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Artemis Resources Limited Interim / Quarterly Report 2021

Jul 28, 2021

10429_rns_2021-07-28_e9e1bb20-70b6-4d5e-8739-5a9f16c411bf.pdf

Interim / Quarterly Report

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ASX Announcement

June 2021 Quarterly Report

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29 July 2021

Highlights

Paterson Project

Final diamond drill hole locations for the Apollo, Atlas, Juno and Voyager targets were determined, and sufficient funds allocated to budget in the quarter to drill these targets and more upon receipt of final heritage clearances from the Traditional Owners.

As detailed and extensive planning in advance of the Q3/Q4 2021 Paterson drill campaign is now largely complete with the Paterson Central exploration team currently in the pre-mobilisation phase with respect to rig booking and logistical planning in advance of receiving final heritage clearances. Once complete, the Company will then move to immediately commence drilling and intends to drill continuously for the remainder of the calendar year.

The Company intends to provide a more detailed update on the proposed final drill program hole locations and site mobilisation start dates in the near future.

Carlow Castle Au-Cu-Co Project

The commencement of the newly planned campaign of drilling for circa 11,000 metres, signals a new phase of exploration and evaluation at the Carlow Castle Project. This drilling is also designed to test the long-awaited Good Luck and Little Fortune Projects, located approximately one kilometre to the south of Carlow Castle.

As at 30 of June, a total of 16 holes have been drilled for a total of 3,506 metres of which 2,020 metres was RC and 1,486 metres was diamond.

Results for RC holes ARC310 to 313 and ARC315 have been received which focussed on the Carlow Castle Western Zone. These holes returned significant results of:

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  • 6m @ 14.97g/t Au, 7.09% Cu, 0.06% Co from 53 metres Hole ARC310

  • Including; 3m @ 13.92g/t Au, 5.11% Cu 0.03% Co from 54 metres

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  • 6m @ 2.61g/t Au, 0.54% Cu, 0.14% Co from 186 metres Hole ARC311

  • Including; 1m @ 6.27g/t Au, 1.07% Cu, 0.05% Co from 187 metres

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  • 4m @ 2.09g/t Au, 0.50% Cu, 0.06% Co from 121 metres Hole ARC313

  • Including; 1m @ 5.76g/t Au, 1.74% Cu, 0.07% Co from 124 metres

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  • 1m @ 9.29g/t Au, 0.67% Cu, 0.17% Co from 114 metres Hole ARC312

Diamond drilling results are pending review and RC drilling at Carlow Castle is currently in progress, testing the new interpretation designed to add significant ounces to the project.

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Carlow Castle Mineral Resource Estimate

The Mineral Resource report was completed by CSA and submitted in May. The updated Mineral Resource is 14.3 million tonnes at 0.7 g/t Au, 0.4% Cu, and 0.05% Co for 320,000 ounces gold, 53,000 tonnes contained copper, and 7,000 tonnes contained cobalt. The difference in resource numbers occurred due to additional drilling, redefinition and increase in the confidence of the model.

The Company is currently reviewing the recent Mineral Resource estimate with a view to approaching the Carlow Castle Project via a new strategy, aiming to increase tonnages and grade by targeting the higher-grade mineralised features, thus allowing for more effective geological control to drive project development. The current Q3 2021 RC drill program has been designed to achieve this objective and combined with the Mineral Resource review should, with success, allow the Company to clearly demonstrate the potential of the project to host a robust and significant gold, copper and cobalt resource.

Munni Munni Project

Drilling at Munni Munni comprised of 15 RC drill holes for 2,740 metres, completed between April and May, with drill holes spread through the entire upper portion of the mineralisation, to a maximum depth of 250 metres.

Significant intersections include:

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  • 7m @ 2.20g/t 2PGE + Au (1.46g/t Pd, 0.67 g/t Pt, 0.07g/t Au) from 124 metres, 21MMRC005;

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  • 7m @ 2.35g/t 2PGE + Au (1.33g/t Pd, 0.84 g/t Pt, 0.18g/t Au), from 96 metres , 21MMRC006;

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  • 4m @ 2.45g/t 2PGE + Au (1.31g/t Pd, 0.85g/t Pt, 0.29g/t Au) from 60 metres , 21MMRC007;

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  • 5m @ 2.35g/t 2PGE + Au (1.36g/t Pd, 0.68g/t Pt, 0.31g/t Au) from 75 metres , 21MMRC008;

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  • 4m @ 2.87g/t 2PGE + Au (1.76g/t Pd, 0.89g/t Pt, 0.22g/t Au) from 115 metres, 2MMRC010.

Artemis is pleased to have now executed a full Joint Venture Agreement and associated documents that will proceed to a Joint Venture Agreement for 100% of the Munni Munni Project with Platina Resources Limited in the ratio of beneficial interests, 70% ARV and 30% PGM.

Artemis and Platina continue to explore ways to monetise Munni Munni for the benefit of shareholders.

Radio Hill FLEM Survey

A Fixed-Loop Electromagnetic (FLEM) survey was completed in May which detected deep and untested conductor anomaly zones of interest identified from historic deep drilling and follow-up DHEM survey data. From this survey, the Radio Hill Project is still considered prospective for additional Ni-Cu-Co-PGE discoveries. Recommendations for further work at Radio Hill are pending.

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Whundo GAIP Survey

A Gradient-Array Induced Polarisation (GAIP) survey was conducted at the Whundo VMS project to identify VMS-style mineralisation along target trends located to the northeast of the main Whundo deposit. Additional work has been recommended postsurvey that has identified anomalous trends that will require another GAIP survey and drilling.

SUMMARY OF DRILLING AT CARLOW CASTLE

Artemis Resources (ASX: ARV) is pleased to release this June Quarterly, highlighting the achievements gained during the reporting period.

The June Quarterly results include the final assays from the initial holes drilled at the beginning of the circa 11,000m program, which is the follow up program from the 2020 Q4 drilling campaign. This program will continue into Q3.

Drill statistics and completed holes are shown in Table 1 and Figure 1, respectively.

Table 1: Drill statistics for June Quarterly

Location No of
Holes
RC (m) Diamond
(m)
No of
Samples
No Samples
Submitted
No Samples
Received
No of Samples
Outstanding
East Zone 6 1290.7 1276 1097 782 494
West Zone 9 2020 2046 2046 2046 0
Cross-Cut 1 195.3 201 0 0 201

Several assays from the beginning of the planned drilling program have returned significant results and these have been used to define and update the remaining holes in the program. These are shown in Table 2.

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Figure 1: Location of drill collars drilled during the June Q2 period. Section lines are shown in red with corresponding section co-ordinates.

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The rationale behind the new drilling program was to test the interpreted shallow plunging high-grade gold and copper shoots in and below the Carlow Castle Western Zone, the steeply dipping high-grade shoots on the eastern zone, the steep down-plunging gold shoots at Quod Est and the new interpretation of Cross-Cut.

Table 2: Carlow Castle drilling assay results averaged over significant drill intercept intervals bases on 1m assay samples, intersections defined by either >0.5g/t Au or >0.5%Cu, max 2m internal dilution. NSI = no significant intercept with values above lower cut off.

Hole No Comment From To Downhole
Width (m)
True
Width (m)
Au (g/t) Cu (%) Co (%)
ARC310 53 59 6 5.4 14.97 7.09 0.06
Including 54 57 3 2.7 13.92 5.11 0.03
112 113 1 0.9 1.42 0.05 0.03
168 170 2 1.8 1.61 0.16 0.13
225 226 1 0.9 1.37 0.06 0.01
ARC311 136 142 6 5.4 1.35 0.34 0.07
154 155 1 0.9 2.49 0.49 0.02
186 192 6 5.4 2.61 0.54 0.14
Including 187 188 1 0.9 6.27 1.07 0.05
ARC312 9 10 1 0.9 1.61 2.33 0.05
28 34 6 5.4 2.68 1.10 0.02
Including 31 34 3 2.7 4.34 1.75 0.01
56 61 5 4.5 1.66 0.26 0.04
83 85 2 1.8 1.15 0.19 0.03
114 115 1 0.9 9.29 0.67 0.17
144 145 1 0.9 2.63 0.23 0.01
ARC313 35 36 1 0.9 1.11 0.05 0.01
44 45 1 0.9 1.21 0.28 0.03
82 83 1 0.9 1.06 3.93 0.01
105 106 1 0.9 1.30 0.08 0.18
110 112 2 1.8 2.07 0.44 0.31
121 125 4 3.6 2.09 0.50 0.06
Including 124 125 1 0.9 5.76 1.74 0.07
147 148 1 0.9 1.35 0.14 0.10
199 200 1 0.9 5.17 0.38 0.01
ARC315 NSI

A reinterpretation of the structural setting and mineralising events have returned high-grade gold, copper and cobalt assays on the main shoots (Figure 2) and is defining the extent of the rich, lower grade gold-copper-cobalt “halo envelop” surrounding the internal high-grade zones.

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The Mineral Resource Estimate (MRE) completed by CSA Global and released in May, is being reviewed, considering the updated interpretation of the Carlow Castle system. This information, along with the updated interpretation will be incorporated into the new model and drive future drilling campaigns.

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Figure 2: Longsection of Carlow Castle looking north showing the high-grade trends (hot colours) in the 2021 block model. The dots denote the target pierce points of the drill holes.

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Figure 3: Section 506730mE, intersections for Hole ARC310. (Refer to Figure 1 for location)

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Figure 4: Section 506670mE showing intersections for holes ARC311 and ARC312 (refer to Figure 1 for location)

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Figure 5: Section 506770mE showing intersections for hole ARC313 (Refer to Figure 1 for location)

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Along with the potential in the Carlow Castle main zone, the Quod Est System located to the immediate north, is another area developing into a significant gold and copper resource, (refer to Figure 1 for location).

Quod Est mineralisation trends north to northeast, with a steeply dipping mineralisation plunge to the southeast, controlled by a gabbro/basalt contact. Significant results for Quod Est are included in the 23 April 2021 ASX release. Drilling at Quod Est is in progress.

Discovery of the Cross-Cut Zone by testing geophysical targets had intersected several high grade zones associated with north-westerly striking structures, (refer to Figure 1).

A new interpretation has been put forward, using airborne magnetic data and the SAM survey which suggests that Cross-Cut may be a series of en-echelon mineralised structures, as shown in Figure 6. Previous drilling had intersected significant copper and gold numbers, which are noted in the 23 April 2021 ASX release. Drilling at Cross-Cut is in progress.

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Figure 6: Updated interpretation (plan view) of the Crosscut Zone showing the potential for repeated mineralised structures of an en echelon nature. Holes have been repositioned in the current drill program to test these features. Background image of SAM survey.

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CARLOW CASTLE MINERAL RESOURCE ESTIMATE

During the quarter, the Mineral Resource for the Carlow Castle Project was updated by CSA Global using all data available as of 19 May 2021; this includes an additional 129 drill holes for 22,395 m since the 2019 Mineral Resource update. The additional drillholes were mainly at the eastern end of the Carlow Main zone and in the newly discovered Cross-Cut zone.

An open pit optimisation was completed to constrain the reported Mineral Resource. The updated Carlow Castle Mineral Resource is 14.3 million tonnes at 0.7 g/t Au, 0.4% Cu, and 0.05% Co for 320,000 ounces gold, 53,000 tonnes contained copper, and 7,000 tonnes contained cobalt.

Table 3 shows the updated resource numbers compared to the 2019 resources numbers.

Table 3. Comparison between 2021 and 2019 Mineral Resource estimates

Type 2021 Inferred 2021 Inferred 2021 Inferred 2021 Inferred 2019 Inferred 2019 Inferred 2019 Inferred 2019 Inferred
Tonnes (kt) Au
(g/t)
Cu
(%)
Co
(%)
Tonnes
(kt)
Au (g/t) Cu (%) Co (%)
Oxide 4,400 0.4 0.3 0.04 5,100 2.1 0.6 0.1
Transitional 3,100 0.7 0.5 0.06 - - - -
Fresh 6,900 0.9 0.4 0.06 2,800 0.7 0.6 0.05
Total 14,300 0.7 0.4 0.05 8,000 1.6 0.6 0.08

The 2021 Mineral Resource is materially different to the previously reported 2019 Mineral Resource, with a significant decrease in Au, Cu, and Co grades, and an increase in resource tonnes. The contained gold decreased by 98,000 ounces, contained copper increased 5,000 tonnes, and contained cobalt was approximately the same (Figures 7 and 8).

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Figure 7. Waterfall chart of changes in the MRE for contained gold between 2019 and 2021 estimates

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Figure 8. Waterfall chart of changes in the MRE for contained copper between 2019 and 2021 estimates.

Comparison between the 2019 and 2021 Mineral Resource

The 2021 Mineral Resource for Carlow Castle incorporated a significant amount of additional surface RC and diamond drilling. The decrease in resource grades and contained metal is a direct result of increased drilling below the -100mRL (approximately 140m below surface) as shown in Figure 9.

Below -100 mRL, the estimated mean gold grade decreased from 1.25 g/t Au in the 2019 model to 0.5 g/t Au in the 2021 model. Similarly, copper decreased from 0.3% Cu to 0.25% Cu, and cobalt from 0.05% Co to 0.03% Co. Material differences in the data and estimation methodology between the 2019 and 2020 Mineral Resource models are discussed below.

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Carlow Main Au grade by RL
2000000 2.0
1500000 1.5
1000000 1.0
500000 0.5
0 0.0
2021 tonnes 2019 tonnes 2019 Au g/t 2021 Au g/t
40 30 20 10 0 -10 -20 -30 -40 -50 -60 -70 -80 -90 -100 -110 -120 -130 -140 -150 -160 -170 -180 -190 -200 -210 -220 -230 -240 -250 -260
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Figure 9. Carlow Main zone 2019 and 2021 model tonnes and Au grades by RL

Differences in the Input Datasets

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Several very high-grade drill holes were drilled down dip in 2018: ARC133, ARC138, ARC139, and 18CCAD010. The 2021 Mineral Resource included several additional infill drillholes drilled across the mineralisation adjacent to ARC133, ARC138 and ARC139 and 18CCAD010 that reported lower Au, Cu, and Co grades and improved the confidence in the mineralisation interpretation (Figure 10).

