Azincourt Energy Begins Data Compilation at the Snegamook Uranium Project

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Azincourt Energy Corp.
Azincourt Energy Corp.

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VANCOUVER, British Columbia, Nov. 13, 2024 (GLOBE NEWSWIRE) -- AZINCOURT ENERGY CORP. (“Azincourt” or the “Company”) (TSX.V: AAZ, OTC: AZURF), is pleased to announce that it has begun historic data compilation on it’s recently acquired Snegamook uranium project, located in the Province of Newfoundland and Labrador.

The Project is strategically located to the southeast of Snegamook Lake within Labrador’s Central Mineral Belt and less than 1 km south of the Two Time Zone (Indicated and Inferred resource of 5.55 Mlb U3O8, June 2008)*, formerly held by Silver Spruce Resources Inc. as part of a larger land package, and consists of a mineral licence block comprised of 17 contiguous claims covering 423 hectares.

The Central Mineral Belt in Labrador also hosts Paladin Energy Limited’s recently acquired Michelin deposit (Measured and Indicated resource of 82.2Mlb U3O8).*   Uranium was first discovered in the Central Mineral Belt in 1951. Readers are cautioned that past results or discoveries on properties in proximity to the Project are not necessarily indicative of the presence of similar mineralization on the Project.

Exploration work conducted on the Project by Silver Spring Resources Inc. between 2006 and 2008 consisted of airborne radiometric and magnetic surveys, follow-up prospecting, lake sediment and soil sampling, radon gas surveys, geological mapping, trenching, and diamond drilling. The exact number of diamond drill holes completed within the current Project has not yet been verified.

Drilling to follow up a radon gas anomaly identified the “Snegamook Zone” uranium occurrence located 1.3 km along strike to the southeast of the Two Time Zone. 17 drill holes intersected a 20 to 50 m wide section of uranium bearing brecciated and altered monzodiorite with moderate to strong chlorite, hematite and carbonate alteration, the same geological setting as the Two Time Zone. The Snegamook Zone is located near several large-scale uranium discoveries including the Two Time, Moran, Kitts, and Jacques Lake deposits.

Four mineralized lenses were traced over a strike length of 300 meters and to a vertical depth of 200 meters. The lenses are shallow dipping (15 to 20 degrees west) and vary in width from five to 53 meters with values ranging from 225 to 771 ppm U3O8. Individual one meter sample values range from 50 to 1,110 ppm U3O8, with the widest section in drill hole SN-08-8 averaging 206 ppm U3O8 over 73 meters. Mineralization and related hydrothermal alteration appears to be structurally controlled within lineaments cross-cutting the host intrusive gneissic units. The zones appear to be disrupted to the south and down dip by steeply dipping fault structures that displace the basement gneiss but remain open to the north.