006 29 30 0.014 0.039 <0.001 <0.001 0.004 <0.001 <0.001
HCRC006 30 31 0.006 0.026 <0.001 <0.001 <0.001 0.007 <0.001
HCRC006 31 32 0.006 0.022 <0.001 <0.001 <0.001 0.010 0.003
HCRC006 32 33 0.007 0.025 <0.001 <0.001 <0.001 0.011 <0.001
HCRC006 33 34 0.023 0.037 <0.001 <0.001 <0.001 0.008 <0.001
HCRC006 34 35 0.025 0.020 <0.001 <0.001 0.001 0.005 <0.001
HCRC006 35 36 0.017 0.014 <0.001 0.001 <0.001 0.008 0.015
HCRC006 36 37 0.014 0.010 <0.001 <0.001 0.002 0.007 0.017
HCRC006 37 38 0.034 0.232 <0.001 0.002 <0.001 0.011 0.065

9

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC006 38 39 0.030 0.288 <0.001 0.001 <0.001 0.013 0.021
HCRC006 39 40 0.040 0.099 <0.001 <0.001 <0.001 0.008 0.023
HCRC007 0 1 0.013 0.006 <0.001 <0.001 <0.001 0.002 0.004
HCRC007 1 2 0.003 0.009 <0.001 <0.001 <0.001 <0.001 0.015
HCRC007 2 3 0.006 0.005 <0.001 <0.001 <0.001 <0.001 0.030
HCRC007 3 4 0.004 0.003 <0.001 <0.001 <0.001 <0.001 0.006
HCRC007 4 5 0.002 0.005 <0.001 <0.001 <0.001 <0.001 0.001
HCRC007 5 6 0.005 0.029 <0.001 <0.001 <0.001 0.002 0.002
HCRC007 6 7 0.008 0.087 <0.001 <0.001 0.004 0.002 0.003
HCRC007 7 8 0.010 0.083 <0.001 0.002 <0.001 0.004 0.001
HCRC007 8 9 0.003 0.168 <0.001 <0.001 0.002 <0.001 0.002
HCRC007 9 10 0.042 0.113 <0.001 0.001 <0.001 <0.001 <0.001
HCRC007 10 11 0.010 0.200 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC007 11 12 0.004 0.107 <0.001 <0.001 0.002 <0.001 <0.001
HCRC007 12 13 0.003 0.019 <0.001 <0.001 <0.001 0.002 <0.001
HCRC007 13 14 0.004 0.005 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC007 14 15 0.004 0.002 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC007 15 16 0.006 0.001 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC007 16 17 0.002 0.003 <0.001 0.001 <0.001 <0.001 0.002
HCRC007 17 18 0.004 0.002 <0.001 0.001 <0.001 <0.001 0.013
HCRC007 18 19 0.004 0.002 <0.001 <0.001 <0.001 0.002 <0.001
HCRC007 19 20 0.010 0.001 <0.001 <0.001 0.002 <0.001 <0.001
HCRC007 20 21 0.170 0.065 <0.001 <0.001 <0.001 0.003 <0.001
HCRC007 21 22 0.014 0.045 <0.001 <0.001 <0.001 0.003 <0.001
HCRC007 22 23 0.009 0.041 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC007 23 24 0.014 0.062 <0.001 0.001 <0.001 0.005 <0.001
HCRC007 24 25 0.016 0.063 <0.001 <0.001 <0.001 0.004 <0.001
HCRC007 25 26 0.017 0.055 <0.001 <0.001 <0.001 0.006 <0.001
HCRC007 26 27 0.166 0.126 <0.001 0.003 <0.001 0.010 <0.001
HCRC007 27 28 0.029 0.021 <0.001 0.001 <0.001 0.008 0.002
HCRC007 28 29 0.033 0.002 <0.001 0.002 <0.001 <0.001 <0.001
HCRC007 29 30 0.012 0.001 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC007 30 31 0.008 0.001 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC007 31 32 0.007 <0.001 <0.001 <0.001 <0.001 0.002 0.002
HCRC007 32 33 0.003 0.001 <0.001 <0.001 0.005 <0.001 0.008
HCRC007 33 34 0.004 <0.001 <0.001 <0.001 <0.001 0.002 <0.001
HCRC007 34 35 0.005 0.001 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC007 35 36 0.003 0.002 <0.001 <0.001 <0.001 <0.001 0.052
HCRC007 36 37 0.007 0.008 <0.001 0.001 <0.001 <0.001 0.015
HCRC007 37 38 0.009 0.005 <0.001 <0.001 0.004 0.004 0.002
HCRC007 38 39 0.013 0.012 <0.001 <0.001 <0.001 0.010 <0.001
HCRC007 39 40 0.011 0.047 <0.001 <0.001 <0.001 0.002 <0.001
HCRC007 40 41 0.026 0.397 <0.001 0.001 <0.001 0.008 0.046
HCRC007 41 42 0.036 0.265 0.002 0.001 <0.001 0.013 0.019
HCRC007 42 43 0.018 0.177 <0.001 0.002 <0.001 0.020 0.030
HCRC007 43 44 0.016 0.113 <0.001 0.002 <0.001 0.016 0.008
HCRC007 44 45 0.005 0.052 <0.001 <0.001 0.003 0.013 0.002
HCRC007 45 46 0.012 0.081 <0.001 <0.001 0.003 0.004 <0.001
HCRC007 46 47 0.004 0.019 <0.001 <0.001 <0.001 <0.001 0.008
HCRC007 47 48 0.008 0.048 <0.001 0.002 0.003 0.005 0.009
HCRC007 48 49 0.014 0.060 <0.001 0.001 <0.001 0.003 0.009
HCRC007 49 50 0.016 0.037 <0.001 <0.001 <0.001 0.006 0.008
HCRC008 0 1 No Sample

10

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC008 1 2 0.003 0.006 <0.001 <0.001 <0.001 <0.001 0.002
HCRC008 2 3 0.010 0.005 <0.001 <0.001 <0.001 0.002 0.052
HCRC008 3 4 0.021 0.005 <0.001 <0.001 0.013 <0.001 0.010
HCRC008 4 5 0.012 0.024 <0.001 <0.001 <0.001 <0.001 0.006
HCRC008 5 6 0.011 0.071 <0.001 <0.001 <0.001 <0.001 0.006
HCRC008 6 7 0.012 0.076 <0.001 <0.001 <0.001 0.005 0.003
HCRC008 7 8 0.015 0.079 <0.001 0.002 0.004 0.005 0.003
HCRC008 8 9 0.034 0.088 <0.001 0.001 0.003 0.006 0.007
HCRC008 9 10 0.014 0.078 <0.001 0.001 <0.001 0.004 0.006
HCRC008 10 11 0.010 0.060 <0.001 <0.001 0.007 0.002 0.003
HCRC008 11 12 0.008 0.053 <0.001 <0.001 <0.001 0.004 0.002
HCRC008 12 13 0.010 0.039 <0.001 0.001 <0.001 0.006 0.004
HCRC008 13 14 0.013 0.006 <0.001 <0.001 <0.001 0.006 0.002
HCRC008 14 15 0.014 0.006 <0.001 <0.001 <0.001 0.005 0.003
HCRC008 15 16 0.009 0.015 <0.001 <0.001 <0.001 0.005 0.002
HCRC008 16 17 0.007 0.004 <0.001 <0.001 <0.001 0.006 <0.001
HCRC008 17 18 0.006 0.005 <0.001 <0.001 0.002 0.006 <0.001
HCRC008 18 19 0.006 0.003 <0.001 <0.001 <0.001 0.004 <0.001
HCRC008 19 20 0.006 0.002 <0.001 <0.001 <0.001 0.005 <0.001
HCRC008 20 21 0.010 0.009 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC008 21 22 0.010 0.003 <0.001 0.001 <0.001 0.002 <0.001
HCRC008 22 23 0.011 0.004 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC008 23 24 0.010 0.010 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC008 24 25 0.005 0.011 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC008 25 26 0.012 0.056 <0.001 0.001 <0.001 0.005 <0.001
HCRC008 26 27 0.021 0.117 <0.001 <0.001 <0.001 0.008 <0.001
HCRC008 27 28 0.010 0.021 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC008 28 29 0.010 0.038 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC008 29 30 0.024 0.095 <0.001 <0.001 <0.001 0.003 <0.001
HCRC008 30 31 0.021 0.138 <0.001 <0.001 <0.001 0.007 0.003
HCRC008 31 32 0.011 0.500 0.001 <0.001 <0.001 0.003 0.269
HCRC008 32 33 0.006 0.173 <0.001 <0.001 <0.001 <0.001 0.072
HCRC008 33 34 0.004 0.038 <0.001 <0.001 0.002 <0.001 0.030
HCRC008 34 35 0.005 0.112 <0.001 <0.001 <0.001 <0.001 0.130
HCRC008 35 36 0.008 0.151 <0.001 <0.001 <0.001 0.002 0.090
HCRC008 36 37 0.002 0.019 <0.001 <0.001 <0.001 <0.001 0.003
HCRC008 37 38 0.004 0.021 <0.001 <0.001 <0.001 0.002 <0.001
HCRC008 38 39 0.004 0.011 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC008 39 40 0.007 0.267 <0.001 <0.001 <0.001 0.005 0.026
HCRC008 40 41 0.008 0.165 <0.001 0.001 <0.001 0.009 0.021
HCRC008 41 42 0.008 0.154 <0.001 0.002 <0.001 0.002 0.125
HCRC008 42 43 0.003 0.052 <0.001 <0.001 <0.001 <0.001 0.066
HCRC008 43 44 0.003 0.047 <0.001 <0.001 <0.001 <0.001 0.102
HCRC008 44 45 0.009 0.394 0.001 <0.001 <0.001 0.002 0.263
HCRC008 45 46 0.010 0.134 <0.001 <0.001 <0.001 0.003 0.153
HCRC008 46 47 0.007 0.017 <0.001 <0.001 0.003 <0.001 0.003
HCRC008 47 48 0.005 0.018 <0.001 <0.001 0.002 <0.001 0.001
HCRC008 48 49 0.005 0.022 <0.001 <0.001 <0.001 0.002 <0.001
HCRC008 49 50 0.001 0.013 <0.001 <0.001 <0.001 0.003 <0.001
HCRC008 50 51 0.002 0.008 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC008 51 52 0.007 0.011 <0.001 0.001 0.002 0.002 0.003
HCRC008 52 53 0.003 0.032 <0.001 <0.001 <0.001 0.003 0.006
HCRC008 53 54 0.006 0.501 <0.001 0.002 0.006 <0.001 0.191

11

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC008 54 55 0.003 0.081 <0.001 <0.001 0.002 <0.001 0.041
HCRC008 55 56 0.004 0.015 <0.001 0.002 <0.001 0.002 0.002
HCRC008 56 57 0.003 0.013 <0.001 0.001 <0.001 0.002 0.002
HCRC008 57 58 0.002 0.009 <0.001 <0.001 <0.001 0.002 0.001
HCRC008 58 59 0.001 0.041 <0.001 <0.001 <0.001 <0.001 0.015
HCRC008 59 60 0.004 0.067 <0.001 <0.001 <0.001 0.002 0.054
HCRC008 60 61 0.007 0.224 0.002 0.002 <0.001 0.005 0.229
HCRC008 61 62 0.008 0.329 0.006 0.003 0.010 0.003 0.176
HCRC008 62 63 0.009 0.394 0.002 0.003 <0.001 0.006 0.158
HCRC008 63 64 0.004 0.050 <0.001 <0.001 <0.001 0.005 0.020
HCRC008 64 65 0.007 0.016 <0.001 0.001 <0.001 0.002 0.003
HCRC008 65 66 0.004 0.016 <0.001 <0.001 <0.001 <0.001 0.002
HCRC008 66 67 0.004 0.010 <0.001 0.002 <0.001 <0.001 0.002
HCRC008 67 68 0.004 0.007 <0.001 0.001 <0.001 0.002 0.002
HCRC008 68 69 0.004 0.007 <0.001 0.001 <0.001 <0.001 0.010
HCRC008 69 70 0.002 0.028 0.003 <0.001 <0.001 <0.001 0.527
HCRC008 70 71 0.001 0.022 0.002 <0.001 <0.001 0.002 0.561
HCRC008 71 72 0.004 0.014 0.002 0.002 <0.001 <0.001 0.299
HCRC008 72 73 0.003 0.019 <0.001 0.001 <0.001 0.002 0.189
HCRC008 73 74 0.003 0.024 0.003 <0.001 0.002 <0.001 0.387
HCRC008 74 75 0.003 0.014 <0.001 0.002 <0.001 <0.001 0.238
HCRC008 75 76 0.003 0.003 <0.001 <0.001 0.003 0.003 0.007
HCRC008 76 77 0.004 0.005 <0.001 0.002 <0.001 0.003 0.006
HCRC008 77 78 0.005 0.035 <0.001 0.005 <0.001 <0.001 0.067
HCRC008 78 79 0.004 0.036 0.004 0.001 <0.001 0.002 0.465
HCRC008 79 80 0.002 0.037 0.003 <0.001 0.002 <0.001 0.518
HCRC008 80 81 0.003 0.010 <0.001 <0.001 <0.001 <0.001 0.227
HCRC008 81 82 0.003 0.010 <0.001 0.001 <0.001 0.002 0.190
HCRC008 82 83 0.006 0.076 0.002 0.002 <0.001 0.004 0.566
HCRC008 83 84 0.010 0.134 0.001 0.002 <0.001 0.002 0.200
HCRC008 84 85 0.004 0.023 0.002 <0.001 <0.001 <0.001 0.391
HCRC008 85 86 0.005 0.112 0.003 <0.001 <0.001 <0.001 0.467
HCRC008 86 87 0.003 0.030 <0.001 <0.001 <0.001 0.002 0.074
HCRC008 87 88 0.002 0.008 0.001 <0.001 0.006 <0.001 0.406
HCRC008 88 89 0.009 0.098 0.006 0.002 <0.001 0.002 0.718
HCRC008 89 90 0.009 0.056 0.004 <0.001 <0.001 <0.001 0.235
HCRC008 90 91 0.003 0.004 0.001 0.001 <0.001 <0.001 0.119
HCRC008 91 92 0.003 0.003 0.001 <0.001 <0.001 <0.001 0.255
HCRC008 92 93 0.002 0.005 0.004 <0.001 <0.001 <0.001 0.584
HCRC008 93 94 0.002 0.005 0.002 0.002 0.002 0.002 0.276
HCRC008 94 95 0.003 0.044 <0.001 0.002 <0.001 <0.001 0.062
HCRC008 95 96 0.002 0.042 0.001 0.002 0.003 <0.001 0.212
HCRC008 96 97 0.003 0.040 <0.001 0.002 0.001 0.002 0.300
HCRC008 97 98 0.007 0.060 0.003 0.001 <0.001 0.002 0.243
HCRC008 98 99 0.084 0.088 0.002 0.001 <0.001 <0.001 0.150
HCRC008 99 100 0.014 0.026 0.001 0.001 0.003 0.003 0.031
HCRC009 0 1 No Sample
HCRC009 1 2 0.040 0.035 0.001 0.003 <0.001 0.013 0.008
HCRC009 2 3 0.024 0.058 0.001 0.003 0.002 0.008 0.011
HCRC009 3 4 0.013 0.134 <0.001 0.003 <0.001 <0.001 0.019
HCRC009 4 5 0.016 0.207 <0.001 0.002 <0.001 0.002 0.009
HCRC009 5 6 0.037 0.267 <0.001 0.004 <0.001 0.002 0.005
HCRC009 6 7 0.037 0.113 <0.001 0.004 <0.001 0.006 0.005

