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WESTERN MINES GROUP LTD Capital/Financing Update 2022

Jul 25, 2022

66068_rns_2022-07-25_0a09df91-51b5-4e1e-9425-997d6a099fdc.pdf

Capital/Financing Update

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ASX RELEASE
26 JULY 2022
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DISSEMINATED SULPHIDES SEEN OVER >300M IN HOLE MTD020

HIGHLIGHTS

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  • Three further diamond drill holes completed at the Mulga Tank Ni-Cu-PGE Project

  • Disseminated magmatic sulphides observed over >300m in hole MTD020 - clear indication of a large scale working mineral system at Mulga Tank

  • Potential for Mt Keith-style (Type 2) disseminate sulphide as well as Perseverance-style (Type 1) basal massive sulphide deposits

  • a wide area and range of exploration targets - highlighting the prospectivity of the project

  • Samples from all holes up to MTD020 have been delivered to the lab for geochemical assay with first results expected from end of July through August

  • Diamond drilling program remains ongoing with the rig currently drilling hole MTD021

  • DHEM survey to be undertaken on completed holes looking for off hole follow-up targets

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Western Mines Group Ltd (WMG or Company) (ASX:WMG) is pleased to update shareholders on the completion of three further diamond drill holes at the flagship Mulga Tank Ni-Cu-PGE Project, on the Minigwal Greenstone Belt, in Western Australia’s Eastern Goldfields.

Holes MTD018 and MTD020 were designed to follow-up on historical drilling results at the project, whereas hole MTD019 was drilled to test a discrete EM target on the southern margin of the Mulga Tank intrusion.

disseminated magmatic sulphides (trace to 2%) that coalesced into interstitial blebs towards the base of the unit (3 to 5% sulphide). This is the clearest indication to date of a magmatic sulphide mineral system at Mulga Tank and the potential for a large scale Type 2 Mt Keith-style disseminated sulphide deposit and/or a Type 1 Perseverance-style basal massive sulphide deposit where sulphides may accumulate on the basal contact.

Commenting on the Mulga Tank Project, WMG Managing Director Caedmon Marriott said:

“Hole MTD020 was drilled more towards the centre of the Mulga Tank body and was designed to test beneath historical hole MTD011, which showed numerous intersections of Ni-Cu-PGE mineralisation. Visible disseminated sulphides were seen throughout a thick high MgO dunite unit; this is very exciting and offers great encouragement for the prospectivity of this large ultramafic body to host both Mt Keith-style or Perseverance-style nickel sulphide deposits.”

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Western Mines Group Ltd

Shares on Issue: 44.65m Share Price: $0.165 Market Cap: $7.37m Cash: $4.2m (31/03/22)

Telephone: +61 475 116 798 Email: [email protected]

Level 3, 33 Ord Street West Perth WA 6005

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MULGA TANK DIAMOND DRILLING PROGRAM

WMG is undertaking an initial ten-hole diamond drilling program, totalling 4,050m, at the Mulga Tank Ni-Cu-PGE Project. The program aims to test numerous drill targets designed from the Company’s geological targeting work ( ASX, Major EM Targets Identified at Mulga Tank Ni-Cu-PGE Project, 7 March 2022; Mulga Tank Ni-CuPGE Project: Major Targets Drill Ready, 6 April 2022 ).

HOLE MTD018

The seventh hole of the program MTD018 (planned hole MTP019) was drilled to a total depth of 501.2m and was designed to test the western margin and basal contact at depth beneath historical hole MTD003 - hole MTD003 showed indications of nickel sulphide mineralisation returning 1m at 1.00% Ni and 0.5g/t PGE from 209m. Hole MTD018 intersected 330.6m of variably altered mesocumulate dunite (from 68.5-399.1m), beneath 68.5m of sand cover (0-68.5m), before encountering a footwall of predominantly cherts and some interbedded black shales (399.1-501.2m) at 399.1m depth.

