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TARUGA MINERALS LIMITED Capital/Financing Update 2021

Oct 31, 2021

65895_rns_2021-10-31_48ef2365-b753-4c8d-8377-6f40e082e851.pdf

Capital/Financing Update

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ASX ANNOUNCEMENT

DIAMOND DRILLING UPDATE – MT CRAIG COPPER PROJECT

HIGHLIGHTS:

  • Diamond drilling program is ongoing at Morgan’s Creek, with the 6[th] and final hole in the program recently completed at the Hydrothermal Hill Prospect

  • Visible copper-oxide and sulphide mineralisation successfully intercepted at Morgan’s Bore Prospect

  • The third and final hole completed at the recently identified Hydrothermal Hill Prospect

    • Serpentinized mafic-ultramafic intrusion intercepted at Hydrothermal Hill target along with visible disseminated sulphides (pyrite + minor chalcopyrite)

    • Biotite-magnetite and calc-silicate (potential contact skarn) alteration surrounding the mafic intrusions

  • Diamond core from 3 completed holes at Wyacca are almost finished being processed

  • Visible copper oxide or sulphide mineralisation successfully intercepted in all 3 holes

  • o Detailed structural and lithological logging ongoing with core samples to be despatched to the lab shortly

  • Detailed ground-based gravity and magnetic geophysical programs currently underway across the Mt Craig Copper Project

  • Wyacca and Morgan’s Creek undergoing a gravity survey on a 200m x 50m spacing (and broader 400m x 50m spacing), and 50m line spacing high resolution ground magnetics

  • Extensive new soils and rock chip results, along with structural mapping and new geophysics to be released to the market soon

  • RC drilling planned at Morgan’s Creek following completion of the final diamond hole at Hydrothermal Hill

Taruga Minerals Limited (ASX: TAR , Taruga or the Company ) is pleased to present an exploration update for the Mt Craig Copper Project (MCCP), where an extensive reconnaissance exploration and drilling program is ongoing.

CEO Thomas Line Commented: “We are undertaking a vast exploration program at the Morgan’s Creek and Wyacca prospects within the MCCP, which is revealing new insights into the significant potential of the mineral systems identified at the project. We look forward to providing the market with further updates regarding the exciting developments at the project over the coming weeks.”

Wyacca

The diamond drilling at Wyacca successfully intercepted visible copper mineralisation in all 3 holes. At Worrumba 19, blebby to semi-massive chalcopyrite ( Figures 1 and 2 ) hosted within massive dolomite was intercepted in the primary ore zone, which started at 92.5m through to 95.2m, and transitioned into finely disseminated chalcopyrite in shale downhole.

ASX:TAR tarugaminerals.com.au

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Figure 1. Primary Ore Zone at Worrumba-19, Comprised of Blebby to Semi-Massive Chalcopyrite in Massive Dolomite, and Disseminated Chalcopyrite in Black Shale at the Base of the Tindelpina Shale Member (Drillhole WCDD001).

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Figure 2. (left)Semi-massive to Blebby Chalcopyrite Mineralisation along with Dolomite and Arsenopyrite within the Primary Ore Zone at Worrumba 19 (Drillhole WCDD001); and (right) Alteration Zone at the Base of the Tindelpina Shale Member at the Beginning of the Ore Zone.

At Powder Hill, in drillhole WCDD002, a gossanous zone was intercepted from 6m, before transitioning into the primary Ore Zone from 18 – 24 metres. The overall alteration zone extended for 18m from 6 to 24m ( Figure 3 ). The primary ore zone is comprised of manganese and iron oxide minerals which contain fine chalcocite banding throughout.

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Figure 3. The Primary Ore Zone at Powder Hill, Showing Progression from Left to Right Downhole from Oxidised and Leached Shales into the Thick Alteration/Ore Zone.

At Worrumba 21, shallow mineralisation was targeted to understand the mineralisation, lithology and structural controls. A 0.55m zone of copper-oxide mineralisation was intercepted from 12.25m, within a dolomite-siderite carbonate matrix. RC drilling has identified broader chalcopyrite-bornite mineralisation downdip of this intercept, and has further identified potential for multiple stacked lenses of copper mineralisation where structures cross cut the Tapley Hill Formation sediments.

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Figure 4. The Oxide Ore Zone at Worrumba 21, Hosted within Lower Tapley Hill Formation Shales, showing Malachite Mineralisation within Siderite-Ankerite and Dolomite Matrix.

