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Artemis Resources Limited Capital/Financing Update 2021

May 19, 2021

10429_rns_2021-05-19_3bbf6390-8550-452c-85c9-2da971000327.pdf

Capital/Financing Update

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20 May 2021

ASX Announcement

Carlow Castle Update and Proposed Capital Raise.

Artemis (“the Company”) today announces that it is now in receipt of guidance from the independent mineral resource consultants (“CSA”) currently estimating the new mineral resource statement for the Carlow Castle Project.

The updated resource estimate is based upon an additional 129 drill holes of drilling completed during October 2020 to March 2021. The drilling completed included a change in orientation in high grade zones that was better orientated to intersect mineralisation at a more representative angle. This additional data has had a material difference on the preliminary mineral resource estimate. As such from this guidance we can report that gold grades and contained ounces have declined, copper tonnes have risen but grade fallen and cobalt tonnes remained static but grades declined compared to those previously reported in the 2019 resource update reported to the ASX on 20 November 2019.

A copy of that guidance has been provided by CSA below.

Upon receiving verbal guidance from the mineral resource consultants at 7am EST on 17 May 2021 the Company immediately commenced taking steps to understand the impact of the new drilling on the updated resource estimate. The timing to conclude the final report is estimated at two weeks and the Company will, upon receipt, release this to shareholders.

The Company has now ceased resource drilling activity at Carlow Castle, and upon receipt of the final resource estimation for Carlow Castle from CSA, the Company will undertake a review to determine next steps in moving the Carlow Castle project forward.

However, mineralisation at Carlow remains open in multiple directions and several exploration targets have been identified and are yet to be drill tested. The Greater Carlow Castle tenements remain highly prospective for gold and copper mineralisation.

Artemis intend to refine the current drill targeting to optimise targeting higher grade mineralised zones as part of the Carlow Castle deeps identified at the eastern end of the deposit.

As a consequence of this news, the Board have taken the decision to defer drilling and cancel the proposed capital raise announced to the ASX on 12 May 2021.

The Company has a significant cash and marketable securities balance of $3.7m.

The Company’s primary focus in the short term remains expediting the planning and approvals process for the upcoming Paterson Central drill programme which continues at pace and remains totally unaffected by these developments announced today.

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Mineral Resource Statement

The Mineral Resource for the Carlow Castle Project as at 19 May 2021 is presented below. All three deposits are open at depth, and Quod Est and Cross-cut are open along strike.

The difference in methodology in the determination of the 2019 and 2021 resource estimate is outlined below.

CSA Global Mineral Resource Guidance

Table 1. Carlow Castle Mineral Resources by classification reported above a cut-off of 0.3 g/t AuEq within an optimised pit shell (current as at 19 May 2021)

‘000 Tonnes **AuEq (g/t) ** **Au(g/t) ** **Cu(%) ** **Co(%) ** **Au(koz) ** **Cu(kt) ** Co(kt)
Oxide 4,400 0.9 0.4 0.3 0.04 53 13 2
Transitional 3,100 1.6 0.7 0.5 0.06 67 15 2
Fresh 6,900 1.7 0.9 0.4 0.06 199 26 4
Total 14,300 1.4 0.7 0.4 0.05 320 53 7

Competent Person Statement

The information in this announcement 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 announcement of the matters based on this information in the form and context in which it appears.

2021 Resource Estimate

The Mineral Resources for the Carlow Caste Project has been estimated, using all drilling data available as at 16 April 2021. The mineralisation for the Carlow Main, Quod Est and Cross-Cut deposits have been interpreted, and grades of Au, Cu and Co estimated. An open pit optimisation has been completed to constrain the reported Mineral Resource. Compared to the previously reported Mineral Resource Estimate, this current estimate includes an additional 129 drillholes for 22,395m, drilled mainly at the eastern end of the Carlow Main deposit, and in the newly discovered Cross-Cut deposit.

Previous Resource Estimate (2019)

In November 2019, CSA Global estimated Inferred Mineral Resources at Carlow Main 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.

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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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 parameters presented in Table 2.

Table 2: Carlow Castle 2019 Resource Mining and Metallurgical Assumptions

Input Value
Overall Slope Angles 50°
Processing Cost $48.1/t
Gold Recovery 94.8%
Copper Recovery 85%
Cobalt Recovery 73%
Mining Costs $2.57/t to $5.77/t, incremented by depth
Gold Price $2,000/oz
Copper Price $9,000/t
Cobalt Price $48,000/t
Au Royalty 2.5%
Cu Royalty 5%
Co Royalty 5%

Geology and Geological interpretation

The Carlow Castle Project is hosted by mainly mafic Archean volcanic arc rocks. The Carlow Castle Main and Quod Est deposits are hosted within structurally controlled, mineralised zones occurring almost at right-angles to each other. The recently defined Cross-Cut deposit is located approximately 200 m north of north of Carlow Main and strikes north-south, sub-parallel to Quod Est (Figure 1).

Mineralisation is hosted within chloritic shear zones in basalts focussed along contacts between the host basalt and footwall and hanging wall gabbro units. At Carlow Main, mineralisation dips steeply north at the western end, while at the eastern end the mineralisation dips steeply south. The Carlow Main deposit strikes over 1.2 km and is partially oxidised to depths of 40 m to as much as 100 m in the east. Mineralisation trends at are complex with gold, copper, cobalt occurring across multiple lithologies, with limited structural control.

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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The Quod Est and Cross-Cut mineralisation is hosted by north-south chloritic shear zones, and are partially oxidised above 25 m.

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Figure 1: Map of Carlow Castle deposits with drillhole traces

Geological modelling was undertaken using Leapfrog Geo software. Mineralisation wireframes were generated using indicator interpolants based on copper and gold cut-off grades. These defined concentric high and low grade domains.