One occurrence of visible nickel sulphide mineralisation was observed down the hole, with a remobilised nickel sulphide vein (pentlandite-pyrrhotite) seen at 159.9m depth - with sulphide identification confirmed by spot pXRF readings. Hole MTD018 was cased and will be tested with a planned Downhole Electromagnetic (DHEM) survey.

HOLE MTD019

The eighth hole of the program MTD019 (planned hole MTP018) was drilled to a total depth of 264.6m and was designed to test a discrete EM anomaly situated on the southern margin of the ultramafic body. The hole intersected 75m of variably altered and silicified orthocumulate and mesocumulate dunite ultramafic (from 84.6-159.6.m), beneath 84.6m of sand and Permian mudstone and conglomerate cover (0-84.6m), before encountering a footwall of basalt, shales and chert (159.6-264.6m) at 159.6m depth.

No visible nickel mineralisation was observed down the hole. Due to a number of drilling challenges in broken ground the hole was not able to be cased for downhole EM. Nothing observed down the hole was able to conclusively explain the discrete EM anomaly in this area but it is most likely caused by a sulphidic black shale unit in the footwall.

HOLE MTD020

The ninth hole of the program MTD020 (planned hole MTP020) was drilled to a total depth of 564.4m and was designed to test beneath historical hole MTD011 - hole MTD011 showed multiple indications of nickel sulphide mineralisation including of 1m at 1.95% Ni and 0.21g/t Pt+Pd from 103m, 1m at 0.83% Ni and 0.18g/t Pt+Pd from 114m and 0.5m at 1.18% Ni and 0.1g/t Pt+Pd from 211.7m. Hole MTD020 intersected 453.3m of variably altered ortho-mesocumulate dunite (from 65.7-519m), beneath 65.7m of sand cover (0-65.7m), before encountering a footwall of predominantly basalt at 519m depth.

Two styles of visible nickel mineralisation were observed down the hole including remobilised nickel sulphide veins (pentlandite-pyrrhotite) and disseminated magmatic sulphides (pyrite-pyrrhotite-pentlandite). Disseminated sulphides (trace to 5% sulphide) occurred over in excess of 300m from 120 to 512m. Towards the base of dunite unit these disseminated sulphides coalesced into interstitial blebs (3-5% sulphide) between the olivine grains of the meso-adcumulate dunite.

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clearest indication to date of a working magmatic sulphide mineral system, though it is cautioned that geochemical assaying of the hole has not yet been undertaken. The observations suggest the potential for both large scale Type 2 Mt Keith-style disseminated sulphide deposits and/or a Type 1 Perseverance-style basal massive sulphide deposits, where sulphides may accumulate on the basal contact, possibly deeper within the intrusion ( deposit types after Lesher and Keays, 2002 ).

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MTD020
NQ2 Core
2” Diameter
(Ni, Fe)9S8
Spot XRF Readings: 37.5% Nickel 1.7% Copper
Depth: 370.8m
Remobilised Nickel Sulphides (pentlandite-pyrrhotite-chalcopyrite)
within Talc-Carbonate Altered Dunite
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Figure 1: Photo showing examples of visible sulphides in hole MTD020 Note: core is NQ2 being 2 inches or 50mm diameter

Komatiite-associated Ni-Cu-PGE Deposits: Geology, Mineralogy, Geochemistry and Genesis; Lesher and Keays, 2002

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Figures 2A and 2B: Photo showing examples of visible sulphides in hole MTD020 with disseminated sulphide forming interstitial blebs between olivine grains Note: core is NQ2 being 2 inches or 50mm diameter

DOWN HOLE pXRF

and geochemical vectoring approach during the drilling program. Spot pXRF readings for holes MTD018, MTD019 and MTD020 were taken at 50cm intervals down the core.

magmatic mineral processes and lithogeochemical vectors to aid further exploration and drill targeting. Processed pXRF data is presented for hole MTD020 below.

Cautionary statement on pXRF

pXRF data is used as an exploration tool and a guide only and should never be considered a proxy or substitute for laboratory analysis. The measurements recorded are for a single spot location and may not be representative of the whole rock. Only subsequent laboratory geochemical assay can be used to determine the widths and grade of mineralisation. WMG will update shareholders when laboratory results become available.