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Figure 10. Cross-section 507 520 mE showing ARC138 and ARC139, 2019 block model, and 2019 Whittle shell

A comparison of the composite data for the Carlow Main zone showed the mean composite Au grade decreased from 0.60 g/t in 2019 to 0.55 g/t in 2021, while Cu composite grades increased from 2,935 ppm to 3,720 ppm, and Co composite grades stayed approximately the same. The changes in mean grades for Au and Cu are reflected in the Mineral Resource.

Differences in the Interpretation Approach

The 2019 mineralisation wireframe for Carlow Main used manual sectional interpretation on 40 m spacings at a nominal 500 ppm Cu cut-off. The 2021 model utilised a probabilistic indicator modelling method to model the complex and variable grade and geological continuity effectively. Nested indicator grade shells were generated at 200 ppm Cu, 500 ppm Cu, and 0.5 g/t Au cutoffs.

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The additional 0.5 g/t Au sub-domain was created for the 2021 model to constrain the influence of the high-grade down-dip drillholes. In areas with no infill drilling the 500 ppm Cu wireframes in 2019 and 2021 are generally comparable.

Differences in the Volume Covered

Infill drilling led to a refinement in the mineralisation interpretation and subsequent decrease in volume below -100 mRL. The decrease in volume was largely driven by infill drilling on four sections (507 380 mE; 507 500 mE; 507 540 mE; and 507 620 mE).

The additional drilling removed poorly constrained volume that had been projected down-dip in 2019, especially on the footwall.

Differences in the Estimation Parameters

The two models used different treatments of outlier grades. For the 2019 model, no top cuts were applied; grades above certain thresholds were restricted to a search distance of 10 m, or inside the OK panel in which they were situated. For the 2021 model, a top cut was applied to high grades before estimation.

Differences in the Open Pit Optimisation Parameters

Both the 2019 and 2021 models were constrained by a Whittle open pit optimisation to account for the reasonable prospects for eventual economic extraction (RPEEE) test of the JORC Code. The optimisation parameters for both models were identical except for increased commodity prices in 2021.

Differences in Mineral Resource Classification Approach

The resource classification followed similar approaches in the 2019 and 2021 models. In the 2019 model, the lower extents of the optimized resource shell were constrained by the extent of the mineralisation wireframe. The 2021 Whittle shell was not limited by the wireframe, but by grade and tonnage of mineralisation. Material below the -220 mRL was left unclassified based on limited drill data. The Carlow Main zone remains open at depth.

Differences in the Estimation Method

The change from a localised uniform conditioning (LUC) estimation method in 2019 to a global ordinary kriging (OK) method in 2021 was based on the improved mineralisation domaining and population statistics with infill drilling.

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Figure 11. 2019 block model resource classification (Inferred – 3; Unclassified – 4) with 2019 Whittle shell

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Figure 12. 2021 block model resource classification (Inferred – 3; Unclassified – 4) with 2021 Whittle shell

Summary of Findings from the 2021 and 2019 Resource Comparisons

  • Some of the 2020 and 2021 drilling has drilled through parts of the 2019 Carlow Main zone resource model.

  • This drilling has reduced the volume of the mineralisation and the contained metal below the -100mRL.

  • Additional resource has been added in the newly discovered Cross-cut zone.

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  • The balance of the 2020-2021 drilling has extended the Carlow Main mineralisation at depth; none of this additional mineralisation is reported in the current Mineral Resource as it is below the optimized resource pit shell.

  • Three drillholes that were drilled down-dip had a disproportionate effect on the Au grade below -100 mRL in the 2019 model; this has been rectified by the additional infill drilling and revised domaining.

  • The change from LUC to OK has not significantly changed the grade-tonnage selectivity prediction, due to the additional data available for the 2021 model.

  • The optimisation parameters for the 2021 model are the same as those used in 2019, except for higher commodity prices.

  • The 2019 and 2021 Inferred Mineral Resiurce classification is justified given the changes described above.

Strategy for Carlow Castle

Following the Mineral Resource update for Carlow Castle, a detailed review of the current resource and exploration strategy has been conducted.

It is proposed that a structural review and interpretation be completed, and drill targets identified and tested. The new interpretation will include a re-modeling of Carlow Castle using previous drill data, current drilling data, assay results and mineralisation trends.

  • Interpretation of the geology and structural setting;

  • Remodel and generate additional drill targets;

  • Step out drilling to add additional ounces to a currently increasing resource base;

  • Regional review to stitch together data from various disciplines and generate new targets.

MUNNI MUNNI PGE PROJECT H1 DRILL PROGRAM

Reverse Circulation (RC) drilling of 15 drill holes for 2,740 metres has been completed in May, with drill holes spread through the entire upper portion of the mineralisation, to a maximum depth of 250 metres. Samples were processed at ALS Global.

Joint Venture Formation with Platina Resources Limited

Following a period of constructive dialogue, Artemis is pleased to have now executed a full Joint Venture Agreement and associated documents that allow for to formal formation of a Joint Venture over 100% of the Munni Munni Project with Platina Resources Limited in the ratio of beneficial interests, 70% ARV and 30% PGM.

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Drilling and Multi-elements Results

The RC drilling program was designed to confirm the PGE horizon located on the northern nose of the >20km long Munni Munni mafic intrusive Complex, on a 50 x 50 metre drill pattern.

A non-JORC resource estimation was calculated using historic holes which had defined the mineralised horizon. The recent drill program was designed to infill the historic drilling.

Holes 2MMRC0014 & 015 were targeted to test mineralisation along the poorly defined eastern side of the mafic intrusive Complex.

As the PGE horizon is essentially a stratigraphic zone, historical drilling has been widely spaced and very selectively assayed; Artemis has undertaken a broad multi-element analytical suite to improve the subtle lithological variations.

Location of Munni Munni tenements and completed drill hole collars are located in Figure 13. Sections relating to the completed drilling are located in Figures 14 and 15.

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Figure 13: Munni munni location map highlighting recent drilling in red and section locations in yellow.

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Figure 14: Section 481800mE – 2PGE + Au intercepts.

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Figure 15: Section 481700mE – 2PGE + Au intercepts.

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In the diamond drill core from 2018 essentially only gabbros and pyroxenites were recognised, likewise in the RC chips only gabbros, pyroxenites and sediments with various minor intrusive dykes were noted.

Holes 18MMAD006 with 21MMRC003 and 21MMRC004 show the direct correlation of the PGE results and the remarkable continuity and consistency of the lithochemistry.

The RC data shows slightly lower absolute results for the PGE but occurs in the same relative ’stratigraphic‘ position. Virtually all PGE occur within the websterite lithology with a lesser amount in the pyroxenite due the PGE occurring very close to the contact between the two units.

Significant results from the PGE zone in this drilling program include:

  • 7m @ 2.20g/t 2PGE + Au (1.46g/t Pd, 0.67 g/t Pt, 0.07g/t Au) from 124m, 21MMRC005;

  • 7m @ 2.35g/t 2PGE + Au (1.33g/t Pd, 0.84 g/t Pt, 0.18g/t Au), from 96m, 21MMRC006;

  • 4m @ 2.45g/t 2PGE + Au (1.31g/t Pd, 0.85g/t Pt, 0.29g/t Au) from 60m, 21MMRC007;

  • 5m @ 2.35g/t 2PGE + Au (1.36g/t Pd, 0.68g/t Pt, 0.31g/t Au) from 75m, 21MMRC008;

  • 4m @ 2.87g/t 2PGE + Au (1.76g/t Pd, 0.89g/t Pt, 0.22g/t Au) from 115m, 2MMRC010.

RADIO HILL FIXED-LOOP ELECTROMAGNETIC (FLEM) SURVEY

Resource Potentials Pty Ltd (ResPot) completed a high-level review of Radio Hill project tenements M47/161 and M47/337 to determine what geophysical exploration datasets are available, highlight geophysical anomaly zones, identify anomalies and target areas of interest that remain untested, or are under- tested by drilling.

The aim is to provide recommendations for additional geophysical surveying, and then to plan, monitor, process and interpret new geophysical surveys carried out over target areas of interest. FLEM surveying was completed by GAP Geophysics in April 2021.

This study identified deep and untested conductor anomaly zones of interest identified from historic deep drilling and follow-up DHEM survey data and reports, with DHEM targets shown projected to surface on the map in Figure 16.

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Figure 16: Radio Hill Project tenements M47/161 and M47/337 (black outlines), mine infrastructure (dashed blue outlines), and the Radio Hill resource wireframes projected to surface (red) over a satellite image. The recent FLEM survey coverage area is outlined in yellow.

The Radio Hill project area is still considered to hold potential for additional discoveries of NiCu-Co-PGE sulphide deposits at depths >500m and to the south of the mined out NiS deposits, where long conduits likely follow the base of the intrusion. However, additional deposits are most likely located at least 600m below surface based on drilling and DHEM results and are therefore too hard to identify using airborne or surface-based EM survey methods.

Recommendations to this program are pending.

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WHUNDO GRADIENT-ARRAY INDUCED POLARISATION (GAIP) SURVEY

Artemis Resources hold mining rights to the Whundo VMS project tenements, located approximately 45km S of Karratha in Western Australia. The Whundo Zn-Cu-Pb-Ag VMS deposit has been mined in places and is now in care-and-maintenance status. The project area still holds some un-mined deposits and has potential for additional VMS deposits that remain to be discovered.

This study identified VMS mineralisation potential along a target trend located to the NE of the main Whundo deposit and covers the Yannery and Ayshia prospect areas. These prospect areas may host only weakly-conductive base metal mineralisation, such as sphalerite-rich or disseminated sulphide deposits, that were not identified using previous electromagnetic (EM) survey methods. Therefore, a new induced polarisation (IP) survey was planned and carried out over this area to identify chargeable sulphide mineralisation that was not detected by historic EM surveying. This is highlighted in green on Figure 17.

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Figure 17: Whundo Project tenements M47/007 and M47/009 (black outlines), and the Whundo resource wireframe (red) over a satellite image. The recent GAIP survey area is outlined in green, and the known prospect locations are highlighted by blue arrows

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A new GAIP survey area is recommended to be surveyed between the Whundo deposit and the recent GAIP survey area, as highlighted by the yellow square, (Figure 18).

This proposed GAIP survey area will cover a gap in survey coverage between Whundo and Yannery and cover the highest-amplitude chargeability anomaly located in the SW corner of the recent GAIP survey block.

Shallow RC drilling is recommended to test the chargeable and resistive target trend identified between Yannery and Ayshia prospects, as highlighted by the dashed black outline. This anomaly trend can be tested by RC drill transects planned across the trend. Untested VTEM target outlines to the NE and W of Whundo should also be RC drill tested. These targets are shown in Figure 18.

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Figure 18: Whundo Project tenements M47/007 and M47/009 (black outlines), VTEM anomaly outlines from late-time VTEM data (pink), early-time anomalies (dashed blue), historic Whundo drillhole collar locations coloured by max Zn, and a semi-transparent colour GAIP ternary image where conductivity is red, chargeability is green and resistivity is blue, all overlying a greyscale derivative magnetic image background

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ARTEMIS RESOURCES

W www.artemisresources.com.au

CORPORATE

Health and Safety

The Company continues to comply with all State guidelines to ensure the health and safety of its workforce, contractors, and the community in which it operates.

There is currently no significant impact on operations as a result of COVID-19.

Artemis has had no Occupational Health and Safety incidences during the quarter.

The Company ended the Quarter with a cash balance of $9.1m and liquid listed investments of circa $590,000.

Capital Raising

The Company raised $7 million at 6 cents a share in early June 2021 issuing 116.7 million new shares. The raise was strongly supported by European and Australian Institutional Investors.

Board of Directors

The Board welcomed Dr Simon Dominy as a Director on 1 July 2021. Dr Dominy is Adjunct Professor at the Western Australian School of Mines (WASM), Curtin University, and a Visiting Associate Professor at the Camborne School of Mines (CSM), University of Exeter, UK.

A mining geologist-engineer with over 25 years’ experience, Dr Dominy has since 2015 been working with a number of private and listed entities developing/operating gold projects including: MG Gold Ltd; Novo Resources Corporation (TSV: NVO); Scotgold Resources Ltd (AIM: SGZ) and OCX Gold Group.

Between 2004-2014 he was an Executive Consultant/General Manager with the Snowden Group based in Australia and UK, including two years contracted out to LionGold Corporation (SGX: A78).

Simon is a Fellow of the Australasian Institute of Mining and Metallurgy (“FAusIMM”) and the Australian Institute of Geoscientists (“FAIG”).

Mr Boyd Timler resigned as a director on 24 May 2021.

Other

The Company spent ~$1.8 million on exploration in the quarter ended 30 June 2021, principally on the drilling programs at Carlow Castle and Munni Munni, and exploration planning at Paterson’s outlined above.

Payments to Directors, related parties and their associates during the quarter amounted to $192,000, being salaries, superannuation and directors’ fees.

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About Artemis Resources

Artemis Resources (ASX: ARV; FRA: ATY; US: ARTTF) is a Perth-based exploration and development company, led by an experienced team that has a singular focus on delivering shareholder value from its Pilbara gold projects – the Greater Carlow Gold Project in the West Pilbara and the Paterson Central exploration project in the East Pilbara.

For more information, please visit www.artemisresources.com.au

This report has been approved for release by the Board.

COMPETENT PERSONS STATEMENT PATERSONS RANGE:

The information in this announcement that relates to Exploration Results complies with the 2012 Edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves (JORC Code) and has been compiled and assessed under the supervision of Dr Jayson Meyers, a consultant to Artemis Resources Limited and a Director of Resource Potentials Pty Ltd. Dr Meyers is a Fellow of the Australasian Institute of Geoscientists. He has sufficient experience that is relevant to the style of mineralisation and type of deposit under consideration and to the activity being undertaken to qualify as a Competent Person as defined in the 2012 Edition of the JORC Code. Dr Meyers consents to the inclusion in this announcement of the matters based on his information in the form and context in which it appears. Dr Meyers does not hold securities in the Company.

