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CASPIN RESOURCES LIMITED Capital/Financing Update 2026

Mar 29, 2026

64694_rns_2026-03-29_234eb604-ff84-4a8a-af75-3ed200a2fc02.pdf

Capital/Financing Update

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30 March 2026

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New Targets Emerging at Bygoo Tin Project

HIGHLIGHTS

  • Exploration campaign accelerating following $6M Placement

  • RC Drill program at the Kelpie Deposit progressing well with 23 RC holes for approximately 4,000m completed to date, all assays pending

  • Now assisted by results of Induced Polarisation survey revealing potential mineralisation controls and multiple opportunities for future resource growth

  • IP emerging as a powerful tool to assist exploration across the Bygoo Project

  • First results from Ardlethan East, adjacent to the Ardlethan Mine, opens second active exploration front

  • Multiple tin in soil geochemical anomalies with more soil assays pending

  • Rock chip results up to 3.78% Sn with associated Cu, Pb, Zn, Ag, Bi & Sb

  • Preparing to immediately drill test

Caspin Resources Limited (Caspin or the Company) (ASX: CPN ) is pleased to provide an update on exploration activities at the Bygoo Tin Project in New South Wales. The Company is making rapid progress at the Kelpie Tin Deposit where drilling has been underway for several weeks aiming to grow the Kelpie resource. In parallel, the Company has developing targets at the Ardlethan East Prospect ready for reconnaissance-style drilling.

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Sunrise over the Kelpie Deposit, Bygoo Tin Project, NSW.
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Induced Polarisation Survey Provides New Insights to Mineralisation

The Company completed an Induced Polarisation (IP) survey early in February 2026, to assist subsurface mapping and drill targeting of the prospective granite contact. IP measures chargeability, which typically relates to the presence of disseminated sulphides, and resistivity, commonly a response of silica alteration. Both responses have the potential to be associated with tin greisen-style mineralisation systems.

The survey has clearly highlighted NE-SW trending and NNE trending chargeability and resistivity anomalies (Figure 1). These anomalies coincide with mineralisation at the historical Dumbrells workings as well at the ‘Stewarts Zone’ to the northwest. Historical workings in the Kelpie area also tend to be aligned along similar NE and NNE trends, leading to the conclusion that these IP anomalies are likely to be mapping fault structures which have acted as fluid pathways for mineralisation. The strongest mineralisation is anticipated at the intersection of these NE-SW and NNE trending faults and the Ardlethan Granite contact (Figure 1), which is likely to be a structural boundary within the regionally extensive, NNW-trending Cobar-Wagga Shear. Such intersections of major fault systems provide a mechanism for concentrating fluid flow and subsequent mineralisation.

RC drilling is progressing steadily, with 23 holes for approximately 4,000m drilled to date. All assays remain pending. The IP survey has allowed the Company to refine the drilling program to ensure that drilling is oriented approximately perpendicular to those structures imaged by the IP, rather than targeting the granite contact alone, with the objective extending mineralisation along these trends (Figure 2 & Table 1, Appendix A). It should be noted that mineralisation is also observed beyond these IP anomalies, possibly in unrecognised subsidiary structures, indicating additional opportunities to grow the resource.

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Figure 1. Kelpie Deposit IP chargeability and resistivity results and interpretation.

The IP survey was co-funded by the NSW Government Critical Minerals and High-Tech Metals Exploration Program, providing a cheap, low-risk opportunity to trial a potentially critical technology to assist exploration. The results from the survey have validated this approach and because mineralisation (eg historical workings, anomalous rock chips) is also recognised outside the area of the IP survey, the company now intends to extend

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this survey significantly. In particular, the area to the north of the current Kelpie resource is considered highly prospective, with significant anomalism and historical workings recognised at the “Area 1” target.

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Figure 2. Current Kelpie Deposit RC drilling over IP chargeability anomaly with resource blocks projected to surface.

New Targets Emerging at Ardlethan East

First soil geochemistry results have now been received from the Ardlethan East area and have presented targets for immediate drill testing. Approximately 350 samples have been returned with a further 800 samples still pending. Further areas to the south of Ardlethan are scheduled for sampling in the coming weeks.