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Figure 3: Processed pXRF data for hole MTD020

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The mean average Ni value across all the 1131 readings for the hole was 0.26% Ni, the mean average for 1028 readings of the logged ultramafic portion of the hole was 0.29% Ni, with individual spot values of up to 37.5% Ni where sulphide mineralisation was observed.

in the drilling program, these correlated well with observed sulphide abundance. Three possible broad dunite units can be seen down the hole, all showing suitably high MgO content.

NEXT HOLE

The rig has now moved to the northwest and has commenced drilling at planned hole MTP021. This hole targets the up-dip component of the high conductance NW3 Conductor EM anomaly within the Panhandle area of the project.

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Figure 4: Mulga Tank MLEM late channel CH40BZ image showing EM plates

and WMG’s planned drill holes

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Core selected for sampling for all holes up to MTD020 has been delivered to ALS in Perth for geochemical assay. The Company will update shareholders on the assay results as they become available.

The Company looks forward to updating shareholders on the continuing progress as this exciting drilling program develops.

For further information please contact: Dr Caedmon Marriott Managing Director Tel: +61 475 116 798 Email: [email protected]

This announcement has been authorised for release to the ASX by Dr Caedmon Marriott, Managing Director

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HoleID From
(m)
To
(m)
Primary
Lithology
Alteration Comments
MTD020 0.0 65.7 Sand cover Rock-rolled sands
MTD020 65.7 101.2 Mesocumulate dunite tc, cl Bright green olivine-peridotite, mesocumulate texture with remobilised
sulphides (Fe) in veinlets, some with Ni
MTD020 101.2 116.35 Dunite tc, cl Diffculty determining texture in darker matrix
MTD020 116.35 117.2 Fault Zone tc, cb
MTD020 117.2 130 Dunite si, cl Disseminated Py and Po in intercumulus around crystal faces
MTD020 130 149 Dunite si
MTD020 149 155 Dunite si
MTD020 155 162 Dunite si, cl Disseminated to blebby sulphides in silica-chlorite altered dunite +NiS
Pn bearing veinlet
MTD020 162 278 Dunite si, tc, cl Broad zone of dunite with trace sulphides and multiple Ni-S veinlet
intercepts
MTD020 278 285 Dunite si, tc, cl
MTD020 285 291 Dunite si
MTD020 291 360 Orthocumulate dunite si, cl Dark, weakly altered orthocumulate dunite, zones of varying sulphide
abundance
MTD020 360 375 Mesocumulate dunite si Strongly disseminated Py and Po, up to 5% abundance in dark
mesocumulate textured dunite + 250mm Ni-S Pn vein
MTD020 375 481 Mesocumulate dunite si, cl
MTD020 481 501 Mesocumulate dunite si Diffculty determining sulphide abundance in bright green olivine-
peridotite
MTD020 501 519 Mesocumulate dunite si, tc, cl
MTD020 518 564 Basalt Basalt footwall