COMPETENT PERSONS STATEMENT WEST PILBARA:

The information in this announcement that relates to Exploration Results is based on information compiled or reviewed by Steve Boda, who is a Member of the Australasian Institute of Geoscientists (AIG). Mr Boda is an employee of Artemis Resources Limited. Mr Boda has sufficient experience that 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, Mineral Resources and Ore Reserves’. Mr Boda consents to the inclusion in the announcement of the matters based on his information in the form and context in which it appears.

COMPETENT PERSONS STATEMENT MINERAL RESOURCE ESTIMATION (MRE)

The information in this report that relates to Mineral Resources is based on information compiled by Mr Phil Jankowski, who is a Member of the Australasian Institute of Mining and Metallurgy. Mr Jankowski has sufficient experience that is relevant to the style of mineralisation and type of deposit under consideration and to the activity being undertaken to qualify as a Competent Person as defined in the 2012 Edition of the Joint Ore Reserves Committee (JORC) ‘Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves’. Mr Jankowski consents to the inclusion in this website of the matters based on this information in the form and context in which it appears.

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Tenement List - All tenements are located in Western Australia.

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Project Tenement
Status
Company
Purdy’s Reward L47/782
Pending
KML No 2 Pty Ltd
Carlow Castle E47/1797
Live
KML No 2 Pty Ltd
Rh Wll P47/1929
Live
KML No 2 Pty Ltd
E47/3719
Live
KML No 2 Pty Ltd
ut e E47/3487¹
Live
Elysian Resources Pty Ltd
E47/3341¹
Live
Hard Rock Resources Pty Ltd
47 Patch E47/3361¹
Live
Elysian Resources Pty Ltd
E47/3564¹
Live
Elysian Resources Pty Ltd
E47/3340¹
Live
Hard Rock Resources Pty Ltd
E47/3390¹
Live
Hard Rock Resources Pty Ltd
Elysian / Hard P47/1832¹
Live
Hard Rock Resources Pty Ltd
Rock P47/1881¹
Live
Hard Rock Resources Pty Ltd
E47/3534¹
Live
Jindalee Resources Pty Ltd
E47/3535¹
Pending
Jindalee Resources Pty Ltd
P47/1833¹
Pending
Jindalee Resources Pty Ltd
Whundo L47/163
Live
Fox Radio Hill Pty Ltd
M47/7
Live
Fox Radio Hill Pty Ltd
M47/9
Live
Fox Radio Hill Pty Ltd
Radio Hill M47/161
Live
Fox Radio Hill Pty Ltd
M47/337
Live
Fox Radio Hill Pty Ltd
L47/93
Live
Fox Radio Hill Pty Ltd
Weerianna M47/223²
Live
Western Metals Pty Ltd
Silica Hills L47/781
Pending
KML No 2 Pty Ltd
ARTEMIS
RESOURCES
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E47/1746
Live
KML No 2 Pty Ltd
Telfer E45/5276
Live
Armada Mining Pty Ltd
Sing Well P47/1622
Live
KML No 2 Pty Ltd
P47/1112
Live
KML No 2 Pty Ltd
Nickol River P47/1126
Live
KML No 2 Pty Ltd
P47/1925
Live
KML No 2 Pty Ltd
E47/3322⁵
Live
Karratha Metals Pty Ltd
M47/123⁵
Live
Platina Resources Ltd
Munni Munni M47/124⁵
Live
Platina Resources Ltd
M47/125⁵
Live
Platina Resources Ltd
M47/126⁵
Live
Platina Resources Ltd

1– 70% Artemis – Karratha Gold Joint Venture

2 – 80% Artemis

3 – 70% Artemis

4 – 70% Artemis – Joint Venture with Platina Resources

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Table 4:Carlow Drill Collar Survey June Q2 2021 (MGA50 Grid)

HoleID Type Easting
GDA94
Northing
GDA94
RL (m) Dip Azimuth
Mag
Total
Depth
(m)
ARC310 RC 506720 7698808 37 -60.71 179.89 260
ARC311 RC 506670 7698822 37 -60.53 180.39 260
ARC312 RC 506670 7698768 36 -59.99 180.03 200
ARC313 RC 506760 7698762 36 -60.65 180.05 220
ARC315 RC 506560 7698740 35 -60.14 180 150
21CCDD001 DD 507540 7698470 30 -60.11 359.72 300.2
21CCDD002 DD 507580 7698590 30 -60.27 1.92 110.6
21CCDD003 DD 507580 7698550 30 -60.43 359.96 177.3

Table 5: Significant results for the Q2 June RC drilling at Carlow Castle. Results are >0.5g/t Au or >0.5% Cu

Hole No From (m) To (m) Downhole
Width (m)
Au (g/t) Cu (%) Co (%)
ARC310 34 35 1 0.300 0.014 0.042
ARC310 40 41 1 0.900 1.585 0.009
ARC310 53 54 1 1.430 1.700 0.050
ARC310 54 55 1 47.300 11.250 0.065
ARC310 55 56 1 26.500 9.510 0.060
ARC310 56 57 1 9.700 9.900 0.057
ARC310 57 58 1 4.350 6.900 0.050
ARC310 58 59 1 0.530 3.250 0.035
ARC310 59 60 1 0.320 0.266 0.009
ARC310 112 113 1 1.420 0.053 0.027
ARC310 113 114 1 0.380 0.870 0.074
ARC310 129 130 1 0.670 0.264 0.141
ARC310 136 137 1 0.320 0.145 0.007
ARC310 137 138 1 0.320 0.116 0.009
ARC310 138 139 1 0.450 0.090 0.034
ARC310 142 143 1 0.370 0.640 0.036
ARC310 143 144 1 0.330 0.159 0.012
ARC310 168 169 1 1.650 0.177 0.102
ARC310 169 170 1 1.570 0.136 0.155
ARC310 204 205 1 0.330 0.573 0.029
ARC310 214 215 1 0.450 0.068 0.228
ARC310 222 223 1 0.300 0.211 0.011
ARC310 225 226 1 1.370 0.063 0.003
ARC311 6 7 1 0.550 0.139 0.007
ARC311 45 46 1 0.570 0.180 0.021
ARC311 53 54 1 0.280 0.126 0.060
ARC311 56 57 1 0.480 0.181 **0.082 **
ARC311 100 101 1 0.540 0.214 0.066
ARC311 109 110 1 0.320 0.090 0.060
ARC311 117 118 1 0.280 0.715 0.014
ARC311 132 133 1 0.330 0.047 0.010
ARC311 136 137 1 2.550 0.223 0.058
ARC311 139 140 1 1.650 0.570 0.058

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Hole No From (m) To (m) Downhole
Width (m)
Au (g/t) Cu (%) Co (%)
ARC311 140 141 1 2.870 0.565 **0.157 **
ARC311 141 142 1 0.690 0.269 0.072
ARC311 154 155 1 2.490 0.486 0.016
ARC311 175 176 1 0.460 0.068 0.012
ARC311 176 177 1 0.570 0.099 0.016
ARC311 181 182 1 0.340 0.090 0.008
ARC311 182 183 1 0.780 0.187 0.011
ARC311 186 187 1 0.650 0.155 0.024
ARC311 187 188 1 6.270 1.075 0.054
ARC311 189 190 1 1.460 0.106 0.083
ARC311 190 191 1 5.930 1.630 0.610
ARC311 191 192 1 1.140 0.199 **0.061 **
ARC312 9 10 1 1.610 2.330 0.053
ARC312 28 29 1 0.860 0.340 0.025
ARC312 29 30 1 0.840 0.385 0.030
ARC312 30 31 1 1.350 0.621 0.015
ARC312 31 32 1 6.950 0.570 0.011
ARC312 32 33 1 1.700 0.841 0.013
ARC312 33 34 1 4.370 3.830 0.022
ARC312 35 36 1 0.320 0.297 0.011
ARC312 46 47 1 0.330 0.186 0.053
ARC312 47 48 1 0.420 0.196 0.045
ARC312 49 50 1 0.290 0.282 0.026
ARC312 53 54 1 0.480 0.363 0.030
ARC312 55 56 1 0.310 0.059 0.010
ARC312 56 57 1 2.440 0.125 0.015
ARC312 57 58 1 1.450 0.328 0.016
ARC312 59 60 1 0.260 0.066 0.018
ARC312 60 61 1 4.010 0.713 0.118
ARC312 66 67 1 0.880 0.051 **0.397 **
ARC312 77 78 1 0.490 0.563 0.025
ARC312 78 79 1 0.480 1.410 0.018
ARC312 83 84 1 0.760 0.073 0.050
ARC312 84 85 1 1.530 0.304 0.014
ARC312 93 94 1 0.300 **0.664 ** 0.013
ARC312 105 106 1 0.560 0.295 0.013
ARC312 114 115 1 9.290 0.673 0.169
ARC312 115 116 1 0.380 0.098 0.014
ARC312 116 117 1 0.390 0.112 0.015
ARC312 118 119 1 0.570 0.049 0.022
ARC312 125 126 1 0.370 0.221 0.030
ARC312 134 135 1 0.330 0.099 0.023
ARC312 144 145 1 2.630 0.234 0.006
ARC313 14 15 1 0.460 0.058 0.010
ARC313 35 36 1 1.110 0.046 0.010
ARC313 43 44 1 0.480 0.128 0.034
ARC313 44 45 1 1.210 0.283 0.028
ARC313 82 83 1 1.060 3.930 0.010
ARC313 90 91 1 0.340 2.110 0.011
ARC313 103 104 1 0.320 0.222 0.030
ARC313 105 106 1 1.300 0.079 0.185
ARC313 110 111 1 0.990 0.421 0.570

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Hole No From (m) To (m) Downhole
Width (m)
Au (g/t) Cu (%) Co (%)
ARC313 111 112 1 3.150 0.463 0.047
ARC313 121 122 1 2.170 0.018 0.083
ARC313 122 123 1 0.360 0.156 0.083
ARC313 124 125 1 5.760 1.740 0.071
ARC313 130 131 1 0.370 0.050 0.007
ARC313 140 141 1 0.440 0.172 **0.062 **
ARC313 147 148 1 1.350 0.145 0.098
ARC313 148 149 1 0.360 0.091 0.046
ARC313 151 152 1 0.640 0.393 0.243
ARC313 152 153 1 0.420 0.128 0.090
ARC313 170 171 1 0.280 0.574 0.013
ARC313 195 196 1 0.730 2.070 0.007
ARC313 199 200 1 5.170 0.376 0.002
ARC315 NSI

Table 6: Drill Collar Locations for Munni Munni

Hole ID Type Easting Northing RL Grid Azimuth(True) Dip Depth
18MMAD001 DDH 482199.26 7664902.04 86.73 MGA-50 4.11 -60.1 100.5
18MMAD002 DDH 482660.00 7664952.82 81.86 MGA-50 5.17 -60.1 101.8
18MMAD003 DDH 482340.74 7664909.75 89.17 MGA-50 5.77 -60.2 100
18MMAD004 DDH 482454.88 7664874.92 85.70 MGA-50 4.47 -59.2 120
18MMAD005 DDH 481898.96 7664872.90 83.68 MGA-50 0 -70 100
18MMAD006 DDH 481796.57 7664865.99 82.57 MGA-50 0.84 -60.3 108.8
18MMAD007 DDH 482143.34 7664922.90 94.51 MGA-50 0 -80 110
18MMAD008 DDH 482454.50 7664875.00 85.70 MGA-50 0 -80 110
20MMRC001 RC 485794.94 7661174.67 96.57 MGA-50 90 -60 160
20MMRC002 RC 485863.85 7662228.67 92.18 MGA-50 90 -60 200
20MMRC003 RC 485901.19 7662571.11 91.25 MGA-50 90 -60 180
20MMRC004 RC 486293.89 7663240.68 89.82 MGA-50 90 -60 80
20MMRC005 RC 481923.45 7664887.17 82.84 MGA-50 0 -60 100
20MMRC006 RC 482201.58 7664896.23 86.94 MGA-50 0 -90 160
20MMRC007 RC 482492.96 7664856.56 88.47 MGA-50 180 -80 190
20MMRC008 RC 479730.23 7664005.47 102.58 MGA-50 330 -70 150
20MMRC009 RC 480200.52 7663223.59 104.73 MGA-50 0 -90 150
20MMRC010 RC 480309.48 7662943.32 106.57 MGA-50 0 -90 160
20MMRC011 RC 479598.19 7663830.25 123.01 MGA-50 320 -60 200
20MMRC012 RC 479696.24 7663809.66 112.06 MGA-50 330 -60 198
21MMRC001 RC 481699.73 7664781.70 83.18 MGA-51 0.00 -60 150
21MMRC002 RC 481699.72 7664779.73 83.07 MGA-52 0.00 -90 150
21MMRC003 RC 481814.44 7664795.24 83.58 MGA-53 0.00 -90 150
21MMRC004 RC 481814.52 7664797.22 83.51 MGA-54 0.00 -60 150
21MMRC005 RC 481844.03 7664739.96 84.73 MGA-55 0.00 -60 150
21MMRC006 RC 481862.44 7664843.06 83.49 MGA-56 0.00 -90 150
21MMRC007 RC 481864.87 7664843.26 83.67 MGA-57 30.00 -60 150
21MMRC008 RC 481974.29 7664875.13 86.89 MGA-58 20.00 -60 150
21MMRC009 RC 482895.77 7664802.80 82.58 MGA-59 0.00 -60 150
21MMRC010 RC 482502.76 7664821.49 98.79 MGA-60 350.00 -60 150
21MMRC011 RC 482798.12 7664827.12 82.19 MGA-61 0.00 -60 170
21MMRC012 RC 482713.67 7664884.68 85.61 MGA-62 0.00 -60 150
21MMRC013 RC 486247.37 7660700.45 98.29 MGA-63 0.00 -60 150
21MMRC014 RC 485899.50 7660489.58 99.18 MGA-64 0.00 -60 250
21MMRC015 RC 486247.366 7660700.47 98.29 MGA-65 0.00 -60 250

