District Copper Adds More Claims to Copper Keg Project in British Columbia

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Vancouver, British Columbia--(Newsfile Corp. - June 12, 2024) - District Copper Corp. (TSXV: DCOP) ("District Copper", "District", or the "Company") is pleased to report that it has added 3 new claims to its highly prospective the Copper Keg project. The Copper Keg porphyry copper project is located approximately 55 kms west of Kamloops British Columbia. The property now covers approximately 6,628 ha, an increase of over 20% to the land holdings. The property is located at the north end of the Guichon Creek batholith which hosts Teck's Highland Valley Copper operations.

Two of the new claims cover extensions of the Guichon Creek Batholith across the Thompson River where multiple historic soil geochemistry anomalies occur. The third claim lies in the centre of the property.

The company is currently developing an exploration program for the upcoming field season.

Jevin Werbes, President and CEO of District Copper, commented, "We are pleased to have added these additional claims to the Copper Keg as these now give District Copper complete control over the porphyry target and the associated anomalies."

Acquisition Terms

  • $20,000 cash ($5,000 on signing, balance on TSX-V approval

  • 1,500,000 shares upon TSX-V approval

  • 2% NSR with 50% purchasable for $1,000,000

About the Copper Keg property

Historical exploration spans from the late 1800's to 2012. The early stage exploration is reported to consist of mining high grade copper veins.

The property exhibits the geochemical/alteration/lithologic features typical of the argillic altered potion of a porphyry copper system at/along the potassic/propylitic contact. The property is characterized by a large, pyrite bearing, argillic zone exposed along the surface trace of the Barnes Creek fault, a major NNW trending that crosses the Guichon Creek Batholith. The high-grade copper veins noted above, reflect supergene enrichment of distal base metal veins typically associated with a porphyry copper system.

Mapping has described pale grey-green (possibly phyllic alteration) outcrops of Guichon intrusive and late-stage Quartz Feldspar and Quartz Feldspar Hornblende dikes indicating multi-phase intrusive activity. The hydrothermal alteration is post Guichon intrusive and pre-dates the late-stage intrusive dikes.

The erratic and wide range of copper values (0.025 to 0.76%), in the gossanous (after pyrite), argillic altered zone, exhibit characteristics typical of a leach cap to a porphyry system.

The project is underlain by an intrusive phase of the Guichon Creek batholith intruded the surrounding Nicola Group rocks.