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Eastfield Resources : Exploration Progress Report on Eastfield’s Base and Precious Metal Projects
Eastfield Resources : Exploration Progress Report on Eastfield’s Base and Precious Metal

About this update from Eastfield Resources Ltd.
March 24, 2026 View in PDF formatVancouver, BC- March 24, 2026 - Eastfield Resources Ltd. ("Eastfield" or the "Company") (TSX-V: ETF) provides an update on its copper, gold, and platinum group metal projects in British Columbia. Eastfield operates on a model where projects are acquired and subsequent option agreements with other companies for some projects derive both income and exploration leverage. Factors which make this viable, in addition to having projects that possess large deposit attributes, include acquiring large acreage tenures, keeping expiry dates well into the future and having the projects fully permitted. A summary of the more important 2026 projects, all of which are located in British Columbia, follows. Zymo: The 100% owned, 18,184 hectare, Zymo copper-gold porphyry project is located 45 km west of Smithers, British Columbia. The property is underlain by Hazelton, Bowser Lake and Skeena lithologies intruded by porphyritic diorite and granodiorite believed to be Creteceous in age. It was acquired in 2007 via an arms length option which was fully satisfied in 2012. In 2024 the claim group was expanded to cover additional airborne geophysical targets and an area underlain by the prospective Quock Group of the Hazelton Formation which is host to the world class Eskay Creek high-grade gold-silver mine. Since acquisition, the company has secured approximately $5 million in exploration expenditures for the project. Of major significance is the discovery of an 8 km long by 2 km wide strong induced polarization anomaly defining a copper-gold porphyry system containing several 1 km square targets with extensive areas having chargeability responses greater than 20 mv/V. Thirty-four drill holes (10,810 meters) have now been completed. Mineralization occurs in a porphyritic intrusive and adjacent sediments in zones of strong potassic alteration. Two of the more notable zones discovered to date are the Hobbes and FM Zones (five zones in total now discovered). Mineralization is surrounded by extensive areas of potassic, phyllic and argillic alteration that contain occurrences of quartz-sulfide and massive sulfide veins up to 1 m thickness suggesting that highly prospective potassic alteration likely occurs both latterly and at depth. Results to date include the following drill intercepts which are provided as examples of the copper-gold endowment: Hol...
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