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Figure 5. Late Time VTEM Image Showing Diamond Drillhole Locations, Prospect Names, and Recent Taruga RC Drilling Results and Historical Drilling Results.

Morgan’s Creek

Diamond drillhole MCDD001 successfully intercepted visible malachite mineralisation from 27m – 32m ( Figure 6 ). Following this, Strontium and Barium ore (Celestite and Baryte) were intercepted along with minor chalcopyrite and galena from 49.25m to 74 metres (24.75m) ( Figure 7 ).

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Figure 6 . Malachite mineralisation intercepted at MCDD01, from 27 – 32m.

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Figure 7 . Map of Morgan’s Creek Focus Area, Showing Prospect Names and Recent Diamond Drillhole Locations.

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Figure 8 . (left) Minor chalcopyrite (+pyrite + galena) mineralisation intercepted from 49.25m to 74m (24.75m), with more prominent celestite and baryte breccia vein fracture fill (centre), and (right)brecciated siltstone with calcite veining and celestite.

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Drillhole MCDD003 ( Figures 8 & 9 ) targeted zinc, lithium and REE mineralisation identified from recent RC drilling (RC drillholes MCRC009, MCRC010, and MCRC022) at the Oxide Hill prospect. Heavily oxidised and brecciated sediments known to contain lithium, zinc and REE mineralisation were intercepted from surface. The brecciated marble unit which recently reported the highest grade REE intercepts (up to 0.46% TREO - MCRC009) along the margin of the adjacent dolerite was intercepted from 65.7m to 185.3m end of hole ( Figure 9 ), where the hole was terminated. The drillhole skimmed the edge of the mafic-ultramafic intrusion which is host to the primary scandium and vanadium mineralisation intercepted from surface in MCRC009.

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Figure 9 . (left) Near-surface core from MCDD003, showing heavily brecciated and oxidised metasediments containing Zinc, Lithium and REE mineralisation identified from recent RC drilling (5-17m in image)), (centre) more competent oxidised sedimentary breccia (~22-26m in photo); and (right) brecciated crystalline marble unit contacting on brecciated mafic-ultramafic intrusion.

At Hydrothermal Hill ( Figure 5 ), the diamond drill rig recently completed the final diamond hole for the program. So far at Hydrothermal Hill, heavily altered brecciated mafic-ultramafic intrusions and dolomite-carbonates have been intercepted with accompanying serpentine, biotite, chlorite, magnetite, haematite and pyrite alteration ( Figures 11 & 12 ). This alteration zone contacts on the western margin of a diapiric breccia, which the hole was collared into. Sulphides including pyrite and minor chalcopyrite ( Figure 10 ) have been noted within the sediments and mafic-ultramafic intrusions. The alteration identified at Hydrothermal Hill so far is indicative of intense hydrothermal alteration, with the altered carbonates potentially representing contact skarn metamorphism.

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Figure 10 . MCDD004 Chalcopyrite Mineralisation within calcite veining in Gabbro at approximately 149m.

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Figure 11 . MCDD004 ( left) Biotite-calcite-magnetite-serpentine-pyrite alteration at approximately 31m; (centre) magnetite and pyrite (+ minor arsenopyrite + chalcopyrite) alteration ~45m; and (right) chloritized ultramafic on the margin of the diapir at approximately 26m.

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Figure 12 . MCDD004 (left ) 30-35m biotite altered carbonate breccia with hydrothermal alteration, including sericite and sodic alteration ; and (right) – 37 – 43m strongly serpentinized carbonate breccia with magnetite and hematite alteration.

Geophysics

Detailed ground gravity and magnetics surveys are currently underway at Wyacca and Morgan’s Creek. The ground gravity surveys are being completed using ATV’s ( Figure 13 , using a 200m x 50m spacing in key areas and 400m x 50m grid spacing surrounding key areas. The ground magnetic surveys are being conducted on foot ( Figure 13 ) over selective portions of Wyacca and Morgan’s Creek, using a high resolution 50m line spacing. The gravity and magnetic data are expected to highlight key structures, intrusions, lithologies and alteration zones which will used in combination with the soils, rock chip and previous drilling data to undertake further precision RC drill-testing. The geophysical data will also be used to conduct inversion modelling of prospective anomalies to assist with drill planning. The Company will present the results of the geophysical program, including new areas of interest to the market shortly, once processing is complete.

