Completion of Reynolds & Reitenbach Inaugural Field Programs
Released
Released
Announcement PDF
ASX Announcement
Released 3 October 2025
Infini Resources Limited ABN 77 656 098 583 www.infiniresources.com.au
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Uraninite Showing at Reitenbach Lake and
Completion of Inaugural Field Programs
Uraninite showing at Reitenbach Lake, a newly identified outcrop where visible
uraninite1
has been identified at surface, with scintillometer readings up to 67,540
cps2
.
At Reynolds Lake, systematic fieldwork confirmed widespread radiometric
anomalism with 59 radioactive occurrences above 1,000 cps2
, up to a maximum of
9,700 cps2
, in combination with observed hydrothermal alteration.
Multiple >10 km long conductors coincident with radiometric anomalies and
uranium-in-lake sediments identified along key structural corridors, indicating
potential for shallow unconformity-style uranium mineralisation.
The 100%-owned Reynolds Lake Project lies on the eastern outboard margin of the
Athabasca Basin, within a geological setting highly prospective for unconformity
type uranium deposits.
Over 900 soil and rock samples collected across both projects with assay results
due in Q4 CY2025.
Results from field programs at Reynolds and Reitenbach complementary to Infini’s
aggressive uranium exploration strategy, with Phase 2 drilling underway at the
highly prospective Portland Creek Uranium Project.
Geochemical results to be integrated with geophysical and structural datasets to
define drill targets.
Infini Resources Limited (ASX:I88) (“Infini” or the “Company”) is pleased to advise that the 2025
field programs at its Reynolds Lake and Reitenbach Lake uranium projects, on the outboard edge of the
Athabasca Basin margin, in Saskatchewan, Canada, have now been successfully completed. Both
programs were designed around priority target areas generated from the property-wide 2025 EM survey
and interpretation of historical geological datasets.
A combined 921 samples (148 rock and 773 soil) were collected. All samples have been dispatched to
ALS Global Laboratories for comprehensive geochemical analysis. Results are expected in Q4 2025,
providing critical data for refining targets for a potential drill program in 2026.
1
Cautionary Statement: In relation to the disclosure of visual mineralisation, the Company cautions that visual estimates of mineral
abundance should never be considered a proxy or substitute for laboratory analysis where concentrates or grades are the factor of
principal exonymic interest. Visual estimates also potentially provide no information regarding impurities or deleterious physical
properties relevant to valuations. The presence of uranium minerals, including uraninite, is based on field observations and
scintillometer readings only. These indicators are preliminary in nature and should not be considered a substitute for laboratory
analysis. The identification of uranium mineralisation remains conceptual until confirmed through geochemical assay and
mineralogical reporting from accredited laboratories.
2
Cautionary Statement: In relation to handheld scintillometer readings, the Company cautions that measurements of radioactivity
from scintillometer readings are preliminary in nature and should not be considered a proxy or substitute for quantitative analysis of
a laboratory assay result. While scintillometers confirm the presence of radioactivity, it does not accurately determine elemental
uranium concentrations and can also be influenced by the presence of thorium and potassium.
Uraninite Showing at Reitenbach Lake and Completion of Inaugural Field
Programs
Infini Resources Limited ABN 77 656 098 583 www.infiniresources.com.au
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Infini’s Chief Executive Officer, Rohan Bone, said: "The identification of the uraninite1 showing at
Reitenbach Lake is a significant breakthrough and underscores the quality of our Athabasca Basin
portfolio. Combined with the widespread anomalism we have confirmed at Reynolds Lake, these results
strongly validate our exploration model. We are now looking forward to receiving assays in Q4, which will
allow us to define and prioritise high-value drill targets as we position for a potential drilling campaign in
2026.”
Figure 1: Identification of visible disseminated uraninite1
showing at Reitenbach Lake (sample site
25RNBP083, 623459E, 6423998N, UTM Zone 13), with scintillometer readings up to 67,540 cps2
. (<= 10%
visual estimate of uraninite).
Uraninite Showing at Reitenbach Lake and Completion of Inaugural Field
Programs
Infini Resources Limited ABN 77 656 098 583 www.infiniresources.com.au
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Cautionary Statement: In relation to the disclosure of visual mineralisation, the Company cautions that
visual estimates of mineral abundance should never be considered a proxy or substitute for laboratory
analysis where concentrates or grades are the factor of principal exonymic interest. Visual estimates also
potentially provide no information regarding impurities or deleterious physical properties relevant to
valuations The presence of uranium minerals, including uraninite, is based on field observations and
scintillometer readings only. These indicators are preliminary in nature and should not be considered a
substitute for laboratory analysis. The identification of uranium mineralisation remains conceptual until
confirmed through geochemical assay and mineralogical reporting from accredited laboratories.
