Airborne EM & U Anomalism Confirm Reitenbach Lake Potential
Released
Released
Announcement PDF
ASX Announcement
Released 28 January 2026
Infini Resources Limited ABN 77 656 098 583 www.infiniresources.com.au
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Airborne EM and Uranium Anomalism
Confirm Additional Scale Potential at
Reitenbach Lake
Newly interpreted 2025 airborne EM survey identifies continuation of major
conductive trends into recently expanded Reitenbach Lake tenements, defining an
additional ~20 × 5 km prospective corridor.
Historical and recent exploration highlight elevated uranium lake-sediment
geochemistry and uranium anomalism across Reynolds and Reitenbach Lake,
including the 1.90% U₃O₈ Titus Showing, with a strong spatial association to
regionally extensive EM conductors and key structural features.
Target refinement and drill planning integrating structural, geophysical and
geochemical datasets underway, with expected completion in Q1 CY2026.
Results materially enhance confidence in the scale and continuity of anomalism
across Reynolds and Reitenbach Lake ahead of a planned maiden drill program in
Q2 CY2026.
Infini Resources Limited (ASX:I88) (“Infini” or the “Company”) is pleased to announce the
completion of work packages over its recently expanded Reitenbach Lake tenements, comprising the
acquisition and interpretation of airborne electromagnetic (EM) survey data and a desktop review of
historical exploration data.
Together, these programs further reinforce the potential scale, continuity and prospectivity of the
Reitenbach Lake Uranium Project, ahead of a planned maiden drill program in Q2 CY2026.
Infini’s Chief Executive Officer, Rohan Bone, said: "These two work programs are an important step
in unlocking the full potential and scale of the Reitenbach Lake project. Identifying an additional ~20 x 5
km prospective EM corridor across our recently expanded tenements, and now having approximately 80
kilometres of EM conductors defined across the broader project area, really highlights the size of the
opportunity we are dealing with.
When this is combined with extensive uranium lake-sediment anomalies and prominent structural
features identified in the desktop review, it significantly strengthens our confidence as we progress toward
final target definition and commencement of our planned maiden drill program on the margins of the
Athabasca Basin.”
Acquisition of airborne EM survey data over newly staked Reitenbach Lake claims
A portion of the recently expanded Reitenbach Lake tenements was also covered as part of Infini’s
airborne EM survey flown over the Reynolds Lake and Reitenbach Lake projects in 2025. The Company
has now processed and interpreted this dataset in full. Note, the airborne survey did not fully cover the
recently expanded tenement MC00023249, data recorded within this area has been excluded from the
interpretation.
Interpretation of the airborne EM data indicates that conductive trends identified within Infini’s original
Reitenbach Lake holdings extend for approximately 20 km through the recently expanded tenements,
demonstrating strong geological continuity. When combined with conductors defined elsewhere across
Reynolds Lake and Reitenbach Lake, Infini has now identified approximately 80 km of EM conductors
Airborne EM and Uranium Anomalism Confirm Additional Scale Potential at
Reitenbach Lake
Infini Resources Limited ABN 77 656 098 583 www.infiniresources.com.au
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strike length across the broader project area.
These conductors are interpreted to represent prospective graphitic and structurally controlled horizons
that are considered favourable for basement-hosted uranium mineralisation. The absence of EM
coverage over MC00023249 reflects survey extent only and does not preclude the presence of conductive
or prospective lithologies within this tenement.
Figure 1: Geophysics survey results indicate that EM anomalism continues through the recently expanded
Reitenbach Lake tenements, resulting in ~80 km of prospective EM conductors reinforcing the potential for
a large, structurally controlled uranium system.
Desktop study of historical exploration data over the newly staked Reitenbach Lake claims
Infini has also completed a desktop study of historical exploration data covering the recently expanded
tenements, which are located directly adjacent to the Company’s 100% owned Reitenbach Lake Uranium
Project.
The review confirms the presence of historical elevated uranium lake-sediment geochemistry (including
uranium values up to ~46 ppm), and multiple zones where geochemical anomalism coincides with EM
conductors, major shear zones and cross-cutting structures. Several priority target areas have been
identified where overlapping geochemistry, EM conductors, airborne radiometric anomalies and structural
complexity occur.
