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Ore minerals from the dolomitic veins in the serpentinite rocks of the Letovice crystalline complex (Czech Republic)

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FOJT Bohuslav DOBEŠ Pavel MALÝ Karel ŠKODA Radek

Rok publikování 2008
Druh Článek v odborném periodiku
Časopis / Zdroj Mineralogia Polonica - Special Papers
Fakulta / Pracoviště MU

Přírodovědecká fakulta

Citace
Obor Geologie a mineralogie
Klíčová slova bornite; chalcocite; covellite; millerite; parkerite; wittichenite; Letovice; Czech Republic
Popis Minerals found in dolomite veins cutting serpentine rocks around Letovice and its surroundings composed remarkably heterogeneous set which is different from any other locality in the Bohemian Massif. The composition of copper minerals (bornite, chalcocite, covellite, chalcopyrite), millerite, dolomite veins and magnetite is similar to the composition of their host ultrabasic rocks. Lead and bismuth (galena, native Bi) are considered in this environment as atypical. Parkerite and wittichenite are transitional - they consist of elements of both groups.

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