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Position of the Marmarosh Flysch (Eastern Carpathians) and its Relation to Magura Nappe (Western Carpathians)
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Geolines
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January 1, 2004
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Copyright informationCopyright Institute of Geology 2004. Provided by ProQuest LLC. (Hide copyright information)
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The Magura nappe is the innermost tectonic unit of the Western Carpathians and is linked with the Rheno-Danubian flysch of the Eastern Alps. Towards the east this unit runs as an arc from the Wienerwald (Austria) through Moravia (Czechia) and Poland, then narrows in Eastern Slovakia before disappearing beneath the Miocene volcanic rocks east of Uzhhorod (Trans-Carpathian Ukraine). The oldest Jurassic-Lower Cretaceous rocks are known from the peri-Pieniny Klippen Belt (PKB) in Poland and a few localities in Southern Moravia. The youngest (Early Miocene) deposits of the Magura Nappe are known from Poland. The Magura Nappe is separated from PKB by a sub-vertical Miocene strike-slip boundary, ...
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