Balerion Drilling Intersects Sulphide-Bearing Contact Zone
Released
Released
Announcement PDF
Level 8, 216 St Georges Terrace, Perth, Western Australia 6000
T: +61 (08) 9481 0389 E: info@exultantmining.com.au
ACN 684 147
13th
August 2026
www.exultantmining.com.au
BALERION DRILLING INTERSECTS SULPHIDE-BEARING
CONTACT ZONE
HIGHLIGHTS
• BLRCDD004 and BLRCDD005 successfully tested the interpreted
mineralised sheared contact down-dip of historical high-grade
polymetallic intersections with visible sphalerite-galena-chalcopyrite
sulphides observed
• Core photos and visual logging from BLRCDD004 and BLRCDD005 show
disseminated, semi-massive and narrow massive sulphides within the
targeted shear zone, with BLRCDD005 displaying the stronger visual
sulphide development.
• Results support an emerging interpretation that stronger sulphide
development is focused along the sheared rhyolite-volcaniclastic
contact
• Assay results from BLRCDD001 & BLRCDD002 confirm base metal and
silver anomalism
• BLRCDD006 is underway as the planned final hole of the current
program, after which drilling, assay, geological, geochemical and
geophysical datasets will be integrated to determine the next phase of
exploration
Exultant Mining Limited (ASX: 10X) (“Exultant” or “the Company”) is pleased to provide an update on
its maiden drilling program at the Balerion Prospect, located within the Company’s Peak View Project in
New South Wales.
This announcement reports laboratory assays from BLRCDD001 and BLRCDD002 and preliminary visual
observations from BLRCDD004 and BLRCDD005. Laboratory assays for BLRCDD004 and BLRCDD005
remain pending.
Comment from Executive Chairman, Brett Grosvenor:
“The latest drilling has advanced our understanding of Balerion and, importantly, has intersected the
targeted rhyolite-volcaniclastic contact in BLRCDD004 and BLRCDD005 down-dip of historical high-grade
mineralisation.
The presence of disseminated, semi-massive and narrow massive sulphides within the sheared contact
zone is encouraging, particularly in BLRCDD005 where visible sulphides appear more abundant than in
BLRCDD004. While laboratory assays are required before grade can be determined, the visual
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observations are consistent with our current interpretation that the sheared contact is an important
control on stronger sulphide development.
The assays received from BLRCDD001 and BLRCDD002 were generally low grade, but they are still useful
in refining our geological model. They suggest that the underlying volcaniclastic package is mineralised,
with higher-grade sulphides more likely to be concentrated where hydrothermal fluids have exploited
the sheared contact with the overlying rhyolite.
This is a positive step for the program and we look forward to the receipt of the outstanding assays from
BLRCDD004 and BLRCDD005 to confirm our understanding. With BLRCDD006 now underway, we look
forward to integrating the full drilling, assay, geological, geochemical and geophysical datasets to guide
the next phase of exploration at Balerion.”
BALERION DRILLING SUMMARY
Balerion is contained within Exultant’s 100%-owned EL9411 tenement, located approximately 35km
northeast of Cooma in New South Wales. The prospect comprises multi-element geochemical
anomalism together with IP chargeability, resistivity, gravity and magnetic responses associated with
altered volcanic and sedimentary rocks.
Exultant has completed five reverse circulation and diamond drill holes (BLRCDD001-BLRCDD005) at the
Balerion Prospect during the current program. The holes were designed to test priority geophysical and
geochemical targets defined by surveys previously completed by Exultant. Historical assay results and
drilling completed to date have demonstrated the presence of a consistent, sheared and mineralised
contact between an overlying unit of coarse-grained rhyolite and an underlying volcaniclastic sandstone.
The higher-grade sulphide intersections identified to date are associated with the shear zone developed
along this contact, while lower-grade disseminated and vein-hosted sulphides occur within the
underlying volcaniclastic package.
The results from these holes are discussed and presented below.