Reynolds Lake Program
The 100%-owned Reynolds Lake Project lies on the eastern outboard margin of the Athabasca Basin,
within a geological setting highly prospective for unconformity-type uranium deposits. Infini’s 2025 field
campaign followed extensive target generation work, including airborne TDEM surveys, magnetic
surveys, and historical geochemistry, which collectively identified 14 high-priority target areas.
The field program focused on priority targets where EM conductors coincide with radiometric anomalies,
uranium-in-lake sediments, and regional structures, including the Needle Falls Shear Zone and kilometre
scale cross-cutting north-south faults.
Key outcomes from the program include the collection of 604 soil samples collected down ice on 200m
lines and 100m stations, and 115 lithogeochemical rock samples. A total of 79 radioactive occurrences
were recorded above 1,000 cps2 on handheld scintillometer, with peak readings of 9,700 cps2. Notable
results include Sample K668350, a quartz-rich float boulder with smoky quartz alteration recording 9,700
cps2, and Sample K668349, a float boulder recording 7,000 cps2. Numerous additional samples recorded
between 2,000–5,000 cps2, highlighting widespread radiometric anomalism across the project.
These results suggest uranium mineralisation spatially associated with EM conductors and shear zones,
consistent with the exploration model for structurally hosted uranium systems. The presence of clay,
hematite, chlorite, and silica alteration further supports the potential for hydrothermal fluid pathways
analogous to other major Athabasca Basin deposits.
Cautionary Statement: In relation to handheld scintillometer readings, the Company cautions that
measurements of radioactivity from scintillometer readings are preliminary in nature and should not be
considered a proxy or substitute for quantitative analysis of a laboratory assay result. While scintillometers
confirm the presence of radioactivity, it does not accurately determine elemental uranium concentrations
and can also be influenced by the presence of thorium and potassium.
Uraninite Showing at Reitenbach Lake and Completion of Inaugural Field
Programs
Infini Resources Limited ABN 77 656 098 583 www.infiniresources.com.au
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Figure 2: Results from the field program at Reynolds Lake highlighting coincidence of scintillometer
readings1
heatmap with EM anomalies, RAD anomalies and key interpreted geological structures.
Reitenbach Lake Program
At the contiguous Reitenbach Lake Project, the 2025 field program delivered a breakthrough result with
the identification of a visible uraninite1 showing (Figure 1), a previously undocumented uranium-bearing
outcrop. Systematic prospecting and structural mapping revealed fracture-controlled uraninite associated
with alteration zones, confirming the project’s potential.
At the uraninite1 showing, Sample K668386 (sample site 25RNBP083, 623459E, 6423998N, UTM Zone
13) returned a scintillometer reading of 67,540 cps2, with sub-metallic uraninite1 observed lining a fracture.
Sample K665300, collected from a nearby mafic–felsic gneiss, returned 8,090 cps2, hosted in a
subvertical structure containing hematite and chlorite alteration.
The identification of the visible uraninite1 showing suggests primary uranium mineralisation at surface
within the Reitenbach property. Mineralisation is clearly fracture-controlled and structurally aligned,
providing direct vectors for future drill targeting. This represents a significant breakthrough that
establishes Reitenbach Lake as a high-priority project for follow-up exploration and drilling.
Uraninite Showing at Reitenbach Lake and Completion of Inaugural Field
Programs
Infini Resources Limited ABN 77 656 098 583 www.infiniresources.com.au
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Figure 3: Results from the field program at Reitenbach Lake highlighting the uraninite1
showing in
combination with the coincidence of scintillometer readings2
heatmap with EM anomalies, RAD anomalies
and key interpreted geological structures.
Next Steps
All samples from the field programs at Reynolds Lake and Reitenbach Lake will be analysed at ALS
Global Laboratories, with assays due in Q4 2025. Assays of samples with scintillometer readings > 5,000
cps2 will be prioritised.
The results will be integrated with existing geophysics and structural data to prioritise exploration areas
across both projects. Future work will focus on systematically testing high-priority EM conductors and
shear-zone intersections, with a potential drill program in 2026 to validate uranium mineralisation in
bedrock.
