Uwagi o mineralizacji skał paleozoicznych w okolicy Krakowa

Authors

  • Stanisław Bukowy

Abstract

REMARKS ON MINERALIZATION OF PALAEOZOIC ROCKS IN REGION OF CRACOWIn the Jurassic and Cretaceous deposits building eastern slope of the Silesia-Cracow anticlinorium negligible traces of mineralization are well known (J. Morozewicz, 1909; A. Gaweł, 1949; S. Dźułyński, W. Żabiński, 1955; S. Bukowy, 1956). It may be assumed that this mineralization has been caused by descending solutions which mobilized mineral deposits in the substratum of the Jurassic.A feeble mineralization of the substratum of the Jurassic deposits has been ascertained at Bębło in the form of a pyrite-quartz vein (S. Bukowy, 1968), and at Karniowice in the form of metasomatic marcasites.

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Issue

Vol. 5 No. 2 (1961)

Section

Articles

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