Low-grade copper domains (Domains 10, 20,30, and 32) (Table 3) were defined using a lower indicator cut-off grade of 200 ppm Cu, and a probability of 0.5; high-grade domains were defined generated using a cut-off grade of 500 ppm Cu, and probabilities of 0.2 to 0.8, in 0.1 increments. A very high grade gold domain (Domain 12) at the eastern end of Carlow Main was interpreted around four high grade gold intersections at a 0.5g/t Au cutoff. The domain interpretation for Carlow CMain was constrained to above the -600mRL, and for Quod Est and Cross-Cut to the -150mRL.

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Table 3: Mineralisation Domain descriptions

Deposit Domain Code Description
Carlow Main 10 Low-grade zone – Cu, Co +/- Au
Carlow Main 11 High-grade zone – Au, Cu, Co
Carlow Main 12 Very high-grade zone – Au, Cu, Co
Quod Est 20 Low-grade zone – Cu, Co +/- Au
Quod Est 21 High-grade zone – Au, Cu, Co
Cross Cut 30 Low-grade zone – Cu, Co +/- Au
Cross Cut 31 High-grade zone – Au, Cu, Co
Cross Cut 32 Low-grade zone – Cu, Co +/- Au
Cross Cut 33 High-grade zone – Au, Cu, Co

Drilling Techniques

A summary of all drilling is provided in Table 4. The total number of drill holes informing the MRE update is 330, comprising 307 RC and 23 diamond core for a total of 47,139 drill metres. Holes were drilled by a Schramm TD685 rig for RC and an Evolution FH3000 rig for diamond core holes.

Table 4: Drilling History

Year(s) Company No. of holes Hole type Hole size (mm) Metres Hole ID (from) Hole ID (to)
2017 Artemis 81 RC 133 7,357 ARC001 ARC081
2018 Artemis 108 RC 133 15,882 ARC082 ARC189
2018 Artemis 12 DD 96.1 (HQ3) 1,505 18CCAD001 18CCAD012
2020* Artemis 62 RC 133 7,574 ARC190 ARC254
2020* Artemis 11 DD 96.1 (HQ3) 3,788 20CCAD001 20CCAD010
2021* Artemis 56 RC 133 11,033 ARC255 ARC309

*new data for the 2021 MRE update

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Sampling Techniques

RC samples were collected using a face-sampling 115 mm diameter bit via the inner tube to a rig-mounted, Sandvik tri-cone splitter to yield subsamples of approximately 3 kg from a 1 m sample length. The average sample recovery for 1 m RC samples for 16,115 records was 96.5%.

All core was collected by HQ3 sized triple-tube core barrels. Sample intervals ranged from 0.1 to 1.5 m, with an average of 1 m. The average sample recovery for core samples for 1,690 records was 97.3%.

Core from 2020 was cut in half using a diamond core saw, while the 2018 core was cut into two quarters. One half of the core from 2020 and one quarter core from 2018 was sampled by placing into numbered calico bags, which were tied and placed in plastic or polyweave bags.

Sample preparation consisted of drying, riffle splitting samples >3 kg, coarse crushing, pulverising to >85% passing 75 microns and homogenising the pulp.

Sample Analysis Method

All samples were assayed by ALS in Perth. The counts of the lab methods used, and upper limits for the methods, are shown in Table 5.

Table 5: Count of lab assay methods used by variable, ordered by variable

Variable Lab
Method
Code
Generic
Method
Name
Description Count Range (g/t) Max
Value
(g/t)
Cu ME-ICP61
ME-ICP61A
Cu-OG62
4A_ICPES
4A_ICPES
4AOG_UN
0.25 g sample, four acid
digest with ICP-AES finish
0.4 g sample, four acid digest
with ICP-AES finish
0.4 g sample, four acid digest
with “ore grade” over-limit
finish
43,758
170
931
1–10,000
1–100,000
1,000–500,000
10,000
32,700
157,000
Au Au-AA25
Au-AA26
Au-DIL26
FAOG_AAS
FAOG_AAS
DIL_UN
30 g sample, fire assay, AAS
finish
50 g sample, fire assay, AAS
finish
Unknown
852
43,073
3
0.01–100
0.01–100
?
23.6
100
108
Co ME-ICP61
ME-ICP61A
Co-OG62
4A_ICPES
4A_ICPES
4AOG_UN
0.25 g sample, four acid
digest with ICP-AES finish
0.4 g sample, four acid digest
with ICP-AES finish
0.4 g sample, four acid digest
with “ore grade” over-limit
finish
43,758
170
99
10–10,000
10–50,000
500–300,000
10,000
6,800
65,400

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Estimation methodology

Drillholes were composited to 1m downhole lengths, within each of the interpreted mineralisation domains. Statistical analysis indicated there is no significant change in gold, copper and cobalt grades between oxide, transitional, and fresh mineralisation types. There is a moderate correlation between gold and copper, and weaker correlation of between gold and cobalt. Copper and cobalt are moderately correlated.

Grade outliers were treated by reviewing the histograms, log-probability plots and mean-variance plots for each domain variable; topcuts were applied to reduce the risk of local over-estimation (Table 6).

Table 6: Top cuts applied by Domain and Element

Deposit Domain Au Cu Co
Carlow Main 10 50 20,000 10,000
11 50 50,000 10,000
12 50 150,000* 30,000*
Quod Est 20 50 20,000* 10,000
21 50 50,000* 10,000
Cross Cut 30 50 10,000 2,000
31 50 50,000 5,000
32 50 10,000* 2,000
33 50 50,000 5,000

Normal score experimental variograms were generated in the strike, dip and across-strike directions. The direction of maximum continuity for gold, copper, and cobalt at Carlow Main was modelled with moderate east plunges whereas Quod Est was modelled with steep north plunges. Kriging neighbourhood analysis was completed to optimise the estimation search parameters. The maximum number of samples allowed per each individual drill hole per estimate, was set to six.