The Ardlethan East area is highly prospective, located within a short distance of the Ardlethan Mine which produced over 31,000t of tin in concentrate until 1986 from both open pit and underground mines. Significant alluvial production also occurred from the Yithan Lead which cuts through the prospect area. Key structures that facilitate mineralisation at Ardlethan continue into Caspin’s tenure at Ardlethan East. The area is

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prospective for both breccia-style (Ardlethan-style) and greisen-style (Kelpie-style) mineralisation, which may be potentially subcropping, or concealed under shallow lithological cover. An illustration of these mineralisation models is shown in Figure 3.

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Figure 3. Schematic diagram of mineralisation styles within the Bygoo Project

Fundamental to all styles of mineralisation are major fault structures, in this case, a splay of the Cobar-Wagga shear, which appears to be key to mineralisation at Ardlethan as well as the Yithan Lead, and the interplay with NE-SW cross-cutting faults. The faults are recognised in Caspin’s high-resolution aeromagnetic survey and are often associated with surficial mineralisation and historical prospecting/mining.

The results received thus far show multiple areas of tin anomalism, often associated with fault structures, supported by pathfinder elements common in hydrothermal tin mineralisation, including Sb, Cu, Pb, Zn, Ag, In and Bi. Some of the anomalism is on the edge of the survey, which will be delineated with further sampling. The strongest area of anomalism is approximately only 500m from the edge of the Ardlethan pit (Figure 4).

Further support is provided by rock chip sampling, with numerous outcrops returning significant values of tin (>250ppm) and accessory metals (Table 2, Appendix A). The highest rock chip grades of up to 3.78% Sn have been returned from a historical mining area known as Ford’s Gossan, where the Company is still anticipating the return of soil geochemistry. Other samples have returned values of 2.01% Sn, 1.77% Sn & 1.16% Sn .

Ardlethan-style breccia pipes can have relatively small horizontal footprints, in the order of several hundred meters in diameter, but can be vertically extensive. Within the pipe, Sn mineralisation represents a relatively small volume of the total pipe-like complex. Alteration halos with mixed metal signatures of Cu, Pb, Zn, Sb & As may be far broader. Therefore, small anomalies on the scale of the geochemistry program may be significant, particularly if there is associated metal anomalism and/or a conducive structural setting.

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Figure 4. Ardlethan East tin in soil geochemistry, highlighting new anomalies (magenta contours) and rock chip results.

The Company is mobilising the RC rig to drill test some of these anomalies immediately.

This early-stage exploration at Ardlethan East is a key part of the Company’s strategy to recognise the full potential of the Bygoo Project with over 20km of prospective strike, which the Company believes can host multiple, large, high-grade open pit deposits. With the effectiveness of soil geochemistry demonstrated, combined with magnetics, gravity and increasingly with IP, the Company is now looking to expand coverage across the Bygoo Project area.

This announcement is authorised for release by the Board of Caspin Resources Limited.

-ENDS-

For further details, please contact:

Greg Miles Managing Director [email protected] Tel: +61 8 6373 2000

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APPENDIX A

TABLE 1: Drill hole collar locations (GDA2020 MGA Zone 55)

Hole ID Easting Northing RL (m) Dip Azimuth EOH (m)
BRC017 484442 6208359 251 -60 180 192
BRC018 484526 6208358 249 -70 225 180
BRC019 484762 6208154 245 -70 225 210
BRC020 484715 6208174 246 -70 225 150
BRC021 484766 6207978 247 -65 300 168
BRC022 484826 6208002 246 -65 300 198
BRC023 484746 6207957 248 -70 300 174
BRC024 484681 6207800 249 -60 225 120
BRC025 484423 6208375 251 -70 180 180
BRC026 484404 6208364 252 -65 180 168
BRC027 484365 6208368 252 -60 180 150
BRC028 484353 6208385 252 -57 140 204
BRC029 484573 6208325 247 -60 245 162
BRC030 484460 6208248 253 -62 310 198
BRC031 484576 6208343 247 -60 314 210
BRC032 484598 6208374 246 -60 310 234
BRC033 484555 6208360 248 -60 310 180
BRC034 484537 6208382 248 -60 310 192
BRC035 484477 6208235 252 -60 310 198
BRC036 484442 6208212 254 -60 310 169
BRC037 484447 6208089 254 -60 310 180
BRC038 484525 6208179 250 -60 310 180