[END]
Release authorised by the Board of of Infini Resources Ltd.
Contacts
Rohan Bone
Chief Executive Officer
E: info@infiniresources.com.au
Uraninite Showing at Reitenbach Lake and Completion of Inaugural Field
Programs
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About Reynolds Lake & Reitenbach Lake
The Reynolds Lake and Reitenbach Lake Uranium Projects collectively comprise 19 mineral claims
covering a total footprint of 677 km² on the eastern outboard margin of the Athabasca Basin in northern
Saskatchewan. The projects are contiguous, with Reynolds Lake consisting of 12 claims (386 km²) and
Reitenbach Lake consisting of 7 claims (291 km²) adjoining its northern boundary.
The properties are underlain by Archean to Paleoproterozoic metamorphic and igneous rocks and are
bisected by the crustal-scale Needle Falls Shear Zone, a major structural corridor separating the
Wollaston Domain to the west from the Peter Lake Domain to the east. The Wollaston Domain is
dominated by Paleoproterozoic siliciclastic metasediments including paragneiss, quartzite, and calc-
silicate units, while the Peter Lake Domain contains Archean to Paleoproterozoic granitoid gneisses and
supracrustal rocks. Both domains are strongly deformed and metamorphosed, with northeast-trending
isoclinal folding and later cross-cutting north–south fault systems that provide structural complexity and
potential pathways for hydrothermal fluid flow.
Graphitic schists and gneisses — key lithologies known to host unconformity-associated uranium
mineralisation — have been identified within the project area. These are spatially associated with
electromagnetic conductors, radiometric anomalies, and elevated uranium-in-lake sediment samples.
Regionally, the geological setting is considered analogous to uranium systems at Eagle Point and Rabbit
Lake, where mineralisation occurs along graphitic shear zones at the boundary between Wollaston
metasediments and granitoid basement.
Figure 4: Location of the Reynolds Lake Uranium Project and Reitenbach Uranium Project relative to the
world-renowned Athabasca Basin, synonymous with high-grade uranium deposits, and in close proximity to
existing operations, access and infrastructure.
Uraninite Showing at Reitenbach Lake and Completion of Inaugural Field
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About Infini Resources Ltd (ASX: I88)
Infini Resources Ltd is an Australian energy metals company focused on mineral exploration in Canada and Western Australia for
uranium and lithium. The company has a diversified and highly prospective portfolio of assets that includes greenfield and more
advanced brownfield projects. The company’s mission is to increase shareholder wealth through exploration growth and mine
development.
JORC 2012 Mineral Resource Deposit JORC 2012 Classification Tonnes and Grade
Des Herbiers (U) Inferred Combined Resource 162 Mt @ 123ppm U3O8 (43.95mlb)
Figure 5: Overview of Infini's portfolio of projects and global footprint.
Competent Person & Compliance Statement
The information in this report that relates to exploration results for the Reynolds Lake Uranium Project and Reitenbach Lake Uranium
Project is based on, and fairly represents, information and supporting documentation compiled and evaluated by Mark Couzens,
Principal Geologist of the Company who is a Member of the AusIMM. Mr. Couzens has sufficient experience relevant to the style
of mineralisation, type of deposit under consideration, and the activity being undertaken to qualify as a Competent Person as defined
in the 2012 Edition of the Australian Code for Reporting of Exploration Results, Mineral Resources, and Ore Reserves (JORC
Code). Mr. Couzens consents to the inclusion of the information in the form and context in which it appears. The information in the
market announcement is an accurate representation of the available data and studies for the Reynolds Lake Uranium Project and
the Reitenbach Lake Uranium Project.
This announcement contains information on the Reynolds Lake Uranium Project and the Reitenbach Lake Uranium Project
extracted from ASX market announcements dated 25 February 2025, 31 March 2025, 24 July 2025, 20 August 2025, 9 September
2025, 22 September 2025 and 2 October 2025 reported in accordance with the 2012 edition of the “Australian Code for Reporting
of Exploration Results, Mineral Resources and Ore Reserves” (JORC Code). The original market announcements are available to
view on www.infiniresources.com.au and www.asx.com.au. The Company is not aware of any new information or data that
materially affects the information included in the original market announcement.
