Author:
Novák F.,Blűml A.,Tacl A.
Abstract
SummaryThe 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.
Cited by
2 articles.
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