American Future Fuel Acquires Prospective Red Basin Uranium Project

American Future Fuel Corporation
American Future Fuel Corporation

VANCOUVER, British Columbia, Sept. 27, 2022 (GLOBE NEWSWIRE) -- American Future Fuel Corporation (CSE: AMPS, Frankfurt: K14, WKN: A3DQFB, OTCQB: AFFCF) (the “Company”, or “American Future Fuel”) is pleased to announce that it has acquired (the “Acquisition”) the Red Basin Uranium Project (the “Project” or “Red Basin”) located in the Red Basin – Pie Town Mining District of Catron and McKinley counties of New Mexico. The Acquisition was completed pursuant to a definitive share purchase agreement (the “Purchase Agreement”), dated September 27, 2022, in which the Company acquired all of the outstanding share capital of 1344726 B.C. Ltd. (“1344726”), a privately held company which controls the Project.

Location and Geologic Environment
Red Basin is located approximately 90 kilometers (km) south of the Grants Mineral Belt and 21 km north of the town of Datil and is comprised of 400 lode claims containing a 7,320 acres land mass.

The Project is underlain by the southerly dipping Eocene Baca Formation and the Cretaceous Crevasse Formation. The Baca Formation is approximately 550 – 580m (1,800 – 1,900ft) thick and consists of sandstones, mudstones, and conglomerates. The Crevasse Canyon Formation is 335 – 520m (1,100 ‐1700ft) thick and consist of sandstones, shales, and coal.

A well‐developed paleosol is preserved at the boundary between the formations. Uranium is mainly associated with redox boundaries and organic material in both formations and particularly within the paleosol. The Cretaceous – Eocene sedimentary package is overlain by Oligocend Datil‐Mogollon volcanics comprised of rhyolite, andesite, and volcanoclastic rocks.

Geologic History
Late Cretaceous: deposition of the Crevasse Canyon Formation, primarily sandstones and shales. Folding and faulting during the Laramide Orogeny (Late Cretaceous).

Paleocene: development of a paleosol at the top of the Crevasse Canyon Formation and deposition of uranium at redox boundaries. The uranium was likely leached from shales and Late Cretaceous intrusions.

Eocene: flushing of uranium‐rich waters from the Mogollon uplift into the Baca Basin. Deposition of the Baca Formation and burial of the paleosol and Late Cretaceous uranium deposits. Deposition of the Mogollon‐Datil volcanic rocks, uplift and deposition of roll‐type deposits in the Baca Formation.

Existing Uranium Occurrence and Prospectivity
Uranium occurs in three different stratigraphic horizons on the Project: the Crevasse Canyon Formation, the Baca Formation, and the paleosol developed on and within the Crevasse Canyon Formation. The location of uranium occurrences were determined from radiometric anomalies defined with hand‐held gamma‐ray scintillometer (measured in counts per second, cps). Background gamma radiation of the Crevasse Canyon and Baca Formations typically range 30 – 50 cps (unweathered shales of the Crevasse Canyon Formation produced 60‐90 cps). The Oligocene volcanic rocks are also show elevated background gamma radiation. Intermediate volcanic breccias average 20 – 40 cps and rhyolitic tuffs can exhibit 60 – 100 cps.