Azincourt Energy Identifies Uranium Enrichment at the East Preston Project

Azincourt Energy Identifies Uranium Enrichment at the East Preston Project

AZINCOURT ENERGY CORP. ("Azincourt" or the "Company") (TSX.V: AAZ, OTCQB: AZURF) is pleased to present the analytical results from the Winter 2022 drill program at the East Preston uranium project, located in the western Athabasca Basin, Saskatchewan, Canada.

Drilling for the 2022 winter season at the East Preston Project resulted in 5,004.5 meters completed in 19 drill holes between January and March of 2022. Preliminary results of this program were reported in a news release dated March 29 th , 2022. Drilling during the 2022 program focused on the A-G and K-H-Q trends and commenced in the G-Zone where the 2021 drill program ended (Figure 3).

A total of 420 samples were collected throughout the program and sent to the Geoanalytical Laboratory at the Saskatchewan Research Council in Saskatoon, Saskatchewan for analysis. After unexpected delays at the lab, results were finally received by TerraLogic Exploration in late June and immediately underwent a thorough quality control assessment prior to being accepted.

"The analysis from drill core is encouraging," said VP, Exploration, Trevor Perkins. "The uranium enrichment within the alteration zones is a sign that uranium bearing fluids were present within the alteration system. We have the alteration system, and uranium moving around within it. The next step is identifying the areas of concentration within the system where significant uranium is dropping out," continued Mr. Perkins.

An analysis of the results shows uranium enrichment within the previously identified alteration zones along the G, K, and H target zones (Figure 2). Uranium enrichment is identified as uranium (U) values and a uranium/thorium ratio (U/Th) above what would normally be expected in the given rock type or area.

Along the northeast trending G-Zone, extensive hydrothermal alteration, and evidence of east-west cross-cutting structures were highlighted in holes EP0030 and EP0037. The primary rock types in the alteration zone are granodiorite and diorite gneiss with average expected values of 2-3 ppm U and U/Th ratios of 0.25-0.3. A sample from Hole EP0037 returned 14.6 ppm U and a U/Th ratio of 1.5, five times the expected values. A sample from EP0032 returned 19.5 ppm U and a U/Th ratio of 0.8.

The H-Zone covers a change in orientation of the structural and conductive trend from north south to southwest trending and contains a thick zone of hydrothermal alteration and an intense graphitic fault and mylonite zone. A sample from EP0041 retuned 12.5 ppm U and a 0.5 U/Th ratio within a mylonite in the fault zone.

Along the north-south trending K-Zone extensive zones of hydrothermal hematite have been intersected in all holes, with clay alteration also being present. A zone of localized elevated radioactivity more than 10 times background values was identified in EP0035 (Azincourt Energy news release dated March 1 st , 2022). The rock type in this zone is gabbro with average expected values of 0.5-1.5 ppm U and U/Th ratios of 0.25-0.5. A sample from this zone in EP0035 returned 5.4 ppm U and a 1.2 U/Th ratio.

The company considers sample analysis results to be an important indicator that uranium bearing fluids were present within the alteration systems identified. Continued testing of the alteration system to identify the extents of the alteration and areas of fluid concentration and strong uranium enrichment will be the aim of follow-up programs.

"The results of this drill program continue to support our exploration model at East Preston," said President and CEO, Alex Klenman. "The alteration zones are considerable in both size and scope. The results now confirm uranium is present within these alteration zones, which is a significant and critical step in the exploration process. We are eager to get the next round of drilling completed as the knowledge gained from this winter's program will aid immensely in vectoring toward areas of more significant mineralization," continued Mr. Klenman.

A thorough review and interpretation of the results of the winter 2022 program at East Preston is underway and preparation for an extensive follow up program in the winter of 2022-2023 is planned to continue evaluating alteration and structure on the G-, K-, and H-Zones as well as get a first look at the Q-Zone.

The Company is also planning to complete its first drill program at the 13,711-ha Hatchet Lake project, located along the Wollaston Domain on the northeastern side of the Athabasca Basin, in September and October of this year. This well known structural corridor hosts the majority of known high-grade uranium deposits and all of Canada's operating uranium mines. High-grade mineralization, up to 2.43% U308, has already been established at Hatchet Lake. Azincourt is earning up to 75% interest in the project as part of an earn-in agreement with ValOre Metals. The permitting and consultation process is in progress, and updates will be provided over the next several weeks.

"The next eight to ten months will be busy for Azincourt as we follow up at East Preston, and we also begin drilling at Hatchet Lake, which we plan to drill as early as this fall," said Mr. Klenman. "Despite the recent decline in overall market sentiment, we're in an excellent position. Our treasury is extremely strong, and we're fully funded to execute all of our exploration plans over the next year, and beyond. We're going to be very active and plan to be aggressive with the drills," continued Mr. Klenman.

Webinar Today

The Company will be conducting a live webinar, in conjunction with Red Cloud Securities, to discuss the drill results in more detail, today Wednesday, July 13, at 11am PST/2pm EST. We invite readers to register and attend, please follow this URL to participate:

https://redcloudfs.com/rcwebinar-aaz-3/

East Preston Target Areas

The primary target area on the East Preston Project is the conductive corridors from the A-Zone through to the G-Zone (A-G Trend) and the K-Zone through to the H and Q-Zones (K-H-Q Trend) (Figures 1 and 3). The selection of these trends is based on a compilation of results from the 2018 through 2020 ground-based EM and gravity surveys, property wide VTEM and magnetic surveys, and the 2019 through 2022 drill programs, the 2020 HLEM survey indicates multiple prospective conductors and structural complexity along these corridors.

