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INFINI RESOURCES LIMITED Capital/Financing Update 2025

Feb 24, 2025

65087_rns_2025-02-24_e01d71ae-bd83-4b2c-8f2b-6792bb775cc8.pdf

Capital/Financing Update

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ASX Announcement Released 25 February 2025

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Infini To Acquire Major Footprint In Athabasca Basin

Infini strengthens its Canadian Uranium portfolio through the acquisition of Reynolds and Boulding Lake properties, prospective for unconformity-style uranium deposits

Highlights

Infini has entered into a binding agreement to acquire 100% of the Reynolds and Boulding Lake Uranium Projects, located in the Athabasca Basin region of Saskatchewan, Canada

The Reynolds and Boulding Lake Projects comprises a total landholding of 931km[2] , with both projects located within a 100km of the world class McArthur River and Eagle Point high grade uranium camps

The Athabasca Basin, located in northern Saskatchewan and Alberta, Canada, is one of the world's richest sources of high-grade uranium. Spanning approximately 100,000 km[2] , it is host to some of the most prolific uranium deposits, including the Cigar Lake and McArthur River mines

The acquisition aligns with Infini’s vision to become one of the most active uranium exploration companies listed on the ASX, with highly anticipated maiden drilling currently underway at its flagship Portland Creek Uranium Project The Reynolds Lake Project comprises a 677 km[2 ] landholding and contains reported anomalous uranium in lake sediments and radiometric anomalies in proximity to the underexplored Needle Falls shear zone. Boulding Lake is a 254 km[2] property directly adjacent to claims containing a large number of radioactive boulders, with the potential for a primary uranium source within the project area indicated by a magnetic low (interpreted basin sediments) and south-west trending ice flow directions

Geophysical surveys to commence shortly across both Reynolds and Boulding Lake projects to generate targets for follow up exploration activities

Upfront consideration of $1.6 million comprising the issue of 2,622,378 fully paid ordinary shares at an issue price of $0.572 per share (15 day VWAP, 36% premium to last close price) and $0.1m cash, plus $0.75m in performance rights subject to drilling and resource milestones (convertible at the higher of the 15DWAP at achievement or $0.572).

- ’ High resolution magnetic imagery has returned from Infini s Tinco Project, - identifying a major north south trending shear zone that contains the historical mineralized grab sample of 600ppm U3O8, 0.5% Nb. This provides the Company with a large U-Nb follow up target for future exploration activities.

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Infini Resources Limited

www.infiniresources.com.au

ABN 77 656 098 583

InfiniResources

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Infini To Acquire Major Footprint In Athabasca Basin

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Infini Resources Ltd (ASX: I88 , “Infini” or the “Company”) is pleased to announce that it has entered into a binding share purchase agreement to acquire a 100% interest in the Reynolds and Boulding Lake Uranium Projects, further strengthening the Company’s position as a major energy minerals focused explorer.

Infini’s Managing Director and CEO, Charles Armstrong said : “The opportunistic acquisition of the Reynolds and Boulding Lake properties provides Infini with a strategic foothold in the world-renowned Athabasca Basin. After extensive review by our team, we believe these assets have the potential to deliver substantial long-term value for our shareholders. As global demand for clean, reliable energy grows, securing high-potential uranium exploration projects is increasingly vital to addressing the world's future energy needs. These new assets complement our vision of building a diversified portfolio of uranium targets, alongside our Portland Creek Uranium Project.

We remain highly focused on and committed to advancing our flagship Portland Creek Uranium Project. The acquisition of the Reynolds and Boulding Lake properties further strengthens our exploration strategy, but Portland Creek continues to be at the heart of our efforts. With drilling activities set to intensify in the coming weeks, weather permitting, we are eager to continue unlocking the full potential of this world-class exploration opportunity.”

About Reynolds and Boulding Lake

The Reynolds Lake Project comprises a significant 677km[2] land package in the Athabasca basin area, offering immediate exposure to a shallow unconformity-style uranium exploration opportunity in a premier, uranium mining-friendly jurisdiction. The project is characterised by a regional fault, multiple surface showings immediately along strike in either direction and radioactive boulders along trend. The geology of the Reynolds Lake property comprises Paleoproterozoic Wollaston group rocks that lie unconformably above Paleoproterozoic-modified Neoarchean granitoid basement and the Peter Lake Domain to the east, with the Needle Falls SZ propagating in a northeast direction along the boundary between the two (Figure 2).

Boulding Lake is a uranium exploration project located in Saskatchewan, Canada, 32km west of Cigar Lake Uranium Mine. The Boulding Lake project is a traditional exploration play in the Athabasca basin that offers exposure to several unconformity-style uranium plays in a premier, uranium mining-friendly jurisdiction. The project is immediately west of Denison Mines’ Johnston Lake and 92 Energy’s Clover projects. The total area of the project is 254km[2] . It is located adjacent to claims containing a large number of radioactive boulders, with the potential for a primary uranium source within the project area indicated by a magnetic low (interpreted basin sediments) and south-west trending ice flow directions (Figure 3).

Acquisition Terms

The Company has entered into a binding share purchase agreement to acquire 100% of the issued share capital of U Energy Metals Pty Ltd, which holds a 100% interest in the Reynolds and Boulding Lake Uranium projects in Saskatchewan, Canada. The Company has agreed to acquire a 100% interest in the Reynolds and Boulding Lake projects in consideration for:

  • (a) Cash payment: At completion, the Company will pay cash payments to the vendors of AUD$100,000.

  • (b) Consideration Shares: At completion the Company will issue 2,622,378 fully paid I88 shares, at the Company’s 15 trading day VWAP ($0.572 per share) (total value AUD$1,500,000), subject to 12 months escrow.

