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
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
- Information
- Mineralogical magazine and journal of the Mineralogical Society , Volume 33 , Issue 259 , December 1962 , pp. 339 - 342
- Copyright
- Copyright © 1962, The Mineralogical Society
References
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