BLRCDD004 – visual results
BLRCDD004 was drilled to a total depth of 267.4m and intersected a package of sedimentary and volcanic
rocks with a strongly altered, talc-rich shear zone at the contact between an overlying rhyolite and
underlying volcaniclastic sandstone. Narrow intervals of semi-massive and locally massive sulphides
were observed within the shear zone (Fig. 1).
BLRCDD004 targeted a resistivity-low anomaly approximately 190m down-dip from high-grade massive
sulphides intersected in historical drillhole PVI003 which previously returned 2.5m @ 5.87% Zn, 3.33%
Pb, 0.67% Cu & 22g/t Ag from 53.7m1
and approximately 80m down-dip of PVI008, which previously
returned 0.8m @ 22.0% Zn, 11.6% Pb, 1.2% Cu, 155g/t Ag and 0.5g/t Au from 152.6m¹ (Fig. 2).
Visual sulphide estimates for BLRCDD004 are provided in Table 2. Visual estimates of mineral abundance
are preliminary and should not be considered a proxy or substitute for laboratory analysis. They do not
determine metal grades and may not identify impurities or deleterious physical properties relevant to
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valuation. Samples from BLRCDD004 have been submitted to the laboratory for analysis, with results
expected in 4 - 6 weeks. BLRCDD005 samples are expected to be dispatched in 1 week with results
expected in 6 - 8 weeks.
BLRCDD005 – visual results
BLRCDD005 targeted a resistivity-low anomaly approximately 220m down-dip of historical drillhole
PVI006 (Fig. 3), which previously intersected 4.4m @ 342.7g/t Ag, 4.0% Pb, 1.1% Cu, 0.74g/t Au & 0.84%
Zn from 48.7m.¹
The hole was drilled to a total depth of 271.9m and intersected the same stratigraphic package and
strongly altered, talc-rich sulphide-bearing shear zone observed in BLRCDD004 (Fig. 1). Disseminated,
semi-massive and massive sulphides were more abundant in BLRCDD005 than in BLRCDD004.
Visual sulphide estimates for BLRCDD005 are provided in Table 2. The abundance and distribution of
visible sulphides do not establish metal grades, which can only be determined by laboratory analysis.
Samples from BLRCDD005 are pending submission.
6.5cm
(a)
(b)
6.5cm
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Figure 1. (a) Massive sphalerite-pyrite-galena-chalcopyrite mineralisation hosted within a talc shear zone in
BLRCDD005, 251.75m. (b) Heavy disseminated sphalerite-pyrite-galena-chalcopyrite mineralisation in
BLRCDD004, 212.5m. (c) Semi-massive sphalerite-pyrite-galena in talc-rich shear zone in BLRCDD005, 247m. (d)
Sphalerite-galena-pyrite mineralisation in talc-rich shear zone in BLRCDD005, 251.4m. Visual estimate only;
assays pending. Refer to Table 2 for visual sulphide estimates and cautionary statement.
(c)
(d)
6.5cm
6.5cm
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Figure 2. Section 6006865 (+/-20m) showing BLRCDD004 targeting a resistivity low anomaly (green shells) down
dip of historic high-grade mineralisation intersected in PVI003 (2.5m @ 5.87% Zn, 3.33% Pb, 0.67% Cu &
22g/t Ag from 53.7m)¹ and PVI008 (0.8m @ 22.0% Zn, 11.6% Pb, 1.2% Cu, 155g/t Ag and 0.5g/t Au
from 152.6m)¹
Figure 3. Section 6006825 (+/-20m) showing BLRCDD005 targeting a resistivity low anomaly (green shells) down
dip of historic high-grade mineralisation intersected in PVI006 (4.4m @ 342.7g/t Ag, 4.0% Pb, 1.1% Cu,
0.74g/t Au & 0.84% Zn from 48.7m)¹
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ASSAY RESULTS
BLRCDD001
BLRCDD001 targeted a coincident chargeability and resistivity high located within the volcaniclastic
footwall (Fig. 4). The hole intersected strongly altered volcanic and sedimentary rocks containing
disseminated and narrow vein-hosted zinc-lead-copper sulphides.
