3D STAVBA LOMŮ MOKRÁ (PŘEDBĚŽNÉ VÝSLEDKY)
Vol.11,(2004)
Abstract
Keywords:
Thrusting; folding; Moravian Karst
The limestones in Mokrá quarries (Moravian Karst) underwent complex folding and thrusting during the Variscan orogeny. Two systems of folds were recognised: the older one is oriented NNWSSE and refolded by a younger system of ENE–WSW direction. A precise stratigraphic research in combination with structural data made possible to interpret the 3D tectonics of the area as a large anticline plunging to the SE with the angle of 20°. The lower overturned branch of this anticline was ruptured and duplicated during thrusting in the end of folding. This structure was affected by several phases of brittle fracturing.
Thrusting; folding; Moravian Karst
References
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