This announcement contains information regarding the Des Herbiers Mineral Resources Estimate extracted from the Company’s
Prospectus dated 30 November 2023 and released to the ASX market announcements platform on 10 January 2024, reported in
accordance with the 2012 edition of the “Australian Code for Reporting of Exploration Results, Mineral Resources and Ore
Reserves” (JORC Code). The Company confirms that it is not aware of any new information or data that materially affects the
information included in any original announcement and that all material assumptions and technical parameters underpinning the
estimates in the original market announcement continue to apply and have not materially changed. The original market
announcements are available to view on www.infiniresources.com.au and www.asx.com.au.
Forward Looking Statements
This announcement may contain certain forward-looking statements and projections. Such forward looking statements/projections
are estimates for discussion purposes only and should not be relied upon. Forward looking statements/projections are inherently
uncertain and may therefore differ materially from results ultimately achieved. Infini Resources Limited does not make any
representations and provides no warranties concerning the accuracy of the projections and disclaims any obligation to update or
revise any forward-looking statements/projects based on new information, future events or otherwise except to the extent required
by applicable laws. While the information contained in this report has been prepared in good faith, neither Infini Resources Limited
or any of its directors, officers, agents, employees or advisors give any representation or warranty, express or implied, as to the
fairness, accuracy, completeness or correctness of the information, opinions and conclusions contained in this announcement.
Uraninite Showing at Reitenbach Lake and Completion of Inaugural Field
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Appendix
Table 1: Scintillometer readings (greater than 1,000 counts per second) of samples taken during the field
program at Reynolds Lake and Reitenbach Lake.
Sample Site Easting (m) Northing (m) Elevation (m)
Scintillometer
Reading (cps)1
25RNJG001 619445 6416518 451 1,240
25RNJG002 619364 6416381 444 1,200
25RNJG004 619771 6415847 429 1,200
25RNJG008 619984 6416156 427 1,500
25RNCF002 619730 6416592 409 1,070
25RNCF004 619744 6416185 399 1,500
25RNCF008 620037 6416380 396 1,137
25RNBP004 620154 6416667 Not available 1,140
25RNBP005 620450 6416270 Not available 1,210
25RNGG008 618888 6416389 415 1,038
25RNGG010 619148 6415773 418 1,025
25RNGG011 619139 6415746 412 1,266
25RNGG012 619023 6415730 421 1,739
25RNJG021 620664 6417733 440 2,168
25RNJG025 621400 6418249 419 1,377
25RNJG027 621564 6418468 416 1,509
25RNJG031 620599 6417982 433 1,400
25RNCF010 620594 6416809 408 3,685
25RNCF011 620719 6416794 400 1,046
25RNCF015 621060 6417162 397 2,162
25RNCF017 621220 6417230 393 1,700
25RNCF018 621093 6417356 400 1,700
25RNBP023 618950 6415403 Not available 1,570
25RNGG017 618615 6415295 398 1,106
25RNGG018 618392 6415100 399 1,177
25RNGG019 618220 6415043 405 1,314
25RNGG025 617577 6415495 409 5,287
25RNJG035 620179 6418260 451 1,167
25RNJG037 620757 6418393 421 9,700
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Sample Site Easting (m) Northing (m) Elevation (m)
Scintillometer
Reading (cps)1
25RNJG038 620911 6418434 425 1,700
25RNJG039 621044 6418830 428 1,300
25RNGG32 622029 6420000 409 1,027
25RNGG36 621436 6420190 417 2,121
25RNGG38 621198 6419951 413 2,338
25RNGG40 621519 6419621 395 1,120
25RNGG41 621766 6419534 395 1,127
25RNGG45 622029 6419737 391 1,020
25RNBP042 622468 6417875 Not available 2,730
25RNJG042 622351 6420337 429 1,134
25RNJG043 622279 6420354 436 2,845
25RNJG048 622111 6420969 438 1,100
25RNJG049 622085 6421189 428 2,900
25RNJG053 622395 6420898 426 1,100
25RNCF031 623191 6421929 377 1,085
25RNCF032 623253 6422042 376 1,042
25RNGG45B 623752 6419460 375 1,200
25RNGG56 623772 6419624 371 1,073
25RNBP048 623767 6419511 Not available 1,400
25RNBP049 624440 6419326 Not available 2,100
25RNBP054 625171 6419908 Not available 1,300
25RNBP055 624495 6420873 Not available 3,000
25RNCF042 624439 6417961 373 1,050
25RNGG059 620666 6418437 398 1,650
25RNGG060 620463 6418370 416 1,418
25RNJG069 620747 6418396 Not available 3,300
25RNJG070 620739 6418341 Not available 2,500
25RNJG071 620669 6418254 Not available 2,300
25RNJG072 620464 6418356 458 7,000
25RNCF047 624912 6425506 391 2,000
25RNGG063 624745 6425249 389 1,003
25RNGG070 623916 6425833 380 3,125
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Sample Site Easting (m) Northing (m) Elevation (m)
Scintillometer
Reading (cps)1
25RNGG075 624296 6426525 386 1,510
25RNGG076 624362 6426528 399 1,676
25RNJG074 625289 6426686 389 3,500
25RNJG085 625030 6426276 402 3,800
25RNCF57 623579 6424310 394 8,090
25RNCF58 623470 6424215 387 3,000
25RNBP082 623485 6424067 Not available 3,300
25RNBP083 623459 6423998 Not available 65,550
25RNGG79 624155 6425131 389 2,800
25RNGG083 623442 6424792 389 1,002
25RNGG79 624155 6425131 389 2,800
25RNGG083 623442 6424792 389 1,002
25RNJG086 624156 6425131 396 4,000
25RNJG087 623607 6424225 380 1,452
25RNJG088 623631 6424132 375 3,327
25RNJG089 623616 6424099 378 2,181
ASX Announcement
Released 3 October 2025
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11
JORC Code, 2012 Edition – Table 1
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.
