CanAlaska Uranium Announces Airborne Electromagnetic Survey Completed at Geikie Project in Athabasca Basin

CanAlaska Uranium Announces Airborne Electromagnetic Survey Completed at Geikie Project in Athabasca Basin

Multiple Priority Targets Associated with Regional Scale Fault Structures

Preparation Underway for First Drill Program

Drilling Continues at West McArthur JV and Key Extension Projects

CanAlaska Uranium Ltd. (TSXV: CVV) (OTCQX: CVVUF) (FSE: DH7N) ("CanAlaska" or the "Company") is pleased to announce completion of a high-resolution airborne Versatile Time Domain Electromagnetic ("VTEM Plus") survey on it's 60%-owned Geikie project in the Athabasca Basin (Figure 1). The purpose of the VTEM Plus survey was to identify basement conductors, characterize lithological and alteration variations, refine the structural setting, and prioritize drill targets for the Geikie project. Preliminary survey results confirm the objectives have been met, with multiple target areas identified that consist of conductive anomalies associated with regional-scale fault structures (Figure 2). The survey was completed by Geotech Ltd. of Aurora, Ontario and consisted of 1,399 line-kms of surveying at 400 m line spacing in the northern part and 200 m line spacing in the southern part of the property.

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Figure 1 – Geikie Project Location

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Preliminary VTEM Plus Survey Results

The complete preliminary VTEM Plus data for the Geikie project, which still requires full processing and levelling, has been received. The initial preliminary data highlights a series of priority target areas that require further detailed investigation and modelling (Figure 2).

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Figure 2 – Locations of VTEM Plus priority targets over Channel 10 VTEM data (left) and 2022 magnetic data (right).

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The primary target areas consist of a strong northeast trending conductor system, striking through the southern half of the property. A series of splays and offsets along this conductor are visible, often in correlation with intersections of regionally significant deep-seated north-south trending faults, interpreted to be part of the Tabbernor Fault System. In addition, historical drillholes completed on this conductor trend identified stratigraphically-controlled and structurally-enhanced graphite proximal to the main conductor. Graphite rich metasedimentary rocks are important hosts for basement-hosted uranium targets within and along the margins of the Athabasca Basin.

The secondary target areas include conductivity anomalies associated with prominent regional north-south trending faults, also interpreted to be part of the Tabbernor Fault System, that were previously delineated in the airborne magnetic and radiometric survey (see News Release dated October 18th, 2022). Recent discoveries near the Geikie project have spatial associations with north-south trending Tabbernor fault features. These deep-seated structural corridors may provide fluid conduits for the circulation of uranium-bearing fluids into the basement rocks. Uranium-bearing fluids penetrating conductive basement rocks provide a favourable depositional environment for basement-hosted uranium mineralization. Alteration associated with a mineralizing event may appear as a conductivity high along or in proximity to these north-south fault features.

NEXT STEPS

All preliminary data from the VTEM Plus survey has been received and final processed data is expected in Q2 2023. The Company will be undertaking subsequent modelling of the primary and secondary target areas that were identified, utilizing the final processed data, to generate a series of high priority drill targets. Basin Energy and the Company are currently evaluating the application of airborne gravity surveys as a way of mapping broader alteration associated with mineralizing processes and further refinement of priority drill targets.

Drill targets will be prioritized based on the stacking of geophysical and geological layers that have been collected on the project to date. These layers include airborne magnetics, radiometrics, and electromagnetics, in addition to geological prospecting and historical information compilation.

CanAlaska CEO, Cory Belyk, comments, "Results from this airborne survey are very encouraging with multiple priority targets identified for drill testing. The CanAlaska and Basin Energy teams have developed a solid and measured approach for target development to provide maximum value to our shareholders on future drill programs. Every layer of new information added to Geikie supports and emphasizes its growing discovery potential."

Geikie Project Overview

The Geikie Project is located just outside the eastern margin of the Athabasca Basin within the Wollaston Domain. The Project area has been subject to minimal exploration for uranium, with most significant work targeting base metals between 1967 and 1980. During this regional work, a series of mineralized showings were discovered in the Mud Lake and Marina areas. The Mud Lake uranium-molybdenum showing recorded a series of anomalous rock chips with grades of up to 0.225% U, 5.2% Mo, and 1.4% Cu. The Marina lead-zinc prospect recorded anomalous mineralization in outcrop of up to 2.03% Pb, 7.2% Zn and 0.93 oz/t Ag. Recent ground prospecting on the project has since confirmed the Mud Lake uranium-molybdenum showing results with up to 3,250 ppm molybdenum total and 0.21% uranium total in grab samples.

The primary target on the Geikie project is basement-hosted uranium mineralization where uranium bearing structures intersect favourable intercalated pelitic and calc-silicate host rocks. The Geikie project is located within 10 km of recent discoveries of basement-hosted uranium mineralization at the nearby Gemini Mineralized Zone and ACKIO.

The Geikie project is currently being sole-funded by Basin Energy Limited under an option earn-in agreement with the Company.

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.

In addition, the Company is drilling on its Key Extension project, located in the southeastern Athabasca Basin region near the Key Lake mine and mill complex. The 2023 Key Extension drill program is focused on exploration of newly defined targets generated through a series of geophysical programs completed in 2022.

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

The Company will be attending and presenting at the Resource Connect Asia "Future Facing Commodities" Conference from April 4th to 6th at the Raffles City Convention Centre, Singapore.

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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