Grades were then estimated using Ordinary Kriging into a block model with a block size of 20 mE by 10 mN by 10 mRL. Domain boundaries were treated as hard; only composites within a domain were used to estimate blocks within that domain.

Downhole gamma-density readings composited to 1 m were used to estimate density in mineralised domains in the block mode. Waste densities were assigned from assumed values.

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Cutoff Grades

For reporting, an Au equivalent (AuEq) cutoff grade of 0.3ppm Au was applied to the block model. The AuEq was calculated by a weighted average of the three components of Au, Cu and Co (Table 7), using the same commodity prices and metallurgical recoveries as the optimisation. The formula for the Au equivalent is:

Au.Eq = Au (ppm) + Cu (%)x1.19 + Co (%) x 5.44

Table 7: Au Equivalent calculation derivation

Element Price Realised Price per unit Unit Realised Price per unit Unit Recovery % In Situ Unit Price Unit Au Eq Factor In Situ Unit Price Unit Au Eq Factor In Situ Unit Price Unit Au Eq Factor
Au 2200 70.74 $/g 95% 67.1 $/g 1.00
Cu 9400 9400 $/t 85% 79.9 $/t 1.19
Co 50000 50000 $/t 73% 365.0 $/t 5.44

Resource Classification

The Mineral Resource has been classified as Inferred. The classification level is based upon assessment of geological understanding of the deposit, geological and mineralisation continuity, drill hole spacing, QC results, search and interpolation parameters, analysis of available density information and current metallurgical testwork.

Mining and Metallurgical factors

In 2019, ALS Metallurgy in Perth completed preliminary metallurgical testwork on two 100 kg drill core composite samples. The metallurgical testwork demonstrated a potential Carlow Castle ore flowsheet utilising gravity and cyanide leach for gold, and flotation to produce copper and cobalt concentrates.

  • 48% of the 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. The total recovery of gold achieved was 94.8%

  • 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 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.

The mining and metallurgical factors used for the current resource estimate are presented in Table 8. They are largely unchanged from 2019, with the exception of the mining cost and the metal prices.

In the Company’s opinion all elements have reasonable potential to be recoverable and sold.

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Table 8: Carlow Castle 2021 Resource Mining and Metallurgical Assumptions

Input Value
Overall Slope Angles 50°
Processing Cost $48.1/t
Gold Recovery 94.8%
Copper Recovery 85%
Cobalt Recovery 73%
Mining Costs $2.57/t to $6.35/t, incremented by depth
Gold Price $2,200/oz
Copper Price $9,400/t
Cobalt Price $50,000/t
Au Royalty 2.5%
Cu Royalty 5%
Co Royalty 5%

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Figure 2: Oblique view of the Carlow Castle Inferred Resource pit optimisation; blocks coloured by Au grade

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Figure 3: Oblique view of the Carlow Castle Inferred Resource pit optimisation; blocks coloured by Cu grade

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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This announcement was approved for release by the Board.

For further information contact:

Alastair Clayton Executive Director [email protected]

Boyd Timler Executive Director [email protected]

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Artemis Resources – Carlow Castle JORC 2012 Table 1

JORC 2012 Table 1 Section 1 – Sampling Techniques and Data

Criteria JORC Code explanation Commentary
Sampling
techniques
Nature and quality of sampling (e.g. cut
channels, random chips, or specific specialised
industry standard measurement tools
appropriate to the minerals under
investigation, such as downhole gamma
sondes, or handheld XRF instruments, etc.).
These examples should not be taken as limiting
the broad meaning of sampling.
Sampling consisted of reverse circulation (RC) and ¼ core
HQ3 sized diamond samples.
Geophysical data, including gamma, density, resistivity and
hole calliper, were collected downhole by Wireline Services
Group (WSG) using industry standard, calibrated tools.
Include reference to measures taken to ensure
sample representivity and the appropriate
calibration of any measurement tools or
systems used.
The entire RC and diamond drilling sample was extracted
prior to subsampling at surface next to the rig. Diamond and
RC field duplicates were taken on selected intervals within
the
interpreted
mineralised
horizons
to
measure
representativity of sample splits.
Aspects of the determination of mineralisation
that are Material to the Public Report. In cases
where ‘industry standard’ work has been done
this would be relatively simple (e.g. ‘reverse
circulation drilling was used to obtain 1 m
samples from which 3 kg was pulverised to
produce a 30 g charge for fire assay’). In other
cases more explanation may be required, such
as where there is coarse gold that has inherent
sampling problems. Unusual commodities or
mineralisation types (e.g. submarine nodules)
may warrant disclosure of detailed information
1 m RC samples comprised 39,930 m or 91%, HQ3 quarter
and half core samples comprised 3,998 m or 9%.
Sample intervals for RC and Diamond ranged from 0.3 m –
1.5 m, of which 97% are 1 m length.
Sample preparation consisted of coarse crushing a maximum
of 3 kg of the submitted sample, pulverising to >85% passing
75 microns and homogenising the pulp.
The original assay technique used for copper and cobalt
involving digesting a 0.25 g sample (by four acid digest) and
ICP-AES finish.
Both 30 g and 50 g sample sizes were chosen for analysis of
gold, with fire assay fusion and detection by atomic
absorption spectrometry (AAS).
Drilling
techniques
Drill type (e.g. core, reverse circulation, open-
hole hammer, rotary air blast, auger, Bangka,
sonic, etc.) and details (e.g. core diameter,
triple or standard tube, depth of diamond tails,
face-sampling bit or other type, whether core is
oriented and if so, by what method, etc.).
Drillhole data comprised 330 holes, consisting of 397 RC and
23 HQ3 diamond holes. Holes were drilled by TopDrill. RC by
a Schramm TD685 rig and diamond by an Evolution FH3000
rig.
RC samples were collected using a face-sampling, 4.5-inch
diameter bit via the inner return tube to a rig-mounted,
Sandvik tri-cone splitter.
All diamond core was collected by HQ3 sized triple-splitter
core barrels. Core was orientated by ReflexTMorientation
tools.