  • (c) Performance Rights: At completion, the Company will issue $750,000 worth of performance rights, subject to the following vesting conditions;

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Infini Resources Limited

www.infiniresources.com.au

ABN 77 656 098 583

InfiniResources

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Infini To Acquire Major Footprint In Athabasca Basin

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Ref Number of Performance Rights Vesting condition Expiry
A The number that converts to I88 Shares to the
value of A$250,000 with reference to the
higher of the 15-Day VWAP prior to:
(a)
the date the Vesting Condition A is
satisfied; or
(b)
the Execution Date ($0.572 per share).
Infini announcing to ASX one drill intercept at
the Reynolds or Boulder projects of at least 10
metres of U3O8with a minimum grade of 0.1%
or higher grade equivalent (eg 5m @ 0.2%
U3O8) (Vesting Condition A).
5:00pm (AWST) on the date
which is 3 years after the
date
of
issue
of
the
Performance Rights
B The number that converts to I88 Shares to the
value of A$250,000 with reference to the
higher of the 15-Day VWAP prior to:
(a)
the date the Vesting Condition B is
satisfied; or
(b)
the Execution Date ($0.572 per share).
Infini announcing to ASX 5 separate drill
intercepts at the Reynolds or Boulder projects
of at least 10 metres of U3O8with a minimum
grade of 0.1% or higher grade equivalent (eg
5m @ 0.2% U3O8) (Vesting Condition B).
5:00pm (AWST) on the date
which is 3 years after the
date
of
issue
of
the
Performance Rights
C The number that converts to I88 Shares to the
value of A$250,000 with reference to the
higher of the 15-Day VWAP prior to:
(a)
the date the Vesting Condition C is
satisfied; or
(b)
the Execution Date ($0.572 per share).
Infini announcing to ASX a JORC compliant
Mineral Resources Estimate in respect of the
Reynolds or Boulder projects of at least 10
million pounds of U3O8, with a grade of 0.1%
or greater (Vesting Condition C).
5:00pm (AWST) on the date
which is 5 years after the
date of issue of the
Performance Rights

Note: 15-Day VWAP means the volume weighted average price of Buyer Shares calculated over 15 consecutive trading days.

The acquisition is subject to due diligence to the Company’s satisfaction and receipt of any required regulatory, statutory and governmental consents and approvals and escrow agreements. Completion is required to be completed by 31 March 2025. The Company will pay the cash component of the transaction out of existing working capital. The projects vendors are unrelated parties of the Company. The abovementioned consideration shares will be issued pursuant to the Company’s placement capacity under ASX Listing Rule 7.1.

An Appendix 3B for the proposed issue of securities will follow this announcement.

Effect on Capital Structure

The capital structure of the Company on completion of the acquisitions will be as follows:

Capital Structure Shares Options Performance
Rights
Existing Securities 70,931,891 10,766,666 1,660,000
Project Consideration Shares 2,622,378 - 1,311,189
Total 73,554,269 10,766,666 2,971,189

Note: Project Consideration Shares is based on 15 trading day VWAP of $0.572. Performance rights represents the maximum number that may vest based on current VWAP. Should the respective performance hurdle be satisfied within the required performance period, the number of shares may vary depending upon the 15 trading day VWAP at the time.

References

1 U Energy Metals, (2023). J.W. Patrick Lengyel. Compilation Report Reynolds Lake Project.

2 U Energy Metals. (2022). Information Memorandum Reynolds Lake Project

3 U Energy Metals, (2023). J.W. Patrick Lengyel. Compilation Report Boulding Lake Project.

4 U Energy Metals. (2022). Information Memorandum Boulding Lake Project

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Infini Resources Limited

www.infiniresources.com.au

ABN 77 656 098 583

InfiniResources

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Infini To Acquire Major Footprint In Athabasca Basin

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Figure 1: Location of the Reynolds Lake and Boulding Lake projects in the world class Athabasca Basin.

Infini Resources Limited

www.infiniresources.com.au InfiniResources

ABN 77 656 098 583

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Infini To Acquire Major Footprint In Athabasca Basin

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Figure 2: Location of the Reynolds Lake project showing anomalous lake sediment analyses and airborne radiometric anomalies.

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Infini Resources Limited

www.infiniresources.com.au

ABN 77 656 098 583

InfiniResources

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Infini To Acquire Major Footprint In Athabasca Basin

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Figure 3: The Boulding Lake Project with government regional magnetics shown. Note the interpreted basin sediments characterised by a magnetic low, running in a northeast-southwest direction through the claims.

Tinco Project Geophysical Survey

A heliborne magnetic, radiometric and time-domain electromagnetic survey has been completed over Infini’s Tinco uranium project (both claims). The survey was flown along a west-northwest orientation with lines spaced 100m apart. The total survey comprised of 1030-line kms, flown at an average height of 36 m. Southern Geoscience Consultants processed the data to produce a set of filtered images. These images were interpreted to delineate magnetic and radiometric trends, classification of structures, lineaments, faults and folds, delineation and interpretation of stratigraphic relationships including contacts, and to produce a set of targets.

As indicated by the survey results in Figure 4, the high-resolution magnetic imagery has identified the presence of a major north-south trending shear zone that contains the historical mineralized grab sample of 600ppm U3O8, 0.5% Nb. This provides the Company with a large U-Nb follow up target for future exploration activities. In addition, there are several large ovoid magnetic features of interest in the centre of the claims which are an additional area of interest that can be followed up with surface geochemical surveys.

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Infini Resources Limited

www.infiniresources.com.au

ABN 77 656 098 583

InfiniResources

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Infini To Acquire Major Footprint In Athabasca Basin

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Figure 4: The magnetic imagery results of the Tinco survey. Note the location and coincidence of the mineralized grab sample with a major new interpreted shear zone corridor measuring 6km x ~1.5km.

[END]

Release authorised by the Board of Infini Resources Ltd.

Contacts

Charles Armstrong Managing Director and CEO P: +61 (08) 9465 1051

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 greenfields and more advanced brownfields projects. The Company’s mission is to increase shareholder wealth through exploration growth and mine development.

JOR 2012 Mineral Resource Deposit JORC 2012 Classification Tonnes and Grade
Des Herbiers (U) Inferred Combined Resource 162 Mt @ 123ppm U3O8(43.95mlb)

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Infini Resources Limited

www.infiniresources.com.au

ABN 77 656 098 583

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Competent Person Compliance Statement

The information contained in this announcement that relates to historical exploration results for the Reynolds and Boulding Lake uranium projects is based on, and fairly represents, information and supporting documentation prepared by Mr Charles Armstrong, who is Managing Director of the Company and is a member of the Australasian Institute of Mining and Metallurgy (AusIMM) and the Society of Economic Geologists (SEG). Mr Armstrong has sufficient experience that is relevant to the style of mineralisation and type of deposit under consideration, and to the activity being undertaken to qualify as a Competent Person, as defined in the JORC 2012 edition of the “Australasian Code for Reporting of Mineral Resources and Ore Reserves”. Mr Armstrong has 9 years’ experience as an exploration geologist. Mr Armstrong consents to the inclusion in this report of the matters based on this information in the form and context in which they appear. The information in the market announcement is an accurate representation of the available data and studies for the Reynolds and Boulding Lake projects in Canada.

