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SABRE RESOURCES LIMITED Capital/Financing Update 2025

Jan 21, 2025

65750_rns_2025-01-21_19fbbedd-dc0d-46fc-b415-ad3c8cb98139.pdf

Capital/Financing Update

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ASX:SBR ANNOUNCEMENT 22 JANUARY 2025

Imaging and Interpretation of Induced Polarisation Data Highlights New Uranium Targets at the Dingo Project in the NT

Sabre Resources Ltd has received imagery from final processing of new Gradient Array Induced Polarisation (GAIP) data which has highlighted a series of IP chargeability uranium targets on its Dingo Uranium Project . The Dingo Project is part of the Company’s extensive tenement package in the Ngalia Basin uranium province, 300km north-west of Alice Springs in the Northern Territory (see Figure 1).

The GAIP survey was carried out over a 4km strike-length corridor extending northeast of an excised retention lease held by Energy Metals Ltd (ASX:EME) which hosts the Camel Flat Inferred Mineral Resource of 211,300t @ 1,384ppm U3O8[1] (see Figures 1 and 2).

The imagery from the new GAIP survey has highlighted four distinct IP chargeability anomalies extending northeast of Camel Flat over an aggregate strike-length of approximately 3.5km (see Figure 2). The IP anomalies have been offset by potentially mineralised faults and represent targets for uranium bearing carbonaceous/pyritic units within the Mt Eclipse Sandstone .

The Mt Eclipse Sandstone is host to several high-grade uranium deposits close to Sabre’s tenements, including the Bigrlyi Mineral Resource of 6.32Mt @ 1,530ppm U3O8 and 960ppm V2O5[2] , as well as Camel Flat (see Figure 1). These deposits are roll-front type uranium deposits hosted by reduced carbonaceous/pyrite bearing horizons which can be detected as IP chargeability anomalies.

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Figure 1: Dingo Project showing existing uranium deposits, interpreted Mt Eclipse Sandstone and IP survey location

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2

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Figure 2: Dingo Project, Gradient Array IP image showing four new IP chargeability anomalies along strike from Camel flat uranium resource

3

The Company is targeting further roll-front/tabular sandstone-hosted deposits within the Mt Eclipse Sandstone. Previous drone magnetics and radiometric imagery indicates that the Mt Eclipse Sandstone is extensive on the Dingo Project tenements[3] (see Figure 1).

Previous shallow vacuum and selective RC and diamond drilling has only partially tested a 3km strikelength of the Mt Eclipse Sandstone, centred on the Camel Flat resource (Figure 3). High-grade uranium results of up to 1.3m @ 5,914ppm eU3O8[4 ] have been identified in historical drilling within the Company’s tenements immediately south of Camel Flat (see Figure 3 and Appendix 2 for drilling details). The new GAIP chargeability anomaly targets extending northeast of Camel flat have not been effectively tested by previous drilling.

The Company intends to test these new uranium targets, initially with aircore drilling. The program will be incorporated into the Mine Management Plan (MMP) which is in the advanced stages of approval with the NT Government (see Figure 2).

Approval of the MMP would allow selected aircore drilling traverses across the key GAIP chargeability anomalies, targeting high-grade uranium-vanadium mineralisation hosted by the favourable horizons in the Mt Eclipse Sandstone (see Figure 3).

The GAIP survey included 24 line-km of 200m x 50m stations on four 1km x 1km grids extending northeast of the Camel Flat retention lease (see Figure’s 1 and 2). Processing and imaging of the data produced chargeability (Figure 2) and conductivity / resistivity images. The layout of the GAIP survey is shown on Figure 3 below.

Details of the GAIP survey are included in JORC table 1 (Appendix 1).

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Figure 3: Layout of the Dingo Project GAIP Survey.

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4

About Sabre Resources Ltd

ASX-listed Sabre Resources Ltd (ASX: SBR) is focused on exploration of a prospective portfolio of gold, nickelcopper sulphide and lithium assets in Western Australia, and uranium-vanadium prospects in the Northern Territory.

