CanAlaska Drills Elevated Radioactivity at Key Extension Project

CanAlaska Drills Elevated Radioactivity at Key Extension Project

Multiple Graphitic Fault Structures with Hydrothermal Alteration Intersected

16 Kilometres of New Uranium Target Corridor Identified

Drilling Continues at West McArthur JV and Moon Lake South Projects

CanAlaska Uranium Ltd. (TSXV: CVV) (OTCQX: CVVUF) (FES: DH7N) ("CanAlaska" or the "Company") is pleased to announce successful completion of the 2023 drilling program at the Key Extension project (Figure 1). The program focused on initial drill testing of newly defined targets generated through a series of geophysical programs completed in 2022. The Company reports the objectives of the program were met, identifying multiple graphitic packages with large reactivated and brecciated fault zones, associated hydrothermal alteration, and elevated radioactivity.

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Figure 1 – Key Extension Project Location

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The Key Extension project is located approximately 10 kilometres southwest of the Key Lake uranium mine and mill near Highway 914. The 2023 drill program consisted of 2,239 metres in seven drill holes. This program represents CanAlaska's first drill holes on the Key Extension project and significant results were received in three main target areas (Figure 2).

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Figure 2 – 2023 Drill Program Target Areas and Results

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Target Area 1, three drill holes were completed, focusing on a large gravity low where the Key Lake fault is interpreted to intersect a conductive package that marks the Wollaston-Mudjatik domain boundary. Drill holes in target area one intersected features commonly associated with basement-hosted uranium deposits, which include the presence of 20 - 40 metre wide stacked graphitic packages containing multiple metre to sub-metre scale semi-brittle fault zones. The semi-brittle fault zones are characterized by graphite-rich clay gouges and breccias associated with hydrothermal chlorite, clay, silicification, and secondary hematite alteration in the structures and surrounding wall rocks (Figure 3). In addition, drill hole KEY010, the last hole completed in the area, intersected a narrow interval of elevated radioactivity over 30 centimetres, ranging from 100 to 320 cps (scintillometer CT007M) from 243.0 to 243.3 metres (Figure 3). The elevated radioactivity is hosted in a sheared limonite, chlorite, and clay altered granite immediately below the faulted and altered graphitic package.

Target Area 2 focused on testing the extension of Target Area 1 along the interpreted Wollaston-Mudjatik domain boundary. Drill hole KEY012 intersected a 30 metre wide graphitic package with several one to three metre wide semi-brittle fault zones. The fault zones, characterized by clay-rich fault gouge, are associated with hydrothermal chlorite and secondary hematite alteration in the structures and the surrounding wall rocks. KEY012 was approximately 2.6 kilometres along strike to the north of Target Area 1 and represents the second location along the main Wollaston-Mudjatik domain boundary on the project where graphitic host rocks were intersected in association with structures and hydrothermal alteration.

Target Area 3, two drill holes were completed and focused on a gravity low anomaly and electromagnetic conductor along the interpreted Key Lake fault. Drill hole KEY011 collared immediately into a 30 metre wide graphitic package which contained localized shearing and brecciation. Alteration within the graphitic package consisted of weak hydrothermal chlorite and clay associated with the fault. Based on the results of KEY011, it is interpreted the drill hole intersected the edge of the graphitic package, likely overshooting the Key Lake fault. No large-scale structure was intersected in Target Area 3, however given the interpreted thickness of the graphitic package and the localized faulting intersected near the base, the Company believes the main target exists immediately southeast of KEY011.

The 2023 drilling program successfully intersected graphitic host rocks showing evidence of multiple post-Athabasca structural reactivation events, hydrothermal alteration, and elevated radioactivity. These features are commonly associated with basement-hosted uranium deposits. Results of this inaugural drill program indicate evidence for likely uranium-bearing hydrothermal fluids moving through the basement rocks on the Key Extension project. Beyond follow-up of the significant early results from Target Area 1, the Company believes more than 16 kilometres of untested target corridor have now been identified as high priority for further drill testing.

Geochemical assay results for the 2023 winter drilling program are pending.

CanAlaska CEO, Cory Belyk, comments, "I am very pleased with the outcome of this drill program. The first drill holes completed on Key Extension have intersected all the indicators of uranium mineralizing processes the team would have hoped to observe including large fault structures, diagnostic hydrothermal alteration and uranium enrichment. This is a very significant outcome and has the geologists encouraged they are on the right track to discovery. Key Extension is very well positioned near the Key Lake mill complex and associated infrastructure in an area of the eastern Athabasca Basin that needs to identify the next Tier 1 uranium deposit to supply clean carbon-free energy to the world."