12

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC009 7 8 0.035 0.215 <0.001 0.004 <0.001 0.008 0.005
HCRC009 8 9 0.013 0.245 <0.001 0.003 <0.001 <0.001 0.008
HCRC009 9 10 0.023 0.220 <0.001 0.003 0.001 0.007 0.006
HCRC009 10 11 0.025 0.294 <0.001 0.002 <0.001 0.002 0.007
HCRC009 11 12 0.035 0.183 <0.001 0.003 0.003 0.003 0.006
HCRC009 12 13 0.074 0.255 0.002 0.018 0.002 0.010 0.006
HCRC009 13 14 0.083 0.123 0.002 0.010 <0.001 0.031 0.005
HCRC009 14 15 0.070 0.099 0.003 0.005 <0.001 0.008 0.003
HCRC009 15 16 0.052 0.165 0.002 0.004 <0.001 0.014 0.001
HCRC009 16 17 0.055 0.384 <0.001 <0.001 <0.001 0.005 0.004
HCRC009 17 18 0.028 0.373 <0.001 0.002 <0.001 0.010 0.003
HCRC009 18 19 0.048 0.328 0.001 0.002 <0.001 0.010 0.003
HCRC009 19 20 0.030 0.113 <0.001 <0.001 0.001 0.006 0.005
HCRC009 20 21 0.055 0.083 0.001 0.004 <0.001 0.005 0.007
HCRC009 21 22 0.049 0.129 0.001 0.006 <0.001 0.008 0.001
HCRC009 22 23 0.060 0.196 <0.001 0.005 <0.001 0.006 0.002
HCRC009 23 24 0.077 0.248 <0.001 0.003 <0.001 0.004 <0.001
HCRC009 24 25 0.063 0.152 <0.001 0.004 0.008 0.005 0.002
HCRC009 25 26 0.032 0.068 <0.001 0.003 0.003 0.004 0.002
HCRC009 26 27 0.012 0.022 <0.001 <0.001 0.003 <0.001 0.002
HCRC009 27 28 0.026 0.025 <0.001 0.002 <0.001 0.003 0.001
HCRC009 28 29 0.035 0.031 0.001 0.003 0.001 0.014 0.001
HCRC009 29 30 0.017 0.047 0.001 0.002 0.005 0.009 <0.001
HCRC009 30 31 0.013 0.051 <0.001 0.003 0.001 0.009 <0.001
HCRC009 31 32 0.012 0.028 <0.001 0.002 0.004 0.058 0.001
HCRC009 32 33 0.015 0.040 0.003 0.003 0.003 0.006 0.002
HCRC009 33 34 0.037 0.050 0.001 0.008 0.005 0.005 0.003
HCRC009 34 35 0.099 0.064 0.005 0.014 0.001 0.012 0.002
HCRC009 35 36 0.030 0.105 0.003 0.007 <0.001 0.004 0.002
HCRC009 36 37 0.049 0.072 0.003 0.003 0.002 0.008 <0.001
HCRC009 37 38 0.029 0.156 0.006 0.005 0.001 0.010 <0.001
HCRC009 38 39 0.034 0.068 0.003 0.004 0.011 0.008 <0.001
HCRC009 39 40 0.023 0.056 0.003 0.004 0.002 0.006 <0.001
HCRC009 40 41 0.021 0.046 0.002 0.003 0.004 0.006 0.001
HCRC009 41 42 0.015 0.020 <0.001 0.002 0.004 0.006 <0.001
HCRC009 42 43 0.009 0.010 <0.001 0.002 <0.001 0.006 0.003
HCRC009 43 44 0.006 0.006 <0.001 0.003 <0.001 <0.001 0.006
HCRC009 44 45 0.003 0.005 <0.001 0.001 0.002 <0.001 0.007
HCRC009 45 46 0.009 0.017 0.001 0.002 0.004 0.002 0.006
HCRC009 46 47 0.026 0.049 0.001 0.003 0.002 0.006 0.004
HCRC009 47 48 0.009 0.020 <0.001 0.002 0.001 0.002 0.003
HCRC009 48 49 0.012 0.013 <0.001 0.001 0.004 0.002 0.002
HCRC009 49 50 0.030 0.007 <0.001 0.002 <0.001 0.005 0.005
HCRC009 50 51 0.006 0.015 <0.001 0.001 <0.001 0.004 0.003
HCRC009 51 52 0.005 0.011 0.002 0.002 <0.001 0.003 0.002
HCRC009 52 53 0.010 0.011 <0.001 0.002 0.002 0.009 0.004
HCRC009 53 54 0.007 0.011 <0.001 0.003 0.006 0.002 0.003
HCRC009 54 55 0.007 0.006 0.001 0.003 <0.001 0.003 0.003
HCRC009 55 56 0.201 0.005 0.005 0.001 0.003 0.006 0.002
HCRC009 56 57 0.009 0.006 <0.001 0.003 0.002 0.005 0.003
HCRC009 57 58 0.010 0.045 0.003 0.001 <0.001 0.005 0.007
HCRC009 58 59 0.017 0.055 0.003 0.003 0.002 0.006 0.020
HCRC009 59 60 0.013 0.012 0.001 0.002 <0.001 0.004 0.010

13

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC009 60 61 0.019 0.011 0.001 <0.001 0.004 <0.001 0.011
HCRC009 61 62 0.007 0.006 <0.001 <0.001 0.009 0.004 0.005
HCRC009 62 63 0.002 0.015 <0.001 <0.001 <0.001 0.002 0.004
HCRC009 63 64 0.004 0.018 <0.001 <0.001 <0.001 0.006 0.008
HCRC009 64 65 0.004 0.009 <0.001 <0.001 0.005 0.005 0.003
HCRC009 65 66 0.004 0.006 <0.001 <0.001 <0.001 0.006 0.003
HCRC009 66 67 0.009 0.013 <0.001 0.008 0.004 0.005 0.007
HCRC009 67 68 0.003 0.007 <0.001 <0.001 <0.001 0.005 0.003
HCRC009 68 69 0.003 0.003 <0.001 <0.001 0.004 0.004 0.002
HCRC009 69 70 0.006 0.006 <0.001 0.003 0.004 0.002 0.004
HCRC009 70 71 0.013 0.039 <0.001 0.003 0.002 0.003 0.010
HCRC009 71 72 0.020 0.007 0.007 <0.001 0.004 0.004 0.017
HCRC009 72 73 0.016 0.003 0.004 <0.001 <0.001 0.007 0.015
HCRC009 73 74 1.186 0.002 0.005 0.002 0.008 0.005 0.009
HCRC009 74 75 0.143 0.003 0.003 0.001 0.001 0.002 0.008
HCRC009 75 76 0.028 0.124 0.003 0.004 0.004 0.008 0.073
HCRC009 76 77 0.015 0.018 0.004 0.002 <0.001 0.004 0.009
HCRC009 77 78 0.005 0.066 0.007 <0.001 0.004 <0.001 0.022
HCRC009 78 79 0.011 0.026 0.003 0.002 0.003 <0.001 0.011
HCRC009 79 80 0.023 0.012 0.006 0.002 0.003 0.004 0.013
HCRC009 80 81 0.094 0.002 0.006 <0.001 0.006 0.002 0.006
HCRC009 81 82 0.040 0.002 0.006 <0.001 0.003 0.003 0.008
HCRC009 82 83 0.036 0.011 0.002 <0.001 0.002 0.002 0.005
HCRC009 83 84 0.023 0.005 0.006 0.002 0.007 0.003 0.007
HCRC009 84 85 1.708 0.005 0.048 0.002 0.005 0.002 0.036
HCRC009 85 86 0.099 0.001 0.008 0.003 0.005 0.008 0.013
HCRC009 86 87 0.208 0.019 0.009 0.003 0.004 0.006 0.019
HCRC009 87 88 0.022 0.040 0.004 0.003 0.005 0.002 0.015
HCRC009 88 89 0.065 0.075 0.020 0.008 0.002 0.006 0.043
HCRC009 89 90 0.067 0.004 0.004 0.001 0.004 0.007 0.002
HCRC009 90 91 0.054 0.002 0.009 0.002 0.004 0.004 0.004
HCRC009 91 92 1.162 0.003 0.143 0.003 <0.001 0.004 0.025
HCRC009 92 93 0.105 0.002 0.015 <0.001 0.003 0.005 0.004
HCRC009 93 94 0.036 <0.001 0.007 0.001 <0.001 0.006 0.006
HCRC009 94 95 0.096 0.001 0.003 <0.001 <0.001 0.002 0.005
HCRC009 95 96 0.025 0.004 0.003 0.001 <0.001 0.003 0.009
HCRC009 96 97 0.009 0.003 0.004 0.003 <0.001 0.004 0.011
HCRC009 97 98 0.263 0.002 0.004 0.002 0.003 0.005 0.011
HCRC009 98 99 0.043 0.001 0.003 0.002 <0.001 0.002 0.007
HCRC009 99 100 0.009 0.003 <0.001 0.002 0.001 0.005 <0.001
HCRC010 0 1 0.115 0.012 0.003 0.009 <0.001 0.006 0.006
HCRC010 1 2 0.040 0.008 0.001 0.004 <0.001 0.007 0.005
HCRC010 2 3 0.041 0.011 <0.001 0.010 <0.001 0.006 0.004
HCRC010 3 4 0.325 0.014 0.005 0.007 <0.001 0.007 0.023
HCRC010 4 5 8.679 0.043 0.019 0.030 0.003 0.013 0.030
HCRC010 5 6 0.132 0.008 0.006 0.003 <0.001 0.004 0.019
HCRC010 6 7 0.092 0.007 <0.001 0.008 <0.001 0.003 0.010
HCRC010 7 8 0.068 0.009 <0.001 0.005 0.003 0.010 0.007
HCRC010 8 9 0.087 0.014 <0.001 0.004 0.005 0.013 0.007
HCRC010 9 10 0.070 0.008 <0.001 0.003 0.004 0.012 0.019
HCRC010 10 11 0.060 0.012 0.001 0.003 <0.001 0.006 0.019
HCRC010 11 12 0.045 0.010 <0.001 0.004 0.004 0.006 0.015
HCRC010 12 13 0.046 0.012 <0.001 0.004 0.003 0.003 0.021

14

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC010 13 14 0.035 0.017 0.002 0.005 <0.001 <0.001 0.016
HCRC010 14 15 0.030 0.009 0.001 0.003 <0.001 0.006 0.018
HCRC010 15 16 0.036 0.008 0.001 0.002 <0.001 0.003 0.010
HCRC010 16 17 0.107 0.037 0.004 0.010 <0.001 0.008 0.007
HCRC010 17 18 0.034 0.039 <0.001 0.002 0.005 0.005 <0.001
HCRC010 18 19 0.045 0.033 <0.001 0.003 0.002 0.004 <0.001
HCRC010 19 20 0.058 0.029 <0.001 0.003 <0.001 0.006 <0.001
HCRC010 20 21 0.044 0.025 <0.001 0.004 <0.001 0.007 <0.001
HCRC010 21 22 0.033 0.022 <0.001 0.003 <0.001 0.007 <0.001
HCRC010 22 23 0.043 0.024 0.001 0.005 <0.001 0.004 <0.001
HCRC010 23 24 0.033 0.023 <0.001 0.007 <0.001 0.006 <0.001
HCRC010 24 25 0.033 0.020 <0.001 0.007 <0.001 0.009 <0.001
HCRC010 25 26 0.029 0.028 <0.001 0.011 0.002 0.002 <0.001
HCRC010 26 27 0.031 0.033 <0.001 0.006 <0.001 0.005 <0.001
HCRC010 27 28 0.044 0.048 <0.001 0.008 <0.001 0.005 <0.001
HCRC010 28 29 0.038 0.074 <0.001 0.004 0.002 0.006 <0.001
HCRC010 29 30 0.037 0.052 <0.001 0.004 <0.001 0.006 <0.001
HCRC010 30 31 0.023 0.035 <0.001 0.002 <0.001 0.004 <0.001
HCRC010 31 32 0.024 0.038 <0.001 0.020 0.010 0.006 <0.001
HCRC010 32 33 0.021 0.049 <0.001 0.016 <0.001 0.005 <0.001
HCRC010 33 34 0.022 0.048 0.001 0.002 0.004 0.004 <0.001
HCRC010 34 35 0.024 0.077 <0.001 0.029 0.003 0.010 <0.001
HCRC010 35 36 0.028 0.062 <0.001 0.011 <0.001 0.010 <0.001
HCRC010 36 37 0.020 0.026 <0.001 0.016 <0.001 0.006 <0.001
HCRC010 37 38 0.016 0.022 <0.001 0.009 <0.001 0.004 <0.001
HCRC010 38 39 0.023 0.023 <0.001 0.007 <0.001 0.006 <0.001
HCRC010 39 40 0.033 0.044 <0.001 0.013 <0.001 0.005 <0.001
HCRC010 40 41 0.035 0.048 0.001 0.004 0.005 0.005 <0.001
HCRC010 41 42 0.148 0.035 0.003 0.008 <0.001 0.013 0.003
HCRC010 42 43 0.034 0.009 0.001 0.007 <0.001 0.024 0.009
HCRC010 43 44 0.020 0.006 <0.001 0.003 <0.001 0.005 0.009
HCRC010 44 45 0.023 0.010 <0.001 0.003 <0.001 0.006 0.006
HCRC010 45 46 0.036 0.007 0.002 0.005 <0.001 0.009 <0.001
HCRC010 46 47 0.024 0.017 0.001 0.004 <0.001 0.006 <0.001
HCRC010 47 48 0.015 0.014 <0.001 0.003 <0.001 0.002 <0.001
HCRC010 48 49 0.014 0.011 0.001 0.001 <0.001 <0.001 0.002
HCRC010 49 50 0.551 0.013 0.022 0.007 <0.001 0.005 0.002
HCRC010 50 51 0.261 0.004 0.009 0.004 <0.001 0.006 <0.001
HCRC010 51 52 0.033 0.003 <0.001 0.001 <0.001 0.002 <0.001
HCRC010 52 53 0.027 0.006 <0.001 <0.001 0.002 0.003 <0.001
HCRC010 53 54 0.022 0.011 0.001 0.004 <0.001 0.004 0.002
HCRC010 54 55 0.011 0.002 0.001 <0.001 <0.001 0.002 <0.001
HCRC010 55 56 0.012 0.003 0.004 0.001 <0.001 0.002 0.005
HCRC010 56 57 0.012 0.004 0.003 0.001 <0.001 <0.001 0.005
HCRC010 57 58 0.013 0.003 0.003 0.003 <0.001 0.002 0.012
HCRC010 58 59 0.015 0.002 0.001 0.002 <0.001 0.006 0.011
HCRC010 59 60 0.060 0.011 0.011 0.017 <0.001 0.017 0.022
HCRC010 60 61 0.064 0.016 0.017 0.006 0.003 0.022 0.018
HCRC010 61 62 0.316 0.008 0.006 0.002 <0.001 0.006 0.002
HCRC010 62 63 0.166 0.019 0.005 0.004 <0.001 0.009 0.006
HCRC010 63 64 0.076 0.011 0.006 0.003 <0.001 0.008 0.012
HCRC010 64 65 0.010 0.017 0.001 0.002 <0.001 0.003 0.004
HCRC010 65 66 0.033 0.012 0.001 0.003 <0.001 0.010 0.005

