Late Cretaceous age of magmatism at Vršatec in the Pieniny Klippen Belt, Western Carpathians, Slovakia

• Autorzy: Bazarnik, Jakub , Matejová, Marína Molčan , Lenik, Piotr , Plašienka, Dušan , Potočný, Tomáš , Pańczyk, Magdalena
• Języki publikacji: EN

Abstrakty

EN

Volcanic rocks in the Pieniny Klippen Belt (PKB) of the Western Carpathians have been the focus of geologists for over a century (e.g. Uhlig, 1890; Małkowski, 1921). Miocene volcanism is most common in the PKB. However, there are infrequent occurrences of Cretaceous volcanic rocks. Several magmatic bodies of Cretaceous age have already been described in the PKB, including basalts at Hanigovce and Biała Woda, as well as peperites at Vršatec, and Velykyi Kamenets. The magmatic body in Vršatec occurs within the Upper Cretaceous marlstones of the Lalinok Formation, the age of which was previously determined to be younger than 100 Ma (Spišiak et al., 2011). Our new U-Pb zircon dating indicates the magmatic age to be ca. 80 Ma. This new age can be used as a benchmark for the forthcoming provenance studies of the surrounding clastic rocks in the PKB and the Outer Carpathians flysch.

Słowa kluczowe

EN

U-Pb dating; zircon; peperite; Cretaceous; Pieniny Klippen Belt

• Czasopismo: Mineralogia
• Rocznik: 2024
• Tom: Vol. 55, iss. 1
• Strony: 40--47
• Opis fizyczny: Bibliogr. 36 poz., rys., tab.

Twórcy

autor

Bazarnik, Jakub

• Polish Geological Institute – National Research Institute, Carpathian Branch; Skrzatów 1, 31-560 Kraków, Poland,

autor

Matejová, Marína Molčan

• Department of Geology and Paleontology, Faculty of Natural Sciences, Comenius University in Bratislava, Mlynská dolina G,842 15 Bratislava, Slovakia

autor

Lenik, Piotr

• Polish Geological Institute – National Research Institute, Carpathian Branch; Skrzatów 1, 31-560 Kraków, Poland

autor

Plašienka, Dušan

• Department of Geology and Paleontology, Faculty of Natural Sciences, Comenius University in Bratislava, Mlynská dolina G,842 15 Bratislava, Slovakia

autor

Potočný, Tomáš

• Department of Geology and Paleontology, Faculty of Natural Sciences, Comenius University in Bratislava, Mlynská dolina G,842 15 Bratislava, Slovakia
• Faculty of Geology, Geophysics and Environmental Protection, AGH – University of Krakow, al. Mickiewicza 30, 30-059 Kraków, Poland

autor

Pańczyk, Magdalena

• Polish Geological Institute – National Research Institute, Micro-Area Analysis Laboratory; Rakowiecka 4, 00-975 Warszawa, Poland

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Identyfikatory

DOI

10.2478/mipo-2024-0004