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Criteria JORC Code explanation Commentary
Drill sample
recovery
Method of recording and assessing core and
chip sample recoveries and results assessed.
CSA Global did not supervise previous drill programs,
however Artemis have provided the following guidelines for
drill sample recovery which CSA Global consider as adequate.
Sample recoveries were recorded by the field geologist in the
field during logging and sampling. Cor recoveries were
calculated based on nominal run lengths versus measured
length of recovered core.
• If poor sample recovery is encountered during drilling, the
supervising geologist and driller endeavour to rectify the
problem to ensure maximum and representative sample
recovery.
• Visual assessments by a field geologist were made for
moisture, and possible contamination. Minor damp samples
were encountered, and the field geologist and driller ensured
cleanliness of cyclone and splitter was maintained.
• A cyclone and static cone splitter were used to ensure
representative sampling and were routinely inspected and
cleaned.
• Sample recoveries during drilling completed by Artemis
were high with average recovery for RC 1 m samples of 96.5%
and 97.3% for DD samples. Almost all samples were dry.
Measures taken to maximise sample recovery
and ensure representative nature of the
samples.
Triple-tube HQ core drilling was completed to maximise
diamond core recoveries.
Diamond drilling was completed to assist in validating the
results from the RC samples and no identifiable bias was
observed.
Twin hole analysis showed good correlation between
diamond and RC holes analysed.
Whether a relationship exists between sample
recovery and grade and whether sample bias
may have occurred due to preferential
loss/gain of fine/coarse material.
No relationship between sample recovery and grade has
been analysed.
Logging Whether core and chip samples have been
geologically and geotechnically logged to a
level of detail to support appropriate Mineral
Resource estimation, mining studies and
metallurgical studies.
All RC and diamond drillholes were geologically logged to an
industry standard appropriate for the mineralisation present
at the project.
All drill chip samples were geologically logged at 1 m intervals
from surface to the bottom of each drillhole.
Diamond core was photographed, and RC chips were
retained in chip trays for future reference.
The Competent Person considers that the level of detail is
sufficient for the reporting of Mineral Resource estimation.

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Criteria JORC Code explanation Commentary
Whether logging is qualitative or quantitative
in nature. Core (or costean, channel, etc.)
photography.
Lithological logging is qualitative in nature. Logged intervals
were compared to the quantitative geochemical analyses and
geophysical logging to validate the logging.
Quantitative logging was provided by downhole geophysical
density completed on 156 of 201 holes, averaging 75% of the
total hole depth, by WSG in open holes within two months of
the completion of drilling.
The Competent Person considers that the availability of
qualitative and quantitative logging has appropriately
informed the geological modelling, including weathering and
oxidation, water table level and rock type.
The total length and percentage of the relevant
intersections logged.
The total length of all drilling was geologically logged, and an
average of 75% of the total hole depth was quantitatively
logged for geophysical responses by WSG.
Subsampling
techniques and
sample
preparation
If core, whether cut or sawn and whether
quarter, half or all core taken.
For drilling in 2017 and 2018 diamond core was cut into two
quarters and one half using a diamond core saw. One of the
quarters was placed into a numbered calico bag, which was
tied and placed in a plastic/polyweave bag.
For drilling in 2020 and 2021 diamond core was cut into two
halves using a diamond core saw. One of the halves was
placed into a numbered calico bag, which was tied and placed
in a plastic/polyweave bag.
If non-core, whether riffled, tube sampled,
rotary split, etc. and whether sampled wet or
dry.
RC samples were collected via a rig-mounted, Sandvik tri-
cone splitter to yield sub samples of approximately 3 kg from
a 1 m sample length.
For all sample types, the nature, quality and
appropriateness of the sample preparation
technique.
Sample preparation consisted of drying, riffle splitting
samples >3 kg, coarse crushing, pulverising to >85% passing
75 microns and homogenising the pulp. The Competent
Person considers these methods appropriate for this style of
mineralisation.
Quality control procedures adopted for all
subsampling stages to maximise representivity
of samples.
Artemis inserted 17 Internal Reference Standards (IRMs) of
which 11 were used in the 2020 and 2021 drilling in the
Mineral Resource update. IRMs “18A” to “18F” and “A” to
“F” were of significant numbers and were partially matched
with the mineralisation types and matrices (matrix matched)
of materials comprising the Mineral Resources. The
Competent Person considers these IRMs to have been
produced under a rigorous methodology.
RC and diamond field duplicates for the 2020 and 2021
drilling totalled 1,166. 1,160 IRMs and 200 blank samples
were inserted with routine samples at the rate of
approximately one standard, blank or duplicate in every 20
samples.
Campaign-based analysis and reporting of quality control
(QC) data was undertaken of blanks, field duplicates,
laboratory repeats, laboratory blanks, repeats and IRMs in
several groups of batches, and as a project-wide group of all
results.