15

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC010 66 67 0.045 0.005 0.001 0.002 0.003 0.008 <0.001
HCRC010 67 68 0.013 0.004 0.003 0.003 0.001 0.006 0.003
HCRC010 68 69 0.014 0.005 0.003 0.002 0.001 <0.001 0.004
HCRC010 69 70 0.016 0.005 0.002 0.002 <0.001 0.007 0.009
HCRC010 70 71 0.045 0.009 0.006 0.005 0.002 0.015 0.039
HCRC010 71 72 0.022 0.006 0.004 0.003 <0.001 0.005 0.019
HCRC010 72 73 0.022 0.003 0.004 0.004 0.001 0.002 0.018
HCRC010 73 74 0.015 0.003 0.003 0.004 <0.001 0.005 0.016
HCRC010 74 75 0.011 0.003 0.003 <0.001 <0.001 0.002 0.018
HCRC010 75 76 0.020 0.008 0.005 0.004 <0.001 0.005 0.030
HCRC010 76 77 0.019 0.005 0.006 0.004 <0.001 0.008 0.017
HCRC010 77 78 0.039 0.022 0.003 0.004 0.003 0.006 0.032
HCRC010 78 79 0.051 0.006 0.003 0.002 <0.001 0.006 0.011
HCRC010 79 80 0.021 0.003 0.003 0.003 0.004 0.005 0.018
HCRC010 80 81 0.014 0.004 0.003 0.002 0.001 0.007 0.021
HCRC010 81 82 0.014 0.003 0.003 0.003 0.002 0.010 0.021
HCRC010 82 83 0.018 0.004 0.005 0.002 0.001 0.006 0.022
HCRC010 83 84 0.008 0.002 0.005 <0.001 <0.001 0.002 0.009
HCRC010 84 85 0.007 0.002 0.003 0.001 <0.001 0.002 0.010
HCRC010 85 86 0.011 0.002 0.005 <0.001 <0.001 0.004 0.007
HCRC010 86 87 0.010 0.008 0.002 0.002 <0.001 0.007 0.009
HCRC010 87 88 0.015 0.005 0.005 0.003 <0.001 0.006 0.009
HCRC010 88 89 0.009 0.008 0.001 0.003 <0.001 0.006 0.006
HCRC010 89 90 0.009 0.010 <0.001 0.003 <0.001 <0.001 0.007
HCRC010 90 91 0.012 0.007 0.001 0.002 0.006 0.006 0.004
HCRC010 91 92 0.006 0.006 0.002 0.002 <0.001 0.005 0.004
HCRC010 92 93 0.004 0.002 0.001 0.001 <0.001 0.004 0.003
HCRC010 93 94 0.005 0.002 0.001 0.001 0.001 0.004 0.002
HCRC010 94 95 0.005 0.004 <0.001 <0.001 <0.001 0.002 <0.001
HCRC010 95 96 0.007 0.006 <0.001 <0.001 <0.001 0.007 <0.001
HCRC010 96 97 0.008 0.007 <0.001 0.002 0.001 0.007 0.002
HCRC010 97 98 0.016 0.005 <0.001 <0.001 <0.001 0.002 <0.001
HCRC010 98 99 0.012 0.012 0.001 <0.001 <0.001 0.006 0.004
HCRC010 99 100 0.011 0.018 0.001 0.002 0.002 0.005 0.005
HCRC011 0 1 No Sample
HCRC011 1 2 0.537 0.010 0.006 0.010 <0.001 0.010 0.008
HCRC011 2 3 0.087 0.006 0.001 0.004 <0.001 0.003 0.007
HCRC011 3 4 0.018 0.006 <0.001 0.001 0.002 0.004 <0.001
HCRC011 4 5 0.020 0.008 <0.001 0.003 <0.001 0.002 <0.001
HCRC011 5 6 0.016 0.009 <0.001 <0.001 <0.001 0.002 <0.001
HCRC011 6 7 0.026 0.009 <0.001 0.006 <0.001 0.002 <0.001
HCRC011 7 8 0.015 0.007 <0.001 <0.001 <0.001 0.004 <0.001
HCRC011 8 9 0.011 0.004 <0.001 0.001 <0.001 0.004 <0.001
HCRC011 9 10 0.020 0.006 <0.001 <0.001 <0.001 0.003 0.005
HCRC011 10 11 0.022 0.005 <0.001 0.001 0.003 0.004 0.005
HCRC011 11 12 0.025 0.004 <0.001 0.001 <0.001 <0.001 0.002
HCRC011 12 13 0.026 0.004 <0.001 0.003 <0.001 0.002 0.006
HCRC011 13 14 0.022 0.004 <0.001 <0.001 <0.001 0.002 0.001
HCRC011 14 15 0.072 0.005 <0.001 0.002 <0.001 0.002 <0.001
HCRC011 15 16 0.016 0.005 <0.001 0.001 <0.001 0.002 <0.001
HCRC011 16 17 0.051 0.021 0.003 0.002 <0.001 0.011 <0.001
HCRC011 17 18 0.016 0.013 <0.001 <0.001 0.004 0.003 <0.001
HCRC011 18 19 0.015 0.014 <0.001 0.001 <0.001 0.002 <0.001

16

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC011 19 20 0.021 0.011 <0.001 0.001 0.008 0.004 <0.001
HCRC011 20 21 0.020 0.017 <0.001 <0.001 <0.001 0.002 <0.001
HCRC011 21 22 0.022 0.007 <0.001 0.002 <0.001 0.007 <0.001
HCRC011 22 23 0.052 0.021 0.002 0.003 <0.001 0.006 <0.001
HCRC011 23 24 0.033 0.019 0.001 0.002 <0.001 <0.001 <0.001
HCRC011 24 25 0.038 0.035 0.001 0.004 0.002 0.006 <0.001
HCRC011 25 26 0.022 0.043 <0.001 0.002 <0.001 0.005 <0.001
HCRC011 26 27 0.015 0.022 <0.001 0.002 0.003 0.005 <0.001
HCRC011 27 28 0.016 0.016 <0.001 <0.001 <0.001 0.007 <0.001
HCRC011 28 29 0.008 0.008 <0.001 <0.001 <0.001 0.003 <0.001
HCRC011 29 30 0.007 0.006 <0.001 <0.001 <0.001 0.003 <0.001
HCRC011 30 31 0.050 0.007 <0.001 <0.001 <0.001 0.005 <0.001
HCRC011 31 32 0.043 0.011 0.001 0.002 0.002 0.004 <0.001
HCRC011 32 33 0.061 0.029 0.003 0.003 <0.001 0.008 <0.001
HCRC011 33 34 0.034 0.021 0.003 0.002 0.002 0.006 <0.001
HCRC011 34 35 0.032 0.018 <0.001 0.003 <0.001 0.008 <0.001
HCRC011 35 36 0.042 0.028 0.003 0.006 <0.001 0.005 <0.001
HCRC011 36 37 0.024 0.012 0.001 0.012 0.002 0.006 <0.001
HCRC011 37 38 0.112 0.030 0.002 0.018 <0.001 0.014 <0.001
HCRC011 38 39 0.086 0.013 0.003 0.006 <0.001 0.009 <0.001
HCRC011 39 40 0.020 0.004 0.001 0.003 <0.001 0.006 <0.001
HCRC011 40 41 0.021 0.004 0.001 0.004 0.004 0.006 <0.001
HCRC011 41 42 0.014 0.004 0.002 0.003 <0.001 0.005 0.001
HCRC011 42 43 0.017 0.005 0.002 0.003 <0.001 0.005 <0.001
HCRC011 43 44 0.190 0.011 0.003 0.003 0.002 0.009 0.003
HCRC011 44 45 0.012 0.006 <0.001 0.002 <0.001 0.002 <0.001
HCRC011 45 46 0.010 0.006 <0.001 0.005 <0.001 0.002 <0.001
HCRC011 46 47 0.007 0.006 <0.001 0.002 <0.001 0.002 <0.001
HCRC011 47 48 0.037 0.008 0.003 0.015 0.002 0.004 0.003
HCRC011 48 49 0.018 0.024 0.006 0.018 <0.001 0.008 0.068
HCRC011 49 50 0.009 0.006 <0.001 0.003 <0.001 0.006 0.006
HCRC011 50 51 0.020 0.006 0.003 0.005 0.004 0.006 0.005
HCRC011 51 52 0.010 0.006 0.002 0.003 <0.001 0.003 <0.001
HCRC011 52 53 0.677 0.019 0.009 0.006 0.003 0.010 0.007
HCRC011 53 54 0.062 0.011 0.003 0.003 0.002 0.012 0.003
HCRC011 54 55 0.548 0.012 0.011 0.009 0.003 0.009 0.009
HCRC011 55 56 1.391 0.017 0.030 0.032 <0.001 0.035 0.006
HCRC011 56 57 0.066 0.016 0.001 0.002 0.004 0.005 <0.001
HCRC011 57 58 0.028 0.013 0.001 0.002 <0.001 0.004 0.002
HCRC011 58 59 0.013 0.008 0.001 0.003 <0.001 0.005 0.002
HCRC011 59 60 0.016 0.002 0.001 0.002 <0.001 0.004 <0.001
HCRC011 60 61 0.019 0.003 0.001 0.004 0.003 0.003 0.001
HCRC011 61 62 0.092 0.054 0.043 0.017 <0.001 0.005 0.046
HCRC011 62 63 0.305 0.378 0.086 0.069 0.003 0.009 0.176
HCRC011 63 64 0.752 0.186 0.013 0.101 <0.001 0.031 0.129
HCRC011 64 65 0.111 0.024 0.006 0.014 <0.001 0.010 0.019
HCRC011 65 66 0.022 0.003 0.003 0.003 <0.001 0.006 0.004
HCRC011 66 67 0.015 0.011 0.008 0.003 <0.001 0.006 0.006
HCRC011 67 68 0.123 0.075 0.010 0.007 <0.001 0.008 0.025
HCRC011 68 69 0.045 0.083 0.005 0.006 0.001 0.008 0.031
HCRC011 69 70 0.187 0.145 0.007 0.008 0.001 0.007 0.053
HCRC011 70 71 0.207 0.155 0.017 0.009 <0.001 0.006 0.060
HCRC011 71 72 0.091 0.727 0.011 0.072 <0.001 0.017 0.223

17

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC011 72 73 0.098 0.350 0.006 0.022 <0.001 0.012 0.115
HCRC011 73 74 0.066 3.297 0.010 0.245 <0.001 0.037 0.939
HCRC011 74 75 0.009 0.027 <0.001 0.004 <0.001 0.006 0.007
HCRC011 75 76 0.010 0.039 0.001 0.005 <0.001 0.013 0.009
HCRC011 76 77 0.240 0.026 0.010 0.010 0.006 0.010 0.013
HCRC011 77 78 0.025 0.129 0.002 0.013 <0.001 0.010 0.043
HCRC011 78 79 0.195 0.015 0.008 0.007 <0.001 0.012 0.016
HCRC011 79 80 0.010 0.015 0.003 0.003 <0.001 0.003 0.006
HCRC011 80 81 0.010 0.011 0.008 0.003 <0.001 <0.001 0.008
HCRC011 81 82 0.010 0.011 0.004 0.003 <0.001 0.007 0.003
HCRC011 82 83 0.009 0.014 0.002 0.004 <0.001 0.006 0.002
HCRC011 83 84 0.011 0.009 <0.001 0.002 0.001 0.005 0.002
HCRC011 84 85 0.055 0.014 0.005 0.002 <0.001 0.005 0.005
HCRC011 85 86 0.080 0.019 0.008 0.008 <0.001 0.003 0.020
HCRC011 86 87 0.038 1.622 0.006 0.017 0.001 0.036 0.483
HCRC011 87 88 0.689 1.090 0.008 0.025 <0.001 0.024 0.332
HCRC011 88 89 0.056 0.355 0.004 0.014 <0.001 0.009 0.130
HCRC011 89 90 0.036 0.477 0.005 0.015 <0.001 0.011 0.162
HCRC011 90 91 0.024 0.191 0.003 0.008 0.006 0.007 0.061
HCRC011 91 92 0.012 0.019 0.001 0.003 <0.001 0.007 0.004
HCRC011 92 93 0.010 0.008 0.002 0.004 <0.001 0.009 0.003
HCRC011 93 94 0.024 0.023 0.001 0.006 <0.001 0.013 0.003
HCRC011 94 95 0.018 0.011 0.001 0.003 <0.001 0.006 <0.001
HCRC011 95 96 0.020 0.030 0.001 0.004 <0.001 0.007 <0.001
HCRC011 96 97 0.040 0.049 0.002 0.007 0.002 0.008 0.002
HCRC011 97 98 0.208 0.028 0.004 0.006 <0.001 0.009 <0.001
HCRC011 98 99 0.035 0.130 0.001 0.007 0.004 0.009 0.033
HCRC011 99 100 0.037 0.529 0.005 0.013 <0.001 0.006 0.160
HCRC012 0 1 No Sample
HCRC012 1 2 0.031 0.020 <0.001 0.005 <0.001 0.005 0.007
HCRC012 2 3 0.031 0.019 0.005 0.014 0.006 0.014 0.024
HCRC012 3 4 0.035 0.032 0.003 0.006 0.002 0.006 0.016
HCRC012 4 5 0.038 0.047 0.001 0.013 <0.001 0.004 0.009
HCRC012 5 6 0.038 0.047 <0.001 0.003 0.003 0.006 0.013
HCRC012 6 7 0.031 0.031 <0.001 0.003 0.005 0.002 0.009
HCRC012 7 8 0.029 0.038 <0.001 0.006 0.005 0.004 0.010
HCRC012 8 9 0.032 0.041 0.001 0.010 0.005 0.003 0.008
HCRC012 9 10 0.011 0.030 <0.001 0.005 <0.001 0.003 0.002
HCRC012 10 11 0.007 0.023 0.001 0.015 <0.001 0.006 <0.001
HCRC012 11 12 0.008 0.019 <0.001 0.006 <0.001 0.006 <0.001
HCRC012 12 13 0.027 0.033 0.007 0.030 <0.001 0.005 0.001
HCRC012 13 14 0.024 0.024 0.003 0.007 0.006 0.005 <0.001
HCRC012 14 15 0.023 0.022 0.004 0.004 0.004 0.009 <0.001
HCRC012 15 16 0.019 0.029 0.003 0.003 0.003 0.006 0.002
HCRC012 16 17 0.014 0.054 0.003 0.003 0.005 0.008 0.004
HCRC012 17 18 0.042 0.088 0.003 0.004 <0.001 0.008 0.011
HCRC012 18 19 0.024 0.036 <0.001 0.006 0.002 0.005 0.010
HCRC012 19 20 0.047 0.160 0.008 0.006 <0.001 0.010 0.011
HCRC012 20 21 0.079 0.084 0.010 0.018 <0.001 0.011 0.006
HCRC012 21 22 0.046 0.257 0.012 0.007 <0.001 0.020 0.008
HCRC012 22 23 0.346 0.077 0.008 0.011 0.005 0.017 0.003
HCRC012 23 24 No Sample
HCRC012 24 25 0.054 0.024 0.003 0.008 0.004 0.020 0.001