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Figure 13. Ground-based Magnetics (left) and Gravity (right) Programs currently underway at Mt Craig Copper project.

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Appendix:

Table 1. Wyacca Diamond Drillhole Details

Prospect Hole ID X Y Azimuth Dip EOH drilled depth Hole status
Wyacca WCDD001 288580 6481453 95 -60 118.00 Complete
Wyacca WCDD002 287915 6482018 60 -65 41.60 Complete
Wyacca WCDD003 289467 6482578 175 -60 25.20 Complete

Table 2. Wyacca Diamond Drillhole Summary Logs

Prospect Hole ID From To Interval Lithology Comments
Wyacca WCDD001 0 12 12 Shale Weathered oxidised shale
Wyacca WCDD001 12 23 11 Shale Potential fault/fracture zone
Wyacca WCDD001 23 87 64 Carbonaceous
shale
Black shale. Increasingly carbonaceous with depth
Wyacca WCDD001 87 92.5 5.5 Carbonaceous
shale
Broken and faulted interval approaching ore zone.
Suspected chlorite alteration.
Wyacca WCDD001 92.5 94.8 2.3 Dolomite Brecciated ore zone with completed Fe Mn carbonate
replacement. Chalcopyrite mineralisation throughout.
Wyacca WCDD001 94.8 95.2 0.4 Siltstone Thin chalcopyrite veining within Wilyerpa siltstone
Wyacca WCDD001 95.2 118 22.8 Siltstone Wilyerpa siltstone. Relatively unaltered with coarse
pyrite replacement of permeable coarser beds
Wyacca WCDD002 0 6 6 Carbonaceous
shale
Weathered shales
Wyacca WCDD002 6 15 9 Carbonaceous
shale
Oxidised. Goethite rich. Gossaneous zone. Likely Fe
and Mn enriched shales.
Wyacca WCDD002 15 18 3 Carbonaceous
shale
Altered carbonaceous shales.
Wyacca WCDD002 18 24 6 Carbonaceous
shale
Ore zone. Altered and brecciated rock. Cu
mineralisation within Mn oxide minerals. Rich in Fe
and Mn. Carbonate alteration throughout.
Wyacca WCDD002 24 26 2 Carbonaceous
shale
Broken / faulted shale proximal to contact with
Wilyerpa formation
Wyacca WCDD002 26 41.6 15.6 Siltstone Strong intensity veining and associated alteration
within Wilyerpa siltstone. Highly fractured.
Wyacca WCDD003 0 0.4 0.4 Siltstone Soil and weathered rock
Wyacca WCDD003 0.4 6 5.6 Siltstone Siltstones. Tapley Hill Formation
Wyacca WCDD003 6 10.3 4.3 Siltstone Altered siltstones. Highly fractured. Moderate to
intense carbonate veining
Wyacca WCDD003 10.3 12.25 1.95 Siltstone Bedded siltstones. Weakly altered with carbonate
veining.
Wyacca WCDD003 12.25 12.8 0.55 Dolomite Malachite rich ore zone within altered zone of
carbonate and silica replacement.
Wyacca WCDD003 12.8 25.2 12.4 Siltstone Relatively unaltered siltstones with carbonate veining.

Table 3. Morgan’s Creek Diamond Drillhole Details

Prospect Hole ID X Y Azimuth Dip EOH drilled depth Hole status
Morgan’s Bore MCDD001 279046 6457603 220 -60 74.1 Complete
Oxide Hill MCDD002 275504 6458101 180 -60 7.2 Abandoned
Oxide Hill MCDD003 275502 6458101 180 -60 186.65 Complete
Hydrothermal Hill MCDD004 274924 6458698 210 -60 150.2 Complete

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Table 3. Morgan’s Creek Diamond Drillhole Summary Logs