Drilling programs to date have confirmed that identified geophysical conductors comprise structurally disrupted zones that are host to accumulations of graphite, sulphides, and carbonates. Hydrothermal alteration, anomalous radioactivity, and elevated uranium have been demonstrated to exist within these structurally disrupted conductor zones.

While the A-G and K-H-Q trends are the primary focus, many additional trends and zones exist to the east and west of the primary trends on the East Preston property (Figure 1). These additional target areas will require ground geophysics to constrain conductor locations and drilling to properly evaluate their potential.

Permitting and Community Engagement

The permitting process is underway to obtain authorization for the winter 2022-2023 drill program. Azincourt Energy continues to be engaged in regular meetings with the Clearwater River Dene Nation and other rights holders to ensure that concerns of the local communities are addressed. Azincourt looks forward to a continued close working relationship with CRDN and other rights holders to ensure that any potential impacts and concerns are addressed and that the communities can benefit from activities in the area through support of local business, employment opportunities, and sponsorship of select community programs and initiatives. Several members of the Clearwater River Dene Nation were directly employed on site or to provide support and services to keep the camp and program running.

https://www.globenewswire.com/NewsRoom/AttachmentNg/6f71eb63-ed77-4b29-a2c6-348ea24a15e3

Figure 1: Target corridors at the East Preston Uranium Project, Western Athabasca Basin Saskatchewan

https://www.globenewswire.com/NewsRoom/AttachmentNg/0aa363aa-2342-4a4b-97c5-0a20f3e7fae2

Figure 2: 2022 Drill Holes and Target areas at the East Preston Uranium Project

https://www.globenewswire.com/NewsRoom/AttachmentNg/0aef4a37-d9e6-48dc-97f6-771b890422ac

Figure 3: Project Location – Western Athabasca Basin, Saskatchewan, Canada

About East Preston

Azincourt controls a majority 72.8% interest in the 25,000+ hectare East Preston project as part of a joint venture agreement with Skyharbour Resources (TSX.V: SYH), and Dixie Gold. Three prospective conductive, low magnetic signature corridors have been discovered on the property. The three distinct corridors have a total strike length of over 25 km, each with multiple EM conductor trends identified. Ground prospecting and sampling work completed to date has identified outcrop, soil, biogeochemical and radon anomalies, which are key pathfinder elements for unconformity uranium deposit discovery.

The East Preston Project has multiple long linear conductors with flexural changes in orientation and offset breaks in the vicinity of interpreted fault lineaments – classic targets for basement-hosted unconformity uranium deposits. These are not just simple basement conductors; they are clearly upgraded/enhanced prospectivity targets because of the structural complexity.

The targets are basement-hosted unconformity related uranium deposits similar to NexGen's Arrow deposit and Cameco's Eagle Point mine. East Preston is near the southern edge of the western Athabasca Basin, where targets are in a near surface environment without Athabasca sandstone cover – therefore they are relatively shallow targets but can have great depth extent when discovered. The project ground is located along a parallel conductive trend between the PLS-Arrow trend and Cameco's Centennial deposit (Virgin River-Dufferin Lake trend).

Qualified Person

The technical information in this news release has been prepared in accordance with the Canadian regulatory requirements set out in National Instrument 43-101 and reviewed on behalf of the company by C. Trevor Perkins, P.Geo., Vice President, Exploration of Azincourt Energy, and a Qualified Person as defined by National Instrument 43-101.

About Azincourt Energy Corp.

Azincourt Energy is a Canadian-based resource company specializing in the strategic acquisition, exploration, and development of alternative energy/fuel projects, including uranium, lithium, and other critical clean energy elements. The Company is currently active at its joint venture East Preston uranium project in the Athabasca Basin, Saskatchewan, Canada, and the Escalera Group uranium-lithium project located on the Picotani Plateau in southeastern Peru.

ON BEHALF OF THE BOARD OF AZINCOURT ENERGY CORP.

"Alex Klenman"
Alex Klenman, President & CEO

Neither the 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.

This press release includes "forward-looking statements", including forecasts, estimates, expectations and objectives for future operations that are subject to a number of assumptions, risks and uncertainties, many of which are beyond the control of Azincourt. Investors are cautioned that any such statements are not guarantees of future performance and that actual results or developments may differ materially from those projected in the forward-looking statements. Such forward-looking information represents management's best judgment based on information currently available. No forward-looking statement can be guaranteed, and actual future results may vary materially.

For further information please contact:

Alex Klenman, President & CEO
Tel: 604-638-8063
info@azincourtenergy.com

Azincourt Energy Corp.
1430 – 800 West Pender Street
Vancouver, BC V6C 2V6
www.azincourtenergy.com


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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
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  • Drill hole HK24-010 intersected 13.4 metres of continuous radioactivity within a 200 m wide alteration system
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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.

Cannot view this image? Visit: https://images.newsfilecorp.com/files/6412/224182_480ec88df46cda96_001.jpg

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

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/6412/224182_480ec88df46cda96_001full.jpg

Cannot view this image? Visit: https://images.newsfilecorp.com/files/6412/224182_480ec88df46cda96_002.jpg

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

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/6412/224182_480ec88df46cda96_002full.jpg

Cannot view this image? Visit: https://images.newsfilecorp.com/files/6412/224182_480ec88df46cda96_005.jpg

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

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/6412/224182_480ec88df46cda96_005full.jpg

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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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https://images.newsfilecorp.com/files/6412/224182_480ec88df46cda96_007full.jpg

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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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https://images.newsfilecorp.com/files/6412/224182_480ec88df46cda96_020full.jpg

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

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