Laboratory assays confirmed generally low-grade zinc-lead-copper-silver mineralisation. Results
included:
• 3.0m @ 0.14% Zn, 0.11% Pb, 0.01% Cu and 0.58g/t Ag from 82.0m, including:
o 1.0m @ 0.31% Zn, 0.21% Pb, 0.02% Cu and 0.72g/t Ag from 84.0m; and
• 0.5m @ 0.29% Cu, 0.14% Pb and 2.41g/t Ag from 105.5m
BLRCDD002
BLRCDD002 targeted a resistivity-low anomaly (Fig. 5) and intersected a very strongly sheared and
deformed contact between overlying rhyolite and underlying volcaniclastic rocks. The contact zone
contained intense alteration together with disseminated, banded and vein-hosted sulphides.
Assays returned broad, generally low-grade silver and base-metal anomalism, including:
• 10.7m @ 2.70g/t Ag from 125.6m, containing 3.9m of core loss, including:
o 1.5m @ 7.30g/t Ag from 131.8m;
• 10.3m @ 0.21% Zn, 0.05% Pb and 0.57g/t Ag from 149.0m, containing 2.1m of core loss,
including:
o 0.6m @ 1.12% Zn, 0.17% Pb, 0.07% Cu and 2.35g/t Ag from 152.0m; and
• 4.3m @ 0.16% Cu and 1.09g/t Ag from 164.0m
BLRCDD002 intersected multiple zones of significant shearing. The 10.7m interval from 125.6m contains
3.9m of core loss, while the 10.3m interval from 149.0m contains 2.1m of core loss. Core-loss intervals
have been retained within the reported downhole widths and assigned zero grade for Zn, Pb, Cu and Ag
when calculating length-weighted composite grades.
The assay results from BLRCDD001 and BLRCDD002 confirm the presence of zinc-lead-copper-silver
mineralisation, although grades were generally low. The geological and structural information obtained
from the holes will be incorporated into the Company’s interpretation of the Balerion Prospect.
BLRC003
No significant assay results were returned from BLRC003.
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Figure 4. Section 6006565N (+/- 25m) showing BLRCDD001 drill trace and assay results in relation to the
coincident chargeable (green-red shells) - resistive high anomaly it was targeting
Figure 5. Section 60066405N (+/- 25m) showing BLRCDD002 drill trace and assay results in relation to the
resistivity low (green shells) anomaly it was targeting down dip of PVI010 (1.3m @ 3.4% Zn, 1.4% Pb, 21 g/t Ag &
0.14% Cu from 106.1m)1
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PROGRAM STATUS & NEXT STEPS
• BLRCDD006 is currently being drilled and was at a depth of 95m at the time of writing.
• BLRCDD006 is planned as the final hole of the current drilling program, following the completion
of five holes at Balerion and is planned to test a chargeable anomaly up-dip of BLRCDD004 &
BLRCDD005
• The program has tested the priority geophysical and geochemical targets, including targets
down-dip of historical high-grade mineralisation and the interpreted sheared contact between
the rhyolite and underlying volcaniclastic package.
• Outstanding assays from BLRCDD004 and BLRCDD005 will be incorporated into this
interpretation and used to determine the next phase of exploration at Balerion.
• Following completion of BLRCDD006, the Company will integrate the drilling, assay, geological,
geochemical and geophysical datasets to refine its interpretation of the Balerion mineralised
system.
Figure 6. Balerion Drilling Plan with IP chargeability shells (green-yellow-red) and gravity high shells (red)
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This announcement has been approved for release by the Chairman of the Board of Directors of the
Company.
For further information on Exultant Mining Limited please contact:
Brett Grosvenor Paul Berson
Exultant Mining Limited Corporate Storytime
Executive Chairman Investor Relations
Info@exultantmining.com.au paul@corporatestorytime.com
Ph: +61 (08) 9481 0389 Ph: +61 (0) 421 647 445
1 - Refer to ASX announcement dated 9 April 2026, “Multiple High-Priority Drill Targets at Peak View Prospect”
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ABOUT THE PEAK VIEW PROJECT
The Peak View Project is located 35km NE of Cooma within the Lachlan Fold Belt. The project is
prospective for gold, silver, copper & base metals and hosts the Balerion (formerly Peak View), Big Badja
and Undoo Creek prospects.
