INTERPRETACE DEFORMACÍ SEDIMENTŮ KARPATSKÉ PŘEDHLUBNĚ NA KONTAKTU SE ZÓNOU PAVLOVSKO-WASCHBERSKOU (VNĚJŠÍ ZÁPADNÍ KARPATY)
Roč.17,č.1-2(2010)
The Pavlov-Waschberg Zone and its surroundings features complicated structure of Carpathian Foredeep sediments and overthrusted flysch nappes. After Neo-Alpine thrusting this contact was tectonically affected by sinistral transversal strike-slip faults (lateral ramps) to present large-scale en-echelon structure. The structure is well visible in Pavlov Hills, where cross cut large limestone plate into smaller “blocks”. The new research investigates transversal faults’ elongation to the Carpathian Foredeep where fold Karpatian and Lower Badenian sediments. Large geomorphological elevations “Přední and Zadní Dunajovický hřbet” are depicted as remnants of large-scale fault-propagation folds (past-Lower Badenian thrusting) in this text.
Carpathian foredeep; Badenian; Karpatian; fault-propagation fold; anticline; transversal fault; frontal and lateral ramp
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