18

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC012 25 26 0.046 0.010 0.003 0.126 <0.001 0.010 <0.001
HCRC012 26 27 0.060 0.009 0.001 0.019 0.005 0.014 <0.001
HCRC012 27 28 0.434 0.015 0.004 0.005 <0.001 0.009 <0.001
HCRC012 28 29 0.056 0.016 0.001 0.004 <0.001 0.007 0.001
HCRC012 29 30 0.022 0.015 0.001 0.004 0.004 0.007 0.001
HCRC012 30 31 0.024 0.011 0.003 0.029 0.002 0.007 <0.001
HCRC012 31 32 0.021 0.018 0.002 0.010 0.007 0.009 <0.001
HCRC012 32 33 0.020 0.016 0.002 0.005 0.001 0.008 <0.001
HCRC012 33 34 0.063 0.054 0.006 0.011 0.004 0.002 <0.001
HCRC012 34 35 0.015 0.009 0.002 0.007 <0.001 0.003 <0.001
HCRC012 35 36 0.012 0.035 0.001 0.003 0.002 0.006 <0.001
HCRC012 36 37 0.034 0.030 <0.001 0.004 0.003 0.007 0.005
HCRC012 37 38 0.012 0.015 <0.001 0.002 <0.001 0.003 <0.001
HCRC012 38 39 0.017 0.018 0.001 0.002 <0.001 0.002 <0.001
HCRC012 39 40 0.013 0.010 0.002 0.003 0.009 0.002 <0.001
HCRC012 40 41 0.015 0.008 0.003 0.003 0.001 0.002 0.002
HCRC012 41 42 0.111 0.009 0.007 0.003 0.002 0.003 0.004
HCRC012 42 43 0.014 0.024 0.003 0.004 <0.001 0.006 0.015
HCRC012 43 44 0.070 1.865 0.012 0.099 0.004 0.019 0.536
HCRC012 44 45 0.039 2.332 0.015 0.150 0.006 0.030 0.679
HCRC012 45 46 0.064 1.605 0.013 0.150 <0.001 0.026 0.484
HCRC012 46 47 0.059 0.798 0.012 0.132 0.002 0.016 0.268
HCRC012 47 48 0.028 0.114 0.017 0.043 <0.001 0.007 0.055
HCRC012 48 49 0.016 0.005 0.007 0.002 <0.001 0.009 0.002
HCRC012 49 50 0.014 0.007 0.007 0.002 0.004 0.009 0.005
HCRC012 50 51 0.013 0.005 0.006 0.002 <0.001 0.003 0.003
HCRC012 51 52 0.006 0.005 0.006 0.002 <0.001 0.003 <0.001
HCRC012 52 53 0.010 0.010 0.007 0.002 0.002 0.007 0.011
HCRC012 53 54 0.014 0.012 0.002 0.002 0.004 0.004 0.007
HCRC012 54 55 0.009 0.007 0.003 0.002 0.007 0.002 0.002
HCRC012 55 56 0.014 0.010 0.007 0.003 <0.001 0.006 0.009
HCRC012 56 57 0.008 0.005 0.004 0.002 <0.001 0.002 0.002
HCRC012 57 58 0.008 0.009 0.002 0.001 0.004 0.004 0.001
HCRC012 58 59 0.011 0.067 0.002 0.003 <0.001 0.003 0.021
HCRC012 59 60 0.018 1.685 0.011 0.062 0.005 <0.001 0.477
HCRC012 60 61 0.019 0.138 0.001 0.008 0.008 <0.001 0.040
HCRC012 61 62 0.024 0.015 0.001 0.003 0.003 0.006 0.005
HCRC012 62 63 0.438 0.010 0.010 0.004 <0.001 0.013 0.008
HCRC012 63 64 0.060 0.009 0.002 0.002 0.005 0.017 0.004
HCRC012 64 65 0.015 0.004 0.003 0.001 0.004 0.009 0.002
HCRC012 65 66 0.094 0.313 0.004 0.014 <0.001 0.011 0.104
HCRC012 66 67 0.028 0.121 0.006 0.005 <0.001 0.007 0.045
HCRC012 67 68 0.015 0.206 0.004 0.008 0.005 0.011 0.065
HCRC012 68 69 0.013 0.206 0.003 0.007 0.003 0.013 0.064
HCRC012 69 70 0.023 0.347 0.006 0.014 <0.001 0.015 0.117
HCRC012 70 71 0.031 0.264 0.004 0.013 0.003 0.012 0.098
HCRC012 71 72 0.017 1.273 0.008 0.045 0.007 0.020 0.385
HCRC012 72 73 0.219 0.916 0.009 0.096 0.002 0.017 0.306
HCRC012 73 74 0.021 0.528 0.003 0.032 0.005 0.014 0.176
HCRC012 74 75 0.448 0.426 0.009 0.026 0.005 0.018 0.157
HCRC012 75 76 0.123 0.657 0.008 0.012 0.002 0.023 0.226
HCRC012 76 77 0.023 0.256 0.003 0.007 0.004 0.013 0.090
HCRC012 77 78 0.020 0.223 0.006 0.010 0.007 0.013 0.072

19

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC012 78 79 0.016 0.263 0.007 0.006 <0.001 0.015 0.083
HCRC012 79 80 0.198 0.382 0.004 0.009 0.003 0.013 0.113
HCRC012 80 81 0.021 0.081 0.002 0.003 <0.001 0.010 0.026
HCRC012 81 82 0.015 0.012 0.001 0.003 0.001 0.010 0.006
HCRC012 82 83 0.013 0.008 <0.001 0.002 0.001 0.009 0.003
HCRC012 83 84 0.023 0.007 <0.001 0.002 0.003 0.014 0.002
HCRC012 84 85 0.027 0.006 0.001 0.002 0.001 0.014 0.001
HCRC012 85 86 0.010 0.007 0.002 0.002 0.004 0.011 0.002
HCRC012 86 87 0.010 0.005 <0.001 0.002 <0.001 0.013 0.004
HCRC012 87 88 0.044 0.010 0.006 0.007 0.002 0.011 0.012
HCRC012 88 89 0.015 0.006 0.001 0.009 <0.001 0.007 0.003
HCRC012 89 90 0.008 0.005 0.003 0.002 0.011 0.012 0.001
HCRC012 90 91 0.029 0.024 0.006 0.003 <0.001 0.008 0.012
HCRC012 91 92 0.020 0.034 0.010 0.004 0.002 0.011 0.019
HCRC012 92 93 0.035 0.121 0.010 0.008 <0.001 0.011 0.054
HCRC012 93 94 0.047 0.546 0.019 0.025 0.007 0.020 0.175
HCRC012 94 95 0.071 0.312 0.013 0.014 0.003 0.016 0.104
HCRC012 95 96 0.054 0.373 0.017 0.028 <0.001 0.015 0.127
HCRC012 96 97 0.392 0.111 0.023 0.018 0.006 0.011 0.056
HCRC012 97 98 0.579 0.124 0.104 0.027 <0.001 0.007 0.119
HCRC012 98 99 0.086 0.170 0.020 0.012 <0.001 0.013 0.080
HCRC012 99 100 0.055 0.237 0.010 0.009 0.004 0.018 0.094
HCRC013 0 1 0.066 0.046 0.001 0.003 0.002 0.009 0.003
HCRC013 1 2 0.026 0.019 0.002 0.004 0.002 0.009 0.005
HCRC013 2 3 0.028 0.029 <0.001 0.002 <0.001 0.009 0.002
HCRC013 3 4 0.016 0.081 <0.001 0.003 <0.001 0.002 0.003
HCRC013 4 5 0.028 0.111 <0.001 0.003 0.003 0.002 <0.001
HCRC013 5 6 0.025 0.098 0.001 0.007 <0.001 0.006 0.001
HCRC013 6 7 0.094 0.084 0.001 0.006 0.002 0.005 0.002
HCRC013 7 8 0.055 0.077 <0.001 0.006 <0.001 0.005 0.001
HCRC013 8 9 0.115 0.033 0.001 0.009 <0.001 0.007 0.002
HCRC013 9 10 0.048 0.040 0.001 0.009 0.002 0.007 0.002
HCRC013 10 11 0.061 0.021 0.001 0.026 <0.001 0.007 0.001
HCRC013 11 12 0.087 0.041 0.002 0.051 <0.001 0.006 0.002
HCRC013 12 13 0.215 0.031 0.003 0.014 <0.001 0.009 <0.001
HCRC013 13 14 0.287 0.023 0.001 0.019 0.006 0.008 0.003
HCRC013 14 15 0.061 0.051 <0.001 0.014 <0.001 0.006 <0.001
HCRC013 15 16 0.228 0.113 0.001 0.013 <0.001 0.008 0.002
HCRC013 16 17 0.035 0.169 <0.001 0.009 <0.001 0.003 0.012
HCRC013 17 18 0.018 0.156 0.002 0.010 <0.001 0.009 0.006
HCRC013 18 19 0.040 0.121 0.001 0.009 <0.001 0.009 0.003
HCRC013 19 20 0.024 0.129 <0.001 0.014 <0.001 0.005 0.002
HCRC013 20 21 0.013 0.051 <0.001 0.004 0.003 0.002 <0.001
HCRC013 21 22 0.010 0.038 <0.001 0.003 0.005 0.002 <0.001
HCRC013 22 23 0.010 0.042 0.001 0.004 <0.001 0.003 <0.001
HCRC013 23 24 0.009 0.041 0.003 0.003 <0.001 0.005 <0.001
HCRC013 24 25 0.017 0.048 0.002 0.004 0.001 0.003 <0.001
HCRC013 25 26 0.021 0.088 0.001 0.010 <0.001 0.009 <0.001
HCRC013 26 27 0.046 0.012 <0.001 0.013 <0.001 0.007 <0.001
HCRC013 27 28 0.013 0.012 0.001 0.010 <0.001 0.003 <0.001
HCRC013 28 29 0.011 0.014 <0.001 0.018 <0.001 0.012 <0.001
HCRC013 29 30 0.012 0.017 0.001 0.022 <0.001 0.008 <0.001
HCRC013 30 31 0.015 0.018 <0.001 0.009 0.001 0.007 <0.001

20

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC013 31 32 0.008 0.017 0.001 0.007 <0.001 0.011 <0.001
HCRC013 32 33 0.009 0.016 0.003 0.010 0.004 0.007 <0.001
HCRC013 33 34 0.006 0.014 <0.001 0.003 <0.001 0.008 <0.001
HCRC013 34 35 0.006 0.008 <0.001 0.012 <0.001 0.006 <0.001
HCRC013 35 36 0.008 0.005 <0.001 0.008 <0.001 0.005 <0.001
HCRC013 36 37 0.011 0.003 <0.001 0.004 <0.001 0.005 <0.001
HCRC013 37 38 0.009 0.003 <0.001 0.003 <0.001 0.002 <0.001
HCRC013 38 39 0.028 0.005 0.002 0.009 0.002 0.006 <0.001
HCRC013 39 40 0.022 0.010 0.003 0.014 <0.001 0.006 <0.001
HCRC013 40 41 0.019 0.009 0.001 0.008 <0.001 0.006 <0.001
HCRC013 41 42 0.046 0.010 0.001 0.016 <0.001 0.008 0.001
HCRC013 42 43 0.015 0.033 0.002 0.008 0.002 0.006 <0.001
HCRC013 43 44 0.027 0.045 0.005 0.010 0.003 0.020 <0.001
HCRC013 44 45 0.031 0.051 0.002 0.009 0.001 0.009 0.001
HCRC013 45 46 0.073 0.030 0.001 0.003 <0.001 0.012 0.002
HCRC013 46 47 0.028 0.010 0.001 0.003 <0.001 0.006 0.002
HCRC013 47 48 0.013 0.003 <0.001 0.008 <0.001 0.004 0.003
HCRC013 48 49 0.027 0.003 0.001 0.003 <0.001 0.006 0.002
HCRC013 49 50 0.016 0.082 0.003 0.007 <0.001 0.008 0.029
HCRC013 50 51 0.015 0.039 <0.001 0.007 <0.001 0.005 0.018
HCRC013 51 52 0.008 0.046 0.003 0.005 <0.001 0.006 0.018
HCRC013 52 53 0.007 0.008 0.001 0.006 <0.001 0.002 0.005
HCRC013 53 54 0.006 0.033 0.002 0.007 <0.001 0.005 0.014
HCRC013 54 55 0.011 0.031 0.001 0.005 <0.001 0.004 0.014
HCRC013 55 56 0.398 0.121 0.007 0.013 <0.001 0.009 0.037
HCRC013 56 57 0.133 0.274 0.004 0.028 <0.001 0.013 0.069
HCRC013 57 58 0.238 0.109 0.006 0.151 0.002 0.009 0.027
HCRC013 58 59 2.868 0.084 0.010 0.144 <0.001 0.007 0.007
HCRC013 59 60 0.617 0.144 0.006 0.049 0.003 0.008 0.006
HCRC013 60 61 0.148 0.102 0.005 0.007 <0.001 0.012 0.010
HCRC013 61 62 0.078 0.142 0.005 0.030 0.005 0.014 0.034
HCRC013 62 63 0.053 0.048 0.005 0.004 <0.001 0.006 <0.001
HCRC013 63 64 0.215 0.028 0.009 0.092 0.001 0.008 0.008
HCRC013 64 65 0.030 0.054 0.003 0.005 0.001 0.006 0.011
HCRC013 65 66 0.097 0.215 0.007 0.021 <0.001 0.013 0.057
HCRC013 66 67 0.029 0.418 0.004 0.022 <0.001 0.010 0.098
HCRC013 67 68 0.034 0.078 0.002 0.005 <0.001 0.007 0.015
HCRC013 68 69 0.205 0.053 0.031 0.006 0.001 0.006 0.032
HCRC013 69 70 0.139 0.064 0.004 0.020 0.001 0.014 0.014
HCRC013 70 71 0.121 0.032 0.011 0.005 <0.001 0.009 0.014
HCRC013 71 72 0.076 0.011 0.003 0.003 <0.001 0.010 0.009
HCRC013 72 73 0.008 0.014 0.005 0.004 <0.001 0.006 0.009
HCRC013 73 74 0.009 0.012 0.003 0.002 0.001 0.004 0.005
HCRC013 74 75 0.010 0.232 0.003 0.020 <0.001 0.005 0.074
HCRC013 75 76 0.015 0.028 <0.001 0.003 <0.001 0.006 0.009
HCRC013 76 77 0.772 0.014 0.020 0.007 <0.001 0.009 0.018
HCRC013 77 78 0.042 0.012 0.002 0.010 <0.001 0.008 0.004
HCRC013 78 79 0.938 0.017 0.027 0.007 0.002 0.005 0.016
HCRC013 79 80 0.148 0.121 0.007 0.014 <0.001 0.012 0.053
HCRC013 80 81 0.042 0.232 0.009 0.015 0.001 0.011 0.113
HCRC013 81 82 0.049 0.050 0.007 0.005 <0.001 0.006 0.029
HCRC013 82 83 0.032 0.084 0.028 0.005 <0.001 0.013 0.063
HCRC013 83 84 0.017 0.171 0.004 0.011 <0.001 0.016 0.116

