ASGP (2019), vol. 89: 233–257

THE JURASSIC TO PALAEOGENE STRATA IN THE NORTHERN BOUNDARY FAULT ZONE IN DEEP BOREHOLE PD-9 AT SZCZAWNICA, PIENINY KLIPPEN BELT, WEST CARPATHIANS, POLAND: BIOSTRATIGRAPHY AND TECTONIC IMPLICATIONS

Krzysztof BIRKENMAJER † & Przemysław GEDL

† Krzysztof Birkenmajer (1929–2019)
Institute of Geological Sciences, Polish Academy of Sciences, Research Centre in Kraków, Senacka 1, 31-002 Kraków, Poland; e-mail: ndgedl@cyf-kr.edu.pl

Birkenmajer, K. & Gedl, P., 2019. The Jurassic to Palaeogene strata in the northern boundary fault zone in deep borehole PD-9 at Szczawnica, Pieniny Klippen Belt, West Carpathians, Poland: biostratigraphy and tectonic implications. Annales Societatis Geologorum Poloniae, 89: 233 – 257.

Abstract: The Jurassic through Palaeogene stratigraphy and tectonic structure of the PD-9 borehole at Szczawnica, Pieniny Klippen Belt, West Carpathians, Poland, is revised. The borehole was drilled in the strongly tectonized northern boundary fault zone of the Pieniny Klippen Belt, of Miocene age. Age revision is given by dinoflagellate cysts. Late Cretaceous taxa are reported from the Hałuszowa Formation. The Bryjarka Member (previously with the rank of formation) yielded rich Early Eocene (Ypresian) assemblages. Similar ones are reported from the Szczawnica Formation. A tectonic thrust sheet of the Jurassic Szlachtowa Formation (Grajcarek Unit) in the Palaeogene of the Magura Nappe is evidenced; it yielded late Toarcian–Aalenian dinoflagellate cyst assemblages. The succession of strata recorded from the PD-9 borehole shows the steep, almost vertical attitude of the Grajcarek Main Dislocation at Szczawnica, separating the structures of the Magura Nappe (to the north) and the Pieniny Klippen Belt to the south.

Manuscript received 11 November 2018, accepted 10 September 2019