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Location: 80 km NW from San Juanito, Chihuahua, Mexico
Carretera Chihuahua Hermosillo Km. 280 + 600, Sin NumeroChihuahua, Mexico33320
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The Ocampo district is a low-sulfidation system made up of several Ag-Au veins and stockworks. The local structures are dominated by two principal trends described by Byington and Bybee (2000). One consists of northwest trending faults, and another of a west-northwest coeval system; the latter is the NE which contains chiefly of north-trending structures intersected by NW-trending faults.
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