Prospect Hole ID From To Interval Lithology Comments
Morgan’s Bore MCDD001 0 0.9 0.9 Alluvial sediments
Morgan’s Bore MCDD001 0.9 8.6 7.7 Dolerite Dolerite saprock
Morgan’s Bore MCDD001 8.6 14.3 5.7 Diapir Quartzite/Siltstone/Carbonate Breccia
Morgan’s Bore MCDD001 14.3 15 0.7 Dolerite Fault with milled dolerite and dolerite gravel
Morgan’s Bore MCDD001 15 15.8 0.8 Siltstone Carbonate siltstone
Morgan’s Bore MCDD001 15.8 20.1 4.3 Diapir Carbonate Breccia
Morgan’s Bore MCDD001 20.1 38.7 18.6 Siltstone Carbonate siltstone with quartz veining 27-38m in
breccia fill, including Fe and Malachite from 27-
32m.
Morgan’s Bore MCDD001 38.7 43.6 4.9 Breccia Dolomite, Dolerite and Siltstone Breccia. Base of
Complete Oxidation.
Morgan’s Bore MCDD001 43.6 49.25 5.65 Breccia Dolomite breccia, well healed and crystalline
Morgan’s Bore MCDD001 49.25 74 24.75 Siltstone Fine grained carbonate silt/mudstone. Calcite
veining with pyrite and minor chalcopyrite.
Celestine vein breccia fill.
Oxide Hill MCDD003 0 1.2 1.2 Alluvium Alluvial Clays
Oxide Hill MCDD003 1.2 17.45 16.25 Shale Broken core. Brecciated and weathered shales.
Poor core recovery.
Oxide Hill MCDD003 17.45 28.5 11.05 Siltstone Non-calcareous sands and silts with intense
goethite/limonite alteration. Mn oxides 20-21.6m.
Oxide Hill MCDD003 28.5 55.55 27.05 Siltstone Grey siltstone, weakly brecciated with vuggy
matrix. Hematite and goethite alteration
Oxide Hill MCDD003 55.55 65.7 10.15 Limestone Matrix supported siltstone and limestone breccia
(diapir) with carbonate matrix. Strong Goethite
oxidation. Base of Complete Oxidation.
Oxide Hill MCDD003 65.7 186.65 119.6 Marble White to green-grey crystalline marble breccia
with micaceous siltstone clasts.
Hydrothermal
Hill
MCDD004 0 25.5 25.5 Diapir Carbonate Breccia (diapir)
Hydrothermal
Hill
MCDD004 25.5 30.6 5.1 Dolerite Brecciated dolerite with carbonate matrix
Hydrothermal
Hill
MCDD004 30.6 34.4 3.8 Skarn? Biotite altered carbonate breccia, with sericite
and sodic alteration.
Hydrothermal
Hill
MCDD004 34.4 46.2 11.8 Dolerite Strong serpentine alteration plus magnetite and
hematite alt. Hematite and sericite alteration.
Hydrothermal
Hill
MCDD004 46.2 51.95 5.75 Dolerite Semi-massive pyrite and magnetite alteration
gradinginto finegrained chill margin.
Hydrothermal
Hill
MCDD004 51.95 150.2 98.25 Dolerite Strongly altered (serpentinized) mafic-ultramafic.
Magnetite, Pyrite and Calcite alteration. Pyrite
vug/vein infill. Brecciated contact at fine-coarse
grain transition. Chalcopyrite within occasional
carbonate veins. Increasingly gabbroic downhole.

This announcement was approved by the Board of Taruga Minerals Limited.

For more information contact:

Thomas Line Eric de Mori CEO Director +61 8 9486 4036 +61 8 6169 2668

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Competent person’s statement

The information in this report that relates to exploration results is based on, and fairly represents information and supporting documentation prepared by Mr Brent Laws, a Competent Person who is a Member of The Australasian Institute of Mining and Metallurgy. Mr Laws is the Exploration Manager of Taruga Minerals Limited. Mr Laws 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 “Australasian Code for Reporting of Exploration Results, Mineral Resource and Ore Reserves”. Mr Laws consents to the inclusion in this report of the matters based on their information in the form and context in which it appears.

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JORC Code, 2012 Edition – Table 1 report template

