The Coyote Springs property located in southeastern Arizona has excellent potential to discover a large tonnage Cu-Mo+Au porphyry target based upon an untested, strong IP anomaly and potassic alteration associated with pyrite-chalcopyrite mineralization within Laramide andesites and intrusives. The Coyote Springs property is situated at the favorable structural intersection of the northeast trending Morenci-Safford lineament and the west-northwest extension of the Safford porphyry copper and gold belt.
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