Medinah Minerals (MDMN)

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The visible mineralization is predominantly pyrite with patches of replacement chalcopyrite in both the matrix and fragments of the breccia. Pyrite and associated chalcopyrite also occur as disseminations and veinlets in the propylitically altered granodiorite in the hanging wall and in the weakly brecciated horsts that occur between zones of strong hydrothermal breccia. Sulfide content ranges from 2 to 10% overall with narrow zones (veins) that are massive. ~It should be noted that high molybdenum values of up to 168 ppm Mo occur in the zone of highest copper which is a very favorable indication of a potential porphyry association with the breccia.~

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