Section 1 Sampling Techniques and Data

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

Criteria JORC Code explanation JORC Code explanation Commentary Commentary
Sampling Nature and quality of sampling (e.g. cut channels, Core preparation and sampling is ongoing.
techniques random chips, or specific specialised industry standard Core is sampled after geological and
measurement tools appropriate to the minerals under structural logging. Core is cut to ½ core
investigation, such as down hole gamma sondes, or through a standardised procedure that
handheld XRF instruments, etc). These examples includes consistent sampling of the same
should not be taken as limiting the broad meaning of side of the cut core. Core is sampled to
sampling. lithological, structural and mineralised
Include reference to measures taken to ensure sample boundaries with sample intervals between
representivity and the appropriate calibration of any 30cm and 1m in length to allow sufficient
measurement tools or systems used. sample for representative analysis.
Aspects of the determination of mineralisation that are Intervals selected for laboratory analysis
Material to the Public Report. are identified through visual logging by a
In cases where ‘industry standard’ work has been done
this would be relatively simple (e.g. ‘reverse circulation
geologist and utilises a handheld XRF to
confirm the presence of mineralisaton.
drilling was used to obtain 1 m samples from which 3 Each geological interval identified was
kg was pulverised to produce a 30 g charge for fire logged separately including selective pXRF
assay’). In other cases more explanation may be readings to support mineral identification or
required, such as where there is coarse gold that has regular 5cm spaced readings for indicative
inherent sampling problems. Unusual commodities or mineralisation trends over select intervals.
mineralisation types (e.g. submarine nodules) may
warrant disclosure of detailed information.
Drilling Drill type (e.g. core, reverse circulation, open-hole Drilling method included Diamond Core HQ
techniques hammer, rotary air blast, auger, Bangka, sonic, etc) size drilled from surface with a nominal
and details (e.g. core diameter, triple or standard tube, 63.5mm core diameter.
depth of diamond tails, face-sampling bit or other type, Where possible core was orientated to
whether core is oriented and if so, by what method, allow for structural measurements.
etc). Downhole surveys were taken at 6m
(collar), 30m and every subsequent 30m
drilled with a final survey at end of hole
depth.
Drill sample Method of recording and assessing core and chip Core recovery was assessed through
recovery sample recoveries and results asses measurement of core in relation drilled
Measures taken to maximise sample recovery and depths and core blocks. Core recoveries
ensure representative nature of the samples. were above acceptable industry standard
Whether a relationship exists between sample recovery limitations with >98% core recovery.
and grade and whether sample bias may have No sample quality issues are expected.
occurred due to preferential loss/gain of fine/coarse
material.
Logging Whether core and chip samples have been geologically
Drill holes were geologically logged by
and geotechnically logged to a level of detail to support industry standard methods, including
appropriate Mineral Resource estimation, mining lithology, structure, alteration and
studies and metallurgical studies. mineralisation.
Whether logging is qualitative or quantitative in nature. All core trays were photographed wet and
Core (or costean, channel, etc) photography. dry.
The total length and percentage of the relevant The logging is qualitative in nature and of
intersections logged. sufficient detail supporting the current
interpretations.
Sub-sampling
If core, whether cut or sawn and whether quarter, half Core is cut to ½ core through a
techniques or all core taken. standardised procedure that includes
and sample If non-core, whether riffled, tube sampled, rotary split, consistent sampling of the same side of the
preparation etc and whether sampled wet or dry. cut core. Core is sampled to lithological,
For all sample types, the nature, quality and structural and mineralised boundaries with
appropriateness of the samplepreparation technique. sample intervals between 30cm and 1m in

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Criteria
JORC Code explanation
Commentary

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 field duplicate/second-half
sampling.

Whether sample sizes are appropriate to the grain size
of the material being sampled.
length to allow sufficient sample for
representative analysis. Intervals selected
for laboratory analysis are identified
through visual logging by a geologist and
utilises a handheld XRF to confirm the
presence of mineralisaton.

A Vanta pXRF was used with reference
standards (CRM) to ensure accuracy of
readings. No results reported are from
pXRF sampling.
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 (e.g.
standards, blanks, duplicates, external laboratory
checks) and whether acceptable levels of accuracy (i.e.
lack of bias) and precision have been established.

Samples are analysed at Bureau Veritas,
Adelaide for broad suite multi-element
analysis using 4-acid digest ICP-MS. Gold
and PGE analysis was by Fire Assay ICP-
OES.

Sampling QA/QC including standards (6
different CRM to cover low mid and higher-
grade material of various elements
including but not limited to copper, gold,
silver, zinc, scandium, nickel and barium)
and duplicates were included in each
sample despatch and reported in the
laboratory results. QA/QC samples
included Company selected CRM material
including blank material and duplicate
samples. Laboratory QAQC has additional
checks including standards, blanks and
repeat samples that were conducted
regularly on every batch. Company
standards are included every 25thsample
and a duplicate every 30th.

No results from core drilling are included in
this report.
Verification of
sampling and
assaying

The verification of significant intersections by either
independent or alternative company personnel.

The use of twinned holes.

Documentation of primary data, data entry procedures,
data verification, data storage (physical and electronic)
protocols.

Discuss any adjustment to assay data.

Taruga’s geologists have sufficient
experience to carry out core processing
and logging and have experienced senior
geologists and technical consultants
available for verification and validation of
results and measurements.