The information contained in this announcement that relates to exploration results for the Tinco uranium project is based on, and fairly represents, information and supporting documentation prepared by Mr Charles Armstrong, who is Managing Director of the Company and is a member of the Australasian Institute of Mining and Metallurgy (AusIMM) and the Society of Economic Geologists (SEG). Mr Armstrong has sufficient experience that is relevant to the style of mineralisation and type of deposit under consideration, and to the activity being undertaken to qualify as a Competent Person, as defined in the JORC 2012 edition of the “Australasian Code for Reporting of Mineral Resources and Ore Reserves”. Mr Armstrong has 9 years’ experience as an exploration geologist. Mr Armstrong consents to the inclusion in this report of the matters based on this information in the form and context in which they appear.

This report 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.

This report contains information on the Company’s Tino Project 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 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.

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.

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Infini Resources Limited

www.infiniresources.com.au

ABN 77 656 098 583

InfiniResources

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Infini To Acquire Major Footprint In Athabasca Basin

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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

  • Sampling • Nature and quality of sampling (eg cut channels, random techniques 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 (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.

Commentary

Reynolds Lake Project

All surface work was completed prior to 1986, with the majority of it prior to 1970. QAQC protocols prior to 1990 were minor to non-existent. Duplicate samples, sample blanks, and reference standards were not used. Assessment reporting standards were minimal, and technical reporting could be spartan, but most included a basic sampling method description and usually the laboratory and analytical methods used.

Most surface rock and boulder sampling was opportunistic with samples taken wherever outcrops or glacial boulders were present.

No mechanized channel sampling is reported. Rare rock chip sampling was reported where consecutive chip samples were taken across widths ranging up to 1 meter across prospective bedrock mineralization in lieu of mechanized channel sampling. Samples were collected in plastic sample bags secured with tape. Sample tags from prenumbered duplicate sample tag books were used in the field and cross-checked upon return to camp each day.

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Infini Resources Limited

www.infiniresources.com.au

ABN 77 656 098 583

InfiniResources

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Infini To Acquire Major Footprint In Athabasca Basin

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Criteria
JORC Code explanation
Commentary
Soil sampling was completed on grids ranging from
reconnaissance grids established by pace and compass
method with 400-meter spaced lines and 200-meter spaced
sample intervals to cutline grids with 100-meter spaced
lines and 25 meter spaced sample intervals. Individual soil
samples were collected by digging pits by hand with a small
spade. Sampling targeted B horizon material but would
collect Ao horizon material if B horizon material was not
present. Samples were collected in kraft paper sampling
bags with folded tops. Samples numbers were written on
the sample bags and referenced by grid location and on
occasion grid coordinates were used as sample numbers.
While following up on airborne geophysical anomalies, all
field staff typically carried scintillometers and recorded
anomaly locations along reconnaissance or cutline grid
lines.
Lake water and lake bottom sediment samples were taken
at an approximate density of one sample per 0.8 km2.
Till, esker and outwash sediment samples were collected
on 400-meter intervals along 1600-meter spaced lines
using shovels to dig sampling pits that ranged in depth from
approximately 0.3-0.6 meters.
All streams were sampled on approximately 400 to 800
meter spacing and if a stream encountered a lake, samples
were collected at the entrance and outflow of the lake.
Boulding Lake Project
Surface work completed on the property occurred from
1978-2015 in semi-regularly spaced intervals including
1978-79, 1987-88, 1998-99, and 2006-2015.

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Infini Resources Limited

www.infiniresources.com.au

ABN 77 656 098 583

InfiniResources

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Infini To Acquire Major Footprint In Athabasca Basin

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Criteria JORC Code explanation Commentary
1978-1979: Prospecting traverses were carried out on
approximately 400-meter spaced traverses and recorded
scintillometer readings at regular intervals, granitoid
boulders with readings >1000 cps were sampled,
sandstone boulders with readings >100 cps were sampled.
Radon soil gas surveys were completed on 50 meter
intervals along the traverses by inserting the radon probe of
a Pylon Model RM 1003 Radon Detector approximately 40
cm into a hole in the soil and using five strokes of the
provided pump introduced the soil gas into the counting
chamber of the detector. A background reading followed by
three one-minute readings were recorded and after each
sample the probe was removed from the hole and the
system flushed with fresh air.
Helium surveys were completed on grids with line spacings
at either 400 or 800 meters apart and 100-meter sample
intervals along the lines. At each sampling site, barometric
pressure and the temperatures of the air and soil were
recorded and samples were stored in hermitically sealed
aluminum containers and analyzed at a commercial
laboratory where they were subjected to a period of
equilibration at a constant temperature after which two gas
samples were extracted from each container and stored in
Bistable gas samplers. The gaseous contents of one set of
these Bistables were analyzed employing a Chemical
Projects Limited helium analyzer. During each analysis, the
concentration of helium in the sample was compared with
that of standards which have helium concentrations of 5.20
+/- 0.03 and 8.30 +/- 0.05 ppm (by volume). The C1-C3
hydrocarbon concentration was also determined.
Stream sediment sampling was completed along 100-meter
intervals along one stream where sample material was
available.

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Infini Resources Limited

www.infiniresources.com.au

ABN 77 656 098 583

InfiniResources

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Criteria JORC Code explanation Commentary
1987-88: Lake sediment sampling was completed on
approximately 2-kilometer spaced intervals and down to
0.5-kilometer spaced intervals locally and collected via
helicopter in the summer or through the ice in the winter
using a Hornbrook tube sampler.
https://science.gc.ca/site/science/en/educational-
resources/history-geological-survey-canada-175-
objects/115-hornbrook-sampler-1972
1998-99: Boulder sampling was completed on 2-kilometer
spaced lines with 100-meter spaced sample spacing along
each line. At each site, a composite boulder sample was
collected by taking chips from approximately 10 boulders
found within several meters of each sample site from
angular boulders and to avoid basement-derived boulders
entirely. Sample analysis included Na2O to discriminate out
basement chips in samples. Field parameter site data
including sandstone versus basement proportion, size,
angularity of sampled boulders and relative density of
exposed boulders, as well as the number of boulders
sampled were recorded. Duplicate samples were collected
at 13 of 379 sample sites by collecting chips from twice as
many boulders and dividing them equally into two separate
bags. Blank or reference samples were not submitted with
the samples for analysis, but lab reference sample results
were reported.