In the Northern Territory, Sabre holds an 80% interest in the Ngalia Uranium-Vanadium Project , which comprises five granted exploration licences and two applications over an area of 1,100 sq.km in the highly prospective Ngalia Basin uranium province. Drone magnetics completed on the Company’s Dingo Project has defined multiple targets, including along strike from the Camel Flat Uranium [1 ] (excised, held by Energy Metals Ltd, ASX:EME). A Mine Management Plan (MMP), which is close to final approval by the NT Government, will allow drilling of targeted strike extensions of the identified uranium mineralisation, including testing several Gradient Array IP (GAIP) chargeability anomalies described in this release.

The Company has extensive tenement holdings in WA’s north-west Pilbara region, covering over 300 sq.km of geological structures considered highly prospective for the discovery of nickel-copper-cobalt sulphide, gold and lithium deposits. The Sherlock Bay tenements, including EL applications at Andover East and Andover Northeast[5] , lie within the same structural and stratigraphic corridor as the Andover Lithium Project[6] .

The Company’s most advanced project in the north-west Pilbara region is the Sherlock Bay (nickel-coppercobalt) Project – a significant, un-developed, nickel-copper-cobalt sulphide Mineral Resource comprising 24.6Mt @ 0.40% Ni, 0.09% Cu, 0.02% Co containing 99,200t Ni, 21,700t Cu, 5,400t Co (including Measured: 12.48Mt @ 0.38% Ni, 0.11% Cu, 0.025% Co; Indicated: 6.1Mt @ 0.59% Ni, 0.08% Cu, 0.022% Co and Inferred: 6.1Mt @ 0.27% Ni, 0.06% Cu, 0.01% Co)[7] . In 2023 diamond drilling intersected an extensive new sulphide zone[8] southwest of the resource, with Ni-Cu-Co sulphide as well as gold mineralisation[8] , associated with a strong EM conductor. The sulphide zone remains open to the southwest where new aircore drilling intersected copper mineralisation and confirmed potential for new sulphide resources within the 20km long Sholl Shear structural and intrusive corridor within the Company’s tenements at Sherlock Bay[9] .

Sabre also has an 80% interest in the Nepean South tenement (E15/1702) and five granted exploration licences at Cave Hill , covering a >100km strike length of interpreted extensions to the Nepean and Queen Victoria Rocks greenstone belts near Coolgardie in the Eastern Goldfields of WA. The Company previously reported anomalous lithium and gold in soil sampling across its extensive 700sq.km ground holdings in this highlyprospective area[10] . Results of further sampling are currently being reviewed before any further work is recommended.

Sabre’s 100% owned Ninghan Gold Project in WA’s southern Murchison district is located less than 20km along strike from the Mt Gibson gold mine[11] . Previous RAB and aircore drilling has defined two strongly anomalous zones of gold mineralisation. A PoW has been granted for possible drilling to follow up these anomalies.

References

1 Energy Metals Ltd, 13th February 2014, 626 Tonnes U3O8 Combined Maiden Resource Bigrlyi Satellite Deposits

2 Energy Metals Ltd, 1st August 2024, Resource Update - Bigrlyi Project.

3 Sabre Resources Ltd, 28th March 2024. Drone Mag Highlights Li-Pegmatite and Gold Targets at Andover East 4 Sabre Resources Ltd, 18th January 2024. High-Grade Uranium to 5,194ppm eU3O8 on Ngalia Project.