Significant intercepts are reported by
Company representatives based on best
practice and available information.

All significant intercepts are reported as
downhole lengths and are not necessarily
indicative of true thickness unless stated

Logs and measurements were all recorded
in hard copy on paper before digital data
entry. All data is stored securely with digital
backups. All data entry procedures include
data validation.
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.

Specification of the grid system used.

Quality and adequacy of topographic control.

All drillhole collars were surveyed after
drilling using a handheld GPS. Datum used
is GDA94 Zone 54.

Downhole surveys were taken at 6m
(collar), 30m and every subsequent 30m
drilled with a final survey at end of hole
depth.
Criteria
JORC Code explanation
Commentary

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 field duplicate/second-half
sampling.

Whether sample sizes are appropriate to the grain size
of the material being sampled.
length to allow sufficient sample for
representative analysis. Intervals selected
for laboratory analysis are identified
through visual logging by a geologist and
utilises a handheld XRF to confirm the
presence of mineralisaton.

A Vanta pXRF was used with reference
standards (CRM) to ensure accuracy of
readings. No results reported are from
pXRF sampling.
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 (e.g.
standards, blanks, duplicates, external laboratory
checks) and whether acceptable levels of accuracy (i.e.
lack of bias) and precision have been established.

Samples are analysed at Bureau Veritas,
Adelaide for broad suite multi-element
analysis using 4-acid digest ICP-MS. Gold
and PGE analysis was by Fire Assay ICP-
OES.

Sampling QA/QC including standards (6
different CRM to cover low mid and higher-
grade material of various elements
including but not limited to copper, gold,
silver, zinc, scandium, nickel and barium)
and duplicates were included in each
sample despatch and reported in the
laboratory results. QA/QC samples
included Company selected CRM material
including blank material and duplicate
samples. Laboratory QAQC has additional
checks including standards, blanks and
repeat samples that were conducted
regularly on every batch. Company
standards are included every 25thsample
and a duplicate every 30th.

No results from core drilling are included in
this report.
Verification of
sampling and
assaying

The verification of significant intersections by either
independent or alternative company personnel.

The use of twinned holes.

Documentation of primary data, data entry procedures,
data verification, data storage (physical and electronic)
protocols.

Discuss any adjustment to assay data.

Taruga’s geologists have sufficient
experience to carry out core processing
and logging and have experienced senior
geologists and technical consultants
available for verification and validation of
results and measurements.

Significant intercepts are reported by
Company representatives based on best
practice and available information.

All significant intercepts are reported as
downhole lengths and are not necessarily
indicative of true thickness unless stated

Logs and measurements were all recorded
in hard copy on paper before digital data
entry. All data is stored securely with digital
backups. All data entry procedures include
data validation.
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.

Specification of the grid system used.

Quality and adequacy of topographic control.

All drillhole collars were surveyed after
drilling using a handheld GPS. Datum used
is GDA94 Zone 54.

Downhole surveys were taken at 6m
(collar), 30m and every subsequent 30m
drilled with a final survey at end of hole
depth.

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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 sufficient
to establish the degree of geological and grade
continuity appropriate for the Mineral Resource and
Ore Reserve estimation procedure(s) and
classifications applied.

Whether sample compositing has been applied.

Data is insufficient to be used in a Mineral
Resource Estimate. The drilling is
reconnaissance style exploration with data
collected sufficient to guide and define
further exploration activities.

Core sample intervals are based on
lithological, structural and mineralised
boundaries. No sample compositing has
been used.
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 previous and current drilling being
reported has identified and defined a
variable sedimentary package within the
Worumba diapir mega breccia including
various rafted blocks in differing
orientation. Outcrop of the dolomite
metasediments on the margin of the
Worumba Diapir and rafted sediments
within the diapir assist in drillhole design to
best intercept the stratigraphy.

Where possible drillholes are angled
towards the interpreted stratigraphic
horizon so intercepts are generally
reflective of true thickness although some
holes drilled in a deliberate orientation to
gain perspective of stratigraphic or
structural orientation will not be a direct
reflection of true thickness. All reported
lengths are to be considered downhole
lengths unless stated as calculated true
thickness.
Sample
security

The measures taken to ensure sample security.

The samples are collected, processed and
despatched by the Supervising Geologist
before being sent by courier to Bureau
Veritas, Adelaide.
Audits or
reviews

The results of any audits or reviews of sampling
techniques and data.

