Oligocene-Lower Miocene sequences of the Pieniny Klippen Belt and adjacent Magura Nappe between Jarabina and the Poprad River (East Slovakia and South Poland): their tectonic position and palaeogeographic implications

Oszczypko, N.; Oszczypko-Clowes, M.; Golonka, J.; Marko, F.

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Oligocene-Lower Miocene sequences of the Pieniny Klippen Belt and adjacent Magura Nappe between Jarabina and the Poprad River (East Slovakia and South Poland): their tectonic position and palaeogeographic implications

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Oszczypko N. , Oszczypko-Clowes M. , Golonka J. , Marko F.

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This paper provides the results of a new litho- and biostratigraphic study from the contact zone between the Magura Nappe and Pieniny Klippen Belt close to Polish-Slovakian border. In the southernmost part of the Krynica facies zone of the Magura Nappe two new lithostratigraphic units have been established: the Poprad Member and the Kremna Formation. The Late Eocene-Oligocene age of the Malcov Formation (NP 19-NP 24) of the Pieniny Klippen Belt has also been confirmed. A Late Oligocene age (Zone NP 25 and lower part of NN1) was determined in deposits belonging to the Poprad Member of theMagura Formation, while an EarlyMiocene age (upper part of NN1 and NN2 zones) was established for the Kremna Formation. The Late Cretaceous-MiddleMiocene geotectonic evolution of the orogenic suture zone, between the Inner and Outer Carpathians, is outlined.

Słowa kluczowe

Outer Western Carpathians Pieniny Klippen Belt lithostratigraphy biostratigraphy suture zone

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2005

Tom

Vol. 49, No. 4

Strony

379--402

Opis fizyczny

Bibliogr. 87 poz. rys.,tab.

Twórcy

autor

Oszczypko N.

nestor@geos.ing.edu.pl

Jagiellonian University, Institute of Geological Sciences, Oleandry 2a, PL-30-063 Kraków, Poland

autor

Oszczypko-Clowes M.

Jagiellonian University, Institute of Geological Sciences, Oleandry 2a, PL-30-063 Kraków, Poland

autor

Golonka J.

Jagiellonian University, Institute of Geological Sciences, Oleandry 2a, PL-30-063 Kraków, Poland

autor

Marko F.

Department of Geology and Paleontology, Commenius University, Mlynska Dolina, 842-15 Bratislava, Slovak Republic

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