5 Sabre Resources Ltd, 14th May 2024. Magnetics Defines Li-Pegmatite Targets 5km NE of Andover.

6 Azure Minerals Ltd (ASX:AZS), 4h August 2023. 209m High-Grade Lithium Intersection at Andover.

7 Sabre Resources Ltd, 12th June 2018. Resource Estimate Update for the Sherlock Bay Ni-Cu-Co Deposit.

8 Sabre Resources Ltd, 2nd January 2024. Major New Nickel Trend and New Intersections at Sherlock.

9 Sabre Resources Ltd, 9th January 2024. Significant copper in Aircore Drilling at sherlock Bay

10 Sabre Resources Ltd, 9th April 2024. Large New Lithium & gold Anomalies Identified at Cave Hill.

11 Capricorn Metals Ltd announcement, 15th November 2024. MGGP Ore Reserve Grows to 2.59 Million Ounces.

This announcement has been authorised for release by the Board of Directors.

*ENDS***

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5

For background, please refer to the Company’s website or contact:

Jon Dugdale Michael Muhling or Tanya Newby Chief Executive Officer Joint Company Secretaries Sabre Resources Limited Sabre Resources Limited +61 (08) 9481 7833 +61 (08) 9481 7833

Cautionary Statement regarding Forward-Looking information

This document contains forward-looking statements concerning Sabre Resources Ltd. Forward-looking statements are not statements of historical fact and actual events and results may differ materially from those described in the forward-looking statements as a result of a variety of risks, uncertainties, and other factors. Forward-looking statements are inherently subject to business, economic, competitive, political, and social uncertainties, and contingencies. Many factors could cause the Company’s actual results to differ materially from those expressed or implied in any forward-looking information provided by the Company, or on behalf of, the Company. Such factors include, among other things, risks relating to additional funding requirements, metal prices, exploration, development and operating risks, competition, production risks, regulatory restrictions, including environmental regulation and liability and potential title disputes.

Forward looking statements in this document are based on the company’s beliefs, opinions and estimates of Sabre Resources Ltd as of the dates the forward-looking statements are made, and no obligation is assumed to update forward looking statements if these beliefs, opinions, and estimates should change or to reflect other future developments.

Competent Person Statements

The information in this report that relates to exploration results, metallurgy and mining reports and Mineral Resource Estimates has been reviewed, compiled, and fairly represented by Mr Jonathon Dugdale. Mr Dugdale is the Chief Executive Officer of Sabre Resources Ltd and a Fellow of the Australian Institute of Mining and Metallurgy (‘FAusIMM’). Mr Dugdale has sufficient experience, including over 36 years’ experience in exploration, resource evaluation, mine geology, development studies and finance, relevant to the style of mineralisation and type of deposits under consideration 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, Minerals Resources and Ore Reserves. Mr Dugdale consents to the inclusion in this report of the matters based on this information in the form and context in which it appears.

ASX Listing Rules Compliance

In preparing this announcement the Company has relied on the announcements previously made by the Company as listed under “References”. The Company confirms that it is not aware of any new information or data that materially affects those announcements previously made, or that would materially affect the Company from relying on those announcements for the purpose of this announcement.

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6

Appendix 1: JORC Code, 2012 Edition – Table 1

Section 1 Sampling Techniques and Data

Criteria JORC Code Explanation Commentary
Sampling
techniques

Nature and quality of sampling (e.g., cut
channels, random chips, or specific specialised
industry
standard
measurement
tools
appropriate to the minerals under investigation,
such as 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.

Details of the historical drilling are contained in the
release bySabre Resources Ltd, 18thJanuary 2024
titled “High-Grade Uranium to 5,194ppm eU3O8 on
Ngalia Project”._These details are repeated below.

Previous drilling results highlighted in this report by
AGIP Australia Pty Ltd were part of a 21 hole reverse
circulation (RC) drilling program carried out in 1979 by
Davies Drilling Aust (see_AGIP Australia Pty Ltd Annual

Report
for
EL1200,
9/2/1979
to
8/2/1980
on
geoscience.nt.gov.au/gemis).

Drillholes were generally vertical or dipping steeply to
the south and representatively tested the shallow
dipping Mt Eclipse Sandstone unit.