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Figure 3 – Select Core Photographs For Target Area 1

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Table 1 - 2023 Winter Drill Hole Collar Summary

Drill HoleTarget AreaEasting NorthingElevation (m A.S.L.)Azimuth (˚)Dip (˚)EOH (m)
KEY006N/A44347663343925500-90164
KEY007Area 14415266331311525290-60392
KEY008Area 14416536331682530295-60416
KEY009Area 34432846332857531310-70305
KEY010Area 14413656331764530310-65323
KEY011Area 34441576333417568310-70266
KEY012Area 24421306334298519290-60275
Notes: Easting and Northing coordinates are reported in UTM Zone 13N (NAD83 datum). EOH = end of hole.
m A.S.L. = metres above sea level.

 

All reported depths and intervals are drill hole depths and intervals, unless otherwise noted, and do not represent true thicknesses, which have yet to be determined.

Geochemical Sampling Procedures

All drill core samples from the 2023 program have been received by the Saskatchewan Research Council Geoanalytical Laboratories (SRC) in Saskatoon, Saskatchewan. The samples were shipped in secure containment for preparation, processing, and multi-element analysis by ICP-MS and ICP-OES using total (HF:NHO3:HClO4) and partial digestion (HNO3:HCl), boron by fusion, and U3O8 wt% assay by ICP-OES using higher grade standards. Radiometric assay samples are chosen based on downhole probing radiometric equivalent uranium grades and scintillometer (SPP2 or CT007-M) peaks. Assay samples comprise 0.3 - 0.5 metre continuous split-core samples over the mineralized interval. A 0.1% U3O8 cut-off with a maximum internal dilution of 1 metre is used for compositing and reporting the data. The SRC is an ISO/IEC 17025/2005 and Standards Council of Canada certified analytical laboratory. Blanks, standard reference materials, and repeats are inserted into the sample stream at regular intervals by CanAlaska and the SRC in accordance with CanAlaska's quality assurance / quality control (QA/QC) procedures. Geochemical assay data are subject to verification procedures by qualified persons employed by CanAlaska prior to disclosure.

About the Key Extension Project

The Key Extension project is located approximately 10 kilometres south of the Athabasca Basin edge, within the highly prospective Wollaston-Mudjatik Transition Zone. The Key Lake uranium deposits and associated uranium zones are located approximately 10 kilometres from the northeastern project boundary. The Key Lake deposits consisted of a series of east-northeast striking pods of high-grade unconformity associated uranium mineralization, which have historically produced over 150 million lbs U3O8 from the Gaertner and Deilmann open pits. The Company is completing work on the Key Extension project under an option agreement with Durama Enterprises Limited ("Durama"), a private company, which has granted CanAlaska a right to earn up to 100% interest in the project.

Other News

The Company is drilling on its West McArthur project in the eastern Athabasca Basin. The 2023 West McArthur drill program is focused on advancing the Company's new high-grade Pike Zone uranium discovery.

The Company's Joint Venture partner, Denison Mines Corp., is drilling on the Company's 25%-owned Moon Lake South project in the eastern Athabasca Basin.

About CanAlaska Uranium

CanAlaska Uranium Ltd. (TSXV: CVV) (OTCQX: CVVUF) (FSE: DH7N) holds interests in approximately 300,000 hectares (750,000 acres), in Canada's Athabasca Basin - the "Saudi Arabia of Uranium." CanAlaska's strategic holdings have attracted major international mining companies. CanAlaska is currently working with Cameco and Denison at two of the Company's properties in the Eastern Athabasca Basin. CanAlaska is a project generator positioned for discovery success in the world's richest uranium district. The Company also holds properties prospective for nickel, copper, gold and diamonds. For further information visit www.canalaska.com.

The qualified technical person for this news release is Nathan Bridge, MSc., P.Geo., CanAlaska's Vice President, Exploration.

On behalf of the Board of Directors
"Cory Belyk"
Cory Belyk, P.Geo., FGC
CEO, Executive Vice President and Director
CanAlaska Uranium Ltd.

Contacts:

Cory Belyk, Executive VP and CEO
Tel: +1.604.688.3211 x 306
Email: cbelyk@canalaska.com

General Enquiry
Tel: +1.604.688.3211
Email: info@canalaska.com

Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.

