The Upper Cretaceous variegated shales in the Ropianka Formation of the Magura Nappe (Outer Carpathians) : age and lithostratigraphic position

• Autorzy: Waśkowska Anna , Szczęch Mateusz

Identyfikatory

DOI

10.7306/gq.1688

• Języki publikacji: EN

Abstrakty

EN

The lithological characteristics and age analysis of the variegated Farony Shale are presented for the first time. The Farony Shale occurs in the Lubomierz and Rabka areas in the Bystrica Subunit. It is located within medium- and thin-bedded sandy dominated turbidites of the Campanian–Paleocene Ropianka Formation. It is comprised of red shales laminated or interlayered with strongly bioturbated green shales. Exposures of the Farony Shale are observed along a distance of ~25 km, in the form of a narrow belt. The age of the variegated deposits is estimated based on agglutinated foraminifera to late Campanian–earliest Maastrichtian. Their deposition was associated with low-energy conditions and a temporary limitation of the supply of sandy material to the inner part of the Magura Basin.

Słowa kluczowe

EN

Campanian-Maastrichtian; red beds; lithostratigraphy; biostratigraphy; foraminifera

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Geological Quarterly
• Rocznik: 2023
• Tom: Vol. 67, No. 2
• Strony: art. no. 18
• Opis fizyczny: Bibliogr. 50 poz., fot., map., tab., wykr.

Twórcy

autor

Waśkowska Anna

• AGH University of Krakow, Al. Mickiewicza 30, 30-059 Kraków, Poland

• https://orcid.org/0000-0003-4090-8534

autor

Szczęch Mateusz

• Jagiellonian University, Institute of Geological Sciences, Gronostajowa 3a, 30-387 Kraków, Poland

• https://orcid.org/0000-0001-9089-7947

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