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Infini Resources Limited

www.infiniresources.com.au

ABN 77 656 098 583

InfiniResources

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Criteria JORC Code explanation Commentary
2006-2015: Boulder sampling (2006-07) including sampling
Athabasca sandstone boulders on 200-meter intervals
along lines spaced 600 to 800 meters apart. Chips were
taken from 10 boulders at each site preferentially sampling
angular boulders and striving to avoid conglomerate or
basement sourced boulders. Site data collected included
GPS coordinates, landform, drift type, boulder density,
maximum and minimum boulder size, roundness,
percentage of basement boulders, date and sampler. Field
duplicates were taken for every 1 of 20 samples and two
reference standards were inserted for each batch
processed at the laboratory amounting to approximately
one reanalysis and two reference standards for every 30
samples.
Lake sediment samples (2006) were collected via float-
equipped helicopters using a Hornbrooke-type tube
sampler where samples were placed into plastic bags and
site details including GPS coordinate, sample depth,
sample description, colour, date and sampler were
recorded. A duplicate field sample was taken at every 12th
site from the 588-sample survey.

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Infini Resources Limited

www.infiniresources.com.au

ABN 77 656 098 583

InfiniResources

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Criteria JORC Code explanation Commentary
Soil sampling of B & C horizons (2011-12) was completed
on a primary grid with 500-meter spaced sample intervals
where individual sample site locations were obtained using
Garmin GPS equipment. Stainless steel shovels were used
to dig to depths ranging from 40-80 centimeters. A 1-
kilogram sample of soil was collected at each site from
each of the A1 (where present) and C soil horizons, and
from horizon B where A and C were unavailable. Sample
material was taken from the fresh surface of the side of the
hole and placed in double zipper Ziplock bags with
approximately half of each sample submitted for clay
separation and analysis and the remainder stored for
potential future analysis.
Vegetation and tree core samples (2011-12) were collected
on a secondary grid offset from the primary grid, with 500
meter spaced sample intervals where individual sample site
locations were obtained using Garmin GPS equipment.
Vegetation sampling collected twigs and needles jack pine
samples and twigs from black spruce samples. Samples
were taken from multiple limbs around the tree from the
outermost 8-10 inches providing a sample of approximately
10 years of the most recent growth of the trees using
stainless steel tree clippers and collected enough material
to fill a 7 x 12.5-inch polypropylene bag, or approximately
500 grams of sample. Preference was given to black
spruce trees over jack pine trees in the field due to the
higher elemental concentrations of important pathfinder
elements observed in the former.

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Infini Resources Limited

www.infiniresources.com.au

ABN 77 656 098 583

InfiniResources

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Criteria JORC Code explanation Commentary
Tree core samples (2011-12) were collected using a 35.56
cm x 5.15 mm tree bore sampler through the middle of the
tree on a north-south bearing and placed in plastic straws
and sealed with tape for storage and transport. Where
possible, samples were preferentially selected from tree-
ring intervals corresponding to ages between 1970-1985 to
minimize anthropogenic contamination from significant
mining in the Athabasca basin. Preference was given to
black spruce trees over jack pine trees in the field due to
the higher elemental concentrations of important pathfinder
elements observed in the former. Not all areas were
conducive to tree core collection due to large areas of
immature jack pine forest cover. The most mature trees
were sampled at each location and cored immature trees
near the base.
Historical reports mostly dating from the 1970s and 1980s
rarely present comprehensive information on the nature
and quality of sampling.
There is no information in the historical reports on any
measures taken to ensure sample representivity. Geiger
counters and scintillometers were used to record surface
radioactivity in counts per minute or counts per second
(referring to beta- and gamma rays respectively) and
generally do not require calibration.
Drilling Drill type (eg core, reverse circulation, open-hole hammer, Not applicable as no drilling undertaken.
techniques rotary air blast, auger, Bangka, sonic, etc) and details (eg
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).

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Infini Resources Limited

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ABN 77 656 098 583

InfiniResources

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Criteria JORC Code explanation Commentary
Drill sample Method of recording and assessing core and chip sample Not applicable as no drilling undertaken.
recovery recoveries and results assessed.
Measures taken to maximise sample recovery and ensure
the 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.
Logging Whether core and chip samples have been geologically and Not applicable as no drilling undertaken.
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.
Sub-sampling If core, whether cut or sawn and whether quarter, half or all Historical reports mostly dating from the 1970s and 1980s
techniques core taken. provide no details on the nature of core sampling.
and sample
preparation
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.

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ABN 77 656 098 583

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Criteria
JORC Code explanation
Commentary
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 (eg standards,
blanks, duplicates, external laboratory checks) and whether
acceptable levels of accuracy (ie lack of bias) and precision
have been established.
Reynolds Lake Project
Historical reports mostly dating from the 1970s and 1980s
rarely present substantive information on the method of
assaying
Boulding Lake Project
Historical reports mostly dating from the 1970s and 1980s
rarely present substantive information on the method of
assaying
Tinco Project
The magnetic survey was flown with calibrated industry
standard tools and equipment: Airborne Magnetometer –
Geometrics G-822A, Sensitivity of 0.005 nT Recordings
made at 10 Hz with a sensor noise of less than 0.02nT,
GPS - Omnistar DGPS sub 5m accuracy and Time-Domain
EM – Modified Emosquito II. Gamma Ray Spectrometer
System - Radiation Solutions RSX-5 Spectrometer and
detector package. 16 liters (4 crystals) downward-looking
crystal array and 4 liters (1 crystal) upward-looking crystal
monitored using Radiation Solutions Inc. RSX-5 256-
channel spectrometer. Sampling rate of 1 Hz. Used RSX-5
calculated stripping ratios. Attenuation coefficients were
calculated using a test flight.
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 exploration data is received and stored securely in
digital format in the Company’s database.
No external verification has been conducted on the
historical data to date however it will be in the coming
weeks.
No adjustments have been made to the raw assay data.

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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 as no drilling undertaken.
All location data for the Saskatchewan projects is in NAD83
UTM Zone 13N.
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.
Reynolds Lake Project
Rock chip samples randomly spaced according to available
outcrop.
Soil sampling was typically collected at 400 x 200 to 100 x
25-meter spaced intervals.
Lake water and lake sediment sampling were collected on
an approximate density of one sample per 0.8 km2.
Till, esker, and outwash sediment samples were collected
on 400-meter intervals along 1600-meter spaced lines.
Stream sediments were sampled on approximately 400-800
meter spacing where available, and at the inflow and
outflow of each lake.
Boulding Lake Project
Prospecting traverses were completed on traverses spaced
approximately 400 meters apart.
Radon soil gas surveys were completed on 50-meter
intervals along 400 meter spaced traverse lines.
Helium surveys were completed on grids with either 400- or
800-meter line spacing and 100-meter sample intervals
along the lines.
Stream sediment sampling was completed on 100-meter
intervals along the one stream that was sampled.
1987-1988 lake sediment sampling was completed on
approximately 2-kilometer spaced intervals where available.

