Copper Fox Provides Update on Eaglehead Copper Project

In This Article:

Calgary, Alberta--(Newsfile Corp. - May 4, 2022) - Copper Fox Metals Inc. (TSXV: CUU) (OTCQX: CPFXF) ("Copper Fox" or the "Company") through its wholly owned subsidiary Northern Fox Copper Inc. is pleased to provide an update on its 100% owned Eaglehead polymetallic porphyry copper project located approximately 50 kilometers ('km') east of Dease Lake, British Columbia. The Eaglehead project covers a large portion (15,712.9 ha) of the Lower Jurassic age, Eaglehead stock located within Quesnel terrane.

Highlights

  • Moose Mountain Technical Services ('MMTS') has been retained to review all data for the Eaglehead project including the proposed 2022 drilling program.

  • Logistics planning for the 2022 field program is progressing, the drilling and archeological contracts have been executed.

  • Approval of the Notice of Work ('NoW') filed with the BC Ministry of Mines is pending.

  • Age dating of the granodiorite and quartz diorite phases of the Eaglehead intrusive yielded comparable ages to other calc-alkalic porphyry copper systems in British Columbia.

  • Age dating of molybdenite indicates formation of the porphyry mineralization approximately 700,000 years after emplacement of the Eaglehead intrusive.

  • The first installment on the Promissory Note ($340,000), pursuant to the Eaglehead Property Acquisition Agreement, was made on April 19, 2022.

Elmer B. Stewart, President and CEO of Copper Fox stated, "Copper Fox is pleased to be working with MMTS as it continues to advance the Eaglehead project. Positive results from the 2022 drilling program, could indicate a continuous zone of mineralization exceeding 1.5kms in strike length and potentially lead to advancing the project to the resource estimation stage. The compilation work suggests the Thibert Fault system is the main structural control on emplacement of the large, near surface zones of porphyry copper mineralization and that future exploration should be focused on this area exploring for buried porphyry mineralization in a structural setting similar to that at the Red Chris deposit."

Exploration Model
The strong spatial alignment of the open-ended zones of porphyry mineralization and late stage felsic intrusives to the Thibert Fault system suggests that the Thibert Fault system exerted significant control on the emplacement of the late stage felsic intrusives and porphyry mineralization. The mineralization exposed on surface is interpreted to represent the upper level of a deep-seated porphyry system located along and controlled by the Thibert Fault system in a structural setting like that at the Red Chris deposit.


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