TABLE 2: Surface Rock Chip Sampling – Selected Significant results (>250ppm Sn)

Sample ID Easting Northing RL Sn Ag Bi Cu Pb Sb Zn
MGA Z55 MGA Z55 (m) (ppm) (ppm) (ppm) (ppm) (ppm) (ppm) (ppm)
BRK0022 6200491 488684 241 2671 BD 615 737 3547 606 332
BRK0023 6200479 488674 242 20139 BD 1005 1100 42065 6725 638
BRK0024 6200474 488681 242 17662 14 1191 757 14327 2266 874
BRK0033 6200622 488866 240 37793 80 396 1107 191400
808
373
BRK0034 6200612 488888 241 11609 44 1228 122 20223 2575 75
BRK0036 6200314 486798 261 286 BD 22.8 15 619 BD 52
BRK0037 6200311 486801 261 399 BD 188 26 563 BD 160
BRK0041 6199327 486705 243 901 BD 44 36 78 BD 62
BRK0045 6199155 486318 251 309 BD 16.9 BD BD BD 35
BRK0115 6200550 487011 265 1335 BD 7.7 70 115 3.1 50
BRK0117 6200684 487088 256 4570 BD 2 140 141.5 39.8 580
BRK0140 6199118 486238 252 308 BD 9.5 60 48.6 1.4 40
BRK0141 6199150 486255 255 375 BD 3.9 20 150.5 1.5 80
BRK0143 6199225 486251 260 291 BD 31.6 BD 77.3 1.9 40
BRK0146 6199418 486369 252 516 BD 17.2 BD 90.6 2.2 30
BRK0162 6200464 486533 267 273 BD 5.8 BD 326 9.8 50

BD = Below detection

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Competent Persons Statement

The information in this report that relates to Exploration Results is based on information compiled or reviewed by Mr Greg Miles, a Competent Person who is an employee of the company. Mr Miles is a Member of the Australian Institute of Geoscientists and has sufficient experience of relevance to the styles of mineralisation and the types of deposits under consideration, and to the activities undertaken, to qualify as a Competent Person as defined in the 2012 Edition of the Joint Ore Reserves Committee (JORC) Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves. Mr Miles consents to the inclusion in this report of the matters based on his information in the form and context in which it appears.

The information in this report that relates to Estimation and Reporting of Mineral Resources is based on information compiled or reviewed by Mr Michael Job, who is a Fellow of the Australasian Institute of Mining and Metallurgy. Mr Job is an independent consultant employed by Cube Consulting and has sufficient experience of relevance to the styles of mineralisation and the types of deposits under consideration, and to the activities undertaken, to qualify as a Competent Person as defined in the 2012 Edition of the Joint Ore Reserves Committee (JORC) Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves. Mr Job consents to the inclusion in this report of the matters based on his information in the form and context in which it appears.

The Company confirms that it is not aware of any new information or data that materially affects the Exploration Results and Mineral Resource information included in this report from previous Company announcements announced to the ASX 23 September 2024, 13 November 2024, 4 December 2024, 20 March 2025, 27 March 2025, 3 April 2025, 19 June 2025, 1 September 2025, 23 September 2025, 19 January 2026 and 4 February 2026.

ABOUT CASPIN:

Caspin Resources Limited (ASX Code: CPN ) is a mineral exploration company based in Perth, Western Australia, with expertise in early-stage exploration and development. The Company currently has four Australian projects offering a diverse mix of commodities and excellent opportunity to add value through exploration and discovery.

  • The Company’s flagship project is the Bygoo Project in New South Wales, an advanced, high-grade tin project located in a prolific Wagga tin belt. The project surrounds the Ardlethan Mine, one of Australia’s largest producing tin mines on mainland Australia before it closed in 1986. The Company recently announced its maiden Inferred Resource Estimate of 3.94mt @ 0.5% Sn for 19,300t of contained tin.

  • The Company has recently acquired an option to earn 80% of the Weethalle Project in NSW, a

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  • short distance north of the Bygoo Project. The Project is prospective for large-scale intrusive related gold mineralisation, with a structural setting similar to the Hemi deposit in Western Australia. Compelling geophysical and geochemical anomalies have never been drill tested.