Airborne EM and Uranium Anomalism Confirm Additional Scale Potential at
Reitenbach Lake
Infini Resources Limited ABN 77 656 098 583 www.infiniresources.com.au
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The outcomes of the desktop study complement Infini’s recent field results and further refine priority
corridors for follow-up exploration and drill targeting.
Figure 2: Overview of historical geochemistry records at Infini’s recently expanded tenements at Reitenbach
Lake Note the coincidence of elevated uranium lake sediments with EM conductors and adjacent fault
structures.
Next Steps
The airborne EM interpretation and historical data will be fully integrated with Infini’s geological mapping,
geochemistry and structural framework to finalise and prioritise drill targets across the Reynolds Lake
and Reitenbach Lake projects, ahead of a planned maiden drill program. Key upcoming milestones
include:
• Target refinement and drill planning integrating structural, geophysical and geochemical data,
expected in Q1 CY2026.
• Ongoing engagement with local First Nations, including Ya’thi Néné Lands and Resources
(YNLR), alongside government permitting processes, progressing in parallel to support drilling
activities.
• Appointment and mobilisation of key geological and drilling contractors ahead of commencement
of drilling activities, expected in Q1 and Q2 CY2026.
• Commencement of a maiden drill campaign across priority targets at Reynolds and Reitenbach
Lake projects, subject to permitting and stakeholder engagement, targeted for Q2 CY2026.
Airborne EM and Uranium Anomalism Confirm Additional Scale Potential at
Reitenbach Lake
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References
1. ASX announcement, Infini Resources, Phase 2 Rock Chip Assays Confirm Widespread Uranium
Anomalism at Reynolds and Reitenbach Lake, 19 January 2026.
2. ASX announcement, Infini Resources, Infini Expands Reitenbach Lake Uranium Project Footprint by
31%, 12 January 2026.
3. ASX announcement, Infini Resources, High-Grade Uraninite Confirmed at Reitenbach Lake – Phase
1 Assay Results Received, 23 December 2025.
4. ASX announcement, Infini Resources, Amendment to ASX Announcement; Reynolds Lake Field
Program Expanded to Target New EM Anomalies, 2 October 2025 and 22 September 2025.
5. ASX announcement, Infini Resources, Infini Advances its Canadian Uranium Portfolio, 2 June 2025.
[END]
Release authorised by the Board of Infini Resources Ltd.
Contacts
Rohan Bone
Chief Executive Officer
E: info@infiniresources.com.au
Airborne EM and Uranium Anomalism Confirm Additional Scale Potential at
Reitenbach Lake
Infini Resources Limited ABN 77 656 098 583 www.infiniresources.com.au
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About Reynolds Lake & Reitenbach Lake
The Reynolds Lake and Reitenbach Lake Uranium Projects collectively comprise 22 mineral claims
covering a total footprint of 766 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 10 claims (381 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 and are spatially associated with
electromagnetic conductors, radiometric anomalies and elevated uranium-in-lake sediment samples.
Recent exploration has confirmed primary uranium mineralisation at surface at Reitenbach Lake, while
petrographic analysis has validated a structurally prepared and hydrothermally altered basement
environment consistent with an unconformity-related uranium system.
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 3: 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.
Airborne EM and Uranium Anomalism Confirm Additional Scale Potential at
Reitenbach Lake
Infini Resources Limited ABN 77 656 098 583 www.infiniresources.com.au
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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 4: 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, 2 October 2025, 3 October 2025, 26 November 2025, 23 December 2025, 12 January 2026 and 19
January 2026 and 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
Airborne EM and Uranium Anomalism Confirm Additional Scale Potential at
Reitenbach Lake
Infini Resources Limited ABN 77 656 098 583 www.infiniresources.com.au
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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.
Airborne EM and Uranium Anomalism Confirm Additional Scale Potential at
Reitenbach Lake
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Appendix 1: Lake sediment sample assays across newly staked tenements
Table 1: Historical lake sediment survey results across tenements MC00023249 - MC00023251 as published
by SDMC (1979). Note no RL information was documented and all survey sites are projected in NAD83 UTM
Zone 13.