Table 1: Logging table summary for hole MTD020

HoleID From
(m)
To
(m)
Interval
(m)
Lithology Sulphide
Texture
Sulphide
Abundance (%)
Sulphides
Observed
MTD020 120.8 122 1.2 Dunite Disseminated tr-1% Pyrite-Pyrrhotite
MTD020 123.6 124 0.4 Dunite Disseminated tr-2% Pyrite-Pyrrhotite
MTD020 130 155 25 Dunite Disseminated tr-1% Pyrite-Pyrrhotite
MTD020 155 162 7 Dunite Disseminated 2-3% Pyrite-Pyrrhotite-Pentlandite
MTD020 162 270 108 Dunite Disseminated tr-1% Pyrite-Pyrrhotite-Pentlandite
MTD020 278 285 7 Dunite Disseminated 2% Pyrite-Pyrrhotite
MTD020 288 291 3 Dunite Disseminated 3-5% Pyrite-Pyrrhotite
MTD020 291 338 47 Orthocumulate dunite Disseminated tr-1% Pyrite-Pyrrhotite
MTD020 338 349 11 Orthocumulate dunite Disseminated tr-2% Pyrite-Pyrrhotite
MTD020 349 351 2 Orthocumulate dunite Disseminated 1-3% Pyrite-Pyrrhotite
MTD020 351 360 9 Orthocumulate dunite Disseminated 1-2% Pyrite-Pyrrhotite
MTD020 365 369 4 Mesocumulate dunite Disseminated 2-5% Pyrite-Pyrrhotite-Pentlandite
MTD020 371 373 2 Mesocumulate dunite Disseminated 2-5% Pyrite-Pyrrhotite-Pentlandite
MTD020 373 450 77 Mesocumulate dunite Disseminated tr-1% Pyrite-Pyrrhotite
MTD020 450 465 15 Mesocumulate dunite Disseminated tr-2% Pyrite-Pyrrhotite
MTD020 465 473 8 Mesocumulate dunite Disseminated tr-1% Pyrite-Pyrrhotite
MTD020 473 481 8 Mesocumulate dunite Disseminated tr-2% Pyrite-Pyrrhotite
MTD020 501 509 8 Mesocumulate dunite Disseminated 1-2% Pyrite-Pyrrhotite
MTD020 509 512 3 Mesocumulate dunite Blebby 3-5% Pyrite-Pyrrhotite-Pentlandite

Table 2: Visual sulphide table for hole MTD020

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HoleID Spot Depth (m) Ni (%)
(XRF spot reading)
Cu (%)
(XRF spot reading)
MTD020 217.6 19.32% 0.75%
MTD020 262.45 9.37% 0.51%
MTD020 370.8 37.47% 1.72%
HoleID Easting (MGA51) Northing (MGA51) Total Depth (m) Azimuth Dip
MTD020 521493 6688363 564.4 225 -60

Table 4: Collar details for hole MTD020

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ABOUT WMG

Western Mines Group Ltd ACN 640 738 834 Level 3, 33 Ord Street West Perth WA 6005

Board

Rex Turkington Non-Executive Chairman

Dr Caedmon Marriott Managing Director

Francesco Cannavo Non-Executive Director

Paul Burton Non-Executive Director

Capital Structure

Shares: 44.65m Options: 22.85m Share Price: $0.165 Market Cap: $7.37m Cash (31/03/22): $4.2m

Follow us

@westernmines westernmines Western Mines Group

Western Mines Group Ltd (ASX:WMG) is a mineral exploration company driven by the goal to create significant investment returns for our shareholders through exploration and discovery of high-value gold and nickel sulphide deposits across a portfolio of highlyprospective projects located on major mineral belts of Western Australia.

major dunite intrusive found on the under-explored Minigwal Greenstone Belt. Previous work shows significant evidence for a working sulphide mineral system and is considered highly prospective for Ni-Cu-PGE mineralisation.

The Company’s primary gold project is Jasper Hill, where WMG has strategically consolidated a 3km mineralised gold trend with walk-up drill targets. WMG has a diversified portfolio of other projects including Melita (Au, Cu-Pb-Zn), midway between Kookynie and Leonora in the heart of the WA Goldfields; Youanmi (Au), Pavarotti (Ni-Cu-PGE), Rock of Ages (Au), Broken Hill Bore (Au) and Pinyalling (Au, Cu, Li).

COMPETENT PERSONS STATEMENT

The information in this announcement that relates to Exploration Results and other technical information 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 Caedmon Marriott, Managing Director of Western Mines Group Ltd. Caedmon is a Member of the Australian Institute of Geoscientists and a Member of the Australasian Institute of Mining and Metallurgy. 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. Caedmon consents to the inclusion in this announcement of the matters based on his information in the form and context in which it appears.

DISCLAIMER

Some of the statements appearing in this announcement may be in the nature of forward looking statements. You should be aware that such statements are only predictions and are subject to inherent risks and uncertainties. Those risks and uncertainties include factors and risks specific to the industries in which WMG operates and proposes to operate as well as general economic conditions, prevailing exchange rates and interest rates and conditions in the financial markets, among other things. Actual events or results may differ materially from the events or results expressed or implied in any forward looking statement. No forward looking statement is a guarantee or representation as to future performance or any other future matters, which will be influenced by a number of factors and subject to various uncertainties and contingencies, many of which will be outside WMG’s control.

