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Protium Clean Energy Corp. to Arrange Satellite Gas Surveys in British Columbia

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Toronto, Ontario--(Newsfile Corp. - March 27, 2025) - Protium Clean Energy Corp. (CSE: GRUV) (FSE: G071) ("Protium or the "Company"), is pleased to announce that it intends to conduct regional satellite gas surveys over approximately 11,000 sq. kilometres in British Columbia. These surveys will enable Protium to develop the most effective exploration strategy and gain a deeper understanding of the region's prospectivity for hydrogen and other gases, as well as identify prospective areas for staking. Protium is looking to mirror its strategy used in Ontario expand its landholdings in British Columbia.

Central British Columbia exhibits strong geological potential for the discovery of natural hydrogen, also known as white hydrogen, supported by its unique geological history and recent hydrogen exploration activities, which are located some 300 and 550 kilometres southeast of the Cheslatta Claims.

In the survey area, potential for white/natural hydrogen exists in:

  1. The Cheslatta Lake Complex rocks in the survey area exhibit strong geological potential for hydrogen generation due to their mafic-ultramafic rock composition and structural features.

    • It includes olivine-phyric basalt, basanite, and diabase with ultramafic xenoliths. These rocks are rich in iron-magnesium silicates (olivine, pyroxene), which undergo serpentinization-a process where water reacts with minerals to produce hydrogen gas.

    • The region is intersected by deep-seated faults, such as the Pinchi Fault system, which act as pathways for water infiltration and hydrogen migration. Similar fault systems in nearby projects (e.g., Coquihalla H2) are actively explored for natural hydrogen.

  2. The Buck Creek basin is a structural rift basin located on the Nechako Plateau north of François Lake. It is characterized by a faulted depression filled with volcanic, pyroclastic, and sedimentary rocks ranging from the Cretaceous to the Paleogene periods. The basin's structure is controlled by northwest-southeast trending strike-slip faults associated with rifting during the Late Cretaceous to Early Oligocene periods.

The claims are spatially associated with a radial lineament of the Buck Creek Basin, and the geology aligns with global hydrogen generation models:

Ultramafic/Mafic Rock Presence

  • The basin hosts volcanic and intrusive rocks, including basalt and andesite, which are rich in iron and magnesium. These rocks are critical for serpentinization. Similar lithologies in the nearby Cache Creek Terrane (Cogburn Project) have already been identified as potential targets for hydrogen exploration.