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Criteria
JORC Code explanation
Commentary


Till boulder sampling was completed along 2-kilometer
spaced lines with 100-meter sample spacing along each
line in 1998-99 In 2006-07, till boulder sampling was
completed on 100 meter spaced intervals on lines spacing
that ranged from 600-800 meters.
2006 lake sediment sampling was completed on
approximately 1-kilometer spaced intervals.
2011-12 soil sampling, vegetation and tree core sampling
was completed on approximately 500-meter spaced
intervals.
Tinco Project
The geophysical survey flight design of 100m spacing is
considered appropriate for this early stage of greenfields
exploration.
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.
Reynolds Lake Project
Rock chip, lake water, and lake sediment data were
collected on random orientations due to the media being
sampled.
Grid lines on grids established for soil, till, esker, and
outwash sediment were usually oriented in a northwest-
southeast direction, so they traversed across any potential
northeast trending structures.
Boulding Lake Project

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Criteria
JORC Code explanation
Commentary
Prospecting, radon soil gas, helium, boulder, soil,
vegetation, and drill core samples were collected along
grids lines oriented in a northwest-southeast direction, so
they traversed across any potential northeast trending
structures.
Stream sediment and lake sediment data were collected on
random orientations due to the media being sampled.
Tinco Project
The geophysical survey flight lines were flown in a west-
northwest orientation which is considered appropriately
aligned perpendicular to currently interpreted geological
strike and known surface geochemical trends.
Sample
security

The measures taken to ensure sample security.
This is not known from historical data reports.
Audits or
reviews

The results of any audits or reviews of sampling techniques
and data.
None carried out to date.

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.
Reynolds Lake Project
The project is comprised of standard Saskatchewan mining
claims that confer upon the holder the right to explore the
land for minerals according to The Crown Minerals Act C-
50.2 Reg 27. The claims are owned by U Energy Metals
Limited, a wholly owned Canadian subsidiary of U Energy
Metals Pty Ltd.

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Criteria
JORC Code explanation
Commentary
The claims are not subject to any joint ventures,
partnerships, overriding royalties, native title interests,
historical sites, wilderness or national or provincial park or
environmental settings. First Nation consultation is a crown-
managed responsibility that operating companies
incorporate into their exploration programs. Operating
companies must comply with all provincial and federal
environmental regulations.
Claim List Reynolds Lake Project
Boulding Lake Project
Claim Number
Holder
Effective
Date
Good
Standing
Date
Disposition
MC00016423
U EnergyMetals Limited: 100.000%
20221118
20250616
Active
MC00016424
U EnergyMetals Limited: 100.000%
20221118
20250616
Active
MC00016425
U EnergyMetals Limited: 100.000%
20221118
20250616
Active
MC00016426
U EnergyMetals Limited: 100.000%
20221118
20250616
Active
MC00016427
U EnergyMetals Limited: 100.000%
20221118
20250616
Active
MC00016428
U EnergyMetals Limited: 100.000%
20221118
20250616
Active
MC00016429
U EnergyMetals Limited: 100.000%
20221118
20250616
Active
MC00016430
U EnergyMetals Limited: 100.000%
20221118
20250616
Active
MC00016431
U EnergyMetals Limited: 100.000%
20221118
20250616
Active
MC00016432
U EnergyMetals Limited: 100.000%
20221118
20250616
Active
MC00016433
U EnergyMetals Limited: 100.000%
20221118
20250616
Active
MC00016434
U EnergyMetals Limited: 100.000%
20221118
20250616
Active
MC00018042
U EnergyMetals Limited: 100.000%
20231213
20260313
Active
MC00018043
U EnergyMetals Limited: 100.000%
20231213
20260313
Active
MC00018044
U EnergyMetals Limited: 100.000%
20231213
20260313
Active
MC00018045
U EnergyMetals Limited: 100.000%
20231213
20260313
Active
MC00018046
U EnergyMetals Limited: 100.000%
20231213
20260313
Active
MC00018047
U EnergyMetals Limited: 100.000%
20231213
20260313
Active
MC00018048
U EnergyMetals Limited: 100.000%
20231213
20260313
Active

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Criteria
JORC Code explanation
Commentary
The project is comprised of standard Saskatchewan mining
claims that confer upon the holder the right to explore the
land for minerals according to The Crown Minerals Act C-
50.2 Reg 27. The claims are owned by U Energy Metals
Limited, a wholly owned Canadian subsidiary of U Energy
Metals Pty Ltd.
The claims are not subject to any joint ventures,
partnerships, overriding royalties, native title interests,
historical sites, wilderness or national or provincial park or
environmental settings. First Nation consultation is a crown-
managed responsibility that operating companies
incorporate into their exploration programs. Operating
companies must comply with all provincial and federal
environmental regulations.
Claim List Boulding Lake Project
Tinco Project
The project area comprises two claims: MC15793 and
MC17688 which are 100% owned by Infini Resources Ltd
through a Canadian subsidiary.

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Criteria
JORC Code explanation
Commentary
The claims are currently live and in good standing. The
company is not aware of any existing impediments which
may impact ongoing exploration and development activities
at the Project.
Exploration
done by other
parties

Acknowledgment and appraisal of exploration by other
parties.
Reynolds Lake Project
SMDI 1832 Fire Eye Lake Uranium Occurrence located
approximately 4 kilometers southwest of the property on the
north shore of Fire Eye Lake and 1.8 km southesat of the
Middle Lake Uranium Occurrences (SMDI 1710). The area
is underlain by cream to white quartz monzonite to granite
locally unconformably overlain by basal Wollaston Group
graphitic pelitic to semi-pelitic biotite gneiss with significant
intercalated meta-arkose, calc-sillicate, impure marble and
metadiorite horizons. Work completed between ca. 1969-
1978 reported high radioactivity (5-6 times background) that
was stripped to expose two narrow (0.6-0.9-meter-wide
discontinuous zones of anomalous uranium mineralization
within silicified sediments along the west side of a granite
ridge asssociatd with a conductive EM zone. Grab samples
returned values of 0.27%, 0.34%, 0.08% and 0.03% U3O8.
SMDI 1924 Evergeet Lake Trench No. 1 located
approximately 1.0-kilometer northeast of the property on a
trench located approximately 1 kilometer southeast of
Evergeet Lake. The area is underlain by northeast-trending
psammitic metasediments of the Wollaston Domain
crosscut by a series of north-trending faults. Work
completed between 1969-1979 reported a trench exposing
granitized sillimanite-bearing psammite with quartzite layers
and grab samples that reported a maximum of 0.18% U.