WMG does not undertake any obligation to update publicly or release any revisions to these forward looking statements to reflect events or circumstances after today's date or to reflect the occurrence of unanticipated events. No representation or warranty, express or implied, is made as to the fairness, accuracy, completeness or correctness of the information, opinions or conclusions contained in this announcement. To the maximum extent permitted by law, none of WMG, its Directors, employees, advisors or agents, nor any other person, accepts any liability for any loss arising from the use of the information contained in this announcement. You are cautioned not to place undue reliance on any forward looking statement. The forward looking statements in this announcement reflect views held only as at the date of this announcement.

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MULGA TANK PROJECT

JORC CODE, 2012 EDITION - TABLE 1 SECTION 1: SAMPLING TECHNIQUES AND DATA

Criteria JORC Code explanation Commentary
Sampling
techniques
• Nature and quality of sampling (eg cut channels,
random chips, or specifc specialised industry
standard measurement tools appropriate to the
minerals under investigation, such as down hole
gamma sondes, or handheld XRF instruments, etc).
These examples should not be taken as limiting the
broad meaning of sampling.
• Include reference to measures taken to ensure
sample representivity and the appropriate calibration
of any measurement tools or systems used.
• 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 (eg ‘reverse
circulation drilling was used to obtain 1 m samples
from which 3 kg was pulverised to produce a 30 g
charge for fre 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 (eg
submarine nodules) may warrant disclosure of
detailed information.
• Diamond core drilling was completed using
standard industry best practice
• Sampling of NQ2 diamond core has not yet
been undertaken
• Ground Moving Loop Electromagnetic (MLEM)
survey being conducted by GEM Geophysics
Pty Ltd an independent geophysical
contractor
• MLEM B-feld confguration/parameters:
Confguration:Slingram and Inloop
Receiver:SMARTem24
Sensor:JESSY DEEP HT SQUID B-feld
(3D)
Polarity:Z+Up, X+ East and Y+ North
Transmitter:TTX2 - 100A/250V
Loop Size:200m x 200m (single turn)
Current:85A
Line Spacing:200-400m
Station Spacing:100m
Base Frequency:0.25Hz
Stacking:64-72stacks
Readings:2-3 readings per station
• MLEM surveys are an industry standard
practise in testing the presence of bedrock
conductors potentially representing
mineralised sulphide bodies
• Portable XRF data collected at 50cm sample
point spacing downhole, with a 10 second
beam time using 2 beams
• Model of XRF instrument was Olympus Vanta
M Series
Drilling
techniques
• Drill type (eg core, reverse circulation, open-hole
hammer, rotary air blast, auger, Bangka, sonic, etc)
and details (eg 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).
• Diamond drilling comprised HQ and NQ2 core
• The core was orientated using a downhole
orientation tool at the end of every run
Drill sample
recovery
• Method of recording and assessing core and chip
sample recoveries and results assessed.
• Measures taken to maximise sample recovery and
ensure representative nature of the samples.
• Whether a relationship exists between sample
recovery and grade and whether sample bias may
have occurred due to preferential loss/gain of fne/
coarse material.
• Diamond core recoveries were logged and
recorded in the database. Overall recoveries
were reported at >95% with no core loss
issues or signifcant sample recovery problems
• Diamond core was reconstructed into
continuous runs on an angle iron cradle for
orientation marking. Depths were checked
against the depth given on the core blocks
and rod counts were routinely carried out by
the drillers
• No sampling has yet been undertaken but no
sampling bias is anticipated