21

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC013 84 85 0.142 0.087 0.008 0.011 0.005 0.015 0.059
HCRC013 85 86 0.190 0.040 0.019 0.007 <0.001 0.009 0.056
HCRC013 86 87 0.119 0.094 0.007 0.004 0.004 0.010 0.108
HCRC013 87 88 0.062 0.092 0.032 0.015 <0.001 0.013 0.095
HCRC013 88 89 0.073 0.262 0.008 0.010 0.001 0.014 0.243
HCRC013 89 90 0.285 0.121 0.005 0.010 <0.001 0.008 0.129
HCRC013 90 91 0.037 0.054 <0.001 0.006 0.002 0.005 0.061
HCRC013 91 92 0.044 0.198 0.003 0.015 <0.001 0.012 0.186
HCRC013 92 93 0.094 0.140 0.002 0.022 0.001 0.015 0.146
HCRC013 93 94 0.037 0.174 0.007 0.028 <0.001 0.014 0.199
HCRC013 94 95 0.102 0.122 0.007 0.014 <0.001 0.010 0.147
HCRC013 95 96 0.117 0.197 0.012 0.012 <0.001 0.011 0.223
HCRC013 96 97 0.068 0.166 0.026 0.014 0.002 0.011 0.145
HCRC013 97 98 0.048 0.094 0.014 0.009 <0.001 0.015 0.066
HCRC013 98 99 0.237 0.265 0.012 0.020 <0.001 0.012 0.118
HCRC013 99 100 0.034 0.095 0.004 0.004 <0.001 0.016 0.038
HCRC013 100 101 0.018 0.061 0.002 0.006 0.002 0.012 0.029
HCRC013 101 102 0.040 0.225 0.008 0.014 0.004 0.015 0.078
HCRC013 102 103 0.060 0.265 0.005 0.017 <0.001 0.014 0.084
HCRC013 103 104 0.030 0.121 0.001 0.009 0.003 0.011 0.040
HCRC013 104 105 0.138 0.022 0.008 0.006 0.001 0.012 0.010
HCRC013 105 106 0.113 0.006 0.005 0.004 <0.001 0.007 0.002
HCRC013 106 107 0.018 0.008 <0.001 0.002 0.002 0.007 0.002
HCRC013 107 108 0.010 0.010 0.002 0.002 <0.001 0.008 0.003
HCRC013 108 109 0.012 0.019 0.002 0.003 <0.001 0.014 0.005
HCRC013 109 110 0.007 0.011 0.001 0.001 <0.001 0.006 0.003
HCRC013 110 111 0.014 0.007 <0.001 0.001 <0.001 0.005 0.003
HCRC013 111 112 0.147 0.008 0.002 0.002 <0.001 0.006 0.003
HCRC013 112 113 0.027 0.226 0.006 0.009 0.004 0.013 0.081
HCRC013 113 114 0.025 0.263 0.010 0.016 <0.001 0.011 0.087
HCRC013 114 115 1.982 0.381 0.044 0.027 0.002 0.008 0.160
HCRC013 115 116 0.558 0.781 0.055 0.031 <0.001 0.014 0.272
HCRC013 116 117 0.057 0.092 0.007 0.007 <0.001 0.010 0.050
HCRC013 117 118 0.040 0.011 0.004 0.004 <0.001 0.012 0.003
HCRC013 118 119 0.020 0.023 0.003 0.003 <0.001 0.015 0.001
HCRC013 119 120 0.015 0.018 0.003 0.003 <0.001 0.005 0.001
HCRC014 0 1 0.023 0.004 0.007 0.006 0.005 0.002 0.006
HCRC014 1 2 0.213 0.035 0.003 0.010 <0.001 0.007 0.011
HCRC014 2 3 0.082 0.022 <0.001 0.005 0.005 0.005 0.002
HCRC014 3 4 0.108 0.017 <0.001 0.003 0.004 0.006 <0.001
HCRC014 4 5 0.028 0.065 0.001 0.002 <0.001 0.002 0.017
HCRC014 5 6 0.018 0.047 <0.001 0.003 0.006 0.002 0.007
HCRC014 6 7 0.016 0.066 <0.001 0.002 <0.001 0.002 <0.001
HCRC014 7 8 0.016 0.064 0.002 0.003 0.005 <0.001 <0.001
HCRC014 8 9 0.018 0.040 0.001 0.007 0.005 0.006 <0.001
HCRC014 9 10 0.019 0.037 0.002 0.011 <0.001 0.005 <0.001
HCRC014 10 11 0.013 0.045 0.002 0.013 0.002 0.004 <0.001
HCRC014 11 12 0.023 0.039 0.007 0.008 0.002 0.009 0.002
HCRC014 12 13 0.012 0.051 0.005 0.004 0.006 0.002 <0.001
HCRC014 13 14 0.011 0.050 0.003 0.004 0.003 0.002 <0.001
HCRC014 14 15 0.010 0.039 0.001 0.003 <0.001 0.004 0.001
HCRC014 15 16 0.012 0.047 0.001 0.005 0.004 0.002 <0.001
HCRC014 16 17 0.011 0.052 <0.001 0.003 <0.001 0.004 <0.001

22

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC014 17 18 0.008 0.042 <0.001 0.008 0.004 0.002 <0.001
HCRC014 18 19 0.005 0.031 <0.001 0.003 0.006 0.008 <0.001
HCRC014 19 20 0.008 0.037 <0.001 0.002 0.002 0.004 <0.001
HCRC014 20 21 0.010 0.032 0.003 0.001 <0.001 <0.001 <0.001
HCRC014 21 22 0.008 0.023 0.001 0.002 <0.001 0.002 <0.001
HCRC014 22 23 0.005 0.012 <0.001 0.001 <0.001 0.006 <0.001
HCRC014 23 24 0.007 0.004 0.001 0.002 0.001 0.004 <0.001
HCRC014 24 25 0.006 0.002 <0.001 0.002 <0.001 0.003 <0.001
HCRC014 25 26 0.008 0.003 0.003 0.002 <0.001 0.002 <0.001
HCRC014 26 27 0.066 0.013 0.003 0.002 <0.001 0.006 <0.001
HCRC014 27 28 0.043 0.031 0.007 0.004 0.002 0.005 <0.001
HCRC014 28 29 0.060 0.027 0.003 0.002 <0.001 0.005 <0.001
HCRC014 29 30 0.178 0.032 0.004 0.009 <0.001 0.002 <0.001
HCRC014 30 31 0.022 0.039 0.002 0.003 0.002 0.005 <0.001
HCRC014 31 32 0.026 0.079 0.003 0.012 <0.001 0.009 <0.001
HCRC014 32 33 0.055 0.097 0.005 0.013 <0.001 0.006 <0.001
HCRC014 33 34 0.132 0.046 0.006 0.055 <0.001 0.006 <0.001
HCRC014 34 35 0.089 0.056 0.005 0.030 <0.001 0.004 <0.001
HCRC014 35 36 0.057 0.094 0.003 0.014 0.004 0.010 <0.001
HCRC014 36 37 0.500 0.105 0.005 0.013 0.003 0.009 <0.001
HCRC014 37 38 0.061 0.085 0.003 0.011 <0.001 0.004 <0.001
HCRC014 38 39 0.018 0.104 0.004 0.003 <0.001 0.004 <0.001
HCRC014 39 40 0.021 0.052 0.005 0.003 <0.001 0.006 <0.001
HCRC014 40 41 0.018 0.008 0.004 0.001 <0.001 0.004 <0.001
HCRC014 41 42 0.141 0.005 0.003 0.003 <0.001 <0.001 <0.001
HCRC014 42 43 0.078 0.010 0.005 0.002 <0.001 0.002 <0.001
HCRC014 43 44 0.016 0.077 0.005 0.003 0.003 0.003 <0.001
HCRC014 44 45 0.008 0.030 <0.001 0.002 0.004 0.002 <0.001
HCRC014 45 46 0.008 0.009 0.001 0.003 <0.001 0.007 0.002
HCRC014 46 47 0.014 0.004 0.003 0.011 <0.001 0.003 0.003
HCRC014 47 48 0.023 0.003 0.004 0.062 <0.001 0.007 0.004
HCRC014 48 49 0.017 0.015 0.003 0.026 0.001 0.010 0.003
HCRC014 49 50 0.020 0.103 0.004 0.012 <0.001 0.011 0.001
HCRC014 50 51 0.010 0.015 <0.001 0.006 <0.001 0.003 0.002
HCRC014 51 52 0.009 0.010 0.001 0.028 <0.001 0.005 0.006
HCRC014 52 53 0.016 0.008 0.002 0.024 0.002 0.005 0.007
HCRC014 53 54 0.023 0.010 0.002 0.008 <0.001 0.002 0.004
HCRC014 54 55 0.038 0.016 0.002 0.025 <0.001 0.007 0.005
HCRC014 55 56 0.034 0.006 <0.001 0.037 <0.001 0.008 0.004
HCRC014 56 57 0.045 0.009 0.001 0.040 <0.001 0.008 0.003
HCRC014 57 58 0.015 0.007 0.003 0.019 <0.001 0.002 0.003
HCRC014 58 59 0.015 0.009 0.001 0.017 0.007 0.010 0.002
HCRC014 59 60 0.025 0.009 0.002 0.009 0.001 0.003 0.002
HCRC014 60 61 0.088 0.020 0.005 0.024 <0.001 0.009 0.012
HCRC014 61 62 0.018 0.057 0.002 0.011 <0.001 0.010 0.023
HCRC014 62 63 0.015 0.042 0.003 0.005 <0.001 0.003 0.016
HCRC014 63 64 0.138 0.067 0.005 0.005 <0.001 0.003 0.026
HCRC014 64 65 0.718 0.217 0.003 0.008 0.002 0.006 0.071
HCRC014 65 66 0.388 0.144 0.005 0.009 <0.001 0.006 0.055
HCRC014 66 67 0.062 0.084 0.003 0.008 <0.001 0.004 0.032
HCRC014 67 68 0.016 0.109 0.003 0.006 <0.001 0.006 0.035
HCRC014 68 69 0.025 0.102 0.002 0.008 <0.001 0.004 0.032
HCRC014 69 70 0.147 0.899 0.007 0.058 0.004 0.003 0.251

23

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC014 70 71 0.242 0.420 0.005 0.026 <0.001 0.007 0.129
HCRC014 71 72 0.142 0.191 0.002 0.011 0.003 0.006 0.067
HCRC014 72 73 0.027 0.209 0.002 0.013 <0.001 0.006 0.067
HCRC014 73 74 0.141 0.143 0.002 0.012 0.003 0.002 0.043
HCRC014 74 75 0.031 0.179 0.011 0.014 <0.001 0.008 0.061
HCRC014 75 76 0.011 0.023 0.003 0.004 <0.001 0.006 0.009
HCRC014 76 77 0.008 0.004 0.003 0.002 0.006 0.005 0.013
HCRC014 77 78 0.006 0.018 0.005 0.009 <0.001 <0.001 0.012
HCRC014 78 79 0.007 0.027 0.001 0.007 <0.001 0.006 0.014
HCRC014 79 80 0.014 0.024 0.003 0.005 <0.001 0.004 0.015
HCRC014 80 81 0.035 0.121 <0.001 0.006 <0.001 0.007 0.041
HCRC014 81 82 0.096 0.097 0.012 0.012 <0.001 0.008 0.047
HCRC014 82 83 0.018 0.025 0.003 0.006 <0.001 0.005 0.015
HCRC014 83 84 0.010 0.006 0.001 0.003 0.001 0.005 0.004
HCRC014 84 85 0.128 0.003 0.003 0.004 <0.001 0.003 0.004
HCRC014 85 86 0.099 0.039 0.002 0.004 0.002 0.009 0.017
HCRC014 86 87 0.448 0.023 0.009 0.007 <0.001 0.010 0.011
HCRC014 87 88 0.104 0.150 0.054 0.005 0.001 0.011 0.097
HCRC014 88 89 0.321 0.289 0.042 0.016 0.005 0.014 0.151
HCRC014 89 90 0.388 0.236 0.011 0.027 <0.001 0.009 0.103
HCRC014 90 91 0.615 0.137 0.006 0.016 0.003 0.011 0.055
HCRC014 91 92 0.089 0.046 0.002 0.014 <0.001 0.009 0.022
HCRC014 92 93 1.507 0.079 0.019 0.021 0.005 0.012 0.045
HCRC014 93 94 0.220 0.008 0.006 0.006 0.004 0.005 0.009
HCRC014 94 95 0.096 0.004 0.003 0.003 <0.001 0.008 0.004
HCRC014 95 96 0.528 0.008 0.013 0.005 0.004 0.010 0.008
HCRC014 96 97 0.285 0.164 0.025 0.013 0.010 0.013 0.091
HCRC014 97 98 0.198 0.305 0.062 0.017 0.005 0.011 0.189
HCRC014 98 99 0.061 0.048 0.012 0.007 0.003 0.009 0.027
HCRC014 99 100 0.333 0.069 0.005 0.068 <0.001 0.010 0.038
HCRC014 100 101 0.036 0.015 0.005 0.006 0.001 0.012 0.005
HCRC014 101 102 0.023 0.010 0.003 0.004 <0.001 0.011 0.005
HCRC014 102 103 0.020 0.009 0.003 0.002 0.004 0.014 0.038
HCRC014 103 104 0.095 0.046 0.087 0.003 <0.001 0.011 0.096
HCRC014 104 105 0.071 0.076 0.023 0.004 <0.001 0.010 0.054
HCRC014 105 106 0.106 0.164 0.012 0.020 <0.001 0.011 0.078
HCRC014 106 107 0.494 0.693 0.026 0.156 0.003 0.010 0.289
HCRC014 107 108 0.160 0.094 0.006 0.026 <0.001 0.009 0.039
HCRC014 108 109 0.051 0.042 0.003 0.008 <0.001 0.009 0.020
HCRC014 109 110 0.973 0.433 0.014 0.006 <0.001 0.015 0.186
HCRC014 110 111 0.228 0.072 0.005 0.002 0.005 0.008 0.033
HCRC014 111 112 0.061 0.050 0.014 0.006 <0.001 0.009 0.038
HCRC014 112 113 2.380 0.031 0.220 0.003 0.004 0.009 0.177
HCRC014 113 114 1.056 0.110 0.199 0.003 <0.001 0.006 0.225
HCRC014 114 115 0.199 0.101 0.116 0.012 0.002 0.014 0.194
HCRC014 115 116 0.101 0.083 0.024 0.018 <0.001 0.013 0.096
HCRC014 116 117 0.035 0.025 0.006 0.006 <0.001 0.009 0.028
HCRC014 117 118 0.048 0.085 0.023 0.007 <0.001 0.009 0.086
HCRC014 118 119 0.038 0.048 0.006 0.008 <0.001 0.011 0.034
HCRC014 119 120 0.087 0.027 0.010 0.004 <0.001 0.010 0.023
HCRC015 0 1 0.019 0.006 <0.001 0.002 <0.001 0.007 <0.001
HCRC015 1 2 0.019 0.019 <0.001 0.002 0.001 0.007 0.006
HCRC015 2 3 0.011 0.017 <0.001 0.002 0.002 0.006 0.014