Targeted intervals were logged for natural gamma
radiation using a Gearhart-Owen Model 3200 logging
instrument. The total count gamma logging method
used here is a common method used to estimate
uranium grade where the radiation contribution from
thorium and potassium is small (as is the case for
sandstone-hosted
deposits
of
the
Bigrlyi-type
considered here). Background gamma rays from
thorium and potassium add the equivalent of a few
parts per million to the equivalent uranium values and
are relatively constant in each geological unit. Gamma
radiation is measured from a volume surrounding the
drill hole that has a radius of approximately 35cm. The
gamma probe therefore samples a much larger volume
than RC drill spoil or drill core samples recovered from
a drill hole of normal diameter and are therefore
representative. The results were reported aseU3O8
(radiometric equivalent triuranium octoxide).

Estimates of uranium concentrations based on gamma
ray measurements are based on the commonly
accepted initial assumption that the uranium is in
secular equilibrium with its daughter products
(radionuclides), which are the principal gamma ray
emitters along the U-series decay chain. If uranium is
in disequilibrium as a result of the redistribution
(depletion or enhancement) of uranium relative to its
daughter
radionuclides,
then
the
true
uranium
concentration in the holes logged using the gamma
probe will be higher or lower than those reported in the
announcement.

Collars were located on a local grid, which has been
converted to GDA94, MGA Zone 53 coordinates from
the NTGS STRIKE database.
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).

Previous drilling by AGIP Australia included vacuum
drilling, RC drilling and some diamond drillholes in
selected areas – as reported in the_AGIP Australia Pty_
Ltd Annual Report for EL1200, 9/2/1979 to 8/2/1980 (on
geoscience.nt.gov.au/gemis).
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.

AGIP Australia noted “considerable difficulties with
caving conditions in the drillholes”. Consequently,
some holes did not reach target depth and some
contamination/smearing would be expected.

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7

Criteria JORC Code Explanation Commentary

Whether a relationship exists between sample
recovery and grade and whether sample bias
may have occurred due to preferential loss/gain
of fine/coarse material.

No obvious relationships between sample recovery and
grade.
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 holes were/are logged in the field at the time of
drilling.

No core photographs were located from historical
holes.
Sub-sampling
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 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.

As noted above, the total count gamma logging method
used by AGIP Australia is a common method used to
estimate
uranium
grade
where
the
radiation
contribution from thorium and potassium is small (as
is the case for sandstone-hosted deposits of the
Bigrlyi-type considered here).

The gamma probe samples a much larger volume than
RC drill spoil or drill core samples recovered from a drill
hole
of
normal
diameter
and
are
therefore
representative.
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.

As noted above, targeted intervals were logged for
natural gamma radiation using a Gearhart-Owen Model
3200 logging instrument. The total count gamma
logging method used here is a common method used
to estimate uranium grade where the radiation
contribution from thorium and potassium is small (as
is the case for sandstone-hosted deposits of the
Bigrlyi-type considered here). Background gamma rays
from thorium and potassium add the equivalent of a
few parts per million to the equivalent uranium values
and are relatively constant in each geological unit.
Gamma radiation is measured from a volume
surrounding the drill hole that has a radius of
approximately 35cm. The gamma probe therefore
samples a much larger volume than RC drill spoil or drill
core samples recovered from a drill hole of normal
diameter and are therefore representative. The results
were reported aseU3O8(radiometric equivalent
triuranium octoxide).

Estimates of uranium concentrations based on gamma
ray measurements are based on the commonly
accepted initial assumption that the uranium is in
secular equilibrium with its daughter products
(radionuclides), which are the principal gamma ray
emitters along the U-series decay chain. If uranium is
in disequilibrium as a result of the redistribution
(depletion or enhancement) of uranium relative to its
daughter
radionuclides,
then
the
true
uranium
concentration in the holes logged using the gamma
probe will be higher or lower than those reported in the
announcement.