No audits completed.
Criteria
JORC Code explanation
Commentary
Data spacing
and
distribution

Data spacing for reporting of Exploration Results.

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.

Whether sample compositing has been applied.

Data is insufficient to be used in a Mineral
Resource Estimate. The drilling is
reconnaissance style exploration with data
collected sufficient to guide and define
further exploration activities.

Core sample intervals are based on
lithological, structural and mineralised
boundaries. No sample compositing has
been used.
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 previous and current drilling being
reported has identified and defined a
variable sedimentary package within the
Worumba diapir mega breccia including
various rafted blocks in differing
orientation. Outcrop of the dolomite
metasediments on the margin of the
Worumba Diapir and rafted sediments
within the diapir assist in drillhole design to
best intercept the stratigraphy.

Where possible drillholes are angled
towards the interpreted stratigraphic
horizon so intercepts are generally
reflective of true thickness although some
holes drilled in a deliberate orientation to
gain perspective of stratigraphic or
structural orientation will not be a direct
reflection of true thickness. All reported
lengths are to be considered downhole
lengths unless stated as calculated true
thickness.
Sample
security

The measures taken to ensure sample security.

The samples are collected, processed and
despatched by the Supervising Geologist
before being sent by courier to Bureau
Veritas, Adelaide.
Audits or
reviews

The results of any audits or reviews of sampling
techniques and data.

No audits completed.

ASX:TAR

Section 2 Reporting of Exploration Results

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

Criteria JORC Code explanation JORC Code explanation Commentary Commentary
Mineral Type, reference name/number, location and Exploration Licence EL6541 (Mt
tenement and ownership including agreements or material issues Craig/MCCP) is 100% owned by Strikeline
land tenure with third parties such as joint ventures, Resources Pty Ltd a fully owned subsidiary
status partnerships, overriding royalties, native title of Taruga Minerals Ltd. The tenement is in
interests, historical sites, wilderness or national park good standing with no known impediments to
and environmental settings. operate in the area.
The security of the tenure held at the time of
reporting along with any known impediments to
obtaining a licence to operate in the area.
Exploration Acknowledgment and appraisal of exploration by Historical Exploration: Mt Craig
done by other other parties. - Extensive small-scale historic mining for
parties base metals occurred throughout the area.
This occurred most prominently at the
Wyacca Mine and Wirrawilka workings.
Further historic shafts at Iron King are
presumed to have mined Silver and Gold.
- From the 1960’s onwards numerous
companies have explored the region with
soil, stream, rock chip & channel sampling,
geophysics and drilling campaigns. The most
prominent prior exploration was conducted
by Cams Leases Pty Ltd., Copper Range
(SA) Pty Ltd., Gold Copper Exploration Ltd.,
SAEI Triassic Coal Exploration & Utah
Development Company Ltd.
Geology Deposit type, geological setting and style of Mt Craig: The Morgan Creek prospect is
mineralisation. dominated by the Worumba diapir which
include large rafted blocks of sediments
including those of the Tapley Hill Fm, also
within the diapir are mafics of variable origin.
The western margin includes a target contact
between the dolomite metasediments and
the Worumba Diapir. Dolomite is a common
reactive rock type within the diapir related
deposits, trapping mineralisation close to the
diapir margins. Dissolved metalliferous
brines from the diapir travel along structural
conduits to sites of suitable reactive
deposition.
Drill hole A summary of all information material to the All completed drillhole collar information is
Information understanding of the exploration results including a included in the appendices.
tabulation of the following information for all Material
Summary geological logging is included in
drill holes: the appendices.
o easting and northing of the drill hole collar No assay data is being reported at this time.
o elevation or RL (Reduced Level – elevation
above sea level in metres) of the drill hole collar
o dip and azimuth of the hole
o down hole length and interception depth
o hole length.
If the exclusion of this information is justified on the
basis that the information is not Material and this
exclusion does not detract from the understanding
of the report, the Competent Person should clearly
explain why this is the case.

ASX:TAR

Criteria
JORC Code explanation
Commentary
Data
aggregation
methods

In reporting Exploration Results, weighting
averaging techniques, maximum and/or minimum
grade truncations (e.g. cutting of high grades) and
cut-off grades are usually Material and should be
stated.

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 assay data is being reported at this time.
Relationship
between
mineralisation
widths and
intercept
lengths

These relationships are particularly important in the
reporting of Exploration Results.