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Table 7: Significant Intersections for Munni Munni

Hole_ID M From M To Width Sample Type Pd Pt Au 2PGE+Au Co Cu Ni
18MMAD001 40.5 41 0.5 ASSAY 1/4 0.02 0.01 0.20 0.23 100 2660 1320
18MMAD001 41 41.5 0.5 ASSAY 1/4 0.66 0.49 0.60 1.74 130 4130 1910
18MMAD001 41.5 42 0.5 ASSAY 1/4 2.00 1.85 0.40 4.25 90 1430 950
18MMAD001 42 42.5 0.5 ASSAY 1/4 2.13 1.34 0.08 3.55 70 340 530
18MMAD001 42.5 43 0.5 ASSAY 1/4 1.92 0.88 0.04 2.83 70 210 530
18MMAD001 43 43.5 0.5 ASSAY 1/4 1.15 0.45 0.06 1.66 70 320 520
18MMAD001 43.5 44 0.5 ASSAY 1/4 1.34 0.36 0.24 1.93 90 1070 780
18MMAD001 44 44.5 0.5 ASSAY 1/4 0.73 0.14 0.04 0.91 70 380 540
18MMAD001 44.5 45 0.5 ASSAY 1/4 0.95 0.15 0.06 1.16 60 340 500
18MMAD001 45 45.5 0.5 ASSAY 1/4 1.11 0.17 0.12 1.39 100 1090 830
18MMAD001 45.5 46 0.5 ASSAY 1/4 0.59 0.08 0.06 0.73 70 520 570
18MMAD001 46 46.5 0.5 ASSAY 1/4 0.38 0.06 0.02 0.45 80 170 550
18MMAD001 46.5 47 0.5 ASSAY 1/4 0.50 0.41 0.02 0.93 80 120 510
18MMAD001 47 47.5 0.5 ASSAY 1/4 1.28 0.76 0.06 2.10 90 420 610
18MMAD001 47.5 48 0.5 ASSAY 1/4 0.01 0.01 0.01 0.03 80 190 530
18MMAD001 98 98.5 0.5 ASSAY 1/4 0.05 0.02 0.01 0.08 170 100 2260
18MMAD001 98.5 99 0.5 ASSAY 1/4 0.60 0.28 0.16 1.04 140 2080 2660
18MMAD001 99 99.5 0.5 ASSAY 1/4 0.01 0.00 0.00 0.01 90 100 1040
18MMAD002 22 22.5 0.5 ASSAY 1/4 0.01 0.00 0.03 0.04 110 3160 1540
18MMAD002 22.5 23 0.5 ASSAY 1/4 0.59 0.41 0.72 1.71 120 3430 1710
18MMAD002 23 23.5 0.5 ASSAY 1/4 2.09 0.85 0.27 3.21 80 1140 790
18MMAD002 23.5 24 0.5 ASSAY 1/4 0.30 0.04 0.07 0.41 90 890 730
0.22 0.12
18MMAD003 34 34.5 0.5 ASSAY 1/4 0.01 0.01 0.24 0.26 160 4400 1960
18MMAD003 34.5 35 0.5 ASSAY 1/4 0.07 0.04 0.47 0.58 140 3420 1620
18MMAD003 35 35.5 0.5 ASSAY 1/4 2.06 2.01 0.72 4.79 180 3790 2010
18MMAD003 35.5 36 0.5 ASSAY 1/4 2.71 2.53 0.22 5.46 100 1250 940
18MMAD003 36 36.5 0.5 ASSAY 1/4 2.14 1.40 0.29 3.83 80 400 650
18MMAD003 36.5 37 0.5 ASSAY 1/4 1.40 0.46 0.08 1.94 80 240 610
18MMAD003 37 37.5 0.5 ASSAY 1/4 1.62 0.53 0.15 2.30 80 430 730
18MMAD003 37.5 38 0.5 ASSAY 1/4 0.92 0.29 0.04 1.25 160 2290 1370
18MMAD003 38 38.5 0.5 ASSAY 1/4 0.93 0.39 0.17 1.48 140 2070 1190
18MMAD003 38.5 39 0.5 ASSAY 1/4 0.04 0.02 0.00 0.06 80 260 560
18MMAD004 56.7 57 0.3 ASSAY 1/4 0.11 0.07 0.02 0.20 110 1160 620
18MMAD004 57 57.5 0.5 ASSAY 1/4 0.75 0.22 0.07 1.05 120 2090 1160
18MMAD004 57.5 58 0.5 ASSAY 1/4 0.19 0.14 0.03 0.36 90 580 710
18MMAD005 34 34.5 0.5 ASSAY 1/4 0.01 0.01 0.23 0.25 100 2880 1350
18MMAD005 34.5 35 0.5 ASSAY 1/4 0.12 0.09 0.40 0.60 110 3100 1360
18MMAD005 35 35.5 0.5 ASSAY 1/4 1.80 1.83 0.52 4.15 100 2600 1250
18MMAD005 35.5 36 0.5 ASSAY 1/4 1.82 1.79 0.25 3.85 80 930 780
18MMAD005 36 36.5 0.5 ASSAY 1/4 2.05 1.42 0.10 3.57 80 460 620
18MMAD005 36.5 37 0.5 ASSAY 1/4 2.24 1.34 0.06 3.64 80 380 620
18MMAD005 37 37.5 0.5 ASSAY 1/4 1.71 0.92 0.04 2.67 70 250 530
18MMAD005 37.5 38 0.5 ASSAY 1/4 1.23 0.53 0.05 1.80 80 340 590
18MMAD005 38 38.5 0.5 ASSAY 1/4 1.57 0.37 0.16 2.10 110 970 920
18MMAD005 38.5 39 0.5 ASSAY 1/4 1.72 0.24 0.06 2.02 80 260 610
18MMAD005 39 39.5 0.5 ASSAY 1/4 0.75 0.10 0.04 0.88 80 180 580
18MMAD005 59 59.5 0.5 ASSAY 1/4 0.01 0.00 0.00 0.01 60 180 330
18MMAD005 59.5 60 0.5 ASSAY 1/4 0.41 0.17 0.06 0.64 120 3990 1840
18MMAD005 60 60.5 0.5 ASSAY 1/4 0.61 0.35 0.10 1.05 110 2770 1480
18MMAD005 60.5 61 0.5 ASSAY 1/4 0.87 0.60 0.19 1.65 110 3020 1680
18MMAD005 61 61.5 0.5 ASSAY 1/4 0.24 0.14 0.04 0.42 90 1340 1090
0.33 0.17

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Hole_ID M From M To Width Sample Type Pd Pt Au 2PGE+Au Co Cu Ni
18MMAD005 65 65.5 0.5 ASSAY 1/4 0.01 0.00 0.00 0.01 40 60 200
18MMAD005 65.5 66 0.5 ASSAY 1/4 0.30 0.19 0.05 0.53 50 680 420
18MMAD005 66 66.5 0.5 ASSAY 1/4 1.24 0.75 0.20 2.19 130 3290 1880
18MMAD005 66.5 67 0.5 ASSAY 1/4 1.41 0.60 0.18 2.19 140 3310 2200
18MMAD005 67 67.5 0.5 ASSAY 1/4 0.21 0.11 0.04 0.36 80 630 1040
18MMAD005 67.5 68 0.5 ASSAY 1/4 0.35 0.18 0.05 0.58 90 760 1120
18MMAD005 68 68.5 0.5 ASSAY 1/4 0.18 0.10 0.03 0.31 90 570 1000
18MMAD005 68.5 69 0.5 ASSAY 1/4 1.09 0.63 0.10 1.82 130 2320 1630
18MMAD005 69 69.5 0.5 ASSAY 1/4 0.19 0.12 0.05 0.36 90 380 980
18MMAD006 27.5 28 0.5 ASSAY 1/4 0.01 0.00 0.13 0.14 120 3210 1400
18MMAD006 28 28.5 0.5 ASSAY 1/4 0.76 0.69 0.33 1.78 100 2330 1160
18MMAD006 28.5 29 0.5 ASSAY 1/4 1.66 1.21 0.14 3.00 80 420 560
18MMAD006 29 29.5 0.5 ASSAY 1/4 1.49 0.77 0.06 2.32 80 360 540
18MMAD006 29.5 30 0.5 ASSAY 1/4 1.29 0.67 0.06 2.01 80 350 540
18MMAD006 30 30.5 0.5 ASSAY 1/4 0.76 0.14 0.07 0.97 80 440 600
18MMAD006 30.5 31 0.5 ASSAY 1/4 0.48 0.09 0.02 0.59 80 390 580
18MMAD006 31 31.5 0.5 ASSAY 1/4 1.10 0.19 0.08 1.37 70 380 550
18MMAD006 31.5 32 0.5 ASSAY 1/4 0.55 0.26 0.03 0.85 70 260 530
18MMAD006 32 32.5 0.5 ASSAY 1/4 1.16 0.25 0.11 1.51 100 1070 740
18MMAD006 32.5 33 0.5 ASSAY 1/4 0.32 0.17 0.04 0.53 80 230 540
18MMAD006 33 33.5 0.5 ASSAY 1/4 0.04 0.01 0.00 0.05 70 150 500
18MMAD007 65 65.5 0.5 ASSAY 1/4 0.06 0.03 0.36 0.45 110 3440 1490
18MMAD007 65.5 66 0.5 ASSAY 1/4 1.56 1.60 0.49 3.64 100 2410 1160
18MMAD007 66 66.5 0.5 ASSAY 1/4 1.98 1.44 0.09 3.50 90 430 590
18MMAD007 66.5 67 0.5 ASSAY 1/4 1.58 0.55 0.13 2.26 90 770 700
18MMAD007 67 67.5 0.5 ASSAY 1/4 0.91 0.16 0.14 1.21 90 1320 900
18MMAD007 67.5 68 0.5 ASSAY 1/4 0.55 0.12 0.04 0.71 90 410 590
18MMAD007 68 68.5 0.5 ASSAY 1/4 0.68 0.11 0.07 0.85 80 850 700
18MMAD007 68.5 69 0.5 ASSAY 1/4 0.64 0.08 0.04 0.76 90 440 620
18MMAD007 69 69.5 0.5 ASSAY 1/4 0.71 0.23 0.05 0.98 90 380 620
18MMAD007 69.5 70 0.5 ASSAY 1/4 0.34 0.26 0.01 0.61 80 130 530
18MMAD007 70 70.5 0.5 ASSAY 1/4 0.42 0.25 0.02 0.69 90 240 560
18MMAD007 70.5 71 0.5 ASSAY 1/4 0.02 0.01 0.00 0.03 90 160 550
18MMAD008 81.5 82 0.5 ASSAY 1/4 0.01 0.00 0.00 0.01 60 260 470
18MMAD008 82 82.5 0.5 ASSAY 1/4 0.67 0.25 0.07 0.99 80 1520 950
18MMAD008 82.5 83 0.5 ASSAY 1/4 1.46 1.03 0.33 2.81 100 2080 1330
18MMAD008 83 83.5 0.5 ASSAY 1/4 3.14 2.15 0.48 5.77 120 2400 1690
18MMAD008 83.5 84 0.5 ASSAY 1/4 2.66 2.00 0.45 5.11 150 2570 2040
18MMAD008 84 84.5 0.5 ASSAY 1/4 0.74 0.72 0.21 1.67 90 1890 1200
18MMAD008 84.5 85 0.5 ASSAY 1/4 0.73 0.52 0.13 1.39 80 990 1140
18MMAD008 85 85.5 0.5 ASSAY 1/4 0.08 0.06 0.01 0.14 60 190 490
18MMAD008 85.5 86 0.5 ASSAY 1/4 0.66 0.47 0.11 1.24 90 1940 1170
18MMAD008 86 86.5 0.5 ASSAY 1/4 0.64 0.37 0.09 1.10 80 1850 1040
18MMAD008 86.5 87 0.5 ASSAY 1/4 0.03 0.02 0.01 0.05 60 130 520
18MMAD008 87 87.5 0.5 ASSAY 1/4 0.18 0.09 0.03 0.30 70 340 540
18MMAD008 87.5 88 0.5 ASSAY 1/4 0.69 0.57 0.18 1.44 100 1580 1130
18MMAD008 88 89 1 ASSAY 1/4 0.14 0.08 0.02 0.24 80 440 670
20MMRC003 133 134 1 RC 0.25 0.05 0.04 0.33 62 638 336
20MMRC003 134 135 1 RC 0.48 0.19 0.12 0.78 78 1590 613
20MMRC003 135 136 1 RC 0.71 0.25 0.12 1.08 90 2310 870
20MMRC003 136 137 1 RC 0.08 0.02 0.05 0.15 79 356 401