  • The Yarawindah Brook and Mount Squires Projects are new frontier projects located in WA and prospective for Ni-Cu-PGE sulphide mineralisation. Both projects are located in frontier magmatic sulphide provinces with large scale deposits nearby. The Company believes these projects have long-term strategic value and is pursuing avenues to advance alongside its NSW assets.

These projects are strategically positioned in Australia’s premier mineral districts, providing excellent exposure to new critical and technology mineral markets.

FOLLOW US:

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ANNEXURE 1:

The following Tables are provided to ensure compliance with the JORC Code (2012) edition requirements for the reporting of the Exploration Results at the Weethalle Gold Project.

SECTION 1: Sampling Techniques and Data (Criteria in this section apply to all succeeding sections)

CRITERIA JORC CODE EXPLANATION COMMENTARY
Sampling
techniques
Nature and quality of sampling (eg 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.
Soil sampling:
Surface soil samples were collected on east-west
orientated lines at a default 100m spacing with
alternating lines offset by 50m. Samples were
collected by digging a 30x30x20cm pit, cleaning the
base of the pit out before homogenising the sample.
The sample was immediately sieved to 80# or 177
microns, approximately 400g was collected.
Rock Chip sampling:
Samples of outcrop were collected via a geopick at
irregular intervals where encouraging outcropping
geology was encountered.
Include reference to measures taken to ensure sample
representivity and the appropriate calibration of any
measurement tools or systems used.
Soil & Rock Chip sampling:
Sampling has been carried out using standard
protocols and QAQC procedures as per industry best
practice. Soil and rock chip sampling locations were
surveyed by handheld GPS units which have an
accuracy of ±5m.
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 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 (eg submarine nodules) may warrant disclosure
of detailed information.
Soil sampling:
Samples were transported to Brisbane ALS for
pulverising (PUL-31L) and 4-Acid digest analysis via
the ME-MS61L method
Rock Chip sampling:
Samples detailed in this report were transported to
ALS Brisbane and pulverised to <75µm (PUL-23) prior
to ME-MS89L ICP-MS and ICP-AES Fusion Multi
Element and Au-ICP-21 Au analysis.
Drilling
techniques
Drill type (e.g. core, reverse circulation, open-hole
hammer, rotary air blast, auger, Bangka, sonic etc)
and details (e.g. core diameter, triple or standard tube,
depth of diamond tails, face-sampling bit or other type,
whether core is oriented and if so, by what method,
etc).
Not applicable as no drill results are reported in this
announcement.
Drill sample
recovery
Method of recording and assessing core and chip
sample recoveries and results assessed.
Not applicable as drill results are not discussed in this
announcement.
Measures taken to maximise sample recovery and
ensure representative nature of the samples.
Not applicable as drill results are not discussed in this
announcement.
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.
Not applicable as drill results are not discussed in this
announcement.
Logging Whether core and chip samples have been geologically
and geotechnically logged to a level of detail to
support appropriate Mineral Resource estimation,
All rock chip samples were lithologically logged.
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CRITERIA JORC CODE EXPLANATION COMMENTARY
mining studies and metallurgical studies.
Whether logging is qualitative or quantitative in
nature. Core (or costean, channel, etc) photography.
Not applicable as no core was collected.
The total length and percentage of the relevant
intersections logged.
Not applicable as drill results are not discussed in this
announcement.
Sub-sampling
techniques
and sample
preparation
If core, whether cut or sawn and whether quarter, half
or all core taken.
Not applicable as no core was collected.
If non-core, whether riffled, tube sampled, rotary split,
etc and whether sampled wet or dry.
Not applicable as drill results are not discussed in this
announcement.
For all sample types, the nature, quality and
appropriateness of the sample preparation technique.
Preparation techniques are laboratory standard and
considered appropriate for the accuracy of assaying
methods.
Quality control procedures adopted for all sub-
sampling stages to maximise representivity of
samples.
Caspin QC procedures involve the use of duplicates
and certified reference material (CRM) as assay
standards. The insertion rate of these will average
1:25 in surface geochemical 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.
The sampling of duplicated composite samples was
completed as per standard Caspin QC procedures.
Whether sample sizes are appropriate to the grain size
of the material being sampled.
Sample sizes are considered appropriate for the
methods of sampling and stage of exploration.
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.
Soil sampling:
Samples were transported to Brisbane ALS for
pulverising (PUL-31L) and 4-Acid digest analysis via
the ME-MS61L method
Rock Chip sampling:
Samples detailed in this report were transported to
ALS Brisbane and pulverised to <75µm (PUL-23) prior
to ME-MS89L ICP-MS and ICP-AES Fusion Multi
Element and Au-ICP-21 Au analysis.
Sampling, preparation and analytical methods are
considered appropriate for this stage of exploration.
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.
See Annexure 2 at the end of this report for specifics
of IP survey methods.
Nature of quality control procedures adopted (eg
standards, blanks, duplicates, external laboratory
checks) and whether acceptable levels of accuracy
(ie lack of bias) and precision have been established.
Laboratory QAQC involves the use of internal lab
standards using certified reference material, blanks,
splits and replicates as part of the in-house
procedures.
Repeat or duplicate analysis for samples did not
highlight any issues.
Verification of
sampling and
The verification of significant intersections by either
independent or alternative company personnel.
Results have been verified by multiple Caspin
geologists with further reviews and interpretations