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Criteria JORC Code explanation Commentary
Laboratory duplicate checks (pulp duplicates) numbered 905,
which represents duplication of 4.2% of the 2020 and 2021
dataset. Repeatability between duplicate pairs was very high.
Gold assays show a broader scatter within the duplicate
samples than the Copper and Cobalt whose majority of
samples fall within a +/-10% range. IRMs reflect the expected
values of Au and Cu relatively well (suitably accurate), though
precision of gold was considered poor, and homogenisation
of the IRMs requires addressing.
Measures taken to ensure that the sampling is
representative of the in-situ material collected,
including for instance results for field
duplicate/second-half sampling.
Artemis inserted field duplicates to monitor sampling
precision.
Downhole geophysical data were collected within two
months of the drilling for both 2017 and 2018 drilling
campaigns by WSG in open holes.
Whether sample sizes are appropriate to the
grain size of the material being sampled.
Sample sizes are considered to be appropriate to the grain
size of the material being sampled.
Quality of
assay data and
laboratory
tests
The nature, quality and appropriateness of the
assaying and laboratory procedures used and
whether the technique is considered partial or
total.
All 44,006 primary samples were assayed by ALS in Perth,
which is a National Association of Testing Authorities (NATA)
Australia accredited organisation.
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.
For some samples, the sample grades did not exceed the
upper limit of the ME-ICP61A, but a method with a higher
upper limit, being Cu-OG62 for copper and Co-OG62 cobalt,
was used to provide more confidence in the analyses.
In order of decreasing preference, the methods loaded into
the assay table of the database for use in the MRE were: Cu-
OG62/Co-OG62; ME-ICP61A; ME-ICP61.
Both 30 g and 50 g sample sizes were chosen for analysis of
gold, with fire assay and determination by AAS. The limit of
100 g/t was not reached for any samples. The larger sample
size of 50 g was predominantly selected to provide greater
confidence in the analyses. CSA Global has no information on
the Au-DIL26 method, however this method was not used on
a significant proportion of assays.
For geophysical tools, spectrometers, handheld
XRF instruments, etc., the parameters used in
determining the analysis including instrument
make and model, reading times, calibrations
factors applied and their derivation, etc.
The gamma signatures of selected drillholes were logged in
counts-per-second
(cps)
by
WSG.
These
wireline
measurements were then converted to physical property
values using calibrations determined specifically for each
physical property parameter, which produced a density value
based on the mineral assemblage’s present.
The data were provided as an average over 10 cm downhole
spacings for 97% of the readings,1 m for 3% of the readings

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

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Criteria JORC Code explanation Commentary
and a single reading of 3 m. The gamma-density records
numbered 117,859, of which 7,480 (6%) and 110,379 (94%)
are derived from diamond and RC holes respectively.
Nature of quality control procedures adopted
(e.g. standards, blanks, duplicates, external
laboratory checks) and whether acceptable
levels of accuracy (i.e. lack of bias) and
precision have been established.
The gamma-density readings were calibrated by logging of
calibration material at the WSG facility prior to mobilisation
to site.
Verification of
sampling and
assaying
The verification of significant intersections by
either independent or alternative company
personnel.
Senior Artemis geological staff collected and inspected the
samples. On behalf of the Competent Person, Mr Matt Clark,
Senior Resource Geologist inspected several significant
intersections of diamond core. 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.
The use of twinned holes. Diamond holes were drilled to infill areas of RC holes, and
diamond sample results showed moderate correlation to the
nearest RC sample results. A slight bias was observed for Au,
Cu, Co for RC versus diamond assay grades.
Documentation of primary data, data entry
procedures, data verification, data storage
(physical and electronic) protocols.
The data entry, storage and documentation of primary data
was completed on Microsoft Excel spreadsheets and local
hard drives, then imported into a central database managed
by CSA Global.
Discuss any adjustment to assay data. No adjustments or calibrations have been made to any assay
data.
Location of
data points
Accuracy and quality of surveys used to locate
drillholes (collar and downhole surveys),
trenches, mine workings and other locations
used in Mineral Resource estimation.
All hole collars were surveyed by differential global
positioning system (DGPS).
Down-hole locations were predominantly surveyed by
gyroscope, equating to 95% of the total metres surveyed.
Gyroscope values in the database were recorded every 30 m,
except diamond hole 18CCAD001, and RC holes ARC190 to
ARC222 (inclusive) which include records every 10 m. Holes
were also surveyed by Reflex EZ TracTM down-hole camera.
Another unknown method (“UNK”) existed in the database
for the survey records of the collar of RC holes ARC033 and
ARC105, and another record of the latter at 66 m, both of
which had no additional records. The maximum depths of
these holes were 22 m and 66 m. The survey data for ARC033
derive from the planned hole azimuth and dip, and the survey
data for ARC105 derive from DGPS collar survey
measurement, which has been copied to the maximum
depth.
Specification of the grid system used. Topographic data were captured in GDA94 MGA Zone 50 grid
system.
Quality and adequacy of topographic control. A topographic surface was built from high-resolution 5 m
Unmanned Aerial Vehicle (UAV) point data with a resolution
of 10 cm. The Competent Person considers that the surface is
suitable for this Mineral Resource estimate.

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Criteria JORC Code explanation Commentary
Data spacing
and
distribution
Data spacing for reporting of Exploration
Results.
The mineralisation has been defined by two orthogonal
drilling grids to intersect the east-striking Carlow Main lodes
and north-striking Quod Est lodes. The southern boundary of
the Quod Est drilling grid adjoins the northern boundary of
the Carlow Main grid at its central-western area. Aside from
minor mineralisation extension, infill drillholes and several
interpretation-controlling scissor holes, drilling is regularly
spaced 20 m apart on 40 m spaced sections, nominally
averaging –60° dips, which has provided consistent support
to intersections of mineralisation and eliminated any
influence of hole angles on grade.
Drillholes that define the Carlow Main mineralisation lie on
35 sections that shift north or south perpendicular to the
sigmoidal curve that defines the mineralisation trend.
Drillholes in the western-section of the Carlow Main lodes
have been drilled to the south to intersect the very steeply
north-dipping lodes, until section 507,640 mE, where the
holes have been drilled to the north to intersect the very
steeply south-dipping lodes.
Drilling into the Quod Est mineralisation has been intersected
by east-west orientated holes lying on eight sections – two of
which are infill sections – perpendicular to a central easting
of 506,650 mE.
Drilling into the Cross-Cut mineralisation has been
intersected by three sections with east-west orientated drill
holes, two-sections with north-south orientated drill holes,
and three sections with south-west orientated drill holes.
Whether the data spacing and distribution is
sufficient to establish the degree of geological
and grade continuity appropriate for the
Mineral Resource and Ore Reserve estimation
procedure(s) and classifications applied.
The Competent Person believes the mineralised lenses have
sufficient geological and grade continuity to support the
classification applied to the Mineral Resources given the
current drill pattern.
Whether sample compositing has been
applied.
The down-hole intervals logged by the geologist as being
mineralised or showing significant alteration were sampled
and assayed at 1 m intervals. Compositing of samples
occurred for holes ARC036 to ARC081 only. All unmineralised
intervals (based on the field portable XRF readings for Cu, Co
and As) were composited and assayed over 3 m intervals.
Mineralized intervals based on the field XRF readings were
assayed in 1 m intervals.
If a 3 m composite returned assays above normal background
levels, these intervals were re-sampled and assayed at 1 m
intervals.
Orientation of
data in relation
to geological
structure
Whether the orientation of sampling achieves
unbiased sampling of possible structures and
the extent to which this is known, considering
the deposit type.
The regular spaced drilling on consistent sections, and the
orientations orthogonal to the strike of the lodes, have
provided
consistent
support
to
intersections
of
mineralisation to and minimised any bias or influence of hole
angles on grades.