Forward-looking information

All statements included in this press release that address activities, events or developments that the Company expects, believes or anticipates will or may occur in the future are forward-looking statements. These forward-looking statements involve numerous assumptions made by the Company based on its experience, perception of historical trends, current conditions, expected future developments and other factors it believes are appropriate in the circumstances. In addition, these statements involve substantial known and unknown risks and uncertainties that contribute to the possibility that the predictions, forecasts, projections and other forward-looking statements will prove inaccurate, certain of which are beyond the Company's control. Readers should not place undue reliance on forward-looking statements. Except as required by law, the Company does not intend to revise or update these forward-looking statements after the date hereof or revise them to reflect the occurrence of future unanticipated events.

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  • Five drill holes outlined an open massive hydrothermal clay alteration system measuring at least 200 m x 100 m, resembling alteration found in Athabasca high-grade uranium deposits
  • Radioactivity within the clay alteration system increases with depth and remains open
  • Drill hole HK24-010 intersected 13.4 metres of continuous radioactivity within a 200 m wide alteration system
  • New defined target areas are within 6 km of near-surface ACKIO uranium prospect

Baselode Energy Corp. (TSXV: FIND) (OTCQB: BSENF) ("Baselode" or the "Company") is pleased to provide results and findings from the exploration and discovery portion of the drill program on Hook project ("Hook") in the Athabasca Basin area of northern Saskatchewan.

"These results represent an important discovery on our Hook project. While we've already made a discovery at Hook with ACKIO, this is only a small part of the broader Hook land package. The potential on the property is substantial as Hook is an extensive project, and our discovery at ACKIO, combined with our neighbour Atha Energy's discovery in their Gemini Mineralized Zone, highlights that the region has all the geological features needed to host significant uranium deposits. More importantly, we can clearly demonstrate that this area is fertile with uranium mineralization. Large-scale alteration systems are key indicators when it comes to uranium, which tends to occur in smaller deposits relative to other minerals. We're pleased to have uncovered such a large system, exhibiting all the hallmark features needed for a new high-grade Athabasca uranium discovery," commented James Sykes, CEO, President, and Director of Baselode.

Watch this video for a detailed analysis of the two follow-up target areas and a comparison of Hook alteration systems to seven Athabasca high-grade uranium deposits that have combined over 700 million pounds of uranium.

The first alteration system the Company highlights is in the HK24-016 area, measuring more than 250 metres wide by 400 metres deep, with a core of massive clay and bleached alteration styles that measure 100 metres wide by at least 200 metres deep. These core alteration styles are important as they are the same style associated with at least three basement-hosted Athabasca high-grade uranium deposits.

The second alteration system identified in the HK24-010 area is significant due to its similarly large scale, intersecting 13 meters of continuous anomalous radioactivity within pegmatite along the margin of the fluid pathway. While assays are pending, the Company is well-funded and eager to proceed with follow-up drill plans for these high-priority exploration targets.

Hook Exploration Drill Hole Highlights

HK24-016 area

Drill holes HK24-016, HK24-017, and HK24-021 to HK24-023 were collared 5.5 kilometres southwest of ACKIO (Figure 2, Figure 3). HK24-016 intersected 140 metres of massive hydrothermal clay and bleaching alteration (the "clay alteration") within a broader 370 m thick alteration corridor (Figure 4). The drill hole intersected anomalous radioactivity associated with fracture-controlled remobilized hematite alteration within the clay alteration (Figure 5).

Both HK24-017 and HK24-021 targeted the clay alteration up-dip and down-dip, with each intersecting 30 and 145 metres of clay alteration, respectively. HK24-022 was collared 100 metres southeast of HK24-016 and intersected 60 metres of clay alteration, and HK24-023 was collared 50 metres northeast and intersected 110 metres of clay alteration. Initial observations suggests follow-up drilling is required beneath HK24-021 and to the north of HK24-023.

The clay alteration encountered within these Hook drill holes (Figure 6) share numerous similarities to massive hydrothermal clay alteration systems observed in Athabasca basement-hosted, high-grade uranium systems, such as Cameco's Millennium and Eagle Point deposits, Uranium Energy Corp's Roughrider deposits, and Denison Mines' Gryphon deposit.

The upper outer halo of the clay alteration is further identified with unique limonite liesegang banding and fracture-controlled alteration, including a distinct quartz stockwork. These are also similar outer halo alteration styles that have been observed within large-scale Athabasca uranium deposits.

HK24-010 area

Drill holes HK24-009 and HK24-010 were collared 6 kilometres northeast of ACKIO (see Figure 2, Figure 7). Details of these drill holes were initially released on July 17, 2024. HK24-010 has returned the best radioactive intersection outside of Baselode's near-surface ACKIO uranium prospect with 13.2 metres of continuous anomalous radioactivity starting at 186 metres beneath the surface hosted within a pegmatite along the western margin of a 200 m-wide, structurally-controlled, hematite and bleached alteration system. The area remains open in all directions.