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8

Criteria JORC Code Explanation Commentary
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.

Previous reports by AGIP Australia have been reviewed
and verified by independent consultants.

OriginaleU3O8(radiometric equivalent triuranium
octoxide) reported by AGIP Australia have been located
and loaded into an electronic database.

No adjustment 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.

Specification of the grid system used.

Quality and adequacy of topographic control.

A local grid system was used to locate drillholes and
data has been converted to GDA94, MGA zone 53
coordinates.
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.

Previous drilling was not systematic and was based on
follow-up of previous ~200m spaced, north-south
oriented vacuum drilling traverses.

Drill data is not of sufficient spacing to define Mineral
Resources.

Intervals were gamma logged downhole and not
composited.
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.

Drillholes were generally vertical or dipping steeply to
the south and representatively tested the shallow
dipping Mt Eclipse Sandstone unit.
Sample security
The measures taken to ensure sample security.

No data on sample securityinprevious reports.
Audits or reviews
The results of any audits or reviews of sampling
techniques and data.

Previous reports by AGIP Australia have been reviewed
and verified by independent consultants.

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9

Section 2 Reporting of Exploration Results

Criteria JORC Code explanation Commentary
Mineral tenement
and land tenure
status

Type, reference name/number, location and
ownership including agreements or material
issues with third parties such as joint ventures,
partnerships, overriding royalties, native title
interests, historical sites, wilderness or national
park and environmental settings.
The security of the tenure held at the time of
reporting along with any known impediments to
obtaining a license to operate in the area.

Sabre Resources Ltd (Sabre) completed the purchase
of 80% of Chalco Resources Pty Ltd (Chalco), the owner
of the two granted exploration licences EL 32829 and
EL32864 as announced 7thFebruary 2022.

Both tenements were granted on the 23rdMarch 2022
for a period of 6 years to 21 March 2028 and are in good
standing.

Three further tenements, EL33642, EL33644 and
EL33646 were granted on 23 April 2024 for 6 year
terms. Two applications EL33643 and EL33645 are not
yet granted.

SBR retains a 80% beneficial interest in the project.
Exploration done
by other parties

Acknowledgment and appraisal of exploration
by other parties.

The most relevant previous exploration, including
drilling, was conducted by AGIP Australia Pty Ltd from
1978 to 1982. Previous drilling results by AGIP
Australia Pty Ltd were part of a 21 hole reverse
circulation (RC) drilling program carried out in 1979 by
Davies Drilling Aust (see_AGIP Australia Pty Ltd Annual_
Report
for
EL1200,
9/2/1979
to
8/2/1980
on
geoscience.nt.gov.au/gemis).

All previous exploration has been appraised by
consultant Discover Resource Services Pty Ltd, Dr A. L.
Dugdale and verified to be of a good standard.

Energy Metals Australia have carried out extensive
work programs in the region, including drilling of the
Camel Flat Mineral Resource which is in an excised
retention lease within E32829. This work was reported
in an ASX release by_Energy Metals Ltd, 13th February_
2014, “626 Tonnes U3O8 Combined Maiden Resource
Bigrlyi Satellite Deposits”.
Geology
Deposit type, geological setting, and style of
mineralisation.

The project is hosted within the highly prospective
Ngalia Basin in the southwestern Northern Territory,
approximately 300km NW of Alice Springs.

The Ngalia Basin units include the highly prospective
Mount Eclipse Sandstone, which is covered by flat lying
Palaeozoic sediments in the southern part of the
tenement, however drainage anomalies with elevated
uranium highlight the prospectivity of the underlying
units.