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Hole_ID M From M To Width Sample Type Pd Pt Au 2PGE+Au Co Cu Ni
20MMRC005 18 19 1 RC 0.00 0.00 0.04 0.05 95 1640 924
20MMRC005 19 20 1 RC 0.34 0.33 0.23 0.90 125 2810 1350
20MMRC005 20 21 1 RC 1.74 1.37 0.20 3.30 96 1450 981
20MMRC005 21 22 1 RC 1.88 1.03 0.13 3.03 85 861 752
20MMRC005 22 23 1 RC 0.97 0.20 0.09 1.26 94 887 794
20MMRC005 23 24 1 RC 0.50 0.09 0.04 0.63 82 497 616
20MMRC005 24 25 1 RC 0.24 0.17 0.01 0.42 82 177 521
20MMRC006 69 70 1 RC 0.03 0.01 0.10 0.15 100 1275 532
20MMRC006 70 71 1 RC 0.62 0.60 0.30 1.51 76 1520 846
20MMRC006 71 72 1 RC 0.85 0.61 0.06 1.52 85 802 423
20MMRC006 72 73 1 RC 0.90 0.29 0.16 1.35 96 1140 669
20MMRC006 73 74 1 RC 0.62 0.33 0.12 1.06 105 1500 695
20MMRC006 74 75 1 RC 0.16 0.08 0.03 0.26 81 355 605
20MMRC006 101 102 1 RC 0.00 0.00 0.00 0.01 59 296 143
20MMRC006 102 103 1 RC 0.62 0.39 0.08 1.10 131 2280 937
20MMRC006 103 104 1 RC 0.22 0.11 0.04 0.37 87 708 812
20MMRC007 121 122 1 RC 0.01 0.01 0.14 0.16 97 2280 1280
20MMRC007 122 123 1 RC 0.49 0.44 0.33 1.26 95 2810 1280
20MMRC007 123 124 1 RC 1.70 1.50 0.17 3.37 89 1090 736
20MMRC007 124 125 1 RC 1.33 0.76 0.05 2.13 81 511 527
20MMRC007 125 126 1 RC 1.08 0.40 0.12 1.60 82 874 722
20MMRC007 126 127 1 RC 0.57 0.17 0.05 0.80 75 416 572
20MMRC007 127 128 1 RC 0.54 0.16 0.02 0.71 76 380 594
20MMRC007 128 129 1 RC 0.70 0.22 0.03 0.94 76 260 573
20MMRC007 129 130 1 RC 0.09 0.04 0.01 0.14 74 133 528
20MMRC011 143 144 1 RC 0.06 0.04 0.19 0.29 88 1960 873
20MMRC011 144 145 1 RC 0.87 0.82 0.42 2.11 89 2360 1050
20MMRC011 145 146 1 RC 0.78 0.78 0.14 1.69 77 781 587
20MMRC011 146 147 1 RC 0.83 0.44 0.09 1.35 78 829 601
20MMRC011 147 148 1 RC 0.95 0.17 0.07 1.20 83 1460 853
20MMRC011 148 149 1 RC 0.64 0.08 0.04 0.76 75 1200 762
20MMRC011 149 150 1 RC 0.48 0.15 0.05 0.68 76 632 576
20MMRC011 150 151 1 RC 0.21 0.08 0.01 0.30 74 239 473
20MMRC012 193 194 1 RC 0.01 0.01 0.14 0.15 84 2710 1200
20MMRC012 194 195 1 RC 0.37 0.30 0.15 0.82 81 1060 756
20MMRC012 195 196 1 RC 1.00 0.60 0.10 1.70 79 909 651
20MMRC012 196 197 1 RC 0.80 0.37 0.06 1.23 73 659 544
20MMRC012 197 198 1 RC 0.62 0.21 0.04 0.86 73 656 556
21MMRC001 78 79 1 RC 0.01 0.01 0.17 0.19 117 3380 1485
21MMRC001 79 80 1 RC 0.95 1.01 0.20 2.16 87 1400 863
21MMRC001 80 81 1 RC 0.59 1.18 0.05 1.82 79 350 551
21MMRC001 81 82 1 RC 0.17 0.39 0.02 0.58 74 210 519
21MMRC001 82 83 1 RC 0.01 0.02 0.01 0.04 78 214 550
21MMRC002 115 116 1 RC 0.01 0.01 0.19 0.21 102 2470 1285
21MMRC002 116 117 1 RC 0.11 0.16 0.33 0.61 106 2970 1400
21MMRC002 117 118 1 RC 1.37 1.36 0.35 3.07 102 1980 1120
21MMRC002 118 119 1 RC 1.20 1.68 0.11 2.99 89 555 672
21MMRC002 119 120 1 RC 1.00 1.71 0.07 2.78 89 476 644
21MMRC002 120 121 1 RC 0.59 1.36 0.06 2.01 86 462 634
21MMRC002 121 122 1 RC 0.16 0.77 0.08 1.01 91 944 801
21MMRC002 122 123 1 RC 0.09 0.53 0.02 0.64 91 403 673

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Hole_ID M From M To Width Sample Type Pd Pt Au 2PGE+Au Co Cu Ni
21MMRC002 123 124 1 RC 0.15 0.88 0.04 1.07 88 359 644
21MMRC002 124 125 1 RC 0.07 0.35 0.02 0.43 80 185 574
21MMRC002 125 126 1 RC 0.21 0.73 0.07 1.01 90 625 735
21MMRC002 126 127 1 RC 0.03 0.15 0.01 0.19 77 155 578
21MMRC003 107 108 1 RC 0.00 0.01 0.18 0.19 98 2710 1310
21MMRC003 108 109 1 RC 0.54 0.61 0.61 1.76 112 3550 1580
21MMRC003 109 110 1 RC 1.58 1.52 0.36 3.46 98 1630 1020
21MMRC003 110 111 1 RC 1.27 1.64 0.13 3.03 85 632 661
21MMRC003 111 112 1 RC 0.78 1.43 0.05 2.26 81 376 579
21MMRC003 112 113 1 RC 0.26 0.80 0.08 1.14 85 624 687
21MMRC003 113 114 1 RC 0.15 0.70 0.05 0.90 94 1080 865
21MMRC003 114 115 1 RC 0.11 0.56 0.02 0.68 72 302 553
21MMRC003 115 116 1 RC 0.07 0.37 0.01 0.45 75 178 562
21MMRC003 116 117 1 RC 0.06 0.38 0.01 0.46 78 134 566
21MMRC003 117 118 1 RC 0.15 0.77 0.01 0.93 83 160 614
21MMRC003 118 119 1 RC 0.54 1.08 0.02 1.63 87 131 640
21MMRC003 119 120 1 RC 0.03 0.10 0.00 0.13 83 88 599
21MMRC004 80 81 1 RC 0.01 0.01 0.16 0.18 103 3080 1305
21MMRC004 81 82 1 RC 0.68 0.76 0.39 1.82 94 2430 1175
21MMRC004 82 83 1 RC 1.38 1.44 0.26 3.08 91 1300 871
21MMRC004 83 84 1 RC 1.28 1.49 0.16 2.92 88 836 726
21MMRC004 84 85 1 RC 0.18 0.67 0.04 0.88 84 369 571
21MMRC004 85 86 1 RC 0.02 0.04 0.02 0.08 84 187 520
21MMRC005 122 123 1 RC 0.00 0.01 0.18 0.19 102 3850 1710
21MMRC005 123 124 1 RC 0.17 0.19 0.38 0.74 104 3130 1460
21MMRC005 124 125 1 RC 1.48 1.56 0.10 3.14 79 836 705
21MMRC005 125 126 1 RC 1.07 1.73 0.06 2.86 74 326 543
21MMRC005 126 127 1 RC 0.14 0.98 0.14 1.26 95 1225 876
21MMRC005 127 128 1 RC 0.19 0.90 0.05 1.14 86 628 619
21MMRC005 128 129 1 RC 0.07 0.46 0.04 0.57 73 245 368
21MMRC005 129 130 1 RC 1.45 3.67 0.12 5.23 151 2610 1250
21MMRC005 130 131 1 RC 0.33 0.94 0.02 1.29 88 638 730
21MMRC005 131 132 1 RC 0.17 0.56 0.02 0.75 81 292 635
21MMRC005 132 133 1 RC 0.01 0.02 0.00 0.03 79 103 613
21MMRC006 94 95 1 RC 0.00 0.00 0.03 0.03 89 1560 981
21MMRC006 95 96 1 RC 0.13 0.21 0.50 0.84 120 4040 1725
21MMRC006 96 97 1 RC 1.59 1.56 0.50 3.65 100 2420 1250
21MMRC006 97 98 1 RC 1.76 1.69 0.24 3.69 85 1000 824
21MMRC006 98 99 1 RC 1.20 1.79 0.10 3.08 76 410 599
21MMRC006 99 100 1 RC 0.72 1.50 0.05 2.26 78 319 572
21MMRC006 100 101 1 RC 0.31 1.27 0.22 1.80 94 1010 828
21MMRC006 101 102 1 RC 0.12 0.53 0.07 0.72 73 331 587
21MMRC006 102 103 1 RC 0.20 0.97 0.11 1.28 78 391 613
21MMRC006 103 104 1 RC 0.10 0.58 0.04 0.71 77 295 583
21MMRC006 104 105 1 RC 0.06 0.33 0.01 0.40 80 209 587
21MMRC006 105 106 1 RC 0.10 0.57 0.02 0.69 81 268 588
21MMRC006 106 107 1 RC 0.29 1.02 0.03 1.34 81 302 591
21MMRC006 107 108 1 RC 0.04 0.11 0.00 0.16 79 139 575
21MMRC006 136 137 1 RC 0.00 0.01 0.00 0.02 90 310 290
21MMRC006 137 138 1 RC 0.19 0.45 0.07 0.71 101 2060 634
21MMRC006 138 139 1 RC 0.03 0.07 0.01 0.11 80 669 596
21MMRC006 139 140 1 RC 0.55 1.00 0.10 1.65 88 3870 939
21MMRC006 140 141 1 RC 0.06 0.08 0.01 0.14 105 975 1535

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Hole_ID M From M To Width Sample Type Pd Pt Au 2PGE+Au Co Cu Ni
21MMRC007 59 60 1 RC 0.03 0.04 0.28 0.35 121 3230 1440
21MMRC007 60 61 1 RC 1.81 1.76 0.32 3.89 99 1900 982
21MMRC007 61 62 1 RC 1.25 2.02 0.69 3.96 89 1010 742
21MMRC007 62 63 1 RC 0.19 0.95 0.14 1.28 106 1470 917
21MMRC007 63 64 1 RC 0.14 0.52 0.01 0.67 82 252 584
21MMRC007 64 65 1 RC 0.03 0.04 0.01 0.07 89 257 647
21MMRC008 74 75 1 RC 0.00 0.00 0.00 0.01 69 148 509
21MMRC008 75 76 1 RC 0.22 0.38 0.11 0.71 86 1575 838
21MMRC008 76 77 1 RC 0.61 1.03 0.22 1.85 99 3120 1385
21MMRC008 77 78 1 RC 0.75 1.48 0.33 2.55 92 2960 1875
21MMRC008 78 79 1 RC 1.25 2.72 0.64 4.60 121 4950 3110
21MMRC008 79 80 1 RC 0.60 1.23 0.30 2.13 90 2600 1755
21MMRC008 80 81 1 RC 0.09 0.18 0.03 0.30 62 510 691
21MMRC008 81 82 1 RC 0.03 0.06 0.01 0.10 70 212 649
21MMRC008 82 83 1 RC 0.06 0.12 0.03 0.20 72 392 724
21MMRC008 83 84 1 RC 0.16 0.31 0.08 0.56 74 1105 986
21MMRC008 84 85 1 RC 0.18 0.36 0.08 0.62 93 916 1260
21MMRC008 85 86 1 RC 0.02 0.04 0.01 0.07 76 146 788
21MMRC008 86 87 1 RC 0.64 1.27 0.30 2.22 114 4180 2340
21MMRC008 87 88 1 RC 0.35 0.80 0.17 1.32 93 1930 1675
21MMRC008 88 89 1 RC 0.24 0.56 0.13 0.94 90 1295 1445
21MMRC008 89 90 1 RC 0.19 0.45 0.09 0.73 90 992 1380
21MMRC008 90 91 1 RC 0.01 0.03 0.01 0.05 71 135 836
21MMRC009 NSI
21MMRC010 114 115 1 RC 0.02 0.10 0.27 0.39 119 3490 1590
21MMRC010 115 116 1 RC 1.46 1.35 0.61 3.42 141 3410 1735
21MMRC010 116 117 1 RC 1.20 2.21 0.12 3.53 73 418 646
21MMRC010 117 118 1 RC 0.19 0.80 0.07 1.06 71 361 599
21MMRC010 118 119 1 RC 0.73 2.66 0.10 3.49 97 817 925
21MMRC010 119 120 1 RC 0.05 0.17 0.03 0.24 77 277 595
0 RC
21MMRC010 131 132 1 RC 0.01 0.01 0.01 0.03 76 66 588
21MMRC010 132 133 1 RC 1.05 1.59 0.25 2.89 118 2190 1300
21MMRC010 133 134 1 RC 0.05 0.08 0.01 0.14 77 199 604
21MMRC010 141 142 1 RC 0.05 0.09 0.01 0.15 74 301 653
21MMRC010 142 143 1 RC 0.21 0.40 0.05 0.66 93 1420 1055
21MMRC010 143 144 1 RC 0.01 0.02 0.01 0.03 80 101 795
21MMRC011 141 142 1 RC 0.00 0.00 0.07 0.07 78 1710 757
21MMRC011 142 143 1 RC 0.11 0.21 0.36 0.68 98 3000 1260
21MMRC011 143 144 1 RC 1.39 1.94 0.12 3.44 82 609 602
21MMRC011 144 145 1 RC 0.57 1.40 0.09 2.06 80 533 588
21MMRC011 145 146 1 RC 0.06 0.27 0.04 0.37 85 787 726
21MMRC011 151 152 1 RC 0.00 0.01 0.00 0.01 82 154 559
21MMRC011 152 153 1 RC 0.31 0.74 0.11 1.16 101 2180 1115
21MMRC011 153 154 1 RC 0.33 0.84 0.11 1.27 106 3570 1255
21MMRC011 154 155 1 RC 0.07 0.14 0.02 0.24 76 688 649
21MMRC012 82 83 1 RC 0.01 0.10 0.01 0.12 101 1220 771
21MMRC012 83 84 1 RC 0.31 0.39 0.10 0.80 111 2180 1225
21MMRC012 84 85 1 RC 0.13 0.26 0.03 0.42 84 556 731
21MMRC012 85 86 1 RC 0.08 0.26 0.02 0.36 92 838 782
21MMRC012 86 87 1 RC 0.05 0.10 0.03 0.18 84 389 627

