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The origin of stannite by replacement of cassiterite in the Turkaňk zone of the Kutná Hora ore deposit

Published online by Cambridge University Press:  14 March 2018

F. Novák
Affiliation:
Institute of Mineral Raw Materials of Kutná Hora
A. Blűml
Affiliation:
Laboratory of Geochemistry of Ore Mines, Příbram, Czechoslovakia
A. Tacl
Affiliation:
Laboratory of Geochemistry of Ore Mines, Příbram, Czechoslovakia

Summary

The trace-element assemblage of the cassiterite of the Turkaňk and Rejsy zones of the Kutná Hora mining district are typical of a hydrothermal sulphide-cassiterite formation. Polished section studies show replacement of cassiterite by pyrrhotine, with stannite as am intermediate zone.

Type
Research Article
Copyright
Copyright © 1962, The Mineralogical Society

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References

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