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Criteria JORC Code explanation Commentary
SMDI 1925 Hull Lake Trenches located approximately 800
meters east of the property and approximately 3 kilometers
west of the southwest corner of Hull Lake. The area is
underlain by sillimanite-bearing Wollaston Domain
psammites and highly granitized and remobilized biotite-
magnetite psammites, Hudsonian granitoid rocks and
interlayered pelite-quartzite psammite-calc-silicate rocks
cross by north-trending faults with sinistral offsets. Work
completed between 1969-1979 reported values assaying u
to 0.09% U from chip samples taken from a meta-arkose in
a trench in the region of anomalies 10-131, 10-132, and 10-
133.
64E-0008 - 1985 - SMDC-LACANA Geological Survey:
Prospecting, geological mapping - 15 areas Report, 13
maps by F W Gittings et al (Lacana) Analyses: Pt Pd Ni Cu
Ba Be K L Sr Ta (rock), whole rock (rock)
64E-0007 - 1979 -Marline Oil Corp Ground investigation of
28 anomalies Report, 244 pages, 9 compilation maps,
1:20000, by J H Adams (covering parts of 64-E-5 6 10 11
12 13 15, 74-H-8)
64E-0004 - 1978-79 - Marline Oil Corp Lake water and
sediment sampling Geochemical report, 54 maps, by C F
Gleeson Computer report, data listing by L Martin (covering
parts of 64-E-5 6 10 11 12 13 15)
64E04-0003 - 1966 - Don Fisher Syndicate
Reconnaissance E M survey Prospecting notes by D Fisher

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Criteria JORC Code explanation Commentary
64E05-0020 - 1969-70 - Husky Oil Ltd Airborne E M,
magnetic and radiometric survey by Questor and Geo-X
Bi 214, K, Th, & Bi/Th maps by Geo-X Airborne survey
evaluation by D M Leask Aeromagnetic interpretation by
Geoterrex Exploration and prospecting report, 12 maps by
D Fisher and Wollex 4 ddh records (# 1 to 4)
64E11-0004 - 1967 - Patridge, E F Prospecting notes by E
F Partridge Prospecting map (2 in = 1 mile): py po ma sp cp
hem asp gn mag 2 detail maps (1 in = 400 ft) (Cairns-Tighe
Lakes and Spense Lake) Geochemical survey by M R
Keys: Zn Assays: Au Ag Zn Pb Ni (grab samples)
NOTE: prospecting covers 150 square miles"
64E11-0011 - 1966 - Falconbridge Reconnaissance
geological and geochemical report, 5 maps by S Karup-
Moller: Blondeau River area
64E11-0010 - 1966 - Falconbridge Ground magnetic and I
P surveys by H D Maclean Geological report, 2 maps (1 in
= 400 ft) by C Coates: Blondeau River area NOTE: Work
done on Cairns Lake grid
64E11-0016 - 1969 - Great Plains Dev Co Can Ltd 5 ddh
records (#1 1A 2 to 4): py po cp mag Airborne radiometric
survey by Questor (U2 maps only contoured)
Report of ground anomaly check Assays: U3O8 (grab
samples) NOTE: formerly Great Plains Petroleum Permit 1"

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Criteria JORC Code explanation Commentary
64E14-0013 - 1970 - Mullin Lake Mines Ltd 5 ddh records:
py Assays: U3O8 Th Cu (core) Geological report by D A
Sawyer Report by R H Spooner (university seminar)
64E14-0010 - 1969 - Scurry Rainbow Oil Ltd Airborne E M,
magnetic and radiometric surveys by Seigel: 290 square
miles Exploration report by Trigg, Wollett and Assoc
Hydrogeochemical survey by Bondar-Clegg
64E15-0006 - 1969 - Scurry Rainbow Oil Ltd. Airborne
radiometric survey by Scurry Airborne E M and magnetic
survey by Sander Geophysics: 300 square miles
64E15-0009 - 1969-70 - Pathfinder Resources Ltd
Airborne E M, magnetic and radiometric survey by Seigel:
300 square miles Ground E M, magnetic, gravity and
radiometric survey by Seigel
64L-0005 - 1966 - Patridge, E F Prospecting notes and
sample records Maps 1 in = 1 mile: Pow Bay (map 1)
(Brandser Is-Heinz L (maps 2 and 3) Ooms L (map 4)
Charcoal L (map 5) (covering parts of 64-L-2 3 4 5 7 8 9 10
15 and 16 and 64-E-14 and 15) Assays: Au Ag Pb Zn Co
Mo Co (grab samples)
64L-0008 - 1976 - SMDC Airborne E M, magnetic and
radiometric survey by Questor Helicopterborne 'hound-
dogging' and ground follow-up Final report, 91 maps, by D
A Harrigan (covering most of 64L-1 2 7 8)

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Criteria
JORC Code explanation
Commentary
64L-0012 - 1977 - SMDC Lake sediment sampling,
hound-dogging and detailed geological mapping and
sampling (7 grids) Report, 110 maps, 7 appendices, by D A
Harrigan (covering parts of 64L-1, 2, 7, 8)
64L-0013 - 1978 - SMDC Lake sediment and overburden
sampling detailed work 5 grids Report, 121 maps, 13
appendices, by W L Murphy
64L-0017 - 1979 - SMDC Detail (Hull Lake) and regional
Wacker till sampling, anomaly rechecking, break-in-slope
sampling, routine exploration Report, 45 maps, by W L
Murphy Analyses U (boulders, tills, sediments, soils)
(covering most of 64-L-1 2 7 8)
64L-0018 - 1975 - Government of Saskatchewan Ground
evaluation of airborne radiometric anomalies (1973/74
Skyvan) Report, 26 figs, by R J C Munday including
compilation map 64L (Fig 1D) (covering 64L-1 2 7 8)
64LL02-0006 - 1974-75 - Rio Alto Exploration Ltd Airborne
anomaly evaluation Reports by R K Netolitzky and N Gass
Analyses: U3O8 Cu Pb Zn Ni Co Ag Mo (boulders)
Boulding Lake Project
MAW00736 - 2013-2014 - Areva Resources Canada Inc.
Geophysics: Squid Moving Loop TEM survey (28.3km, 6
lines, 3 grids: Parker East, Central and West, Patterson
Geophysics Inc). 1 CD, 9.38 MB, by R Hearst, C Cutts, P
Ledru

