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SEDIMENTOLOGY AND BRACHIOPODS OF THE LOWER JURASSIC LUTY POTOK LIMESTONE (SLOVAKIA, WEST-CARPATHIAN KLIPPEN BELT)

In: Geologica Carpathica, vol. 46, no. 1
Milan Misik - Milan Sykora - Milos Siblik - Roman Aubrecht
Detaily:
Rok, strany: 1995, 41 - 51
O článku:
The crinoidal Luty Potok Limestone formerly considered as a Middle Jurassic part of the Czorsztyn Succession contains Liassic brachiopods and fragments of sponge skeletons. It belongs to the Nizna Succession. Clastic admixture derived from an external source is identical in both successions deposited on the opposite margins of the Pieninicum sedimentary zone. The Luty Potok Limestone is penetrated by a swarm of neptunian dykes which originated during repeated movements along a Liassic synsedimentary fault zone.
Ako citovať:
ISO 690:
Misik, M., Sykora, M., Siblik, M., Aubrecht, R. 1995. SEDIMENTOLOGY AND BRACHIOPODS OF THE LOWER JURASSIC LUTY POTOK LIMESTONE (SLOVAKIA, WEST-CARPATHIAN KLIPPEN BELT). In Geologica Carpathica, vol. 46, no.1, pp. 41-51. 1335-0552.

APA:
Misik, M., Sykora, M., Siblik, M., Aubrecht, R. (1995). SEDIMENTOLOGY AND BRACHIOPODS OF THE LOWER JURASSIC LUTY POTOK LIMESTONE (SLOVAKIA, WEST-CARPATHIAN KLIPPEN BELT). Geologica Carpathica, 46(1), 41-51. 1335-0552.