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Disclaimer
Someofthestatementsappearinginthisannouncementmay beinthenatureofforward-lookingstatements.
You should be aware that such statements are only predictions and are subject to inherent risks and
uncertainties.ThoserisksanduncertaintiesincludefactorsandrisksspecifictotheindustriesinwhichExultant
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 Exultant’s control. Exultant 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 Exultant, 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
of the date of this announcement. This announcement is not an offer, invitation or recommendation to
subscribe for or purchase securities by Exultant. Nor does this announcement constitute investment or
financial product advice (nor tax, accounting or legal advice) and is not intended to be used for the basis of
making an investment decision. Investors should obtain their own advice before making any investment
decision.
Competent Person Statement
The information in this announcement that relates to Exploration Results is based on, and fairly represents,
informationcompiledandreviewedbySebastianHind.Mr Hind isanExplorationManagerforExultantMining
LimitedandaMemberoftheAustralasianInstituteofMiningandMetallurgy(Membershipnumber3116971).
Mr Hind has sufficient experience which is relevant to the style of mineralisation and type of deposit under
consideration and to the activity which he is undertaking to qualify as a Competent Person as defined in the
2012 Edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore
Reserves (JORC Code). Mr Hind consents to the inclusion in this announcement of the matters based on his
information in the form and context in which it appears.
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Table 1: Balerion Prospect Drillhole Locations
HOLE ID MGA20z55_E MGA20z55_N RL DIP AZI (Grid) FINAL DEPTH (m)
BLRCDD001 713551 6006584 940 -60 245 245.5
BLRCDD002 713669 6006639 944 -80 245 189.4
BLRC003 713346 6006618 976 -65 270 198
BLRCDD004 713708 6006859 958 -75 245 267.4
BLRCDD005 713736 6006831 955 -80 240 271.9
Table 2: BLRCDD004 & BLRCDD005 Visual Sulphide Estimates
INTERVAL (M)
Mineralisation Description (%)
From (m) To (m) Width (m)
BLRCDD004
212.5 212.8 0.3 Heavy disseminated to semi-massive
Sp (10%) – Py (10%) – Gn (5%) and lesser Cpy (2.5%)
224.35 225.35 1
Shear hosted Sp (7.5%) – Gn (5%) - Py (5%). Sulphides are
present as narrow (<4cm) bands of massive sulphides and
bands throughout the talc shear foliation.
225.35 226.5 1.15 Blebs/masses of Sp (5%) – Gn (2.5%) – Py (1%) hosted
throughout a brecciated quartz vein
228.4 228.85 0.45 Heavy disseminated Py (7.5%) – Cpy (1%) – Gn (1%) – Sp (1%)
in a talc shear zone
BLRCDD005
240.15 240.55 0.4 Dominantly fine-grained disseminated Sp (12%) – Py (12%) – Gn (5%)
and minor Cpy (1%) in Py-Cpy veins
240.55 244.4 3.85 Fine-grained disseminated Py (1%) – Sp (1%) – Gn (0.5%) throughout
shear zone
245.8 246.3 0.5 Heavy disseminated Sp (5%) – Py (5%)
246.3 246.5 0.2 Brecciated massive Sp (50%) – Py (30%) – Gn (10%)
246.5 247.5 1 Disseminated to semi-massive Sp (5%) – Py (5%) – Gn (2.5%) – Cpy (2%)
250.1 251.75 1.65 Heavy disseminated to semi-massive Sp (10%) – Py (10%) – Gn (5%)
251.75 251.9 0.15 Massive Sp (60%) – Py (20%) – Gn (10%) – Cpy (5%)
Cautionary Statement: In relation to the disclosure of visual mineralisation, the Company cautions that visual
estimates of sulphide material abundance should never be considered a proxy or substitute for laboratory
analysis. Laboratory assay results are required to determine the widths and grade of the visible mineralisation
reported in preliminary geological logging. The Company will update the market when laboratory analytical
results become available.