24

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC015 3 4 0.008 0.017 <0.001 <0.001 <0.001 0.009 0.005
HCRC015 4 5 0.025 0.011 <0.001 0.001 <0.001 0.004 0.005
HCRC015 5 6 0.040 0.015 0.003 0.002 <0.001 0.014 <0.001
HCRC015 6 7 0.014 0.019 <0.001 0.001 <0.001 0.005 0.006
HCRC015 7 8 0.043 0.011 0.001 0.004 <0.001 0.024 0.005
HCRC015 8 9 0.021 0.008 <0.001 0.002 <0.001 0.011 0.001
HCRC015 9 10 0.024 0.007 <0.001 0.003 <0.001 0.011 0.002
HCRC015 10 11 0.026 0.010 <0.001 0.001 <0.001 0.011 <0.001
HCRC015 11 12 0.034 0.009 <0.001 0.004 <0.001 0.006 0.001
HCRC015 12 13 0.036 0.012 <0.001 0.004 0.002 0.005 0.003
HCRC015 13 14 0.023 0.010 <0.001 0.003 <0.001 0.011 0.002
HCRC015 14 15 0.021 0.013 <0.001 0.002 <0.001 0.008 <0.001
HCRC015 15 16 0.035 0.013 <0.001 0.004 <0.001 0.008 <0.001
HCRC015 16 17 0.023 0.011 <0.001 0.002 <0.001 0.006 <0.001
HCRC015 17 18 0.023 0.017 <0.001 0.002 0.004 0.002 <0.001
HCRC015 18 19 0.028 0.016 <0.001 0.002 0.003 0.007 <0.001
HCRC015 19 20 0.034 0.022 <0.001 0.001 <0.001 0.008 <0.001
HCRC015 20 21 0.038 0.022 <0.001 0.003 <0.001 0.008 <0.001
HCRC015 21 22 0.108 0.034 <0.001 0.004 <0.001 0.008 0.002
HCRC015 22 23 0.094 0.029 0.002 0.004 <0.001 0.010 <0.001
HCRC015 23 24 0.163 0.013 <0.001 0.007 <0.001 0.010 <0.001
HCRC015 24 25 0.244 0.013 0.002 0.008 <0.001 0.004 <0.001
HCRC015 25 26 0.085 0.023 <0.001 0.008 <0.001 0.010 <0.001
HCRC015 26 27 0.134 0.030 0.001 0.007 <0.001 0.087 <0.001
HCRC015 27 28 0.030 0.012 0.001 0.011 <0.001 0.005 <0.001
HCRC015 28 29 0.027 0.010 <0.001 0.002 0.004 0.007 <0.001
HCRC015 29 30 0.856 0.011 0.010 0.006 <0.001 0.006 0.004
HCRC015 30 31 1.345 0.011 0.008 0.004 <0.001 0.010 0.005
HCRC015 31 32 0.217 0.007 0.003 0.003 <0.001 0.006 0.004
HCRC015 32 33 0.021 0.007 <0.001 0.003 <0.001 0.009 0.006
HCRC015 33 34 0.032 0.005 0.001 0.002 <0.001 0.006 0.004
HCRC015 34 35 0.013 0.007 <0.001 0.002 0.006 0.003 0.002
HCRC015 35 36 0.022 0.005 <0.001 0.003 0.001 0.002 0.005
HCRC015 36 37 0.033 0.005 0.001 0.003 <0.001 0.009 0.008
HCRC015 37 38 0.013 0.004 <0.001 0.002 <0.001 0.005 0.002
HCRC015 38 39 0.016 0.007 0.002 0.001 <0.001 0.008 <0.001
HCRC015 39 40 0.024 0.002 <0.001 0.002 <0.001 0.007 <0.001
HCRC015 40 41 0.023 0.011 <0.001 0.002 <0.001 0.005 <0.001
HCRC015 41 42 0.028 0.004 <0.001 0.003 0.003 0.005 <0.001
HCRC015 42 43 0.017 0.006 <0.001 0.016 <0.001 0.005 <0.001
HCRC015 43 44 0.026 0.018 <0.001 0.004 <0.001 0.004 <0.001
HCRC015 44 45 0.040 0.022 <0.001 0.003 0.002 0.010 <0.001
HCRC015 45 46 0.013 0.004 <0.001 0.002 <0.001 0.004 <0.001
HCRC015 46 47 0.012 0.007 <0.001 0.001 <0.001 0.007 <0.001
HCRC015 47 48 0.013 0.004 <0.001 <0.001 <0.001 0.005 <0.001
HCRC015 48 49 0.011 0.003 <0.001 0.002 0.001 0.005 <0.001
HCRC015 49 50 0.008 0.002 <0.001 0.002 <0.001 0.005 <0.001
HCRC015 50 51 0.017 0.008 <0.001 0.003 <0.001 0.005 <0.001
HCRC015 51 52 0.028 0.006 <0.001 0.002 <0.001 0.006 <0.001
HCRC015 52 53 0.025 0.011 <0.001 0.003 <0.001 0.005 <0.001
HCRC015 53 54 0.023 0.008 <0.001 0.003 <0.001 0.002 <0.001
HCRC015 54 55 0.023 0.008 <0.001 0.004 <0.001 0.005 <0.001
HCRC015 55 56 0.010 0.007 <0.001 0.003 <0.001 0.003 <0.001

25

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC015 56 57 0.040 0.003 <0.001 0.002 <0.001 0.006 <0.001
HCRC015 57 58 0.012 0.002 <0.001 0.001 0.002 0.004 <0.001
HCRC015 58 59 0.006 0.002 <0.001 <0.001 <0.001 0.003 <0.001
HCRC015 59 60 0.042 0.003 <0.001 0.003 <0.001 0.004 0.001
HCRC015 60 61 0.018 0.003 <0.001 0.003 <0.001 0.004 0.002
HCRC015 61 62 0.008 0.003 <0.001 0.002 <0.001 0.002 0.001
HCRC015 62 63 0.006 0.002 <0.001 0.001 <0.001 0.004 0.001
HCRC015 63 64 0.016 0.011 <0.001 0.003 0.005 0.010 <0.001
HCRC015 64 65 0.009 0.004 0.001 0.002 <0.001 0.003 0.001
HCRC015 65 66 0.007 0.002 <0.001 0.002 <0.001 0.006 <0.001
HCRC015 66 67 0.012 0.006 <0.001 0.001 <0.001 0.002 0.003
HCRC015 67 68 0.011 0.005 <0.001 0.002 <0.001 0.017 <0.001
HCRC015 68 69 0.009 0.002 <0.001 0.001 <0.001 0.004 <0.001
HCRC015 69 70 0.016 0.003 <0.001 0.001 <0.001 0.002 <0.001
HCRC015 70 71 0.006 <0.001 <0.001 0.003 0.004 0.003 <0.001
HCRC015 71 72 0.006 0.002 <0.001 0.001 <0.001 0.002 <0.001
HCRC015 72 73 0.011 0.010 <0.001 0.001 0.002 0.009 <0.001
HCRC015 73 74 0.009 0.005 <0.001 0.002 <0.001 0.005 <0.001
HCRC015 74 75 0.023 0.011 <0.001 0.032 <0.001 0.008 <0.001
HCRC015 75 76 0.017 0.005 <0.001 0.022 <0.001 0.013 <0.001
HCRC015 76 77 0.041 0.015 <0.001 0.027 <0.001 0.011 <0.001
HCRC015 77 78 0.067 0.016 <0.001 0.024 <0.001 0.010 <0.001
HCRC015 78 79 0.020 0.008 <0.001 0.006 <0.001 0.005 <0.001
HCRC015 79 80 0.016 0.004 <0.001 0.002 0.003 0.002 <0.001
HCRC015 80 81 0.028 0.011 <0.001 0.002 <0.001 0.003 <0.001
HCRC015 81 82 0.014 0.008 <0.001 0.001 <0.001 <0.001 <0.001
HCRC015 82 83 0.015 0.011 <0.001 0.007 0.003 0.006 <0.001
HCRC015 83 84 0.018 0.019 <0.001 0.004 <0.001 0.021 <0.001
HCRC015 84 85 0.008 <0.001 <0.001 0.002 0.001 0.005 <0.001
HCRC015 85 86 0.005 0.002 <0.001 0.001 0.002 0.003 <0.001
HCRC015 86 87 0.009 <0.001 <0.001 0.002 <0.001 0.004 <0.001
HCRC015 87 88 0.006 0.006 <0.001 0.004 <0.001 <0.001 <0.001
HCRC015 88 89 0.008 0.056 <0.001 0.002 <0.001 <0.001 <0.001
HCRC015 89 90 0.009 0.035 <0.001 0.002 <0.001 0.003 <0.001
HCRC015 90 91 0.026 0.034 <0.001 0.004 0.001 0.003 0.008
HCRC015 91 92 0.011 0.038 <0.001 0.002 0.003 0.004 <0.001
HCRC015 92 93 0.018 0.028 <0.001 0.003 0.002 0.005 <0.001
HCRC015 93 94 0.011 0.041 <0.001 0.016 0.002 0.009 <0.001
HCRC015 94 95 0.009 0.012 <0.001 0.014 0.003 0.005 <0.001
HCRC015 95 96 0.009 0.005 <0.001 0.011 <0.001 0.002 <0.001
HCRC015 96 97 0.009 0.003 <0.001 0.006 <0.001 0.002 <0.001
HCRC015 97 98 0.024 0.003 <0.001 0.004 <0.001 0.002 <0.001
HCRC015 98 99 0.011 0.004 <0.001 0.008 <0.001 0.006 0.003
HCRC015 99 100 0.009 0.007 <0.001 0.004 <0.001 0.006 0.001
HCRC015 100 101 0.021 0.003 0.001 0.001 <0.001 0.007 <0.001
HCRC015 101 102 0.006 0.005 <0.001 <0.001 <0.001 0.004 0.001
HCRC015 102 103 0.006 0.008 <0.001 <0.001 0.003 0.004 <0.001
HCRC015 103 104 0.010 0.005 <0.001 0.002 <0.001 0.010 <0.001
HCRC015 104 105 0.005 0.007 <0.001 <0.001 <0.001 0.009 <0.001
HCRC015 105 106 0.006 0.007 <0.001 0.001 0.001 0.008 <0.001
HCRC015 106 107 0.007 0.003 <0.001 0.003 <0.001 0.009 <0.001
HCRC015 107 108 0.008 0.008 <0.001 0.002 <0.001 0.009 <0.001
HCRC015 108 109 0.010 0.006 <0.001 0.003 <0.001 0.006 <0.001

26

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC015 109 110 0.005 <0.001 <0.001 <0.001 0.002 0.002 <0.001
HCRC015 110 111 0.010 0.006 <0.001 0.004 <0.001 0.002 0.001
HCRC015 111 112 0.010 0.002 <0.001 0.001 <0.001 0.006 <0.001
HCRC015 112 113 0.010 0.004 <0.001 0.003 <0.001 0.004 <0.001
HCRC015 113 114 0.005 0.002 <0.001 0.001 <0.001 0.003 <0.001
HCRC015 114 115 0.007 0.007 <0.001 0.003 <0.001 0.006 0.004
HCRC015 115 116 0.011 0.006 0.001 0.003 0.004 0.006 0.001
HCRC015 116 117 0.005 0.003 <0.001 0.002 0.002 0.006 <0.001
HCRC015 117 118 0.014 0.002 <0.001 <0.001 0.002 0.004 <0.001
HCRC015 118 119 0.007 0.003 <0.001 0.001 0.001 0.005 <0.001
HCRC015 119 120 0.003 0.003 <0.001 0.001 <0.001 0.004 <0.001
HCRC016 0 1 No Sample
HCRC016 1 2 0.012 0.005 <0.001 0.002 <0.001 0.007 <0.001
HCRC016 2 3 0.013 0.007 <0.001 0.001 0.004 0.007 0.015
HCRC016 3 4 0.011 0.005 <0.001 0.002 0.005 0.005 0.008
HCRC016 4 5 0.008 0.005 <0.001 0.001 <0.001 0.003 <0.001
HCRC016 5 6 0.010 0.007 <0.001 0.001 0.001 0.006 <0.001
HCRC016 6 7 0.006 0.003 <0.001 0.002 <0.001 0.005 <0.001
HCRC016 7 8 0.011 0.007 <0.001 0.004 <0.001 0.006 <0.001
HCRC016 8 9 0.010 0.009 <0.001 0.003 0.002 0.003 <0.001
HCRC016 9 10 0.009 0.006 <0.001 0.002 <0.001 0.005 <0.001
HCRC016 10 11 0.009 0.003 <0.001 0.002 <0.001 0.003 <0.001
HCRC016 11 12 0.009 0.005 <0.001 0.001 0.004 0.002 <0.001
HCRC016 12 13 0.007 0.003 <0.001 0.002 <0.001 0.002 <0.001
HCRC016 13 14 0.011 0.005 <0.001 0.002 <0.001 0.005 <0.001
HCRC016 14 15 0.012 0.009 <0.001 0.004 0.003 0.003 <0.001
HCRC016 15 16 0.018 0.013 <0.001 0.003 <0.001 0.003 <0.001
HCRC016 16 17 0.013 0.008 <0.001 0.003 <0.001 0.005 <0.001
HCRC016 17 18 0.011 0.008 <0.001 0.003 <0.001 0.003 <0.001
HCRC016 18 19 0.011 0.008 <0.001 0.003 <0.001 0.003 <0.001
HCRC016 19 20 0.023 0.007 <0.001 0.002 <0.001 0.006 <0.001
HCRC016 20 21 0.008 0.003 <0.001 0.002 <0.001 0.005 <0.001
HCRC016 21 22 0.012 0.004 <0.001 0.004 <0.001 0.005 <0.001
HCRC016 22 23 0.008 0.001 <0.001 0.001 <0.001 0.002 <0.001
HCRC016 23 24 0.006 <0.001 <0.001 0.003 0.002 0.006 <0.001
HCRC016 24 25 0.007 0.002 <0.001 0.001 <0.001 0.010 <0.001
HCRC016 25 26 0.008 0.003 <0.001 <0.001 <0.001 0.003 <0.001
HCRC016 26 27 0.008 0.007 <0.001 0.002 <0.001 0.005 <0.001
HCRC016 27 28 0.008 0.005 <0.001 0.002 <0.001 0.005 <0.001
HCRC016 28 29 0.007 0.007 <0.001 0.001 <0.001 0.003 <0.001
HCRC016 29 30 0.015 0.008 <0.001 0.002 0.004 0.003 <0.001
HCRC016 30 31 0.015 0.010 <0.001 0.004 0.004 0.003 <0.001
HCRC016 31 32 0.007 0.004 <0.001 <0.001 <0.001 0.006 <0.001
HCRC016 32 33 0.011 0.001 <0.001 0.002 0.006 0.005 <0.001
HCRC016 33 34 0.006 0.007 <0.001 0.002 <0.001 0.003 <0.001
HCRC016 34 35 0.010 0.021 <0.001 0.004 <0.001 0.002 <0.001
HCRC016 35 36 0.006 0.005 <0.001 0.002 0.002 0.002 <0.001
HCRC016 36 37 0.010 0.013 <0.001 0.003 <0.001 0.002 <0.001
HCRC016 37 38 0.011 0.013 <0.001 0.002 <0.001 <0.001 <0.001
HCRC016 38 39 0.006 0.010 <0.001 0.002 0.004 0.006 <0.001
HCRC016 39 40 0.007 0.005 <0.001 <0.001 0.002 0.006 <0.001
HCRC016 40 41 <0.001 0.005 <0.001 <0.001 <0.001 0.005 <0.001
HCRC016 41 42 0.006 0.007 <0.001 0.003 0.004 0.006 <0.001

