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Holy Cross Mountains in the Caledonian, Variscan and Alpine cycles : major problems, open questions

Mizerski W.

Przegląd Geologiczny

2004

Vol. 52, nr 8/2

774-779

Composite tectonic structure of the Holy Cross Mountains originated as a result of multiple tectonic movements dating from Cambrian till Quaternary. The movements had different intensity in the northern (Łysogóry Block and southern (Kielce Block) parts of the area. The Caledonian and Variscan movements formed the fault-block structure with prevalent WNW–ESE directions, while the Alpine movements — disrupted the older units with transpressive slip translocations along already existing longitudinal faults. All the deformations occurred within an anorogenic area — a sinking, fragmented margin of the East European Platform.