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Criteria JORC Code explanation Commentary
If the relationship between the drilling
orientation and the orientation of key
mineralised structures is considered to have
introduced a sampling bias, this should be
assessed and reported if material.
No relationship has been noted between drillhole dip angle
and mineralisation.
A slight positive bias has been noted for Au, Cu, and Co for
drill
holes
with
azimuths
oriented
sub-parallel
to
mineralisation. The bias was limited to the eastern section of
Carlow Main and influence of high-grade sub-parallel drill
holes on the estimation controlled using a small volume
wireframe.
Sample
security
The measures taken to ensure sample security. Samples were bagged, and cable tied upon collection. The
chain of custody was managed by the supervising geologist,
who placed up to 10 calico sample bags in polyweave sacks,
clearly labelled with:

Artemis Resources Ltd

Address of laboratory

Sample range
The polyweave sacks were then loaded directly into a bulka
bag. Each hole was placed in a separate bag, and twice a week
the labelled bags would be collected and delivered to a
transport depot. These were then loaded directly onto a truck
and delivered direct to the laboratory. Each bulka bag or hole
had a separate sample dispatch, which became a separate
analytical batch at the laboratory.
Sample security was maintained through short collection and
delivery turnarounds and the use of secured transport yards.
Audits or
reviews
The results of any audits or reviews of
sampling techniques and data.
No external audit of sampling techniques and data has been
undertaken.

JORC 2012 Table 1 Section 2 – Reporting of Exploration Results

Criteria JORC Code explanation Commentary
Mineral
tenement and
land tenure
status
Type, reference name/number, location and
ownership including agreements or material
issues with third parties such as joint ventures,
partnerships, overriding royalties, native title
interests, historical sites, wilderness or national
park and environmental settings.
The project lies on tenement E47/1797-I, which is held by
KML No. 2 Pty Ltd (KML), a 100% owned subsidiary of
Artemis. The tenement was granted on 07/05/2008 and is
held in good standing.
According to the Department of Mines, Industry and
Regulation (DMIRS) of WA Mineral Titles Online system,
the tenement has an excised portion of land for the expired
tenement M47/385 (DMIRS, 2019).
The tenement is overlapped by a miscellaneous licence,
granted tenement L47/416 held conjointly by Stirling Bay
Holdings and Swan Bay Holdings.
The security of the tenure held at the time of
reporting along with any known impediments to
obtaining a licence to operate in the area.
The tenement is securely held by a 100% owned subsidiary
of Artemis and there are no impediments preventing the
operation of the Lease.

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Criteria JORC Code explanation Commentary
Exploration
done by other
parties
Acknowledgment and appraisal of exploration
by other parties.
Prior to its name as Carlow Castle, the Project area was
known first as Cooper’s.
Pre-1968
As early as the 1870’s, copper ore was mined at the area
formerly known as Glenroebourne. Gold was discovered in
the district in the late 1880’s and numerous, small gold and
gold-copper prospects, and minor silver, were worked to
1960. In the 1930’s, the area was investigated by North
Australian Aerial Geological, Geophysical Survey.
In 1964, Westfield Minerals NL undertook extensive
regional mapping and stream-soil sampling, and identified
and drilled geochemical, magnetic and induced polarisation
(IP) anomalies.
The Geological Survey of Western Australia (GSWA)
published a regional geology map in 1965.
1968 – 1972
In 1968, Consolidated Gold Mining Areas NL drilled seven
DD holes for 759 over mining claims MC387 and MC410,
which are now within E47/1797-I. The holes intersected
mineralisation containing three main chalcopyrite veins
ranging from 23 cm to 76 cm thickness and hosted up to
5.36% Cu, 17.14 g/t Au and 1.42% cobalt in separate 2 ft
samples. Geophysical work was carried out to improve
mineralisation targeting included magnetometer, self-
potential and IP surveys.
In 1969, in partnership with Roebourne Exploration and
Mining Ltd, Amax commenced exploration of the area by
275 wide-spaced magnetometer survey lines and 141 line-
miles of IP survey, 2,800 ft of auger drilling, 14,000 ft of
percussion drilling, 2,800 ft of DD and 475 ft costean/trench.
The details of the exploration program completed are unclear,
as the financing arrangements only allowed for partial
program completion. The trench revealed two vine structures
of high-grade mineralisation, with 8 m @ 1.73% Cu and 14
m @ 2.2% Cu within a wide low-grade copper mineralisation
halo grading 0.38% Cu that contained numerous anomalous
gold and cobalt results. However, Amax’s primary focus for
the drilling program was targeting IP anomalies to the north
of Carlow Castle that were coincident with a chert band
formed from a felsic volcanic horizon that yielded 10 ft @
2.5% zinc. The target was a stratiform zinc deposit, but
instead the source of the IP anomalies was identified as
pyrite, and so Amax lost interest in the project area.
1986 – Openpit Mining Ltd
In a report for Artemis inserted into the annual report for the
combined reporting group to the GSWA, Torbinup
Resources Pty Ltd noted that Openpit Mining Ltd explored
the known base metal mineralized areas for gold
mineralisation in 1986 and 1987, which included detailed
mapping of the main workings at Carlow Castle and the
drilling of 31 RC holes for 1,527 m in the Carlow Castle,
Good Luck and Little Fortune areas (Cahill, 2011, cited in
Voermans,2012). One hole,GC04 intercepted 22 m @ 10.7