Sample ID
UTM East
(m)
UTM North
(m)
U
(ppm)
Pb
(ppm)
Cu
(ppm)
Zn
(ppm)
Ni
(ppm)
IW1896 632433 6438312 3 23 11 97 16
IW1897 633436 6439008 1 9 2 43 7
IW1902 632496 6439344 3 10 11 84 14
IW1901 632492 6439610 1 6 1 18 5
W8L0966 629681 6441762 1 13 7 25 12
W8L0968 629873 6441747 1 7 8 28 11
W8L0967 629814 6441555 1 3 6 24 11
W8L0965 629577 6441473 1 7 7 30 11
W8L0970 630856 6441126 9 6 10 34 14
W8L0969 630849 6440971 7 7 11 33 15
IW1919 632114 6442464 4 8 10 68 21
IW1922 631692 6442487 1 10 3 67 14
IW1920 631855 6442013 1 8 7 98 16
IW1921 631271 6442102 3 17 11 61 21
IW1905 631515 6438985 2 11 8 32 10
IW1904 632017 6439044 3 9 9 39 8
IW1903 632273 6439277 4 21 17 74 12
IW1895 631766 6438678 1 9 8 31 10
IW1584 631677 6438201 0 14 8 143 16
IW1585 631418 6437780 0 10 3 87 11
IW1864 630481 6437856 0 6 8 49 7
IW1863 630245 6437685 0 5 8 47 7
IW1862 630307 6437449 1 5 7 85 7
IW1865 630071 6438758 1 8 7 58 12
IW1933 627653 6440481 2 4 9 61 14
IW1934 627579 6440333 2 5 8 62 14
IW1841 629782 6432849 0 7 3 41 7
IW1842 629819 6433714 3 15 10 106 19
IW1840 628577 6432635 5 13 11 78 13
IW1838 628340 6432213 5 13 11 78 14
IW1837 628302 6431755 5 13 13 81 15
W8L0822 626919 6430609 23 7 11 33 12
Airborne EM and Uranium Anomalism Confirm Additional Scale Potential at
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Sample ID
UTM East
(m)
UTM North
(m)
U
(ppm)
Pb
(ppm)
Cu
(ppm)
Zn
(ppm)
Ni
(ppm)
W8L0823 626734 6430561 30 8 11 33 11
W8L0825 626486 6430324 23 9 10 37 11
W8L0824 626604 6430394 28 12 9 53 14
W8L0826 626168 6429962 26 15 17 94 19
W8L0827 626039 6429899 34 21 20 143 26
W8L0828 625976 6429688 29 21 26 136 22
W8L0829 625839 6429533 36 18 26 151 26
W8L0830 625883 6429414 29 18 19 133 23
W8L0832 625643 6429400 44 19 23 209 28
W8L0831 625795 6429289 46 18 25 199 30
W8L0833 625566 6429274 27 14 19 122 20
W8L0835 625299 6428845 14 13 12 139 12
W8L0834 625458 6429008 27 27 22 141 24
W8L0836 625207 6428741 12 10 7 35 10
IW1828 625333 6428908 17 8 12 48 11
IW1829 625684 6429222 27 14 19 122 20
IW1830 625880 6429381 45 18 25 233 28
IW1832 626079 6429677 31 18 21 158 19
IW1831 625887 6429718 33 16 16 239 24
IW1833 626283 6430076 29 15 20 129 19
IW1834 626553 6430357 27 9 13 74 16
IW1835 626860 6430583 29 7 16 49 12
IW1899 632819 6440118 3 16 13 73 15
IW1900 633047 6439993 0 18 0 78 0
IW1898 633254 6440620 3 15 10 68 13
IW2766 633907 6440824 0 2 3 16 3
IW2765 633822 6441354 0 2 2 15 4
IW1911 632627 6441539 5 8 4 21 10
IW1910 632771 6441965 4 8 6 34 9
IW2763 633756 6442034 2 6 5 18 8
IW2762 634051 6442561 1 5 8 58 12
IW1909 632916 6442455 5 14 12 82 11
IW1906 633229 6442925 3 12 8 174 4
IW2767 633279 6442850 2 13 8 70 14
IW2768 633286 6443207 3 6 14 44 11