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Criteria JORC Code explanation Commentary
74I02-0040 - 1989 - Interuranium Canada Limited,
Cogema, Uranerz, CEGB ddh (# MJ-1, 2A, 3, 4): deviation
surveyed and radiometrically logged -MJ-1, 2 conductors
Core petrographic study, ground UTEM survey Report 3
maps, 4 lithologs by F Hopfengaertner H Quarch and F
Dalidowicz
74I02-0052 - 1996 - Cogema Resources Inc (Operator),
Uranerz Exploration and Mining, Cameco Ground
TDEM/UTEM survey Report, 1 map, 1 diskette by D
Bingham
74I02-0061 - 2000 - Cogema Resources Inc (Operator),
Uranerz Exploration and Mining, Cameco 1 ddh (# MJ-
13): gamma logged and deviation surveyed: ML00-1 grid
Core petrographic study Ground TDEM survey: ML00-1
grid Report, 1 map, 1 log, 1 disk by P Munholland, D
Bingham, C Madore, G Ostapovitch, I Ann
74I06-0012 - 2010 - Uravan Minerals Inc. Geological
Survey: Soil sampling (885 - B&C horizons);
Biogeochemcial sampling (1184-twigs, needles & tree core
samples)Collected on 500m spaced offset grids; Analyses:
multielements and Pb isotopes, 1 data stick, 100MB, by D
Griffiths
MAW00307 - 2011-2012 - Uravan Minerals Inc. Analyses:
358 soil samples collected from B and C horizons.
Analyses: 362 vegetation samples, 304 from pine and 58
from spruce tree twigs and needles. Analyses: 229 tree
core samples: 177 from pine, 13 from spruce and 39 from
burnt pine trees. Samples taken on 500m spaced virtual
grid with surveys overlapping.

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Criteria JORC Code explanation Commentary
74I03-0008 - 1998-1999 - Cogema Resources Inc
(Operator), Uranerz Exploration and Mining Ltd, Cameco,
PNC Exploration Canada, E&B Explorations Ltd. Ground
TDEM survey: C-14 grid: S-101503, S-104813, and S-
105692 Boulder and outcrop sampling: S-105690 to 692
Report, 1 map, 1 diskette by P Munholland, D Bingham, B
Polischuk, and S Earle Analyses: Al2O3 MgO
MAW00584 - 2014 - Denison Mines Corp. Geophysics:
Titan-24 pole-dipole DC/IP resistivity ground geophysical
survey (68.4 km (114 km with extensions), 2 grids, 19 lines
3.6 km long using 150 m dipoles at 400 m spacing; by
Quantec Geoscience. 1 CD, 2.37 GB, by A Carmichael
MAW01738 - 2015 - Uravan Minerals Inc. Geological
Survey: Prospecting, Sampling and SWIR. Analyses: 212
tree core (Jack Pine) for biogeochemistry; 321 sstn boulder
samples from glacial till; 349 soil samples from B2 or C
horizons on 250 m offset grid; and Study of lab comparison
of analytical results obtained
74G08-0057 - 2006 - Canalaska Ventures (come
Canalaska Uranium Ltd, 11/12/2006) Geological Survey:
Boulder and Lacustrine Sampling, 1 CD (58MB), by K
Schimann, S Lopatka, Analyses:Multi-element Spectral
analysis
74I02-0072 - 2005-2006 - Pitchstone Exploration Ltd.
Airborne magnetic survey Ground TDEM survey 1 CD ROM
(446MB) by Goldak Airborne Surveys, E Truman,S Coulson
MEIP: 1418

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Criteria JORC Code explanation Commentary
74I03-0011 - 2007 - Canalaska Uranium Inc Geological
Survey: Sampling (588 sandstone bldr, 35 lake sediment),
1CD 32.1MB, by F Shirmohammad, K Schimann, A
Alizadeh, Analyses: multielement
74I02-0073 - 2006 - Pitchstone Resources Ltd Geophysics:
Airborne magnetic gradiometer survey by Goldak
Geophysics: Ground TDEM (EM-37) moving loop survey:
Quantec 1 CD ROM, 69.3MB By S Publicover, S Coulson
74I06-0005 - 1979-80 - E & B Explorations Ltd. Gravity
profile over Pasfield Lake by Kenting Report, five figures
(bound in report) Gravity profile extension by Geoterrex
Report, profile by S Wardlaw"
74I03-0010 - 2007 - Canalaska Uranium Ltd Geophysics:
Ground Audio-Magnetotelluric (AMT) Soundings (405
stataions, 400m spacing, 33 profiles), 1CD (26.3MB), by
Geosystems Canada Inc
74I-0010 1978 - E & B Explorations Limited Geological
mapping, prospecting and recce geophysical and
geochemical sampling Exploration report, 17 maps by W E
Brereton and P G Schoch Analyses: U (Lake sediment,
stream H2O/silt) Note: MPP 1030 to MPP 1033
74I-0012 - 1979 - E & B Explorations Limited 6 ddh records
(# WC-79A, 79-1 to 79-5) Geological mapping, prospecting,
ground geophysics, stream/spring geochemistry, radon and
helium surveys Exploration report, 17 maps by R J Garber
and P W Mann 2 helium r

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Criteria JORC Code explanation Commentary
74I-0018 - 1979 - Seru Nucleaire (Canada) LimiteeAirborne
E M, magnetic and radiometric survey by Northway Report,
6 maps by A Duffy Lake sediment sampling report, 4 maps"
74I-0019 - 1980 - Seru Nucleaire (Canada) Limitee
Scintillometer prospecting and ground follow- up of
Northway anomalies Report, 5 maps by J Chevalier
(covering parts: 74-I-2 7 10 15)"
74I-0044 - 1986-87 - Interuranium Canada Ltee/Ltd Fixed
wing airborne Geotem E M and magnetic survey Ground
UTEM survey over 1 grid Analyses of remote sensing data
Report, 31 maps by F Hopfengaertner et al"
74I-0045 - 1989-90 - Interuranium Canada Limited, (JV:
Interruanium-Cogema-Uranerz-Cameco) 2 ddh (# MJ-5
and 6): on CBS 3670 Core petrography - 6 holes by L
Hubregtse Ground UTEM survey Report, 1 map, 2 logs by
F Hopfengaertner, H Quarch and F Dalidowicz Analyses:
multi-element clay (core)"
74I-0047 - 1987-88 - Interuranium Canada Limited
reconnaissance lake sediment sampling (samples x 18)
Ground UTEM survey, 3 grids Report, 3 maps by F
Hopfengaertner Analyses: Au Ag multi-element (silt)"