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CRITERIA JORC CODE EXPLANATION COMMENTARY
assaying continuing.
The use of twinned holes. Not applicable as drill results are not discussed in this
announcement.
Documentation
of
primary
data,
data
entry
procedures, data verification, data storage (physical
and electronic) protocols.
Sample locations, sample data and geological
information for drill holes were recorded in field
logging computers. Data was then sent to the
company database managed by MRG Data.
Discuss any adjustment to assay data. No adjustments were made to assay data.
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.
Soil and rock chip sample locations were recorded
using a handheld Garmin GPS which typically have a
±5 metre accuracy. RL Data from handheld GPS is
typically unreliable and was instead sourced from GIS
software utilising imported DTM elevation layers.
Specification of the grid system used. The grid system for the Bygoo Project is GDA2020
MGA Zone 55.
Quality and adequacy of topographic control. Topographic data was obtained from public
download of the relevant 1:250,000 scale map sheets.
The area exhibits subdued, low relief. Topographic
representation is considered sufficiently controlled.
Data spacing and
distribution
Data spacing for reporting of Exploration Results. Rock Chips sample locations are spaced irregularly.
Surface soil samples were collected on east-west
orientated lines at a default 100m spacing with
alternating lines offset by 50m.
Whether the data spacing and distribution is sufficient
to establish the degree of geological and grade
continuity appr_opriate_for the Mineral Resource and
Ore
Reserve
estimation
procedure(s)
and
classifications applied.
Not applicable as no Mineral Resource and Ore
Reserve reported.
Whether sample compositing has been applied. No sample compositing has occurred.
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.
Soil sampling is conducted on a pre-defined grid
pattern and introduces no bias to geological
structures.
Rock chip samples are collected ad-hoc at outcrop
exposures and may unintentionally focus on
structures which focus alteration and mineralisation.
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.
Not applicable as no Mineral Resource and Ore
Reserve reported.
Sample security The measures taken to ensure sample security. Samples were collected on-site by Caspin staff and
transported via third-party freight contractors to
Orange and Brisbane.
Audits or reviews The results of any audits or reviews of sampling
techniques and data.
Company geologists continue to review the data, no
external reviews have been completed.

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Section 2: Reporting of Exploration Results (Criteria listed in the preceding section also apply to this section)