27

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC016 42 43 0.006 0.005 <0.001 0.002 0.006 0.005 <0.001
HCRC016 43 44 0.007 0.008 <0.001 0.002 0.008 0.003 <0.001
HCRC016 44 45 0.009 0.016 <0.001 0.002 0.003 0.004 <0.001
HCRC016 45 46 0.007 0.014 <0.001 0.002 <0.001 0.003 <0.001
HCRC016 46 47 0.006 0.014 <0.001 <0.001 <0.001 0.007 <0.001
HCRC016 47 48 0.007 0.001 <0.001 0.003 <0.001 0.006 <0.001
HCRC016 48 49 0.005 0.003 <0.001 0.001 <0.001 <0.001 <0.001
HCRC016 49 50 0.007 0.004 <0.001 0.002 <0.001 0.008 <0.001
HCRC016 50 51 0.008 0.005 <0.001 0.002 <0.001 0.008 <0.001
HCRC016 51 52 0.007 <0.001 <0.001 0.001 <0.001 0.006 <0.001
HCRC016 52 53 0.009 0.010 <0.001 0.003 0.010 0.007 <0.001
HCRC016 53 54 0.006 0.006 <0.001 0.001 <0.001 0.005 <0.001
HCRC016 54 55 0.007 0.008 <0.001 0.009 <0.001 0.004 <0.001
HCRC016 55 56 0.007 0.007 <0.001 0.007 0.006 0.005 <0.001
HCRC016 56 57 0.006 0.008 <0.001 <0.001 <0.001 0.003 <0.001
HCRC016 57 58 0.007 0.012 <0.001 0.002 0.005 0.003 <0.001
HCRC016 58 59 0.007 0.006 <0.001 0.003 0.002 0.002 <0.001
HCRC016 59 60 0.005 0.007 <0.001 <0.001 <0.001 <0.001 <0.001
HCRC016 60 61 0.005 0.009 <0.001 0.002 <0.001 0.002 <0.001
HCRC016 61 62 0.006 0.005 <0.001 0.016 0.002 0.002 <0.001
HCRC016 62 63 0.011 0.013 <0.001 0.037 0.003 0.007 <0.001
HCRC016 63 64 0.008 0.011 <0.001 0.053 <0.001 <0.001 <0.001
HCRC016 64 65 0.018 0.025 <0.001 0.146 0.003 0.006 <0.001
HCRC016 65 66 0.018 0.021 <0.001 0.028 0.002 0.006 <0.001
HCRC016 66 67 0.008 0.013 <0.001 0.012 0.001 0.003 <0.001
HCRC016 67 68 0.005 0.010 <0.001 0.001 <0.001 <0.001 <0.001
HCRC016 68 69 0.009 0.010 <0.001 0.004 0.005 0.002 <0.001
HCRC016 69 70 0.010 0.012 <0.001 0.018 0.006 0.006 <0.001
HCRC016 70 71 0.313 0.009 0.001 0.004 <0.001 0.002 <0.001
HCRC016 71 72 0.028 0.011 <0.001 0.004 0.002 <0.001 <0.001
HCRC016 72 73 0.010 0.011 <0.001 0.004 <0.001 0.005 <0.001
HCRC016 73 74 0.006 0.009 <0.001 0.003 <0.001 0.004 <0.001
HCRC016 74 75 0.010 0.009 <0.001 0.009 <0.001 0.004 <0.001
HCRC016 75 76 0.009 0.013 <0.001 0.023 0.004 0.006 0.001
HCRC016 76 77 0.015 0.005 <0.001 0.008 <0.001 0.006 <0.001
HCRC016 77 78 0.010 0.012 <0.001 0.013 <0.001 0.003 <0.001
HCRC016 78 79 0.009 0.009 0.001 0.022 <0.001 0.005 0.003
HCRC016 79 80 0.005 <0.001 <0.001 0.004 <0.001 0.003 <0.001
HCRC016 80 81 0.017 0.004 <0.001 0.009 0.004 0.004 <0.001
HCRC016 81 82 0.123 0.003 <0.001 0.012 <0.001 0.007 <0.001
HCRC016 82 83 1.257 0.006 <0.001 0.010 <0.001 <0.001 <0.001
HCRC016 83 84 0.073 0.004 <0.001 0.008 <0.001 0.002 <0.001
HCRC016 84 85 0.022 0.008 <0.001 <0.001 <0.001 0.004 <0.001
HCRC016 85 86 0.009 <0.001 <0.001 0.002 <0.001 0.004 <0.001
HCRC016 86 87 3.533 0.006 0.027 0.008 <0.001 0.010 0.001
HCRC016 87 88 0.118 0.010 <0.001 0.002 0.001 0.010 <0.001
HCRC016 88 89 0.019 0.010 0.001 0.004 <0.001 0.009 <0.001
HCRC016 89 90 0.020 0.011 <0.001 0.002 <0.001 0.009 <0.001
HCRC016 90 91 0.030 0.008 0.010 0.005 0.005 0.010 <0.001
HCRC016 91 92 0.019 0.012 <0.001 0.004 <0.001 0.009 <0.001
HCRC016 92 93 0.076 0.008 0.008 0.009 <0.001 0.015 0.001
HCRC016 93 94 0.018 0.013 <0.001 0.003 <0.001 0.008 <0.001
HCRC016 94 95 0.010 0.005 <0.001 0.003 0.001 0.006 <0.001

28

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC016 95 96 0.013 0.005 <0.001 0.002 <0.001 0.005 <0.001
HCRC016 96 97 0.007 <0.001 <0.001 <0.001 0.003 0.004 <0.001
HCRC016 97 98 0.008 0.005 <0.001 <0.001 0.001 0.007 <0.001
HCRC016 98 99 0.009 0.004 <0.001 <0.001 0.004 0.002 <0.001
HCRC016 99 100 0.009 0.007 <0.001 <0.001 <0.001 0.005 <0.001
HCRC016 100 101 0.013 0.011 <0.001 0.003 <0.001 0.004 <0.001
HCRC016 101 102 0.016 0.009 <0.001 0.002 <0.001 0.006 <0.001
HCRC016 102 103 0.016 0.008 <0.001 0.003 <0.001 0.008 <0.001
HCRC016 103 104 0.009 0.004 <0.001 0.003 <0.001 0.006 <0.001
HCRC016 104 105 0.006 0.002 <0.001 0.003 <0.001 0.002 <0.001
HCRC016 105 106 0.021 0.013 <0.001 0.003 <0.001 0.006 <0.001
HCRC016 106 107 0.008 0.012 <0.001 0.004 <0.001 0.003 <0.001
HCRC016 107 108 0.005 0.008 <0.001 0.004 0.004 0.003 <0.001
HCRC016 108 109 0.005 0.007 <0.001 0.002 <0.001 0.006 0.001
HCRC016 109 110 0.006 0.010 <0.001 0.002 0.003 0.006 <0.001
HCRC016 110 111 0.005 0.008 <0.001 0.002 0.004 0.002 0.001
HCRC016 111 112 0.006 0.005 <0.001 0.002 0.002 <0.001 0.001
HCRC016 112 113 0.005 0.009 <0.001 0.002 <0.001 0.002 <0.001
HCRC016 113 114 0.007 0.005 <0.001 0.004 <0.001 0.006 <0.001
HCRC016 114 115 0.041 0.011 0.001 0.017 <0.001 0.005 <0.001
HCRC016 115 116 0.009 0.016 <0.001 0.014 0.001 0.006 <0.001
HCRC016 116 117 0.009 0.010 <0.001 0.008 0.001 0.008 <0.001
HCRC016 117 118 0.007 0.008 <0.001 0.002 0.004 0.005 <0.001
HCRC016 118 119 0.006 0.007 <0.001 0.002 0.003 0.003 <0.001
HCRC016 119 120 0.016 0.005 <0.001 0.002 <0.001 0.003 0.002
HCRC016 120 121 0.005 0.003 <0.001 0.002 <0.001 0.003 0.002
HCRC016 121 122 0.006 0.001 <0.001 0.003 <0.001 0.004 0.002
HCRC016 122 123 0.004 <0.001 <0.001 0.002 0.008 0.005 0.001
HCRC016 123 124 0.004 0.001 <0.001 0.001 <0.001 0.002 0.002
HCRC016 124 125 0.014 0.002 <0.001 0.002 <0.001 0.005 <0.001
HCRC016 125 126 0.014 0.005 <0.001 0.005 0.006 0.004 <0.001
HCRC016 126 127 0.107 0.082 <0.001 0.005 <0.001 0.004 0.026
HCRC016 127 128 3.145 0.048 0.014 0.009 <0.001 0.035 0.021
HCRC016 128 129 0.421 0.017 0.003 0.006 0.002 0.012 0.007
HCRC016 129 130 0.025 0.007 0.001 0.003 <0.001 0.010 0.001
HCRC016 130 131 0.013 0.005 <0.001 0.011 0.004 0.005 0.001
HCRC016 131 132 0.216 0.006 0.002 0.016 0.003 0.006 0.001
HCRC016 132 133 0.022 0.004 <0.001 0.008 <0.001 0.006 <0.001
HCRC016 133 134 0.007 0.007 <0.001 0.015 0.002 0.010 0.001
HCRC016 134 135 0.006 0.004 <0.001 0.005 <0.001 0.008 0.003
HCRC016 135 136 0.011 0.005 <0.001 0.016 <0.001 0.009 0.002
HCRC016 136 137 0.008 0.093 <0.001 0.008 <0.001 0.005 0.028
HCRC016 137 138 0.005 0.003 <0.001 0.006 0.001 0.002 <0.001
HCRC016 138 139 0.011 0.004 <0.001 0.066 <0.001 0.009 0.001
HCRC016 139 140 0.345 0.079 0.012 0.009 <0.001 0.006 0.029
HCRC016 140 141 0.029 0.341 0.003 0.007 <0.001 0.007 0.098
HCRC016 141 142 0.008 0.004 <0.001 0.012 <0.001 0.003 0.002
HCRC016 142 143 0.016 0.006 <0.001 0.005 0.002 0.007 0.002
HCRC016 143 144 0.386 0.003 0.011 0.009 <0.001 0.006 0.005
HCRC016 144 145 0.020 <0.001 <0.001 0.005 0.003 0.002 <0.001
HCRC016 145 146 0.005 0.004 <0.001 0.004 0.003 0.007 0.002
HCRC016 146 147 0.007 0.001 <0.001 0.002 <0.001 0.006 <0.001
HCRC016 147 148 0.007 0.003 <0.001 0.002 <0.001 0.003 <0.001

29

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC016 148 149 0.003 <0.001 <0.001 0.003 <0.001 0.004 <0.001
HCRC016 149 150 0.005 0.002 <0.001 0.003 <0.001 0.010 <0.001
HCRC017 0 1 No Sample
HCRC017 1 2 0.041 0.024 0.001 0.001 <0.001 0.005 <0.001
HCRC017 2 3 0.012 0.034 <0.001 0.001 <0.001 <0.001 0.016
HCRC017 3 4 0.021 0.038 0.002 0.002 0.001 0.002 0.003
HCRC017 4 5 0.016 0.041 <0.001 0.002 <0.001 0.006 0.001
HCRC017 5 6 0.026 0.022 <0.001 0.009 0.002 0.004 <0.001
HCRC017 6 7 0.733 0.254 0.004 0.006 <0.001 0.011 0.007
HCRC017 7 8 0.089 0.310 0.003 0.015 0.001 0.018 0.017
HCRC017 8 9 0.035 0.130 0.001 0.005 <0.001 0.013 0.003
HCRC017 9 10 0.035 0.086 0.002 0.003 0.004 0.006 <0.001
HCRC017 10 11 0.016 0.035 0.001 0.002 <0.001 0.007 <0.001
HCRC017 11 12 0.027 0.029 0.003 0.004 0.006 0.013 <0.001
HCRC017 12 13 0.015 0.016 0.002 0.003 <0.001 0.009 <0.001
HCRC017 13 14 0.010 0.016 0.002 0.002 0.001 0.006 <0.001
HCRC017 14 15 0.011 0.013 <0.001 0.002 <0.001 0.006 0.001
HCRC017 15 16 0.012 0.014 <0.001 0.003 <0.001 0.004 <0.001
HCRC017 16 17 0.021 0.027 0.001 0.002 <0.001 0.006 <0.001
HCRC017 17 18 0.014 0.025 0.001 0.003 0.003 0.010 <0.001
HCRC017 18 19 0.011 0.018 0.001 0.003 <0.001 0.006 <0.001
HCRC017 19 20 0.012 0.032 <0.001 0.002 <0.001 0.010 <0.001
HCRC017 20 21 0.029 0.059 0.003 0.007 <0.001 0.021 <0.001
HCRC017 21 22 0.053 0.097 0.003 0.013 <0.001 0.007 <0.001
HCRC017 22 23 0.021 0.058 0.003 0.003 <0.001 0.009 <0.001
HCRC017 23 24 0.016 0.039 0.003 0.003 0.005 0.009 <0.001
HCRC017 24 25 0.014 0.011 <0.001 0.002 0.003 0.006 <0.001
HCRC017 25 26 0.012 0.011 0.003 0.012 <0.001 0.007 <0.001
HCRC017 26 27 0.011 0.035 0.003 0.004 <0.001 0.006 <0.001
HCRC017 27 28 0.006 0.013 <0.001 0.006 <0.001 0.007 <0.001
HCRC017 28 29 0.008 0.006 <0.001 0.003 0.002 0.004 <0.001
HCRC017 29 30 0.007 0.004 <0.001 <0.001 <0.001 0.006 <0.001
HCRC017 30 31 0.018 0.009 0.001 0.003 <0.001 0.007 <0.001
HCRC017 31 32 0.023 0.010 <0.001 0.007 <0.001 0.008 <0.001
HCRC017 32 33 0.012 0.006 <0.001 0.003 <0.001 0.007 <0.001
HCRC017 33 34 0.025 0.008 0.003 0.005 <0.001 0.008 <0.001
HCRC017 34 35 0.018 0.015 0.001 0.002 <0.001 0.007 <0.001
HCRC017 35 36 0.015 0.022 0.002 0.004 <0.001 0.010 <0.001
HCRC017 36 37 0.022 0.017 0.001 0.020 <0.001 0.010 <0.001
HCRC017 37 38 0.030 0.021 <0.001 0.007 0.004 0.008 <0.001
HCRC017 38 39 0.058 0.119 0.002 0.011 <0.001 0.009 0.025
HCRC017 39 40 0.084 0.157 0.005 0.011 <0.001 0.009 0.046
HCRC017 40 41 0.028 0.149 0.007 0.007 <0.001 0.005 0.056
HCRC017 41 42 0.017 0.118 0.011 0.006 <0.001 0.007 0.046
HCRC017 42 43 0.015 0.153 0.003 0.004 <0.001 0.012 0.059
HCRC017 43 44 0.031 0.333 0.007 0.011 0.004 0.011 0.110
HCRC017 44 45 0.038 0.055 0.014 0.005 <0.001 0.007 0.032
HCRC017 45 46 0.025 0.038 0.009 0.005 0.003 0.006 0.017
HCRC017 46 47 0.013 0.070 0.015 0.005 0.004 0.004 0.024
HCRC017 47 48 0.009 0.074 0.007 0.005 <0.001 0.006 0.023
HCRC017 48 49 0.018 0.104 0.006 0.005 <0.001 0.004 0.032
HCRC017 49 50 0.021 0.052 0.005 0.004 <0.001 0.010 0.017
HCRC017 50 51 0.034 0.010 0.005 0.010 0.003 0.010 0.007

