Publication details

Analýza synkinematické mineralizace na Drahanské vrchovině

Title in English Analysis of Synkinematic Mineralization in the Drahany Highlands


Year of publication 2013
Type Article in Proceedings
Conference Závěrečná konference projektu PasGeo, Těžební unie, Brno
MU Faculty or unit

Faculty of Science

Field Geology and mineralogy
Keywords Moravian Paleozoicum;Drahany Upland;Lower Carboniferous;tectonic fault;paleostress;hydrothermal mineralization;Alpine paragenesis;zeolites;laumontite
Description Culm conglomerates in the quarry in Luleč are intersected by tectonic fault. Hydrothermal mineralization is formed on their planes. It is typ Alpine Paragenesis. The dominant compressed mode caused formation of reverse faults and overlying landscape began to shift in the direction of East. Quartz-calcite-laumontite mineralization were developed on the planes of the faults from low temperature hydrothermal solutions enriched with calcium. Laumontite is concentrated specially on granulite boulders. The form of mineralization demonstrates its synkimenatic formation which occurred at low pressure and low temperature during regional metamorphism at a depth of 3-4,8 km below the surface.
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