A Note on the Chemical Composition of Nuffieldite Solid-Solution From Sulphide Mineralizations in the Western Carpathians, Slovakia

Jaroslav Prşek 1 , Emil Makovicy 2 , Martin Chovan 1  and Alexander Smirnov 3
  • 1 Department of Mineralogy and Petrology, Comenius University, Mlynská dolina 842 15, Bratislava, Slovakia
  • 2 Department of Mineralogy, Geological Institute, University of Copenhagen, øster Voldgade 10, DK-1350 Copenhagen K, Denmark
  • 3 Department of Geosciences, State University of New York, Stony Brook, NY 11794-2100, USA

A Note on the Chemical Composition of Nuffieldite Solid-Solution From Sulphide Mineralizations in the Western Carpathians, Slovakia

The chemistry of the rare sulphosalt nuffieldite from three localities in Slovakia is examined. Nuffieldite is a part of a complex association of Bi sulphosalts accompanying tetrahedrite mineralization in some sulphide deposits in the Western Carpathians. Cu + Pb = (Bi, Sb) + vac. substitution in nuffieldite and the general formula Cu1+xPb2Bi2(PbxSbyBi1-x-y)S7 where 0 < x < 0.34; and 0.32 < y < 0.45 are confirmed. Decreasing Sb content with increasing copper content indicates a predominant substitution of Bi by Sb in nuffieldite.

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