Fremont Announces Detailed Mapping and Additional Soil Geochemistry Results from Urasar Mineral District, Armenia

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Vancouver, British Columbia--(Newsfile Corp. - September 24, 2024) - Fremont Gold Ltd. (TSXV: FRE) (OTCQB: FRERF) (FSE: FR2) ("Fremont" or the "Company) is pleased to announce the results of detailed geological and structural mapping, as well as an expanded geochemical soil survey at the Company's Urasar Mineral District exploration permit in northern Armenia. This work underscores a major expansion in both the geological understanding and the mineral potential of the area.

Figure 1. Copper soil geochemistry at Urasar

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Recent Mapping Observations

The Company engaged senior consulting geologist L.J. Karr to conduct detailed geological mapping and surface rock chip sampling in mineralized zones within the Urasar District. Mr. Karr stated, "The 2024 fieldwork reveals that the mineralized system is larger than previously believed -- and our work has identified numerous high-quality drill targets indicative of both epithermal gold and porphyry copper-style mineralization."

Key Findings from the Mapping Efforts Include:

  • Yellow River Area: Hosts high sulfidation alteration extending over 4 km, characterized by vuggy silica, hydrothermally altered white clays, and mineralized veins. These features are consistent with an advanced argillic cap overlying a potential porphyry copper system. Alteration, geochemical, and magnetic data indicate the system's potential scale could be larger than initially thought. It includes the Copper Creek and Golden Vein prospects and hosts approximately 10 historic adits as well as a 1960 Soviet drill hole which bottomed in 25m @ 1.67% Cu (see Company news release dated March 1, 2024).

  • Black River Area: Identified as an epithermal precious metal system (high-sulfidation style) associated with dacite intrusives. Geophysical data and geochemical results suggest additional mineralization potential along strike, offering further exploration opportunities.

  • Brick House Zone: Located in the eastern part of the district, this area hosts gold and base metal soil anomalies as well as base metal sulfide mineralization observed in the creeks. It appears to be an intermediate-sulfidation epithermal vein system but the full the extent and characterization is yet to be determined. The ground mag data and particularly recent soil geochemistry results, indicate that this mineralized area could be much larger than previously assumed (See Figures 1 and 2).