Section 2: Reporting of Exploration Results(Criteria listed in the preceding section also apply to this section)
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 Bygoo Tin project comprises of three
Exploration Titles, EL8260, EL9288 and EL9234. The
Titles cover a combined area of 1,183km² and are
now 100% held by Caspin Resources.
The Ardlethan Tin Mine is excised from EL8260 and is
not held by Caspin Resources.
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.
All Titles are currently live and in good standing. No
Mining Agreement has been negotiated.
Exploration done
by other parties
Acknowledgment and appraisal of exploration by
other parties.
Prospecting and small-scale artisanal mining
occurred across the Bygoo Project following the
discovery of the Ardlethan tin mine in 1912.
RAB drilling testing for extensions of the Ardlethan
mine was conducted from 1961 until 1962, followed
by sporadic programs of further RAB and
percussion drilling between 1977 and 1982 testing
for blind alluvial occurrences and extensions of
small-scale workings including the Bald Hill,
Taylors, Killarney, Big Bygoo and Bygoo North
occurrences.
Drilling completed by Thomson Resources from
2015 to 2022 represents the first period of
sustained modern exploration.
Geology
Deposit type, geological setting and style of
mineralisation.
The Bygoo Project is located within the Lachlan
Fold Belt of NSW and part of the ‘Wagga Tin Belt’, a
320 x 80km belt of late Silurian granitoids
extending from the towns of Wagga Wagga to
Condobolin.
Granites
carry
a
background
enrichment of 10ppm Sn and host the greatest
known endowment of tin within the Australian
mainland.
Locally, the Ardlethan granite intrudes Ordovician
sediments with known mineral occurrences
concentrated on the eastern margins of this
contact.
The best understood mineralisation models on the
project are a breccia-pipe porphyry at the
Ardlethan Mine, and greisen-style at Bygoo North.
Extensive alluvial mineralisation has also been
found across the project.
Cassiterite hosts tin mineralisation. Trace copper,
lead, zinc, bismuth, antimony and silver are noted
accessory metals.
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
Drill hole collar information and significant rock chip
results are published in Table 1 of this report.
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CRITERIA JORC CODE EXPLANATION
COMMENTARY

down hole length and interception depth

hole length.
If the exclusion of this information is justified on the
basis that the information is not Material and this
exclusion does not detract from the understanding of
the report, the Competent Person should clearly
explain why this is the case.
Only significant Rock Chip results are reported, with
a >250ppm Sn cutoff applied.
Results of individual Soil Samples are not considered
material in nature.
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.
Rock Chip samples above 250ppm Sn are reported.
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.
No data aggregation has been applied to Rock Chip
results.
The assumptions used for any reporting of metal
equivalent values should be clearly stated.
No metal equivalent values are reported.
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’).
Drill collars were spaced irregularly as first-pass tests
of interpreted geological structures and geophysical
anomalies. The exact orientation of structures and
their true widths is unknown.
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.
Refer to Figures in body of text.
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.
Only significant results have been reported.
Other substantive
exploration data
Other exploration data, if meaningful and material,
should be reported including (but not limited to):
geological observations; geophysical survey results;
geochemical survey results; bulk samples – size and
method of treatment; metallurgical test results; bulk
density, groundwater, geotechnical and
rock
characteristics;
potential
deleterious
or
contaminating substances.
All currently relevant exploration data is detailed in
text, Figures, Table 1 and Annexure 1.
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.
Caspin’s upcoming work program includes:

Further RC drilling

Further IP Surveys

Further soil sampling

Ground Gravity surveys

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ANNEXURE 2:

CRITERIA
JORC CODE EXPLANATION
COMMENTARY
Quality of assay
data and
laboratory tests
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.
IP Survey Technical Specifications:
Dipole-Dipole
Contractor: Merlin Geophysical Solutions
Collection Mode: Inline Static shoot through Dipole-
Dipole – full time serries
Transmitter: (Tx) Dipole 100m
Receiver (Rx) Dipole 50m
Maximum “n” Level: 16
Transmitter Station Interval: 50m
Line Direction: local Orientated grid
Base frequency: 0.125 Hertz
Duty Cycle: 50%
Receiver: SmarTEM 16 channels
IP Chargeability Integration: 590msec to 1540msec
Transmitter: Phoenix TXU-30
IP Data Processing Software: TQIPdb Ver. 5.8.53
IP Data Modelling Software: Zonge 2D smooth
model inversion Ver. 4.40
Gradient Array
Contractor: Merlin Geophysical Solutions
Collection Mode: Multi-channel (4) Gradient Array –
full time serries
Transmitter: (Tx) Dipole 2km
Receiver (Rx) Dipole 25m
Maximum simultaneous Dipoles: 4
Receiver Station Interval: 25m
Line Direction: local Orientated grid
Line spacing: 50m separation
Base frequency: 0.125 Hertz
Duty Cycle: 50%
Receiver: SmarTEM 16 channels – only 4 used
IP Chargeability Integration: 590msec to 1540msec
Transmitter: Phoenix TXU-30
IP Data Processing Software: TQIPdb Ver. 5.8.53
IP Data Conceptual Modelling Software: MG3Dinv
Ver. 2.12

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