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

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Criteria JORC Code explanation Commentary
g/t Au below the No 1 Lode, which included a 6 m interval
of 30.97 g/t Au.
1995 – 2008: Legend Mining Pty Ltd (& others)
The following has been taken from Cahill (2011), cited in
Voermans (2012).
Legend commenced exploration of the area in 1995, initially
concentrating on areas of historic workings.
Dragon Mining NL, (“Dragon”) and Titan Mining NL
(“Titan”) commissioned an Airborne Electromagnetic
(“AEM”) survey over a large portion of the West Pilbara in
1996 and 2001 respectively.
In 1999 and 2000, Legend explored the copper anomaly
identified by AMAX in 1969, which led to the discovery of
high-grade copper-gold mineralisation in a soil covered area
of Carlow South, south of the main workings.
Further field activities included RC drilling, soil geochemical
sampling, detailed ground magnetic surveys, trenching,
preliminary metallurgical testwork, gradient array induced
polarization (“IP”) and transient electromagnetic (“TEM”)
surveys and resource estimates. This program was successful
in identifying a high-grade pod of gold mineralization which
plunges 60° easterly within a broad shear zone and remains
open at depth. This pod is surrounded by an extensive halo of
lower grade gold and copper mineralization over a strike
length of 400 m which is open to the west.
In 2000 estimates of mineralization within 100 m of the
surface were produced using a sectional polygonal method.
A number of other prospects within a 500 m radius of the old
Carlow Castle workings were subject to first pass RC drilling
and results confirm the widespread presence of copper and
gold mineralisation in the area. Approximately 400 m east of
the main workings, drill hole CC54 in Carlow East
intersected two mineralised horizons within a 20 m thick
highly altered zone. The intersections included 4 m grading
1.32% Cu and 4.55 g/t Au from 38 m, and 48 m 5.66% Cu
and 1.87 g/t Au, which included 8m @ 0.16% Co.
Following orientation TEM and IP surveys over the Carlow
South resource, a detailed IP survey was completed over the
main area of interest. A detailed interpretation of the data
resulted in the identification of numerous IP and resistivity
targets. A total of 28 IP targets and 9 resistivity targets were
selected and assigned a follow-up priority for immediate
drilling. This planned drilling was never undertaken.
Small scale mining of the green chrysoprase was undertaken
in the past on M47/385 just north of the Carlow Castle main
workings and several large boulders were mined and
subsequently cut and polished for marketing purposes.
Polished hand specimen show a translucent pattern of very
fine grained, apple green colour chert, transected by milky-
white to blackish quartz veins and veinlets.

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Criteria JORC Code explanation Commentary
In 2007 and 2008, Legend undertook geophysical exploration
surveys over the project area, which used a combination of
AEM and ground-based geophysics, and consisted of:
Compilation and processing of regional aeromagnetic and
radiometric datasets covering the entire the project area. The
compilation involved several historic datasets with line
spacing varying from 25 m to 400 m.
Three Versatile Time Domain Electromagnetic (“VTEM”)
surveys covered an area of approximately 410 km2, with
flight directions ranging from E-W to NW-SE to N-S
depending on the orientation of stratigraphy. Line spacing
was either 200 m or 100 m with infill lines of 100 m or 50 m
respectively if conductive features of interest were identified.
Three Ground Fixed-Loop Transient Electromagnetic
(“FLTEM”) surveys were carried out to investigate 16
conductors identified by the airborne VTEM surveys.
Thirteen of the 16 VTEM targets surveyed identified
conductors considered significant enough to warrant future
drill testing.
2008 – 2016:
No on ground Exploration activities were conducted between
2008 and 2016 as a native title agreement was being
negotiated.
2017 – 2019:
Artemis commenced resource development drilling at
Carlow Castle in 2017 with 81 RC holes completed for 7,357
m.
A sub-audio magnetic (SAM) survey over the Carlow South
area in 2018 and confirmed the 1.2 km strike of the Carlow
Castle Mineral Resource. Resource development drilling in
2018 included 108 RC holes for 15,882 m, and 12 DD holes
for 1,505 m. Drilling focussed on the Carlow South and Quod
Est areas with drill holes nominally spaced 20 m apart on 40
m spaced sections. The drilling confirmed the high-grade
nature of Carlow Castle and results were incorporated into
mineral resource estimates in February 2019 and updated in
November 2019.
In 2019, ALS Metallurgy in Perth completed preliminary
metallurgical testwork on two 100 kg drill core composite
samples. The metallurgical testwork demonstrated a
potential Carlow Castle ore flowsheet utilising gravity and
cyanide leach for gold, and flotation to produce copper and
cobalt concentrates.
2020 – 2021:
In
2020,
Artemis
completed
follow-up
resource
development drilling at Carlow Castle targeting infill and
extensions at depth in the Carlow South and Quod Est areas.
A total of 62 RC holes for 7,574 m and 11 DD holes for 3,788
m
were
completed
and
successfully
intersected
mineralisation up to 250 m below the November 2019
Mineral Resource.