• 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.
• Mapping and Prospecting Samples
Mapping and prospecting include both select grab samples
and lithological geochemical (LGC) grab samples. Select
samples are guided by a handheld scintillometer (RS-125
Super-SPEC), targeting anomalous readings greater than
400 cps. LGC samples are prioritized based on lithology,
alteration, and mineralisation, consistent with industry
standards. For both sampling types, UTM coordinates (UTM
Zone 13), sample site details, and lithology / alteration /
mineralisation descriptions are collected and stored digitally.
• Soil Samples
Soil samples are collected on a predefined grid with NE/SW-
oriented lines spaced 200 m apart, and sample stations
spaced 100 m along each line. Traditional C-horizon soils
are collected where possible; if the C-horizon is absent, B-
horizon samples are taken instead. For each soil sample,
coordinates, site details, and soil horizon are recorded
digitally.
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 due to no drilling undertaken.
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Criteria JORC Code explanation Commentary
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.
• Not applicable due to no drilling undertaken.
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.
• Not applicable due to no drilling undertaken.
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.
• Soil samples were prepared using ALS method PREP-41,
which involves drying and sieving to -180 µm (-80 mesh).
The samples were then analyzed using ME-MS41L, an aqua
regia digestion with ICP-MS multi-element analysis. This
partial digestion method is particularly suited to near-surface
soils and is effective for detecting pathfinder and trace
elements.
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Criteria JORC Code explanation Commentary
• Rock samples were prepared using ALS method PREP-31,
where samples are crushed to 70% passing 2 mm, a ~250 g
split is taken, and the split is pulverized to 85% passing 75
µm. Analytical work was completed with ME-MS61L, a four-
acid digestion followed by ICP-MS multi-element analysis.
For selected samples—particularly those containing quartz
veins, flooded textures, or fine-grained disseminated
sulphides—an additional gold assay was carried out using
Au-AA23, a 30 g fire assay with AAS finish. The four-acid
digestion provides a near-total digestion for most silicate,
oxide, and sulphide minerals, while fire assay is considered
the most reliable technique for gold determination.
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.
• No quality control procedures (e.g. standards, blanks,
duplicates were added to the samples submitted due to the
exploratory nature of the sample types. Normal lab QAQC
insertions will be performed by ALS Global, an ISO-certified
lab in Sudbury, Ontario.
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.
• All sample sites and relevant data regarding the site, material
sampled and Lith, Alt and Mineralisation are recorded by the
geologist and stored in a database.
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Criteria JORC Code explanation Commentary
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.
• Not applicable due to no drilling undertaken.
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.
• Not applicable as no Mineral Resource and Ore Reserves
are reported.
• No sample compositing has been applied.
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.
• Soil samples lines and stations were planned to be directly
down ice, NW of EM conductors identified in the earlier
survey. The details of that survey are reviewed in the earlier
press release.
Sample
security
• The measures taken to ensure sample security. • All samples were within the contractors' possession with a
strong chain of custody protocol. They have been shipped in
sealed and manifested sample bags and delivered by a
bonded courier to ALS Global in Sudbury, Ontario, an ISO
certified lab.
Audits or
reviews
• The results of any audits or reviews of sampling techniques
and data.
• Not applicable
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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
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