Cpy = chalcopyrite; Po = pyrrhotite; Py = pyrite; Sp = sphalerite; Gn = galena; Qtz = quartz; Chl = chlorite; Cb =
Carbonate.
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Table 3: Reported assay intersections from BLRCDD001 and BLRCDD002
HOLE ID
From
(m)
To (m)
Width
(m)
Zn
(%)
Pb
(%)
Cu
(%)
Ag
(g/t)
Notes
BLRCDD001 82.0 85.0 3.0 0.14 0.11 0.01 0.58
83.5 85.0 1.5 0.24 0.17 0.02 0.62 Including
84.0 85.0 1.0 0.31 0.21 0.02 0.72 Including
BLRCDD001 105.5 106.0 0.5 – 0.14 0.29 2.41
BLRCDD002 124.0 125.0 1.0 0.12 – – 0.74
BLRCDD002 125.6 136.3 10.7 – – – 2.70
Contains 3.9m of core
loss
131.8 135.1 3.3 – – – 5.37
Including; contains 0.7m
of core loss
131.8 133.3 1.5 – – – 7.30 Including
134.0 135.1 1.1 – – – 6.16 Including
BLRCDD002 149.0 159.3 10.3 0.21 0.05 – 0.57
Contains 2.1m of core
loss
149.0 157.9 8.9 0.23 0.05 – 0.50
Including; contains 1.7m
of core loss
149.0 152.6 3.6 0.36 0.03 0.01 0.53 Including
152.0 152.6 0.6 1.12 0.17 0.07 2.35 Including
154.3 159.3 5.0 0.18 0.08 – 0.80
Including; contains 0.4m
of core loss
157.0 159.3 2.3 0.22 0.13 – 1.29
Including; contains 0.4m
of core loss
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157.0 157.9 0.9 0.40 0.25 – 1.68 Including
158.3 159.3 1.0 0.14 0.07 – 1.46 Including
BLRCDD002 164.0 168.3 4.3 – – 0.16 1.09
164.0 165.0 1.0 – – 0.37 1.08 Including
167.0 168.3 1.3 – – 0.16 2.22 Including
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Appendix A: Peak View Project JORC Code, 2012 Table
Section 1 Sampling Techniques and Data
Criteria JORC Code Explanation Commentary
Sampling
techniques
• Nature and quality of sampling (e.g. cut
channels, random chips, or specific specialised
industry standard measurement tools
appropriate to the minerals under investigation,
such as down hole gamma sondes, or handheld
XRF instruments, etc). These examples should
not be taken as limiting the broad meaning of
sampling.
• 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 (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.
• The drilling program at the Balerion Prospect used a combination of RC
drilling and HQ diamond drilling. RC drilling was used to collect 1m samples
from the cyclone and cone splitter. Outside visually mineralised zones, 2m
to 6m composite samples were collected using a PVC spear to spear each
1m sample bag and collect a 2kg to 4kg composite sample. Within visually
mineralised zones, individual 1m cyclone split samples were collected for
laboratory analysis. One 1m cyclone split sample was also collected every
30m to provide broad multi-element coverage for later geochemical
analysis. Diamond core sampling was restricted to visually mineralised
intersections, with 1m samples also collected every 30m to provide broad
multi-element coverage. Half HQ core was cut using a brick saw and
submitted for laboratory analysis. Every metre of RC material and diamond
core was analysed in the field using an Evident Vanta Core portable XRF
instrument to support geological logging and sample selection. Portable
XRF readings are preliminary and are not a substitute for laboratory assays.
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-
• Drilling comprised a combination of RC drilling and HQ diamond drilling.
RC drilling used a 125mm hammer and 140mm drill bit, with samples
collected through a cyclone and cone splitter. Diamond drilling was
completed using HQ core. Diamond core was oriented where successful
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Criteria JORC Code Explanation Commentary
sampling bit or other type, whether core is
oriented and if so, by what method, etc).
orientation marks were recorded by the drillers. The program was originally
designed as an RC drilling program; however, significant water inflows in
BLRCDD001 and BLRCDD002 resulted in a change to diamond drilling to
improve geological control and sample quality.
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 fine/coarse material.