IW1907 633142 6443270 3 5 12 41 10
Airborne EM and Uranium Anomalism Confirm Additional Scale Potential at
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Sample ID
UTM East
(m)
UTM North
(m)
U
(ppm)
Pb
(ppm)
Cu
(ppm)
Zn
(ppm)
Ni
(ppm)
IW1908 633367 6443571 3 8 11 55 9
IW2769 633806 6443464 3 6 14 46 13
IW1917 632439 6443082 3 9 11 111 15
IW1918 632502 6443245 2 8 9 57 18
IW1915 632696 6443740 2 9 8 39 15
IW1914 632809 6444104 2 6 8 45 14
IW1913 632157 6444455 1 8 4 23 11
IW1912 632571 6444882 1 6 3 19 8
IW2770 634101 6444129 3 9 11 51 14
IW1916 632928 6443728 2 9 9 77 16
IW2761 634339 6442975 1 2 6 39 8
IW2752 635318 6444041 13 4 9 62 12
IW2754 634785 6444298 8 3 6 43 8
IW2755 634785 6444474 9 5 10 36 11
IW2756 634992 6444700 8 15 10 110 25
IW2738 634923 6444995 9 13 24 126 27
IW2737 635581 6445496 6 16 18 62 12
IW2756 635130 6444430 8 15 10 110 25
IW2735 636971 6447327 7 8 14 121 20
IW2729 637692 6447984 0 31 13 362 49
IW2728 637982 6448288 24 15 19 139 14
IW2730 637508 6448559 5 8 15 61 13
IW2733 636383 6447946 8 25 36 162 29
IW2736 635777 6446139 7 12 16 116 25
IW2740 634531 6446019 2 6 14 49 14
IW2739 634791 6446284 4 8 12 55 13
IW2732 636421 6448332 5 13 29 63 17
IW2727 638242 6448736 0 29 15 279 35
IW2731 636560 6448623 6 7 25 61 15
W8L0167 637660 6448755 8 15 18 60 15
W8L0168 637508 6448534 8 12 11 49 16
W8L0162 637869 6448022 18 13 17 177 23
W8L0163 637723 6448168 1 9 11 33 9
W8L0161 638008 6448243 4 10 5 96 12
W8L0159 638172 6448383 20 30 20 153 28
W8L0160 638071 6448553 40 15 31 336 27
Airborne EM and Uranium Anomalism Confirm Additional Scale Potential at
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Sample ID
UTM East
(m)
UTM North
(m)
U
(ppm)
Pb
(ppm)
Cu
(ppm)
Zn
(ppm)
Ni
(ppm)
W8L0157 638267 6448534 18 29 21 125 25
W8L0158 638121 6448755 3 6 3 17 6
W8L0166 637780 6449046 1 7 16 62 12
W8L0165 637843 6449204 30 8 11 69 18
W8L0164 638033 6449381 2 5 15 47 11
W8L0156 638437 6448863 17 13 26 261 25
W8L0155 638678 6449337 19 19 20 176 21
W8L0154 638507 6449470 13 20 18 146 20
W8L0152 638899 6449716 10 31 18 74 16
W8L0151 639095 6449975 12 17 18 94 18
W8L0150 639158 6450215 16 12 20 122 18
W8L0148 639487 6450620 8 13 10 34 13
W8L0149 639367 6450386 6 10 9 39 13
W8L0147 639354 6450841 4 13 8 28 11
IW1859 630291 6435515 3 14 9 101 15
IW1843 629655 6435175 3 12 7 138 16
IW1462 637984 6450218 1 6 11 46 10
IW1461 637644 6449922 1 6 13 50 14
IW1460 637060 6449752 6 16 21 73 18
IW1459 636816 6449375 3 6 20 58 15
IW1458 636787 6448998 7 6 28 142 20
Airborne EM and Uranium Anomalism Confirm Additional Scale Potential at Reitenbach Lake
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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.
