Główne dyslokacje sudeckie i ich znaczenie w metalogenezie regionu dolnośląskiego

Abstract

PRINCIPAL SUDETIC FAULTS AND THEIR SIGNIFICANCE FOR THE METALLOGENY IN THE LOVER SILESIA AREA

Summary

Geological set-up of barite and fluorite mineralization in the Sudetes mountains is discussed in the present paper. Relationship exists between the mineralization and the main tectonic lines, and particularly with the Main Sudetic fault and another one for which the name “Parasudetic fault” is suggested. The latter parallels the Marginal Sudetic fault along the Stanisławów–Głuszyca –Kletno line.
The above faults provided sites favourable for igneous intrusions and formed avenues for migration of hydrothermal solutions. For both the same deep-seated magmatic centres mobilized by subsequent tectonic impulses might have been the source.