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Criteria
JORC Code explanation
Commentary Commentary Commentary Commentary Commentary Commentary Commentary Commentary Commentary Commentary
SDMI 2460 Drill holes MJ-3, MJ-7, MJ-8 located
approximately 1.6 kilometers southwest of the southwest tip
of the most westerly bay on Johnston Lake and
approximately 5.7 kilometers east of the Boulding Lake
project. The area is underlain by 603 meters of Athabasca
Group basin units MFb, MFc & MFd with the lowest 50
meters exhibiting bleaching, friability, and clay secondary
hematite in the sandstone matrix. Aphebian bedrock below
the unconformity consists of sulfide and graphite rich
metapelites that alternate with pegmatoid “sweat” rocks that
exhibit strong chloritization and minor hematization crosscut
by fracture-controlled pyrite-chalcopyrite+/-carbonate veins
in the first 15 meters below the unconformity. Both rock
groups are strongly fractured throughout. Work completed
between 1978-1996 in drill hole MJ-3 intersected
disseminated uranium oxide and minor pyrite, galena,
sphalerite, and chalcopyrite as fracture fillings within a
graphitic metapelite, with intersection highlights as follows:
DDH No From To Width Uppm Pbppm Nippm Coppm Cuppm Znppm
MJ-3 612.5 612.7 0.2 150 1800 67 10 416 444
612.7 613 0.3 70 433 76 12 101 21
618.5 618.7 0.2 490 632 103 25 22 12
618.7 619 0.3 4100 632 103 25 22 12
616.7 627 0.3 520 106 161 9 126 224
MJ-6 598.3 0 865 7 219 68 3 31
599.3 0 615 7 160 108 3 112
MJ-7 656 656.5 0.5 242 174 50000 18000 11 211
656.5 657 0.5 46 144 28100 18300 9 103
657 657.5 0.5 15 29 16000 15200 6 340
658.4 659 0.6 302 247 99600 43200 18 1001
MJ-8 581.4 581.9 0.5 1980 412 228 91 94 11
581.9 582.5 0.6 2140 771 284 144 352 59
SDMI 5336 Drill hole JL 10-22

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Criteria
JORC Code explanation
Commentary
Drill hole JL10-22 located approximately 6.56 kilometers
east of the Boulding Lake project was completed in a 2010
exploration program intersected 224 ppm U over 0.7 meters
from 617.6-618.3 meters in basal sandstone with minor clay
alteration above the unconformity at 623.5 meters.
SMDI 5710 Drill hole JL 13-32
Drill hole JL 13-32 located approximately 6.2 kilometers
east of the Boulding Lake project was completed in 2013
and intersected 228 ppm U over 0.3 meters from 2 meters
below the unconformity at 572.0 meters in vuggy,
moderately chloritized pelite; 310 ppm Co, 178 ppm Ni, and
204 ppm Pb over 0.1 meter from the lower contact of a
graphitic pelite with a large quartz vein at 636.3 meters with
associated hematite, sericite and pyrite alteration; and 182
ppm Co, 797 ppm Cu, 141 ppm Ni over 0.4 meters at 638.7
meters in fault breccia composed of graphite, pelite, pyrite
and quartz vein material.
Tinco Project
SMDI 1028 Tinco Lake Radioactive Pegmatite: located
immediately north of a small unnamed lake and 1.05km west
of the north end of Tineo Lake. The area is underlain by pink
granite to granodiorite composition felsic gneiss. Assays of
samples returned the following values:

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Criteria JORC Code explanation Commentary
SMDI 1029 – Airways Lake (east of) U-Th Occurrence
Trench: consists of anomalously radioactive areas outlined in
a 1970 airborne survey of the Airways Lake area. The
showing is located approximately 0.37 miles (0.6 km) west of
the Tineo Lake radioactive pegmatite, 0.65 miles (1.05 km)
northeast of the northwest tip of Keller Lake and 1.25 miles
(2.0 km) east of the east end of Airways Lake. The area is
underlain by a northeast-trending series of pink, felsic
gneisses of granitic to granodioritic composition. SMDI 1029
consists of a radioactive pegmatite and biotite granite
gneiss. The occurrence was trenched and returned a sample
assaying0.008% U3O8 and 0.51 % ThO2.
Geology Deposit type, geological setting and style of mineralisation. The targeted deposit types are unconformity and shear
zone style uranium deposits.
Drill hole A summary of all information material to the understanding Not applicable as no drilling undertaken.
Information of the exploration results including a tabulation of the
following information for all Material drill holes:
easting and northing of the drill hole collar

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Infini To Acquire Major Footprint In Athabasca Basin

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Criteria JORC Code explanation Commentary
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
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 In reporting Exploration Results, weighting averaging Not applicable as no drilling undertaken.
aggregation techniques, maximum and/or minimum grade truncations
methods (eg 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.
Relationship These relationships are particularly important in the Not applicable as no drilling undertaken.
between reporting of Exploration Results.
mineralisation
widths and
intercept
lengths

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’).

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Infini To Acquire Major Footprint In Athabasca Basin

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Criteria JORC Code explanation Commentary
Diagrams Appropriate maps and sections (with scales) and Not applicable. No significant discovery is being reported.
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.
Balanced Where comprehensive reporting of all Exploration Results Reporting of historical exploration results is considered
reporting is not practicable, representative reporting of both low and appropriate with their maximum uranium values clearly
high grades and/or widths should be practiced to avoid stated.
misleading reporting of Exploration Results.
Other Other exploration data, if meaningful and material, should No additional meaningful and material exploration data has
substantive be reported including (but not limited to): geological been excluded from this report.
exploration observations; geophysical survey results; geochemical
data survey results; bulk samples – size and method of
treatment; metallurgical test results; bulk density,
groundwater, geotechnical and rock characteristics;
potential deleterious or contaminating substances.
Further work The nature and scale of planned further work (eg tests for Review of Uranium targets within the Saskatchewan portfolio
lateral extensions or depth extensions or large-scale step- is ongoing, with key target areas considered for geophysical
out drilling). surveying, soil sampling, geological mapping and drill
Diagrams clearly highlighting the areas of possible testing.
extensions, including the main geological interpretations
and future drilling areas, provided this information is not
commercially sensitive.

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