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Criteria JORC Code explanation Commentary
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.
• Whether logging is qualitative or quantitative in
nature. Core (or costean, channel, etc) photography.
• The total length and percentage of the relevant
intersections logged.
• Information on structure type, dip, dip
direction, alpha angle, beta angle, texture,
shape and fll material were collected and
stored in the database
• Logging of diamond core recorded lithology,
mineralogy, mineralisation, structural,
weathering, colour, and other features of the
samples. Core was photographed in both dry
and wet form
• Drillhole was logged in full, apart from rock
roller diamond hole pre-collar intervals
Sub-sampling
techniques
and sample
preparation
• If core, whether cut or sawn and whether quarter, half
or all core taken.
• If non-core, whether riffed, tube sampled, rotary split,
etc and whether sampled wet or dry.
• For all sample types, the nature, quality and
appropriateness of the sample preparation technique.
• Quality control procedures adopted for all sub-
sampling stages to maximise representivity of
samples.
• Measures taken to ensure that the sampling is
representative of the in-situ material collected,
including for instance results for feld duplicate/
second-half sampling.
• Whether sample sizes are appropriate to the grain
size of the material being sampled.
• Core has not yet been cut and sampled for
geochemical assay
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.
• 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.
• Nature of quality control procedures adopted (eg
standards, blanks, duplicates, external laboratory
checks) and whether acceptable levels of accuracy
(i.e. lack of bias) and precision have been established.
• Laboratory geochemical assay has not yet
been undertaken
• Ground MLEM survey being undertaken by
GEM Geophysics using equipment described
above
• Daily production reports reviewed and QA/QC
of the data is completed by the Company's
consultant geophysicist
• XRF instrument used was Olympus Vanta M-
Series
• XRF used a 10 beam time, with 2 beams,
using standard calibration procedures
Verifcation of
sampling and
assaying
• The verifcation of signifcant intersections by either
independent or alternative company personnel.
• The use of twinned holes.
• Documentation of primary data, data entry
procedures, data verifcation, data storage (physical
and electronic) protocols.
• Discuss any adjustment to assay data.
• Signifcant XRF readings reported were verifed
by multiple alternative company personnel
onsite
• Primary logging data was collected using
Ocris logging system on a laptop computer,
XRF and magsus data was download into
Excel spreadsheets, all was compiled into a
SQL database server
• No adjustments were made to individual spot
XRF data reported
• Some smoothing and moving averaging
techniques were used when plotting Ni:Cr
ratios in graphical format
Location of
data points
• Accuracy and quality of surveys used to locate drill
holes (collar and down-hole surveys), trenches, mine
workings and other locations used in Mineral
Resource estimation.
• Specifcation of the grid system used.
• Quality and adequacy of topographic control.
• Drill holes located using a handheld GPS with
accuracy of +/-3m, downhole surveys used
continuous gyro readings at 5m intervals
• Coordinates are in GDA94 UTM Zone 51
• MLEM stations located using a handheld GPS
with accuracy of +/-3m

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Criteria JORC Code explanation Commentary
Data spacing
and
distribution
• Data spacing for reporting of Exploration Results.
• Whether the data spacing and distribution is suffcient
to establish the degree of geological and grade
continuity appropriate for the Mineral Resource and
Ore Reserve estimation procedure(s) and
classifcations applied.
• Whether sample compositing has been applied.
• The drilling completed was reconnaissance in
nature designed to test specifc geochemical
and geophysical targets
• The drilling completed was reconnaissance in
nature for frst pass exploration purposes only
• Spacing between MLEM survey lines was
200-400m, with instrument station realigns
taken 100m along survey lines
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.
• 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.
• The drilling was planned to be approximately
perpendicular to the interpreted stratigraphy
and footwall contact
• The MLEM survey line direction in the southern
sector was orientated north-south, broadly
perpendicular to known strike direction of
geological formations and conductor strike
Sample
security
• The measures taken to ensure sample security. • All data acquired by GEM was reported to the
Company’s consultant geophysicist
Audits or
reviews
• The results of any audits or reviews of sampling
techniques and data.
• No audits or reviews of drilling sampling
techniques or data
• MLEM data was independently verifed by the
Company’s consultant geophysicist Russell
Mortimer of Southern Geoscience Consultants

