Geological setting of the Silesian-Cracow Zn-Pb deposits

Authors

  • Ewa Górecka Polish Geological Institute, Rakowiecka 4, PL-00-975 Warszawa

Abstract

In the present paper, the position of the Silesian-Cracow Zn-Pb deposits, on the background of the geological structure of their host area, is discussed and shown on maps and cross-scctions. The connection of the are mineralizntion with disjunctive tectonics is evidenced. The Zn-Pb deposits distribution follows Variscan (and older) as well as Alpine tectonic patterns of that area.

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Published

2013-03-20

Issue

Vol. 37 No. 2 (1993)

Section

Articles

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