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Hole_ID M From M To Width Sample Type Pd Pt Au 2PGE+Au Co Cu Ni
21MMRC012 87 88 1 RC 0.07 0.12 0.02 0.20 86 302 620
21MMRC012 88 89 1 RC 0.13 0.31 0.04 0.47 102 826 775
21MMRC012 89 90 1 RC 0.25 0.55 0.08 0.88 99 1110 849
21MMRC012 90 91 1 RC 0.28 0.50 0.08 0.85 91 979 860
21MMRC012 91 92 1 RC 0.83 1.48 0.36 2.66 111 3690 1980
21MMRC012 92 93 1 RC 1.03 2.99 0.42 4.44 118 4300 2230
21MMRC012 93 94 1 RC 0.22 0.47 0.06 0.76 85 1100 920
21MMRC012 94 95 1 RC 0.01 0.04 0.00 0.05 80 278 594
21MMRC012 95 96 1 RC 0.04 0.07 0.01 0.12 91 901 732
21MMRC012 96 97 1 RC 0.05 0.10 0.02 0.16 93 891 752
21MMRC012 97 98 1 RC 0.14 0.19 0.06 0.40 104 1865 990
21MMRC012 98 99 1 RC 0.04 0.09 0.02 0.14 87 769 736
21MMRC012 99 100 1 RC 0.26 0.27 0.09 0.62 105 2140 1100
21MMRC012 100 101 1 RC 0.21 0.25 0.07 0.53 105 2220 1140
21MMRC012 101 102 1 RC 0.29 0.37 0.31 0.97 120 2870 1370
21MMRC012 102 103 1 RC 0.12 0.21 0.05 0.38 118 2250 1190
21MMRC012 103 104 1 RC 0.19 0.30 0.07 0.56 123 2530 1340
21MMRC012 104 105 1 RC 0.12 0.21 0.04 0.37 112 1780 1130
21MMRC012 133 134 1 RC 0.00 0.01 0.00 0.01 148 34 1980
21MMRC012 134 135 1 RC 0.13 1.09 0.03 1.25 167 1185 2350
21MMRC012 135 136 1 RC 0.27 1.07 0.04 1.38 148 512 2370
21MMRC012 136 137 1 RC 0.01 0.05 0.00 0.07 150 84 2040
21MMRC013 103 104 1 RC 0.03 0.05 0.15 0.23 88 2080 1000
21MMRC013 104 105 1 RC 1.12 1.06 0.34 2.51 88 1230 808
21MMRC013 105 106 1 RC 0.77 1.32 0.06 2.14 81 285 544
21MMRC013 106 107 1 RC 0.30 0.86 0.07 1.23 105 839 765
21MMRC013 107 108 1 RC 0.15 0.67 0.06 0.88 112 1090 918
21MMRC013 108 109 1 RC 0.03 0.05 0.02 0.10 108 1730 899
21MMRC013 109 110 1 RC 0.04 0.21 0.03 0.28 154 5250 1790
21MMRC013 110 111 1 RC 0.03 0.07 0.01 0.11 85 1010 736
21MMRC013 111 112 1 RC 0.08 0.18 0.03 0.29 76 517 592
21MMRC013 112 113 1 RC 0.19 0.41 0.10 0.70 97 1040 898
21MMRC013 113 114 1 RC 0.16 0.36 0.07 0.59 100 1260 928
21MMRC013 114 115 1 RC 0.00 0.02 0.01 0.03 66 122 466
21MMRC013 130 131 1 RC 0.05 0.10 0.02 0.16 53 274 445
21MMRC013 131 132 1 RC 0.23 0.49 0.09 0.82 86 1180 929
21MMRC013 132 133 1 RC 0.01 0.03 0.00 0.04 73 244 527
21MMRC014 NSI
21MMRC015 99 100 1 RC 0.13 0.13 0.06 0.32 80 1670 576
21MMRC015 100 101 1 RC 0.18 0.75 0.07 1.00 88 1915 656
21MMRC015 101 102 1 RC 0.27 0.72 0.14 1.13 89 3200 1100
21MMRC015 102 103 1 RC 0.20 0.50 0.10 0.80 92 2420 915
21MMRC015 103 104 1 RC 0.05 0.22 0.01 0.28 94 621 489

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JORC Code, 2012 Edition – Table 1

SECTION 1 SAMPLING TECHNIQUES AND DATA

(Criteria in this section apply to all succeeding sections.)

Criteria Commentary
Sampling Nature and quality of sampling (eg cut Reverse circulation drilling was used to obtain both
techniques channels, random chips, or specific
specialised
industry
standard
2m composite and one metre samples, using a 5 ¼”
face sampling hammer.
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.
Samples were collected on a 2m composite basis to
a prescribed depth predetermined by previous
drilling, wireframing and assay data. Once the
predetermined depth is achieved, the sampling
reverts to one metre sample through the orezone
to EOH.
Include reference to measures taken to
ensure sample representivity and the
appropriate
calibration
of
any
measurement tools or systems used.
After composite sample results received, all
samples that return a value of >0.1g/t Au will result
in the resplitting of the one metre bulk bags at site
using a 75:25 jones riffle splitter. These one metre
Aspects
of
the
determination
of
samples are then submitted for analysis.
mineralisation that are Material to the
Public Report.
All samples are pulverized to produce a 50g charge
for fire assay.
In cases where ‘industry standard’ work
has been done this would be relatively
simple (eg ‘reverse circulation drilling was
used to obtain 1 m samples from which 3
Drilling sampling techniques employed at the
Artemis core facility include saw cut HQ (63mm)
drill core samples.
kg was pulverised to produce a 30 g Both RC and HQ wireline core is currently being
charge for fire assay’). In other cases more used to drill out the geological sequences and
explanation may be required, such as identify zones of mineralisation that may or may
where there is coarse gold that has not be used in any Mineral Resource estimations,
inherent sampling problems. Unusual mining studies or metallurgical testwork.
commodities or mineralisation types (eg
submarine
nodules)
may
warrant
disclosure of detailed information.
Duplicate samples were collected at the rig from a
static cone splitter, with the primary and duplicate
bag both simultaneously collected from separate
chutes.
For RC, the cyclone was cleared between rod
changes to minimise contamination.
Drilling Drill type (eg core, reverse circulation, Reverse Circulation drilling completed by Topdrill.
techniques open-hole hammer, rotary air blast,
auger, Bangka, sonic, etc) and details (eg
core diameter, triple or standard tube,
Drilling was completed using a truck mounted T685
Schramm rig mounted on 8x8 trucks
depth of diamond tails, face-sampling bit This can produce 1000psi/2700CFM with an axillary
or other type, whether core is oriented booster which is capable of achieving dry samples
and if so, by what method, etc). at depths of around 300m.
Drill sample Method of recording and assessing core Recoveries are recorded on logging sheets along
and chip sample recoveries and results with encounters with water and whether the
recovery assessed. samples are dry, moist or wet.
Measures taken to maximise sample Drilling recoveries for Reverse Circulation drilling
recovery
and
ensure
representative
were >80% with some exceptions that maybe
nature of the samples. caused by loss of return through faults or
Whether a relationship exists between encounters with water.
sample recovery and grade and whether >90% of samples returned dry.

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Criteria Commentary
sample bias may have occurred due to
Statistical analysis shows that no bias of grade
preferential loss/gain
of
fine/coarse

exists due to recoveries
material.
Logging Whether core and chip samples have been
RC samples were collected from the static cone
geologically and geotechnically logged to
splitter as two samples, one bulk sample and one
a level of detail to support appropriate
primary (analytical) sample.
Mineral Resource estimation, mining
studies and metallurgical studies.

The bulk samples are one metre splits.
Whether
logging
is
qualitative
or
quantitative in nature. Core (or costean,


These bags are then placed in neat rows of 50 bags
each clear of the rig for safety reasons.
channel, etc) photography. A field technician mixes the bag by hand before
The total length and percentage of the
relevant intersections logged.

taking a sample using a sieve and sieves the sample
to remove fines.
The sieved sample is then transferred to a wet sieve
in a bucket of water, and the sample is sieved
further until rock fragments are clearly visible.
These rock fragments are then logged by the site
geologist, taking note of colour, grainsize, rock
type, alteration if any, mineralisation if any, veining
if any, structural information if notable and any
other relevant information.
This information is then written down on pre-
printed logging sheets, using codes to describe the
attributes of the geology.
A representative sample is transferred to pre-
labelled chip trays into the corresponding depth
from where the sample was drilled from.
The remainder of the sample from the sieve is then
transferred into a core tray that has been marked
up by depths at metre intervals.
An identification sheet noting the hole number and
from-to depths that correspond to each tray is then
written up and placed above the tray and a
photograph is taken of the chips.
The hole is logged in its entirety, hence 100%
The geological data would be suitable for inclusion
in a Mineral Resource Estimation (MRE)
Sub-sampling If core, whether cut or sawn and whether
RC samples were collected on the drill rig using a
techniques and
sample
quarter, half or all core taken.
If non-core, whether riffled, tube sampled,
rotary split, etc and whether sampled wet


cone splitter. If any mineralised samples were
collected wet these were noted in the drill logs and
database.
preparation or dry. The RC drilling rig is equipped with a rig-mounted
For all sample types, the nature, quality
and appropriateness of the sample
preparation technique.


cyclone and static cone splitter, which provided
one bulk sample of approximately 20-30 kilograms,
and a sub-sample of approximately 2-4 kilograms
for every metre drilled.
Quality control procedures adopted for all
sub-sampling
stages
to
maximise
representivity of samples.


Field QC procedures involve the use of Certified
Reference Materials (CRM’s) as assay standards,
along with duplicates and blank samples. The
Measures taken to ensure that the
insertion rate of these was approximately 1:20.
sampling is representative of the in-situ
material collected, including for instance


For RC drilling, field duplicates were taken on a
routine basis at approximately1:20 ratio usingthe

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Criteria Commentary
results for field duplicate/second-half same sampling techniques (i.e. cone splitter) and
sampling. inserted into the sample run.
Whether sample sizes are appropriate to Primary and duplicates results
have been
the grain size of the material being compared.
sampled. The sample sizes are appropriate, representative
and are considered more than adequate to ensure
that there are no particle size effects relating to the
grain size of the mineralisation.
Quality of assay The nature, quality and appropriateness All samples were assayed by ALS-Chemex (ALS) in
data and of the assaying and laboratory procedures
used and whether the technique is
Perth, which is a National Association of Testing
Authorities
(NATA)
Australia
accredited
laboratory tests considered partial or total. organisation. The laboratory techniques below are
For geophysical tools, spectrometers,
handheld XRF instruments, etc, the
parameters used in determining the
for all samples submitted to ALS and are considered
appropriate for the style of mineralisation defined
within the Carlow Castle Project area
analysis including instrument make and The sample preparation followed industry best
model, reading times, calibrations factors practice. Fire assay samples were dried, coarse
applied and their derivation, etc. crushing to ~10mm, split to 300g subsample,
Nature of quality control procedures
adopted (eg standards, blanks, duplicates,
external laboratory checks) and whether
followed by pulverisation in an LM5 or equivalent
pulverising mill to a grind size of 85% passing 75
micron.
acceptable levels of accuracy (ie lack of This fraction was split again down to a 50g charge
bias) and precision have been established. for fire assay
Both 30g and 50g sample sizes were chosen for
analysis of gold, with fire assay (Au-AA26) with ICP
finish and determination by AAS. The limit of 100
g/t was not reached for any samples. The larger
sample size of 50g was predominantly selected to
provide greater confidence in the analyses.
All samples were dried, crushed, pulverised and
split to produce a sub-sample of 50g which is
digested and refluxed with hydrofluoric, nitric,
hydrochloric and perchloric acid (4 acid digest).
This digest is considered a total dissolution for most
minerals.
Analytical analysis is performed using ICP-AES
Finish (ME-ICP61A) for Ag, Al, As, Ba, Be, Bi, Ca, Cd,
Co, Cr, Cu, Fe, Ga, K, La, Mg, Mn, Mo, Na, Ni, P, Pb,
S, Sb, Sc, Sr, Th, Ti, Tl, U, V, W, Zn.
The original assay technique used for copper and
cobalt was 0.25 g sample with four acid digest and
ICP-AES finish. When the upper limits of the range
recommended by the lab were exceeded, a method
more appropriate method was used to re-assay
another sample of the pulp. For assays that reached
the limits of 1% for the 30 g, the laboratory method
ME-ICP61A was triggered, using 0.40 g samples
with the same liberation and finish techniques.
Standards are matrix matched by using previous
pulps from drilling programs and homogenised
using certified laboratories.
Standards were analysed by round robins to
determine grade.

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Criteria Commentary
Standards were routinely inserted into the sample
run at 1:20.
Laboratory standards and blank samples were
inserted at regular intervals and some duplicate
samples were taken for QC checks.
Verification of The verification of significant intersections Sampling was undertaken by field assistants
sampling and by either independent or alternative
company personnel.
supervised by experienced geologists from Artemis
Resources. Significant intercepts were checked by
assaying The use of twinned holes. senior personnel who confirmed them as
prospective for gold mineralisation.
Documentation of primary data, data
entry procedures, data verification, data
storage
(physical
and
electronic)
No twin holes using RC was completed in this
program.
protocols. Electronic data capture on excel spreadsheets
Discuss any adjustment to assay data. which are then uploaded as .csv files and routinely
sent to certified database management provider.
Routine QC checks performed by Artemis senior
personnel
and
by
database
management
consultant.
PDF laboratory certificates are stored on the server
and are checked by the Exploration Manager.
Location of Accuracy and quality of surveys used to A Garmin GPSMap62 hand-held GPS was used to
data points locate drill holes (collar and down-hole
surveys), trenches, mine workings and
define the location of the initial drill hole collars.
Standard practice is for the GPS to be left at the site
other locations used in Mineral Resource of the collar for a period of 5 minutes to obtain a
estimation. steady reading. Collar locations are considered to
Specification of the grid system used. be accurate to within 5m.
Quality and adequacy of topographic
control.
A high-quality downhole north-seeking multi-shot
or continuous survey gyro-camera was used to
determine the dip and azimuth of the hole at 30m
intervals down the hole
The topographic surface was calculated from the
onsite mine survey pickups and subsequently
verified by RTK GNSS collar surveys.
Zone 50 (GDA 94).
Surface collar coordinates are surveyed via RTK
GNSS with 1cm accuracy by a professional
surveying contractor.
Data spacing Data spacing for reporting of Exploration In certain areas, current drill hole spacing is
and distribution Results.
Whether the data spacing and distribution
variable and dependent on specific geological, and
geochemical targets.
is sufficient to establish the degree of A nominal 40x20m drill spacing is considered
geological
and
grade
continuity
adequate to establish the degree of geological and
appropriate for the Mineral Resource and grade continuity appropriate for JORC (2012)
Ore Reserve estimation procedure(s) and classifications applied.
classifications applied. No sample compositing to date has been used for
Whether sample compositing has been drilling completed by Artemis. All results reported
applied. are the result of 1 metre downhole sample
intervals.