• Historical Reitenbach Lake exploration data
Lake sediment surveys were conducted in 1977 and 1978 by
Saskatchewan Mining Development Corporation (SMDC).
These employed an Eckman dredge from a platform
mounted on the float of a Bell 47G-4A helicopter. Water
depth, sample composition, lake size, percentage exposure
and flow rate were recorded at each location, however this
information was not reported. 3,042 samples were collected
in total, however not all of which are within the Company’s
project area or the tenements MC00023249 - MC00023251.
• Reitenbach Geophysics Survey
The helicopter-borne Time-Domain Electromagnetic
(TDEM) survey over the Reitenbach Lake and Reynolds
Lake projects was flown along 450m spaced traverse lines
oriented 130o – 310o and 4,500m spaced tie-back lines
oriented 040o – 220o for a total of 1,630 line kilometers
flown.
The system utilizes a patented inflatable transmitter loop
with a diameter of approximately 20 meters, suspended
about 30 meters below the helicopter. It features a
programmable waveform with a fast turn-off time, allowing
for flexibility in data acquisition and improved resolution of
both shallow and deep targets. The instrument is able to
measure Dipole moment up to 372,000 NIA (Newton–
ampere).
Airborne EM and Uranium Anomalism Confirm Additional Scale Potential at Reitenbach Lake
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Criteria JORC Code explanation Commentary
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.
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.
• Not applicable due to no drilling undertaken nor assay results
announced.
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Criteria JORC Code explanation Commentary
• 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.
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.
• Not applicable due to no drilling undertaken nor assay results
announced.
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.
• Scintillometer results have not yet been verified.
• No assay results are provided in the announcement.
Location of
data points
• Accuracy and quality of surveys used to locate drill holes
(collar and down-hole surveys), trenches, mine workings
and other locations used in Mineral Resource estimation.
• Specification of the grid system used.
• Quality and adequacy of topographic control.
• All survey location data is in NAD83 UTM Zone 13N.
• The GPS was a Novatel DL-V31L2, with differential
correction and utilizes 12 satellites with a recording rate of
20 Hz.
• A Lazer altimeter was used, SF11/C (loop) and SF00 (Heli)
with a 1cm resolution, recording rate 20Hz.
• The method used is highly accurate and effective.
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Criteria JORC Code explanation Commentary
Data spacing
and
distribution
• Data spacing for reporting of Exploration Results.
• Whether the data spacing and distribution is sufficient to
establish the degree of geological and grade continuity
appropriate for the Mineral Resource and Ore Reserve
estimation procedure(s) and classifications applied.
• Whether sample compositing has been applied.
• 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.
• The helicopter-borne Time-Domain Electromagnetic (TDEM)
survey over the Reitenbach Lake project was flown along
450m spaced traverse lines oriented 130o – 310o and
4,500m spaced tie-back lines oriented 040o – 220o for a total
of 1,630 line kilometers flown.
• The traverse flight lines are oriented perpendicular to the
interpreted major fault system which is considered
appropriate for this early level of exploration.
Sample
security
• The measures taken to ensure sample security. • No assay results are provided in the announcement.
Audits or
reviews
• The results of any audits or reviews of sampling techniques
and data.
Review of the data was carried out by Resources Potentials
1/46 Hasler Road, Osborne Park, WA 6017, website:
www.respot.com.au
Airborne EM and Uranium Anomalism Confirm Additional Scale Potential at Reitenbach Lake
Infini Resources Limited ABN 77 656 098 583 www.infiniresources.com.au
InfiniResources
16
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 security of the tenure held at the time of reporting along
with any known impediments to obtaining a licence to
operate in the area.
• The Reynolds Lake Uranium Project comprises twelve
mineral claims (MC00016423 - MC00016434). The
company acquired the project in 2025 (100% ownership)
and is not aware of any royalties existing on the claims or
impediments to obtaining a license to operate in the area.
• The Reitenbach Lake Uranium Project comprises ten
mineral claims (MC00018042 - MC00018048, MC00023249
- MC00023251). The company acquired the project
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