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 security of the tenure held at the time of reporting
along with any known impediments to obtaining a
licence to operate in the area.
• Tenement E39/2132, tenement applications
E39/2223 and E39/2299
• Held 100% by Western Mines Group Ltd
• 1% NSR to original tenement holder
• Native Title Claim by Upurli Upurli Nguratja not
yet determined
• No known historical or environmentally
sensitive areas within the tenement area
• Tenement is in good standing
Exploration
done by other
parties
• Acknowledgment and appraisal of exploration by
other parties.
• Previous exploration over the Mulga Tank
project area by various companies dates back
to the 1980s
• Of these, more detailed exploration was
completed by BHP Minerals Pty Ltd (1982–
1984), MPI Gold Pty Ltd (1995–1999), North
Limited (1999–2000), King Eagle Resources
Pty Ltd (2004–2012), and Impact (2013–2018)

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ASX RELEASE | DISSEMINATED SULPHIDES >300M IN HOLE MTD020

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Criteria JORC Code explanation Commentary
Geology • Deposit type, geological setting and style of
mineralisation.
• The geology of the project area is dominated
by the irregular shaped Mulga Tank
serpentinised metadunite intrusive body
measuring ~5km x
5km, hosted within metasediments, mafc to
felsic schists and foliated metagranite of the
northwest trending Archean Minigwal
Greenstone Belt
• Previous drilling intersected disseminated and
narrow zones of massive nickel-copper
sulphide mineralisation within the dunite
intrusion
• The intrusion is concealed under variable
thicknesses of cover (reported up to 70 m in
places) with the interpretation of the bedrock
geology based largely on aeromagnetic data
and limited drilling
Drill hole
information
• A summary of all information material to the
understanding of the exploration results including a
tabulation of the following information for all Material
drill holes:
• easting and northing of the drill hole collar
• elevation or RL (Reduced Level – elevation above
sea level in metres) of the drill hole collar
• dip and azimuth of the hole
• down hole length and interception depth hole
length.
• If the exclusion of this information is justifed 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.
• A listing of the drill hole information material to
the understanding of the exploration results
provided in the body of this announcement
• The use of any data is recommended for
indicative purposes only in terms of potential
Ni-Cu-PGE mineralisation and for developing
exploration targets
Data
aggregation
methods
• In reporting Exploration Results, weighting averaging
techniques, maximum and/or minimum grade
truncations (eg cutting of high grades) and cut-off
grades are usually Material and should be stated.
• 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.
• The assumptions used for any reporting of metal
equivalent values should be clearly stated.
• No metal equivalent values have been quoted
• XRF data for Ni:Cr shown in Figure 2 was
processed and smoothed using a moving
average
Relationship
between
mineralisation
widths and
intercept
lengths
• These relationships are particularly important in the
reporting of Exploration Results.
• If the geometry of the mineralisation with respect to
the drill hole angle is known, its nature should be
reported.
• If it is not known and only the down hole lengths are
reported, there should be a clear statement to this
effect (eg ‘down hole length, true width not known’).
• The drillhole was oriented to intersect the dip
of an electromagnetic conductor as interpreted
by WMG’s consultant, Southern Geoscience,
and perpendicular to the mineralisation or
stratigraphy
• The relationship of the downhole length to the
true width is not known
Diagrams • Appropriate maps and sections (with scales) and
tabulations of intercepts should be included for any
signifcant discovery being reported. These should
include, but not be limited to a plan view of drill hole
collar locations and appropriate sectional views.
• Appropriate maps, photos and tabulations are
presented in the body of the announcement

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ASX RELEASE | DISSEMINATED SULPHIDES >300M IN HOLE MTD020

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Criteria JORC Code explanation Commentary
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.
• A complete XRF dataset for the drill hole is
shown in Figure 3
• XRF readings are a single spot reading and
should only be taken as a guide that nickel
sulphide mineralising processes are being
observed, likely within sulphide veins within the
core
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.
• Not applicable
Further work • The nature and scale of planned further work (eg
tests for lateral extensions or depth extensions or
large-scale step-out 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.
• Future exploration planned includes further drill
testing of targets identifed
• Exploration is at an early stage and future
drilling areas will depend on interpretation of
results

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