• RC sample recovery was visually monitored by the supervising geologist
during drilling. Where excessive water was encountered, sample quality and
recovery were monitored, and the drilling method was changed to diamond
drilling to improve geological control and recovery. Diamond core recovery
was assessed by Exultant personnel during core processing. RQD
measurements were collected on diamond core by an Exultant field
assistant. No relationship between sample recovery and mineralisation has
been established at this stage.
• Core recovery and intervals of core loss were recorded during geological
and geotechnical logging. Where core loss occurred, no physical sample
was available for laboratory analysis from the lost interval.
• Core-loss intervals were retained within the reported downhole intersection
widths and were not excluded or compressed when calculating composite
intervals. For the calculation of length-weighted composite grades, core-loss
intervals were assigned zero grade for Zn, Pb, Cu and Ag.
• This treatment is considered conservative because it prevents core loss from
artificially reducing the reported composite width or increasing the calculated
composite grade. The zero grade assigned to core-loss intervals is a
reporting convention and should not be interpreted as an estimate of the in-
situ grade of the unrecovered material.
• Because the lost material was not available for analysis, its grade is
unknown and any relationship between grade and recovery within the core-
loss intervals cannot be directly assessed. The location and length of
material core-loss intervals have therefore been disclosed with the reported
intersections.
• Triple-tube equipment and shortened drill runs were used to try and obtain
maximum sample recovery
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Criteria JORC Code Explanation Commentary
• Assay results for BLRCDD001 and BLRCDD002 have been received. No
relationship between sample recovery and reported grade has been
identified from the returned assay data. Where core loss occurred, the
unrecovered material was unavailable for analysis and its grade cannot be
directly assessed. Laboratory assay results for BLRCDD004 remain
pending. Samples from BLRCDD005 have not yet been dispatched, while
BLRCDD006 remains in progress.
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.
• All RC samples and diamond core were geologically logged by an Exultant
geologist at 1m intervals. Logging recorded lithology, oxidation, alteration,
sulphides, veining and structure. Logging was recorded in Excel
spreadsheets in the field. Diamond core was marked up by Exultant
personnel, and orientation lines were recorded where successful core
orientations were obtained by the drillers. RQD was also collected on
diamond core. Logging is qualitative and quantitative where applicable and
is appropriate for early-stage Exploration Results reporting.
Subsampling
techniques and
sample
preparation
• If core, whether cut or sawn and whether
quarter, half or all core taken.
• If non-core, whether riffled, 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 insitu material collected,
including for instance results for field
duplicate/second-half sampling.
• RC samples were collected through a cyclone and cone splitter. Outside
visually mineralised zones, 2m to 6m composite samples were collected
using a PVC spear to collect 2kg to 4kg composite samples from the 1m
sample bags. Within visually mineralised zones, individual 1m cyclone split
samples were collected. One 1m cyclone split sample was also collected
every 30m for broad multi-element geochemical coverage. Diamond core
sampling was restricted to visually mineralised intervals, with 1m samples
also collected every 30m for multi-element coverage. Half HQ core was
submitted for laboratory analysis. Diamond core was cut using a brick saw
and submitted to ALS Orange. Sample preparation at ALS included LOG-
22, CRU-31, SPL-21, PUL-23 and PUL-23a. A blank, standard and
duplicate were inserted sequentially every 25 samples.
Level 8, 216 St Georges Terrace, Perth, Western Australia 6000
T: +61 (08) 9481 0389 E: info@exultantmining.com.au
ACN 684 147 484
Level 8, 216 St Georges Terrace, Perth, Western Australia 6000
T: +61 (08) 9481 0389 E: info@exultantmining.com.au
ACN 684 147 484
www.exultantmining.com.au
Criteria JORC Code Explanation Commentary
• Whether sample sizes are 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.
• 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.
• RC composite samples collected outside visually mineralised zones were
assayed for gold only using Au-AA23 at ALS Orange. Individual 1m
cyclone split samples collected from visually mineralised zones were
assayed for ME-MS61 and Au-AA23 at ALS Orange. Diamond core
samples from visually mineralised intervals were submitted to ALS Or
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