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Reply to the “Discussion” Oszczypko, N., Oszczypko-Clowes, M. and Olszewska, B. 2020. Geological setting and lithological inventory of the Czarna Woda conglomerates (Magura Nappe, Polish Outer Carpathians). Acta Geologica Polonica, 70, 397-418.

Oszczypko Nestor, Oszczypko-Clowes Marta, Olszewska Barbara

Acta Geologica Polonica

2022

Vol. 72, no. 1

141--144

Geological setting and lithological inventory of the Czarna Woda conglomerates (Magura Nappe, Polish Outer Carpathians)

Oszczypko Nestor, Oszczypko-Clowes Marta, Olszewska Barbara

Acta Geologica Polonica

2020

Vol. 70, no. 3

397--418

During the late Oligocene to early Miocene the residual Magura Basin was located along the front of the Pieniny Klippen Belt (PKB). This basin was supplied with clastic material derived from a south-eastern direction. In the Małe (Little) Pieniny Mts. in Poland, the late Oligocene/early Miocene Kremna Fm. of the Magura Nappe (Krynica subunit) occurs both in front of the PKB as well as in the tectonic windows within the PKB. Lenses of exotic conglomerates in the Kremna Fm. contain frequent clasts of Mesozoic limestones (e.g. limestones with “filaments” microfacies and Urgonian limestones) and Eocene shallow-water limestones. Fragments of crystalline and volcanic rocks occur subordinately. The provenance of these exotic rocks could be probably connected with Eocene exhumation and erosion of the SE part of the Dacia and Tisza Mega-Units.