Copper-pyrite and pyrite base metal deposits of the Caucasian region.

Abstract

An analysis has been made of two pairs of pyrite-bearing structural-formational zones belonging to the Caucasian segment of the Mediterranean fold belt, which evolved during the Alpine tectono-magmatic cycle along the N and S of the Transcaucasian microcontinent. A clustering concentration pattern of basement mineralization has been revealed.-R.E.S.