If the geometry of the mineralisation with respect to
the drill hole angle is known, its nature should be
reported.

If it is not known and only the down hole lengths are
reported, there should be a clear statement to this
effect (e.g. ‘down hole length, true width not
known’).

Where possible interpreted potential
mineralisation widths have been shown on
images or noted within the document. Some
holes drilled in a deliberate orientation to
gain perspective of structural or stratigraphic
orientation and as such will not be a direct
reflection of true thickness. All reported
lengths are to be considered downhole
lengths unless stated as calculated true
thickness.
Diagrams

Appropriate maps and sections (with scales) and
tabulations of intercepts should be included for any
significant discovery being reported These should
include, but not be limited to a plan view of drill hole
collar locations and appropriate sectional views.

Appropriate plan and cross section diagrams
of collar location, surface features and
results are provided in the report.
Balanced
reporting

Where comprehensive reporting of all Exploration
Results is not practicable, representative reporting
of both low and high grades and/or widths should be
practiced to avoid misleading reporting of
Exploration Results.

All relevant information is reported within the
document or included in the appendices if
not reported previously.
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.

All relevant and meaningful recent
exploration or known historical exploration
data is included in this report or has been
previously released.

Recent geophysical programs mentioned in
this report include Wyacca undergoing a
gravity survey on a 200m x 50m spacing
(and broader 400m x 50m spacing), and
50m line spacing high resolution ground
magnetics survey.

Morgan’s Creek undergoing a gravity survey
on a 200m x 50m spacing (and broader
400m x 50m spacing), and 50m line spacing
high resolution ground magnetics.
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).

Diagrams clearly highlighting the areas of possible
extensions, including the main geological
interpretations and future drilling areas, provided
this information is not commercially sensitive.

RC drilling is planned to commence shortly
to continue the assessment of conducive
rock types for hosting mineralisation and will
be planned and guided by ongoing field
mapping and soil sample results combined
with available geophysical data and
geological interpretations.

New and historical data will be combined
and used to finalise further programs.
Criteria
JORC Code explanation
Commentary
Data
aggregation
methods

In reporting Exploration Results, weighting
averaging techniques, maximum and/or minimum
grade truncations (e.g. cutting of high grades) and
cut-off grades are usually Material and should be
stated.

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 assay data is being reported at this time.
Relationship
between
mineralisation
widths and
intercept
lengths

These relationships are particularly important in the
reporting of Exploration Results.

If the geometry of the mineralisation with respect to
the drill hole angle is known, its nature should be
reported.

If it is not known and only the down hole lengths are
reported, there should be a clear statement to this
effect (e.g. ‘down hole length, true width not
known’).

Where possible interpreted potential
mineralisation widths have been shown on
images or noted within the document. Some
holes drilled in a deliberate orientation to
gain perspective of structural or stratigraphic
orientation and as such will not be a direct
reflection of true thickness. All reported
lengths are to be considered downhole
lengths unless stated as calculated true
thickness.
Diagrams

Appropriate maps and sections (with scales) and
tabulations of intercepts should be included for any
significant discovery being reported These should
include, but not be limited to a plan view of drill hole
collar locations and appropriate sectional views.

Appropriate plan and cross section diagrams
of collar location, surface features and
results are provided in the report.
Balanced
reporting

Where comprehensive reporting of all Exploration
Results is not practicable, representative reporting
of both low and high grades and/or widths should be
practiced to avoid misleading reporting of
Exploration Results.

All relevant information is reported within the
document or included in the appendices if
not reported previously.
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.

All relevant and meaningful recent
exploration or known historical exploration
data is included in this report or has been
previously released.

Recent geophysical programs mentioned in
this report include Wyacca undergoing a
gravity survey on a 200m x 50m spacing
(and broader 400m x 50m spacing), and
50m line spacing high resolution ground
magnetics survey.

Morgan’s Creek undergoing a gravity survey
on a 200m x 50m spacing (and broader
400m x 50m spacing), and 50m line spacing
high resolution ground magnetics.
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).

Diagrams clearly highlighting the areas of possible
extensions, including the main geological
interpretations and future drilling areas, provided
this information is not commercially sensitive.

RC drilling is planned to commence shortly
to continue the assessment of conducive
rock types for hosting mineralisation and will
be planned and guided by ongoing field
mapping and soil sample results combined
with available geophysical data and
geological interpretations.

New and historical data will be combined
and used to finalise further programs.

ASX:TAR