Geological setting of the Silesian-Cracow Zn-Pb deposits

Ewa Górecka


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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