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Pattern of the Mesoscopic Thrust Faults in the Central Part of the Silesian Nappe (Polish Western Outer Carpathians)
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Geolines
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January 1, 2005
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Copyright informationCopyright Institute of Geology 2005. Provided by ProQuest LLC. (Hide copyright information)
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Polish Western Outer Carpathians is a north-verging fold-and-thrust belt. The belt is mainly composed of Lower Cretaceous to Lower Miocene flysch sediments (Ksia_zkiewicz 1977). The Outer Carpathians comprise several nappes. One of those nappes, the Silesian nappe, extends along the whole belt. The study area is located in the central part of this nappe, between the Dunajec and Wisloka River.
In the traditional point of view the rocks of the Polish Outer Carpathians are folded during single regional episode (Ksia_zkiewicz 1977). In the two of the biggest nappes of the Carpathians, Magura and Silesian nappes the map-scale fold axes are oriented parallel to the frontal thrust of individual ...
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