The Ngalia ‘Dingo’ tenement EL32829 is highly
prospective for tabular, sandstone - hosted, uranium–
vanadium (U-V) deposits of Carboniferous age. The
targeted deposits are fluvial, sandstone-hosted U-V
deposits which are analogous to the nearby Bigrlyi U-V
deposit.
Drill
hole
information
A summary of all information material to the
under-standing
of
the exploration
results
including
a
tabulation
of
the
following
information for all Material drill holes:
easting and northing of the drill hole collar
elevation or RL (Reduced Level – elevation
above sea level in metres) of the drill hole
collar
dip and azimuth of the hole
down hole length and interception depth

See Appendix 2, significant RC drilling intersections
from AGIP drilling located within E32829.

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10

Criteria JORC Code explanation Commentary
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.
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.

Length weighted average grades have been reported.

No high-grade cuts have been applied.

Metal equivalent values are not being 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 (e.g., down hole length, true width
_not known’). _

The majority of holes have been drilled at angles to
intersect
the
mineralisation
approximately
perpendicular to the orientation of the mineralised
trend.

Some steeper holes will have intersection length greater
than the 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.

The location of previously identified Mineral Resources
and the area of previous RC drilling results highlighted
in this release are shown on Figure 2.
Balanced
Reporting

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.
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.

Collars were located on a local grid, which has been
converted to GDA94, MGA Zone 53 coordinates and
drawn from the NTGS STRIKE database.

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11

Criteria JORC Code explanation Commentary
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.

A Gradient Array Induced Polarisation (GAIP) survey
was carried out on EL32829 by Fender Geophysics.

The GAIP survey measured conductivity/resistivity and
chargeability.

The Receiver type was a GDD Rx32 16-channel
Receiver.

The Transmitter type was a GDD TxII 5kVA Transmitter.

The survey comprised four gradient array IP grids of
1km length by 1km width.

The lines and electrodes were located by Garmin 64s
GPS unit – 3m accuracy.

The grids were located in a 4km long northeast
trending corridor along strike from the excised
tenement containing Energy Metals Ltd Camel Flat
uranium resource (see Figures 2 and 3).

The GAIP survey specifications were:
-
Survey type: Induced Polarisation.
-
Array Type: Gradient Array.
-
Domain and cycle: Time domain – 2s or 0.125Hz.
-
Line bearing 150°.
-
4, 1km spaced Tx (Transmitter) lines.
-
2,000m Tx Dipole length.
-
21, 200m spaced Rx (Receiver) lines (4 grids of 6,
overlap 1 line).
-
1,000m Rx line length.
-
50m Rx Dipole length.
-
Total 24 line km.

The receiver electrodes (non-polarising porous pot
electrodes with a copper sulphate solution) were
connected to the receiver via single-core receiver
cable.

The transmitting electrodes (aluminium plates) were
connected
to
the
transmitter
via
single-core
transmission wire. Heavy-duty alligator clips on the
plates ensured a consistent and safe contact.

The GAIP survey comprised a total of 441 data
acquisition stations.

Final data processing and imaging carried out by
Southern
Geoscience
(SGC).
SGC
generated
chargeability, conductivity, resistivity and “metal
factor” images (ratio of chargeability over resistivity).
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.

The Company plans to drill test, initially with aircore
drilling, the GAIP chargeability anomalies identified
within the extensions of the Mt Eclipse sandstone.

The program will be incorporated into a revised Mine
Management Plan (MMP) which is in the advanced
stages of approval with the NT Government.

Evaluation of other targets on the Dingo tenements will
continue.

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12

Appendix 2: Historical significant RC intersections on E32829:

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Company Years GDA94 MGA Zone 53 Dip Azimuth RL Hole # Type From To Interval eU3O8 ppm
East North
AGIP Australia, EL1200 1977 - 1982 118,618.9 7,519,287.9 90 N/A 640 CF55P RC 167.5 170.3 2.8 2841
incl. 168.5 169.8 1.3 5194
118,600.6 7,519,257.4 90 N/A 640 CF58P RC 124.7 125.5 0.8 1186
118,854.8 7,510,237.1 90 N/A 640 C89P RC 39.1 45.6 4.8 363
39.9 40.6 0.7 782
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