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

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 Kre...

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Veröffentlicht in:	Acta geologica polonica 2020-01, Vol.70 (3), p.397-418
Hauptverfasser:	Oszczypko, Nestor, Oszczypko-Clowes, Marta, Olszewska, Barbara
Format:	Artikel
Sprache:	eng ; pol
Schlagworte:	Conglomerates Eocene Mesozoic Miocene Oligocene Shallow water Volcanic rocks
Online-Zugang:	Volltext
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