Drill hole samples have been sent to Saskatchewan Research Council for uranium and multi-element analysis. Results will be released after being received and reviewed by the Company.

NOTES:

  1. cps* = "counts-per-second", as measured with a handheld RS-125 Gamma-Ray Spectrometer/Scintillometer ("RS-125"). The reader is cautioned that Baselode uses scintillometer readings as a preliminary indication for the presence of radioactive materials (uranium, thorium and/or potassium), and that scintillometer results may not be used directly to quantify or qualify uranium concentrations of the rock samples measured.
  2. The Company defines groupings of RS-125 as i) background radioactivity (50 to 200 cps), ii) above-background radioactivity (200 to 300 cps), and iii) anomalous radioactivity (300 to 1,000 cps).
  3. "Radioactivity (>300 cps)" in Table 1 is defined as drill core length with no greater than 2.0 m of consecutive drill hole length measuring less than 300 cps.
  4. All reported drill hole depths and lengths do not represent true thicknesses.

About Baselode Energy Corp.

Baselode controls 100% of approximately 238,930 hectares for exploration in the Athabasca Basin area of northern Saskatchewan, Canada. The land package is free of any option agreements or underlying royalties.

The Company discovered the ACKIO near-surface, uranium prospect in September 2021. ACKIO measures greater than 375 m along strike, greater than 150 m wide, comprised of at least 9 separate uranium Pods, with mineralization starting as shallow as 28 m and 32 m beneath the surface in Pods 1 and 7, respectively, and down to approximately 300 m depth beneath the surface with the bulk of mineralization occurring in the upper 120 m. ACKIO remains open at depth, and to the north, south and east.

Baselode's Athabasca 2.0 exploration thesis focuses on discovering near-surface, basement-hosted, high-grade uranium orebodies outside the Athabasca Basin. The exploration thesis is further complemented by the Company's preferred use of innovative and well-understood geophysical methods to map deep structural controls to identify shallow targets for diamond drilling.

QP Statement

The technical information contained in this news release has been reviewed and approved by Cameron MacKay, P.Geo., Vice-President, Exploration & Development for Baselode Energy Corp., who is considered to be a Qualified Person as defined in "National Instrument 43-101, Standards of Disclosure for Mineral Projects."

For further information, please contact:

James Sykes, CEO, President and Director
Baselode Energy Corp.
jsykes@oregroup.ca
306-221-8717
www.baselode.com

Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the TSX Venture Exchange policies) accepts responsibility for the adequacy or accuracy of this release.

Certain information in this press release may contain forward-looking statements. This information is based on current expectations that are subject to significant risks and uncertainties that are difficult to predict. Actual results might differ materially from results suggested in any forward-looking statements. Baselode Energy Corp. assumes no obligation to update the forward-looking statements, or to update the reasons why actual results could differ from those reflected in the forward looking-statements unless and until required by securities laws applicable to Baselode Energy Corp. Additional information identifying risks and uncertainties is contained in the Company's filings with Canadian securities regulators, which filings are available under Baselode Energy Corp. profile at www.sedarplus.ca.

This news release does not constitute an offer to sell or a solicitation of an offer to buy any of the securities in the United States. The securities have not been and will not be registered under the United States Securities Act of 1933, as amended (the "U.S. Securities Act") or any state securities laws and may not be offered or sold within the United States or to, or for the account or benefit of, U.S. Persons unless registered under the U.S. Securities Act and applicable state securities laws, unless an exemption from such registration is available.

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FIGURE 1 - Baselode projects location map. ACKIO uranium prospect identified with yellow circle.

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FIGURE 2 - Drill holes (HK24-009 to HK24-023) location map

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FIGURE 3 - HK24-016 target area drill holes (HK24-016, HK24-017, and HK24-021 to HK24-023) location map

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FIGURE 4 - Cross-section interpretation of large hydrothermal fluid system with core massive clay and bleaching alteration (blue)

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FIGURE 5 - Fracture-controlled, hydrothermal remobilized anomalous radioactivity, HK24-016

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FIGURE 6 - Massive clay and bleaching alteration system, HK24-021. NOTE: clay has been gouged with carbon scribe to demonstrate drill core softness

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FIGURE 7 - HK24-010 target area drill holes (HK24-009 and HK24-010) location map

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MOVIE 1 - Clay alteration and bleaching identified within drill hole HK24-021

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