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Criteria Commentary
Orientation of data in Whether the orientation of sampling
Drill holes were designed to be perpendicular to
relation to geological achieves unbiased sampling of possible
the strike of known mineralisation. Due to the
structure structures and the extent to which this is
structural and geological complexity of the area,
known, considering the deposit type. mineralisation of unknown orientation can be
If the relationship between the drilling
intersected.
orientation and the orientation of key
mineralised structures is considered to
have introduced a sampling bias, this
should be assessed and reported if
material.
Sample security The measures taken to ensure sample
The chain of custody is managed by the supervising
security. geologist who places calico sample bags in
polyweave sacks. Up to 10 calico sample bags are
placed in each sack. Each sack is clearly labelled
with:
Artemis Resources Ltd
Address of laboratory
Sample range
Samples were delivered by Artemis personnel to
the transport company in Karratha and shrink
wrapped onto pallets.
The transport company then delivers the samples
directly to the laboratory.
Audits or reviews The results of any audits or reviews of
Data is validated upon up-loading into the master
sampling techniques and data. database. Any validation issues identified are
investigated prior to reporting of results.

SECTION 2 REPORTING OF EXPLORATION RESULTS

(Criteria listed in the preceding section also apply to this section.)

Criteria Commentary
Mineral tenement and
Type, reference name/number, location
Drilling by Artemis was carried out on E47/1797 – 100%
land tenure status and ownership including agreements or owned by Artemis Resources Ltd. This tenement forms
material issues with third parties such as a part of a broader tenement package that comprises
joint ventures, partnerships, overriding the West Pilbara Project.
royalties, native title interests, historical
sites, wilderness or national park and
This tenement is in good standing.
environmental settings.
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.
Exploration done by
Acknowledgment
and
appraisal
of
The most significant work to have been completed
other parties exploration by other parties. historically in the Carlow Castle area, including the Little
Fortune and Good Luck prospects, was completed by
Open Pit Mining Limited between 1985 and 1987, and
subsequently Legend Mining NL between 1995 and
2008.
Work completed by Open Pit consisted of geological
mapping, geophysical surveying (IP), and RC drilling and
sampling.

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Criteria Commentary
Work completed by Legend Mining Ltd consisted of
geological mapping and further RC drilling.
Legend also completed an airborne ATEM survey over
the project area, with follow up ground-based FLTEM
surveying. Re-processing of this data was completed by
Artemis and was critical in developing drill targets for
the completed RC drilling.
Compilation and assessment of historic drilling and
mapping data completed by both Open Pit and Legend
has indicated that this data is compares well with data
collected to date by Artemis. Validation and
compilation of historic data is ongoing.
All exploration and analysis techniques conducted by
both Open Pit and Legend are considered to have been
appropriate for the style of deposit.
Geology Deposit type, geological setting and style The Carlow Castle Co-Cu-Au prospect includes a
of mineralisation. number of mineralised shear zones, located on the
northern margin of the Andover Intrusive Complex.
Mineralisation is exposed in numerous workings at
surface along quartz-rich shear zones. Both oxide and
sulphide mineralisation are evident at surface
associated with these shear zones.
Sulphide
mineralisation
appears
to
consist
of
Chalcopyrite, chalcocite, cobaltite, pyrrhotite and pyrite
Drill hole Information A summary of all information material to Drill hole information is contained within this release.
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.
If the exclusion of this information is
justified
on
the
basis

that
the
information is not Material and this
exclusion does not detract from the
understanding
of
the
report,
the
Competent Person should clearly explain
why this is the case.
Data aggregation
In
reporting
Exploration
Results,
All intervals reported are composed of 1 metre down
methods weighting
averaging
techniques, hole intervals for Reverse Circulation drilling.
maximum
and/or
minimum
grade
truncations (eg cutting of high grades)
and cut-off grades are usually Material
Aggregated intercepts do include reported lengths of
higher-grade internal intercepts.
and should be stated. No upper or lower cut-off grades have been used in
Where aggregate intercepts incorporate reporting results.
short lengths of high grade results and No metal equivalent calculations are used in this report.
longer lengths of low grade results, the
procedure usedfor such aggregation

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Criteria Commentary
should be stated and some typical
examples of such aggregations should be
shown in detail.
The assumptions used for any reporting
of metal equivalent values should be
clearly stated.
Relationship between These relationships are particularly The mineralisation in the Carlow Castle Western Zone
mineralisation widths important in the reporting of Exploration strikes generally E-W and dips to the north at
and intercept lengths Results. approximately -75 to -80 degrees. The drill orientation
If the geometry of the mineralisation
with respect to the drill hole angle is
known, its nature should be reported.
was 180 -60 dip. Drilling is believed to be generally
perpendicular to strike. Given the angle of the drill holes
and the interpreted dip of the host rocks and
mineralisation, reported intercepts approximate true
If it is not known and only the down hole width.
lengths are reported, there should be a
clear statement to this effect (eg ‘down
hole length, true width not known’).
True thicknesses are calculated from interpretation
deriving from orientation of high-grade intervals,
orientation of the main mineralised trend and its dip.
This is an estimation only and can change according to
additional information.
Diagrams Appropriate maps and sections (with Appropriate plans are shown in the text.
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.
Balanced reporting Where comprehensive reporting of all This release reports the results of five RC holes. The
Exploration Results is not practicable, significant results tabulated in the release are reported
representative reporting of both low and at a base grade of >0.5 g/t Au or >0.5% Cu. Internal
high grades and/or widths should be dilution of up to 2 m may be included in an intersection.
practiced to avoid misleading reporting
of Exploration Results.
Other substantive Other exploration data, if meaningful Targeting for the RC drilling completed by Artemis was
exploration data and material, should be reported based on compilation of historic exploration data, and
including (but not limited to): geological the surface expression of the targeted mineralised
observations; geophysical survey results; shear zones and associated historic workings.
geochemical survey results; bulk samples
– size and method of treatment;
metallurgical test results; bulk density,
groundwater, geotechnical and rock
characteristics; potential deleterious or
contaminating substances.
Further work The nature and scale of planned further Further work (RC and diamond drilling) is justified to
work (eg tests for lateral extensions or locate extensions to mineralisation both at depth and
depth extensions or large-scale step-out along strike.
drilling).
Diagrams clearly highlighting the areas
of possible extensions, including the
main geological interpretations and
future drilling areas, provided this
information
is
not
commercially
sensitive.

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SECTION 3 – Estimation and Reporting of Mineral Resources

Criteria JORC Code explanation Commentary
Database
integrity
Measures taken to ensure that data has
not been corrupted by, for example,
transcription or keying errors, between its
initial collection and its use for Mineral
Resource estimation purposes.
Geophysical files were uploaded from the data logging
device to the contractor’s central storage database and
then provided in both raw and corrected/filtered format in
CSV, LAS and PDF format. This has removed the potential
for transcription errors and for reference checks.
Core logging was completed by Artemis on site using
project-specific
logging
codes
and
a
database
management system; DataShed™, with primary key fields
and look-up tables. Collar survey, down hole survey and
assay files were loaded from source files using templates
to load into predefined tables. These measures enforced
strict referential integrity and validation rules to prevent
corruption errors.
The Competent Person found no material errors and
deemed the database was fit for the purpose of Mineral
Resource estimation.
Data validation procedures used. The Competent Person checked the drillhole files for the
following errors prior to Mineral Resource estimation:
• Absent collar data
• Multiple collar entries
• Questionable downhole survey results
• Absent survey data
• Overlapping intervals
• Negative sample lengths
• Sample intervals which extended beyond the hole
depth defined in the collar table.
• Assay values reported as negative detection limits were
updated to half detection limits.
Site visits Comment on any site visits undertaken by
the Competent Person and the outcome of
those visits.
The Competent Person has not visited the site, but has
relied on information from colleague Mr Matt Clark, Senior
Resource Geologist, collected during a site visit in April
2021.
If no site visits have been undertaken,
indicate why this is the case.
The Competent Person considers that the information
provided to him by colleague Mr Matt Clark allows him to
appropriately
consider
the
necessary
factors
in
establishing Mineral Resources for the confidence
estimated.
Geological
interpretation
Confidence in (or conversely, the
uncertainty of) the geological
interpretation of the mineral deposit.
The host lithologies at Carlow Castle are basalt and gabbro,
with mineralisation predominantly in basalt with a strong
lithological control on mineralisation between basalt and
gabbro. The dominant control on mineralisation is by
structures potentially far smaller than the drill hole spacing
and smaller than which can be explicitly modelled.
Therefore, the geological model consisted of waste and
mineralisation.
Nature of the data used and of any
assumptions made.
No material assumptions have been made which affect the
MRE reported herein.
The effect, if any, of alternative
interpretations on Mineral Resource
estimation.
The Competent Person is confident any alternative
interpretations would result in globally immaterial
differences in the Mineral Resource estimate.
The use of geology in guiding and
controlling Mineral Resource estimation.
Mineralisation generally shows a continuous grade
distribution from un-mineralised through to high grade,
with minor inflectionpoints within the log-probability plot

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Criteria JORC Code explanation Commentary
The factors affecting continuity both of
grade and geology.
for the distribution. One such inflection occurs at 200 ppm
Cu, on which definition of mineralisation lodes were
based. A second cut-off at 500 ppm correlated with high-
grade copper, gold, and cobalt, and also correlated with
structural measurements defined by structural logging and
modelling.
The geological model includes a shallow, approximately 3
m thick overburden surface and an oxide horizon that
averages 40 m depth. Transitional material is typically 10
to 20 m thick and extends down to 100 m depth in the
eastern section of Carlow Main.
Dimensions The extent and variability of the Mineral
Resource expressed as length (along strike
or otherwise), plan width, and depth below
surface to the upper and lower limits of the
Mineral Resource.
The Carlow Main lodes have been modelled as a set of
anastomosing fingers extending off and conjoining a major
central zone that follows a broad sigmoidal curve whose
average centreline at 769,660 mN strikes 1,200m east-
west. The anastomosing lodes vary in thickness from 5 m
where they pinch to 90 m in the thickest portion. The high-
grade 500 ppm copper shell averages 30-40m thick, within
the low-grade 200 ppm copper wireframe that extends up
to 50 m to the north and south. At the western end,
mineralisation dips steeply north, and at the eastern end it
dips steeply south. Mineralisation in Carlow Main has been
interpreted to a maximum of 630 m below surface,
averaging 280 m.
The Quod Est and Cross Cut mineralisation have been
modelled similarly with low-grade 200 ppm copper shell
and inner high-grade 500 ppm grade shells. Quod Est and
Cross-Cut lodes have been interpreted as a steeply east
dipping lodes. The major lode at Quod Est outcrops and
strikes NNE, bifurcates at its southern third, and measures
about 200 m overall, with maximum depth of 180 m. The
Cross Cut mineralisation has been interpreted as two lode
structures that strike 150 m NNE and dip steeply east, to a
maximum depth of 180 m.
Estimation and
modelling
techniques
The nature and appropriateness of the
estimation technique(s) applied and key
assumptions, including treatment of
extreme grade values, domaining,
interpolation parameters and maximum
distance of extrapolation from data points.
If a computer assisted estimation method
was chosen, include a description of
computer software and parameters used
The Mineral Resources were estimated within nine
estimation domains, representing Carlow Castle Main,
Quod Est and Cross Cut, formed from the mineralisation
model interpreted at nominal cut-offs of 200 ppm and 500
ppm Cu. The domains were further split into overburden,
oxide and fresh by the oxidation wireframes. A small
volume wireframe was modelled in the eastern section of
Carlow Main based on a 0.5 g/t Au cut-off to control the
influence of high-grade holes that were drilled subparallel
to mineralisation.
All geological modelling was undertaken using Leapfrog
Geo software. Estimation domains were modelled using
indicator interpolants and the nominal 200 ppm Cu, 500
ppm Cu, and 0.5 g/t Au cut-off grades.
Statistics, grade and density estimates, and variography,
were undertaken in Supervisor software, and composite
selection and block coding, undertaken in Surpac software,
used the combined domains as hard boundaries.
Samples were composited to 1 m intervals based on
assessment of the raw drillhole sample interval lengths.
Quantitative Kriging Neighbourhood Analysis (QKNA) was
undertaken usingSupervisor software to assess the effect

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Criteria JORC Code explanation Commentary
of changing key kriging neighbourhood parameters on
block grade and density estimates. Kriging Efficiency and
Slope of Regression were determined for a range of block
sizes, minimum and maximum samples, search dimensions
and discretisation grids. A two-pass search ellipse strategy
was adopted, whereby the first pass equated to the full
range of the relevant variogram model for each domain,
with a minimum of 8 samples, maximum of 20 samples and
a maximum of 6 samples per hole. The second pass search
ellipse was between 2 to 3.5-times the variogram model
range, with a minimum of 8 samples, maximum of 16
samples and a maximum of 6 samples per hole. All blocks
were filled in the first two passes.
A 20 mE x 10 mN x 10 mRL parent cell size was constructed
covering the full volume of the mineralisation and
additional space for mine infrastructure planning. Sub-
celling was employed to 5 mE x 5 mN x 5 mRL to improve
block volume fitting to the complex wireframe.
Mineralisation domains were coded in the block model
below the overburden surface, and further coded by
oxidation domain.
High grade cuts were used to constrain outliers in the
dataset as described above.
Grade interpolation for Au, Cu, Co, As, S was completed
using ordinary kriging (OK) into the parent block cells. The
search employed a dynamic anisotropy to allow the ellipse
to rotate along the sinusoidal mineralisation domains.
The availability of check estimates,
previous estimates and/or mine production
records and whether the Mineral Resource
estimate takes appropriate account of such
data.
Several previous historical resource estimates have been
completed previously. These reports were available to the
Competent Person. These did not necessarily cover the
same area as this Mineral Resource update and were
volumetrically smaller in their extent. Further; while these
Previous Mineral Resources are quoted below, the
approach taken to modelling and estimation differs
fundamentally from that of the current estimate
Consequently, the models are not directly comparable.
In 2018, Mr Philip Jones estimated Mineral Resources
reported in accordance with the JORC Code for Carlow
South using drilling data provided by Artemis to model
mineralisation wireframes that were based on a total net
smelter return of >$30 using the following metal factors:
• Copper: Price: $4.473/lb; Recoveries: 75% (mining and
metallurgical recovery)
• Gold: Price: $USD1282.10/oz; Recoveries: 90% (mining
and metallurgical)
• Cobalt: Price: $54,500/t; Recoveries: 75% mining and
metallurgical
In January 2019 Al Maynard & Associates estimated
Inferred Mineral Resources at Carlow Castle South and
Quod Est of 7.7 Mt @ 0.51% Cu, 1.06 g/t Au and 0.08% Co.
Four domains, based on the strike of the mineralisation,
were used in the modelling. High grade cuts were also
applied using mean grades +2SD of copper, gold and cobalt
per domain. Grades were interpolated by Inverse Distance
Squared (ID2).

