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In the Polish sector of the Magura Nappe, along the front of the Pieniny Klippen Belt, strongly tectonized calcareous flysch up to 1000 m thick is exposed. Previously these deposits, composed of thin- to thick-bedded flysch, with a packet of Łącko-type marls, have been included into several Paleocene/Eocene formations, e.g., the Szczawnica Formation. This formation contains a poor assemblage of agglutinated foraminifera and a relatively rich assemblage of calcareous nannoplankton, with abundant reworked species. The youngest species give evidence of the NN2 Zone (Lower Miocene). Additionally, in three profiles (Szlachtowa, Knurów and Waksmund) of the Kremna Fm., Early Miocene foraminifera have been recognized. This research documented that during the Burdigalian, at the front of Central Western Carpathians, there still existed a residual marine basin probably up to 100 km wide. These deposits also contain thick packages of exotic carbonate conglomerates derived from the SE, previously regarded as the Jarmuta Formation.
Czasopismo
Rocznik
Tom
Strony
597--619
Opis fizyczny
Bibliogr. 117 poz., fot., mapa, rys., tab., wykr.
Twórcy
autor
- Jagiellonian University, Institute of Geological Sciences, Gronostajowa 3a, 30-387 Kraków, Poland
autor
- Jagiellonian University, Institute of Geological Sciences, Gronostajowa 3a, 30-387 Kraków, Poland
autor
- Jagiellonian University, Institute of Geological Sciences, Gronostajowa 3a, 30-387 Kraków, Poland
autor
- Slovak Academy of Sciences, Earth Science Institute, Ďumbierska, 974 11 Banska Bystrica, Slovakia
- KU Ružomberok, Department of Geography, Faculty of Education, Hrabovská cesta 1, 03401 Ružomberok, Slovakia
autor
- Przedsiębiorstwo Geologiczne S.A. w Krakowie, Kijowska 16A, 30-079 Kraków, Poland
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Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-e6b1a6f7-6c5b-403f-b732-08cf3bb8d790