AUTHORS: Jadwiga Pieczonka, Adam Piestrzyński
ABSTRACT: Mineral zonation is discussed in both the scale of minerals and the scale of the deposit. Although zonation of ore minerals is very rarely observed, because of the low-temperature association, however some crystals show perfectly zoned structures that are also refect in their chemical composition. Mineral zonation at the deposit scale is visible in a central ore body composed of chalcocite that is surrounded by bornite with minor chalcopyrite and galena. Mineral zonation helps understand problems of mineral genesis.
KEYWORDS: Kupferschiefer, mineral zonation, SW Poland
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