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Criteria JORC Code explanation Commentary
Geology Deposit type, geological setting and style of
mineralisation.
The project area lies on Archaean volcanic arc rocks, which
overly two unconformable sequences of mainly volcanic and
intrusive rocks. Amphibolites and undifferentiated mafic and
ultramafic rocks dominate the older sequence, which have
been metasomatised by intrusive activity. Gabbros and
calcrete-covered serpentinites have been recognised in the
area.
The Carlow Castle gold-copper-cobalt (Au-Cu-Co) deposits
are located 28 km northeast of the Radio Hill processing
plant. Carlow Castle and Quod Est are structurally controlled
mineralised zones occurring almost at right angles to each
other.
The Quod Est portion strikes approximately north-south
dipping steeply east with a strike length of about 200 m and
is fault terminated to the north and potentially at depth.
The Carlow Castle portion strikes east-west, being fault
disrupted at each end. Drill definition has been completed
over the 1,200 m strike length which has a flattened
sinusoidal form. At the western end mineralisation dips
steeply north, at the eastern end the mineralisation dips
steeply south. Mineralisation in Carlow Castle has been
shown to extend to at least 550 m below surface.
The Cross-Cut mineralisation strikes approximately north-
south dipping steeply east, with a strike of about 150 m.
Drillhole
Information
A summary of all information material to the
understanding of the exploration results
including a tabulation of the following
information for all Material drillholes:
Easting and northing of the drillhole collar
Elevation or RL (Reduced Level – elevation
above sea level in metres) of the drillhole collar
Dip and azimuth of the hole
Downhole length and interception depth
Hole length.
Exploration results are not being reported.
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.
Exploration results are not being reported.
Data
aggregation
methods
In reporting Exploration Results, weighting
averaging techniques, maximum and/or
minimum grade truncations (e.g. cutting of high
grades) and cut-off grades are usually Material
and should be stated.
Exploration results are not being reported.

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Criteria JORC Code explanation Commentary
Where aggregate intercepts incorporate short
lengths of high grade results and longer lengths
of low grade results, the procedure used for
such aggregation should be stated and some
typical examples of such aggregations should be
shown in detail.
Exploration results are not being reported.
The assumptions used for any reporting of metal
equivalent values should be clearly stated.
Exploration results are not being reported.
Relationship
between
mineralisation
widths and
intercept
lengths
These relationships are particularly important
in the reporting of Exploration Results.
The bulk of the Carlow Main mineralisation lodes dip sub-
vertically or steeply to the North and steeply to the South in
the eastern 20%, while Quod Est and Cross-Cut lodes dip
steeply to the East. Other than a low proportion of scissor
holes that provided volume control, drill holes were angled
near to 60° and with an azimuth perpendicular to the lodes
strike to provide as near a ‘true’ intercept thickness as
realistically possibly.
If the geometry of the mineralisation with
respect to the drillhole angle is known, its
nature should be reported.
Exploration results are not being reported.
If it is not known and only the downhole lengths
are reported, there should be a clear statement
to this effect (e.g. ‘downhole length, true width
not known’).
Exploration results are not being reported.
Diagrams Appropriate maps and sections (with scales)
and tabulations of intercepts should be included
for any significant discovery being reported
These should include, but not be limited to a
plan view of drillhole collar locations and
appropriate sectional views.
Relevant maps and diagrams are included in the body of this
announcement.
Balanced
reporting
Where comprehensive reporting of all
Exploration Results is not practicable,
representative reporting of both low and high
grades and/or widths should be practiced to
avoid misleading reporting of Exploration
Results.
Exploration results are not being reported.
Other
substantive
exploration
data
Other exploration data, if meaningful and
material, should be reported including (but not
limited to): geological observations;
geophysical survey results; 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.
Surface geological observations have been incorporated into
the geological interpretation and in concert with the results of
geochemical assays, considered reasonable for this style of
mineralisation.
Downhole geophysical logging was undertaken. The
geophysical probe penetrated >85% of the final hole depth
for 61% of the 36 holes and >60% of the final depth for 78%
of the holes. Six holes penetrated between 40% and 60% of
the final depth, one hole penetrated 33% and one 18% of the
final depth.

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Criteria JORC Code explanation Commentary
Further work The nature and scale of planned further work
(e.g. tests for lateral extensions or depth
extensions or large-scale step-out drilling).
Infill drilling around the higher-grade zones is planned to
improve the geological understanding of the host structures
and the confidence of the geological model, grade estimate
and Mineral Resource confidence in these zones.
Metallurgical testwork samples are planned from the oxide,
transitional, and fresh weathering zones to optimise the
process flowsheet and allow accurate cutoff grades to be
determined.
Scoping-level studies are planned to increase the confidence
in the input parameters for an economic evaluation of the
project.
Diagrams clearly highlighting the areas of
possible extensions, including the main
geological interpretations and future drilling
areas, provided this information is not
commercially sensitive.
Relevant maps and diagrams are included in the body of this
announcement.

JORC 2012 Table 1 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.

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Artemis Resources Limited ABN: 80 107 051 749 Telephone: +61 8 9486 4036| | Email: [email protected] Level 8, 99 St Georges Terrace PERTH WA 6000 Australia

www.artemisresources.com.au

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Criteria JORC Code explanation Commentary
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. The factors
affecting continuity both of grade and geology.
Mineralisation generally shows a continuous grade
distribution from un-mineralised through to high grade, with
minor inflection points within the log-probability plot 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 steeplyeast dipping

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Criteria JORC Code explanation Commentary
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 using Supervisor software to assess the effect 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.

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Criteria JORC Code explanation Commentary
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).
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

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Criteria JORC Code explanation Commentary

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 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 bystatistical analysis includingreview of CV

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Criteria JORC Code explanation Commentary
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 reasonable prospects
for 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.
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.
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.

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Criteria JORC Code explanation Commentary
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
determination of potential environmental
impacts, particularly for a greenfields project,
may not always be well advanced, the status
of early consideration of thesepotential
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
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 for

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Criteria JORC Code explanation Commentary
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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