30

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC017 51 52 0.027 0.002 0.006 0.006 <0.001 0.007 0.001
HCRC017 52 53 0.063 0.018 0.009 0.009 <0.001 0.011 0.010
HCRC017 53 54 No Sample
HCRC017 54 55 0.184 0.193 0.048 0.027 <0.001 0.010 0.153
HCRC017 55 56 0.237 0.182 0.078 0.030 <0.001 0.010 0.166
HCRC017 56 57 0.172 0.163 0.075 0.039 <0.001 0.008 0.152
HCRC017 57 58 0.374 0.179 0.174 0.055 0.006 0.014 0.237
HCRC017 58 59 0.689 0.170 0.123 0.050 0.002 0.012 0.163
HCRC017 59 60 0.066 0.229 0.017 0.014 <0.001 0.015 0.083
HCRC017 60 61 0.066 0.856 0.017 0.038 0.004 0.021 0.295
HCRC017 61 62 0.035 1.141 0.046 0.052 <0.001 0.017 0.334
HCRC017 62 63 0.042 0.937 0.028 0.042 <0.001 0.013 0.278
HCRC017 63 64 0.031 0.559 0.013 0.028 0.003 0.014 0.180
HCRC017 64 65 0.020 0.145 0.020 0.015 <0.001 0.015 0.057
HCRC017 65 66 0.016 0.388 0.019 0.016 0.002 0.018 0.127
HCRC017 66 67 0.012 0.037 0.010 0.013 <0.001 0.005 0.067
HCRC017 67 68 0.006 0.026 0.015 0.005 <0.001 0.005 0.023
HCRC017 68 69 0.004 0.012 0.003 0.003 0.001 0.004 0.009
HCRC017 69 70 0.014 0.214 0.007 0.011 <0.001 0.017 0.068
HCRC017 70 71 0.019 0.091 0.007 0.008 0.002 0.008 0.031
HCRC017 71 72 0.014 0.029 0.009 0.011 <0.001 0.007 0.013
HCRC017 72 73 0.036 0.060 0.005 0.004 <0.001 0.007 0.027
HCRC017 73 74 0.135 0.049 0.012 0.008 <0.001 0.008 0.034
HCRC017 74 75 0.021 0.016 0.004 0.006 <0.001 0.006 0.011
HCRC017 75 76 0.013 0.012 0.003 0.003 <0.001 0.008 0.005
HCRC017 76 77 0.011 0.006 0.001 0.003 <0.001 0.005 0.005
HCRC017 77 78 0.012 0.006 0.003 0.003 <0.001 0.009 0.004
HCRC017 78 79 0.011 0.007 0.005 0.003 <0.001 0.006 0.014
HCRC017 79 80 0.010 0.011 0.003 0.003 <0.001 0.008 0.008
HCRC017 80 81 0.007 0.002 0.003 0.007 0.001 0.008 0.006
HCRC017 81 82 0.008 0.005 0.005 0.008 <0.001 0.005 0.004
HCRC017 82 83 0.009 0.010 0.003 0.010 <0.001 0.003 0.003
HCRC017 83 84 0.008 0.006 0.001 0.041 0.002 0.006 0.004
HCRC017 84 85 0.018 0.007 0.006 0.011 0.002 0.007 0.033
HCRC017 85 86 0.007 0.003 0.003 0.001 <0.001 0.007 0.022
HCRC017 86 87 0.144 0.007 0.011 0.003 <0.001 0.022 0.012
HCRC017 87 88 0.021 0.003 0.002 0.003 <0.001 0.007 0.005
HCRC017 88 89 0.011 0.005 0.003 0.003 <0.001 0.006 0.003
HCRC017 89 90 0.009 0.007 0.004 0.010 <0.001 0.005 0.007
HCRC017 90 91 0.016 0.008 0.005 0.003 0.005 0.006 0.026
HCRC017 91 92 0.015 0.003 0.004 0.003 <0.001 0.005 0.017
HCRC017 92 93 0.447 0.003 0.063 0.011 <0.001 0.004 0.016
HCRC017 93 94 0.052 0.002 0.009 0.013 <0.001 0.008 0.009
HCRC017 94 95 0.019 0.003 0.003 0.018 <0.001 0.004 0.004
HCRC017 95 96 0.014 0.002 0.004 0.003 <0.001 0.005 0.001
HCRC017 96 97 0.014 0.007 0.005 0.004 0.001 0.006 0.022
HCRC017 97 98 0.014 0.007 0.003 0.004 <0.001 0.006 0.007
HCRC017 98 99 0.007 0.013 0.003 0.002 <0.001 0.004 0.009
HCRC017 99 100 0.010 0.013 0.003 0.005 0.004 0.009 0.024
HCRC018 0 1 No Sample
HCRC018 1 2 0.044 0.064 0.002 0.002 <0.001 0.006 0.026
HCRC018 2 3 0.036 0.052 0.001 0.002 0.004 0.007 0.006
HCRC018 3 4 0.041 0.054 <0.001 0.002 0.002 0.011 0.003

31

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC018 4 5 0.043 0.054 <0.001 <0.001 0.006 0.013 0.002
HCRC018 5 6 0.047 0.068 <0.001 0.002 0.005 0.007 0.001
HCRC018 6 7 0.029 0.057 <0.001 0.002 <0.001 0.009 0.002
HCRC018 7 8 0.022 0.060 <0.001 0.001 <0.001 <0.001 0.001
HCRC018 8 9 0.020 0.047 0.001 0.003 0.002 <0.001 0.005
HCRC018 9 10 0.015 0.046 <0.001 0.002 0.001 <0.001 0.001
HCRC018 10 11 0.015 0.051 <0.001 0.003 <0.001 0.003 0.001
HCRC018 11 12 0.018 0.059 <0.001 0.001 <0.001 0.002 <0.001
HCRC018 12 13 0.018 0.051 <0.001 0.001 <0.001 0.006 <0.001
HCRC018 13 14 0.013 0.073 <0.001 0.001 <0.001 0.002 <0.001
HCRC018 14 15 0.010 0.041 <0.001 0.002 <0.001 0.002 <0.001
HCRC018 15 16 0.017 0.047 <0.001 0.002 <0.001 0.007 <0.001
HCRC018 16 17 0.012 0.044 <0.001 0.001 0.004 0.002 <0.001
HCRC018 17 18 0.012 0.052 <0.001 0.002 0.004 <0.001 <0.001
HCRC018 18 19 0.012 0.070 <0.001 0.001 <0.001 0.002 <0.001
HCRC018 19 20 0.013 0.078 0.001 0.001 0.007 0.002 <0.001
HCRC018 20 21 0.017 0.072 <0.001 <0.001 <0.001 0.002 <0.001
HCRC018 21 22 0.016 0.116 <0.001 0.001 0.004 0.004 <0.001
HCRC018 22 23 0.048 0.082 0.001 0.004 0.003 0.006 0.001
HCRC018 23 24 0.043 0.118 <0.001 0.004 <0.001 0.003 0.001
HCRC018 24 25 0.052 0.176 <0.001 0.010 <0.001 0.007 0.006
HCRC018 25 26 0.042 0.350 0.001 0.007 <0.001 0.004 0.005
HCRC018 26 27 0.061 0.203 0.001 0.007 0.001 0.007 0.003
HCRC018 27 28 0.067 0.127 0.002 0.004 0.004 0.009 <0.001
HCRC018 28 29 0.073 0.168 <0.001 0.002 0.002 0.009 <0.001
HCRC018 29 30 0.055 0.144 0.001 0.001 <0.001 0.008 <0.001
HCRC018 30 31 0.032 0.134 <0.001 0.002 0.002 0.011 0.001
HCRC018 31 32 0.044 0.148 0.001 0.003 0.001 0.059 <0.001
HCRC018 32 33 0.036 0.120 0.003 0.003 0.002 0.014 <0.001
HCRC018 33 34 0.045 0.221 0.002 0.002 0.005 0.054 <0.001
HCRC018 34 35 0.027 0.164 <0.001 0.002 0.004 0.021 <0.001
HCRC018 35 36 0.043 0.207 0.003 0.004 <0.001 0.030 <0.001
HCRC018 36 37 0.042 0.142 <0.001 0.002 0.004 0.016 0.001
HCRC018 37 38 0.041 0.120 <0.001 0.002 0.002 0.012 <0.001
HCRC018 38 39 0.020 0.047 <0.001 <0.001 <0.001 0.011 <0.001
HCRC018 39 40 0.031 0.054 0.001 0.003 <0.001 0.004 <0.001
HCRC018 40 41 0.027 0.057 <0.001 0.004 <0.001 0.009 <0.001
HCRC018 41 42 0.018 0.060 <0.001 0.003 0.002 0.005 <0.001
HCRC018 42 43 0.065 0.067 0.004 0.006 <0.001 0.009 0.002
HCRC018 43 44 0.077 0.067 0.004 0.008 <0.001 0.003 0.002
HCRC018 44 45 0.032 0.063 <0.001 0.005 <0.001 0.002 0.002
HCRC018 45 46 0.023 0.030 <0.001 0.002 <0.001 0.003 <0.001
HCRC018 46 47 0.011 0.023 0.002 0.003 0.001 0.006 <0.001
HCRC018 47 48 0.007 0.013 0.002 0.001 <0.001 <0.001 0.003
HCRC018 48 49 0.006 0.015 <0.001 0.001 <0.001 0.003 0.005
HCRC018 49 50 0.005 0.009 0.002 <0.001 <0.001 0.003 0.010
HCRC018 50 51 0.005 0.033 <0.001 <0.001 <0.001 0.002 0.009
HCRC018 51 52 0.009 0.033 <0.001 0.002 <0.001 0.004 0.004
HCRC018 52 53 0.011 0.009 0.003 0.002 0.003 <0.001 0.011
HCRC018 53 54 0.022 0.010 0.005 0.005 <0.001 0.002 0.028
HCRC018 54 55 0.013 0.013 0.001 0.002 0.003 0.002 0.010
HCRC018 55 56 0.005 0.011 <0.001 0.003 <0.001 0.005 0.002
HCRC018 56 57 0.008 0.009 <0.001 0.007 <0.001 0.005 0.008

32

Hole# From
(m)
To
(m)
WO3
(%)
Au
(g/t)
Cu
(%)
Mo
(%)
Bi
(%)
Sb
(%)
Sn
(%)
S
(%)
HCRC018 57 58 0.011 0.014 <0.001 0.002 0.002 <0.001 0.005
HCRC018 58 59 0.006 0.013 <0.001 0.001 0.003 0.004 <0.001
HCRC018 59 60 0.007 0.010 <0.001 0.001 <0.001 0.006 <0.001
HCRC018 60 61 0.015 0.013 <0.001 0.001 <0.001 0.008 <0.001
HCRC018 61 62 0.015 0.015 <0.001 0.002 <0.001 0.004 <0.001
HCRC018 62 63 0.008 0.008 <0.001 0.001 <0.001 0.003 <0.001
HCRC018 63 64 0.038 0.007 0.001 0.002 <0.001 0.004 0.001
HCRC018 64 65 0.018 0.007 0.003 0.002 0.010 0.003 0.016
HCRC018 65 66 0.731 0.006 0.015 0.023 <0.001 0.024 0.024
HCRC018 66 67 0.416 0.157 0.012 0.004 <0.001 0.010 0.060
HCRC018 67 68 0.031 0.180 0.003 0.001 0.003 0.006 0.059
HCRC018 68 69 0.028 0.034 0.001 0.002 0.001 0.004 0.026
HCRC018 69 70 0.010 0.072 0.003 0.001 0.001 0.002 0.028
HCRC018 70 71 0.011 0.017 0.008 0.002 0.003 <0.001 0.014
HCRC018 71 72 0.008 0.055 0.002 <0.001 0.005 <0.001 0.024
HCRC018 72 73 0.026 0.232 0.003 0.004 <0.001 0.006 0.097
HCRC018 73 74 0.012 0.092 0.001 0.002 <0.001 0.004 0.038
HCRC018 74 75 0.011 0.028 0.004 0.002 <0.001 0.004 0.009
HCRC018 75 76 0.007 0.003 <0.001 <0.001 0.003 0.002 <0.001
HCRC018 76 77 0.113 0.006 0.011 0.004 <0.001 0.004 0.125
HCRC018 77 78 0.020 0.008 0.004 0.003 <0.001 0.006 0.008
HCRC018 78 79 0.123 0.054 0.019 0.005 <0.001 0.006 0.043
HCRC018 79 80 0.019 0.018 0.015 <0.001 0.003 0.005 0.018
HCRC018 80 81 0.017 0.146 0.004 0.002 <0.001 0.003 0.057
HCRC018 81 82 0.013 0.070 0.009 0.003 <0.001 0.002 0.036
HCRC018 82 83 0.018 0.182 0.006 0.002 0.003 0.002 0.066
HCRC018 83 84 0.017 0.078 0.011 0.002 0.002 0.008 0.031
HCRC018 84 85 0.008 0.006 0.003 0.001 0.006 0.002 0.001
HCRC018 85 86 0.063 0.005 0.003 0.001 0.003 <0.001 <0.001
HCRC018 86 87 0.010 0.007 0.003 0.001 <0.001 0.004 <0.001
HCRC018 87 88 0.029 0.007 0.001 0.002 <0.001 0.003 0.001
HCRC018 88 89 0.008 0.007 0.003 0.002 <0.001 0.003 0.002
HCRC018 89 90 0.007 0.010 0.001 0.001 0.007 0.005 0.004
HCRC018 90 91 0.005 0.006 0.001 <0.001 <0.001 0.002 <0.001
HCRC018 91 92 0.008 0.012 0.002 0.003 0.001 0.006 0.003
HCRC018 92 93 0.006 0.006 0.001 <0.001 0.001 0.002 0.002
HCRC018 93 94 0.006 0.008 0.002 <0.001 <0.001 0.005 0.002
HCRC018 94 95 0.007 0.012 <0.001 0.002 0.003 0.006 <0.001
HCRC018 95 96 0.005 0.013 <0.001 <0.001 <0.001 0.002 0.002
HCRC018 96 97 0.004 0.007 0.003 <0.001 <0.001 0.002 0.005
HCRC018 97 98 0.003 0.011 <0.001 <0.001 0.007 0.002 <0.001
HCRC018 98 99 0.005 0.013 <0.001 <0.001 0.003 <0.001 <0.001
HCRC018 99 100 0.005 0.011 <0.001 0.001 0.002 0.005 <0.001

33