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Criteria JORC Code explanation Commentary
In November 2019, CSA Global estimated Inferred Mineral
Resources at Carlow Castle South and Quod Est of 8 Mt @
0.6% Cu, 1.6 g/t Au and 0.08% Co, reported above a lower
cut-off of 0.3% Cu, and within a theoretical optimised pit
shell.
Two estimation domains for Carlow Main and Quod Est
were used in the modelling based on a lower cut-off grade
of 500 ppm copper. Grade interpolation was completed
initially by ordinary kriging into panels, with post-
processing using localised uniform conditioning (LUC)
within the panels to derive an estimate at the smaller
selective mining unit (SMU) scale. Grade limiting was
employed in the panel estimates to restrict the influence
of very high grades to 10 m.
The optimised pit shell used for the Mineral Resource
reporting used the following parameters:

50ooverall slope angle

Oxide
and
Fresh
used
same
recoveries/processing costs

$48.1/t processing cost

85% copper recovery

94.8% gold recovery

73% cobalt recovery

Mining costs $/t incremented by depth ranging
from $2.57 through to $5.77 inclusive.

Copper: $9000/t

Gold: $2000/oz

Cobalt: $48,000/t
The assumptions made regarding recovery
of by-products.
The co-products, gold and cobalt, are assumed to be
recoverable within the mineralisation wireframe volumes
that have been modelled on a copper grade cut-off. The
metallurgical testwork for gold and cobalt may not be
representative of the material reported as Mineral
Resources. However, the metallurgical testwork results
show that gold and cobalt can be recovered.
Estimation of deleterious elements or other
non-grade variables of economic
significance (e.g. sulphur for acid mine
drainage characterisation).
Arsenic and sulphur have been estimated, although it is
unknown at this stage of the project if they are deleterious
for copper, gold and cobalt.
In the case of block model interpolation,
the block size in relation to the average
sample spacing and the search employed.
The dimensions of the parent block used for estimation
represents approximately half the drillhole spacing in the
X orientation and one quarter the spacing in the Y
orientation.
Any assumptions behind modelling of
selective mining units.
SMU units were not modelled. The parent block size of 10
m in the Z direction is approximately twice the size of
assumed SMU of 5 m high mining benches.
The assumed SMU has been determined based on the
assumption of a production scenario utilising small to
medium size earthmoving equipment (for reference; 125
tonne excavator, plus CAT 777 or equivalent haul trucks).
In the experience of the Competent Person,this

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Criteria JORC Code explanation Commentary
equipment selection may be considered typical for a
deposit of the size and style of Carlow Castle.
Any assumptions about correlation
between variables
No assumptions have been made regarding the correlation
of variables.
Description of how the geological
interpretation was used to control the
resource estimates.
Logged geology, alteration and structural controls were
used in the interpretation of lodes within the resource
model. Hard boundaries were used for estimation
between mineralised domains.
Discussion of basis for using or not using
grade cutting or capping.
For the estimate of grades, high-grade cuts were applied
to reduce the influence of extreme outliers. These values,
determined by statistical analysis including review of CV
values, histograms, log-probability plots and mean-
variance plots.
The process of validation, the checking
process used, the comparison of model
data to drillhole data, and use of
reconciliation data if available.
Standard model validation was completed using numerical
methods (histogram and swath plots) and validated
visually in section and 3D against the input raw drillhole
data, composites and blocks.
Moisture Whether the tonnages are estimated on a
dry basis or with natural moisture, and the
method of determination of the moisture
content.
Tonnages have been estimated on a dry basis.
Cut-off
parameters
The basis of the adopted cut-off grade(s) or
quality parameters applied.
The Mineral Resources were reported at a 0.3 ppm Au.Eq
cut-off, within a Whittle™ theoretical optimisation that
used the following factors:
• 50° overall slope angle
• Oxide, Transitional and Fresh used same recoveries /
processing costs
• $48.1 / tonne processing (includes refining, insurance
and G&A)
• Recoveries, which in Artemis’ opinion have a
reasonable potential to be achieved, are:
• 85% Cu recovery
• 94.8% Au recovery
• 73% Co recovery
• Mining Costs $ / tonne incremented by depth (coded
into each block in the model by RL), ranging from $2.57
through to $5.77 inclusive
• Prices:
o Cu $9,400 / tonne
o Au $2,200 / oz
o Co $50,000 / tonne
• 2.5% royalty per ounce payable on gold produced. 5%
royalties per tonne payable on both copper and cobalt
produced.
• Au.Eq was calculated from a combined weighted grade
of Au, Cu, Co using the same commodity prices and
metallurgical recoveries as the optimisation.
Au.Eq = Au (ppm) + Cu (%)x1.19 + Co (%) x 5.44
Mining factors
or
assumptions
Assumptions made regarding possible
mining methods, minimum mining
dimensions and internal (or, if applicable,
external) mining dilution. It is always
necessary as part of the process of
determining reasonableprospectsfor
Open pit mining is considered as the appropriate method
for future studies, and the Competent Person believes that
there are reasonable prospects for eventual economic
extraction based on the outputs of the Whittle
optimisation completed.

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Criteria JORC Code explanation Commentary
eventual economic extraction to consider
potential mining methods, but the
assumptions made regarding mining
methods and parameters when estimating
Mineral Resources may not always be
rigorous. Where this is the case, this should
be reported with an explanation of the
basis of the mining assumptions made.
A minimum mining width of 2 m was applied (downhole
composite width). No other mining assumptions were
made.
Detailed mining assumptions such as dilution and
minimum mining widths will be included in any
optimisation, detailed mine planning and Life of Mine plan.
Metallurgical
factors or
assumptions
The basis for assumptions or predictions
regarding metallurgical amenability. It is
always necessary as part of the process of
determining reasonable prospects for
eventual economic extraction to consider
potential metallurgical methods, but the
assumptions regarding metallurgical
treatment processes and parameters made
when reporting Mineral Resources may not
always be rigorous. Where this is the case,
this should be reported with an
explanation of the basis of the
metallurgical assumptions made.
Preliminary metallurgical testwork was conducted by ALS
Metallurgy in 2019 focussing on the metallurgical
amenability of selected samples to a conventional gravity
gold, cyanide leach and flotation processes.
Results are detailed below:
Gold
• 48% of gold by testwork on metallurgical samples was
recovered using gravity separation, and most of the
balance of the non-gravity gold is recoverable in
sulphide concentrates as a by-product using standard
flotation.
Copper
• Quick floating copper minerals produced a high-grade,
premium copper concentrate of approximately 30% Cu.
• Deleterious elements including arsenic may be
managed with a light concentrate polishing using
regrind or blend control. Recoveries depended on
mineralogy, with 77–85% copper recoveries achieved.
• Unrecovered copper minerals are predominantly
represented by non-floating silicates or secondary
oxide copper minerals.
Cobalt
• Cobalt recoveries ranged from 73–79%. Saleable Cobalt
concentrate grades ranging 2.3–5.3% Co were
produced. Cobaltite (CoAsS) is the dominant cobalt
bearing mineral and is therefore intrinsically linked to
arsenic affecting its sale price.
Artemis believe the gold recovered by metallurgical
testwork could be sold in concentrates as a credit or
recovered on site using a cyanide leach process.
Acid soluble copper testwork has been completed for
oxide and transitional ore and estimated in the block
model by inverse distance (ID2) to guide additional
metallurgical sampling.
CSA Global recommend additional metallurgical programs
across the Mineral Resource incorporating results from
acid soluble copper and multi-element analysis. Further
geometallurgical
testwork
to
develop
quantitative
mineralogy and rock mass studies is also recommended.
Environmental
factors or
assumptions
Assumptions made regarding possible
waste and process residue disposal
options. It is always necessary as part of
the process of determining reasonable
prospects for eventual economic extraction
to consider the potential environmental
impacts of the mining and processing
operation. While at this stage the
No assumptions regarding possible waste and process
residue disposal options have been made.
Sulphur and arsenic have been estimated into the model
to allow the assessment of potentially acid forming
minerals and other environmentally sensitive residue.

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Criteria JORC Code explanation Commentary
determination of potential environmental
impacts, particularly for a greenfields
project, may not always be well advanced,
the status of early consideration of these
potential environmental impacts should be
reported. Where these aspects have not
been considered, this should be reported
with an explanation of the environmental
assumptions made.
Bulk density Whether assumed or determined. If
assumed, the basis for the assumptions. If
determined, the method used, whether wet
or dry, the frequency of the measurements,
the nature, size and representativeness of
the samples.
For mineralisation, downhole geophysical gamma density
was used to estimate density by OK using the relevant
variogram and estimation parameters for each statistical
domain.
Only sample points that had a calliper measurement of not
more than 20% of the nominal hole diameter for each hole
type were included in the analysis and data for estimation.
The gamma density was visually correlated point-by-point
to each overlapping water immersion determination of
specific gravity on HQ3 core, which found a strong
correlation.
The size and range of lengths of density determinations are
considered by the Competent Person to be robust. A
correlation of 0.05 was calculated between sample lengths
and density determinations, confirming that the sample
length has no impact on the density.
The gamma-density of the RC hole is weakly low-biased
compared to the diamond core density, while the gamma-
density of the diamond hole is very weakly high-biased.
Sample points were composited to 1 m length prior to
estimation.
Waste densities were applied from nominal values.
The bulk density for bulk material must
have been measured by methods that
adequately account for void spaces (vugs,
porosity, etc.), moisture and differences
between rock and alteration zones within
the deposit.
The
gamma
determines
a
quantitative,
in
situ
measurement of density that accounts for void spaces. The
measurements have been calibrated to regular calibration
holes in iron ore deposits in the Pilbara, and on materials
at the contractor’s facility.
The water immersion method measurements were
determined by measuring the weight of part or the entire
sample in air and water and then applying the formula bulk
density = weight_air/(weight_air-weight_water). Samples
of drill core were sealed with a masonry sealant/wax and
allowed to dry prior to bulk density determination.
The estimate of density was undertaken within oxidation
domains in the mineralisation.
Discuss assumptions for bulk density
estimates used in the evaluation process of
the different materials.
The gamma density data were considered sufficient in
number for all material types, quantitative and unbiased
when large calliper deviations from the nominal hole
diameter were removed. Calibration was undertaken using
comparison to other holes and to density measured by
water immersion. The approach adopted is considered
robust.
Classification The basis for the classification of the
Mineral Resources into varying confidence
categories.
The MRE was classified as Inferred based on the level of
geological understanding of the mineralisation, quality of
samples, density data, drillhole spacing, historical nature
of the drilling,detail of metallurgical information available

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Criteria JORC Code explanation Commentary
for soluble / insoluble copper speciation and sampling and
assaying processes.
Whether appropriate account has been
taken of all relevant factors (i.e. relative
confidence in tonnage/grade estimations,
reliability of input data, confidence in
continuity of geology and metal values,
quality, quantity and distribution of the
data).
The classification reflects the overall level of confidence in
mineralised domain continuity based the mineralisation
drill sample data numbers, spacing and orientation.
Overall mineralisation trends are reasonably consistent
within the various lithotypes over numerous drill sections.
Whether the result appropriately reflects
the Competent Person’s view of the
deposit.
The Mineral Resource classifications applied appropriately
reflect the view of the Competent Person.
Audits or
reviews
The results of any audits or reviews of
Mineral Resource estimates.
Internal audits were completed by CSA Global which
verified the technical inputs, methodology, parameters
and results of the estimate.
Discussion of
relative
accuracy/
confidence
Where appropriate, a statement of the
relative accuracy and confidence level in
the Mineral Resource estimate using an
approach or procedure deemed
appropriate by the Competent Person. For
example, the application of statistical or
geostatistical procedures to quantify the
relative accuracy of the resource within
stated confidence limits, or, if such an
approach is not deemed appropriate, a
qualitative discussion of the factors that
could affect the relative accuracy and
confidence of the estimate.
The accuracy of the MREs is communicated through the
classification assigned to the various parts of the deposits.
The MREs have been classified in accordance with the
JORC Code (2012 Edition) using a qualitative approach. All
factors that have been considered have been adequately
communicated in Section 1 and Section 3 of this table.
The MRE statement relates to a global estimate of in-situ
tonnes and grade.
The statement should specify whether it
relates to global or local estimates, and, if
local, state the relevant tonnages, which
should be relevant to technical and
economic evaluation. Documentation
should include assumptions made and the
procedures used.
The accuracy of the MREs is communicated through the
Inferred classification assigned to the deposit. The MRE
has been classified in accordance with the JORC Code. All
factors that have been considered have been adequately
communicated in Section 1, Section 2 and Section 3 of this
table.
The MRE statement relates to a global estimate of in-situ
tonnes and grade.
These statements of relative accuracy and
confidence of the estimate should be
compared with production data, where
available.
No production data are available.

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