MIDDLE JURASSIC–LOWER CRETACEOUS DEVELOPMENT OF THE PRUSKE UNIT IN THE WESTERN PART OF THE PIENINY KLIPPEN BELT

In: Geologica Carpathica, vol. 45, no. 4

Roman Aubrecht - Ladislava Ozvoldova

Detaily:

Rok, strany: 1994, 211 - 223

O článku:

Two new lithostratigraphic units were distinguished within the Pruske Unit of the Pieniny Klippen Belt: 1. Samasky Formation representing crinoidal flysch of Bajocian-Bathonian age; 2. Horne Srnie Limestone Member — a massive pink organodetritic limestone of Berriasian-Lower Valanginian age. New radiolarian species Orbiculiforma catenaria Ozvoldova, n.sp. was described from the Czajakowa Formation of the Samasky locality.

Ako citovať:

ISO 690:

Aubrecht, R., Ozvoldova, L. 1994. MIDDLE JURASSIC–LOWER CRETACEOUS DEVELOPMENT OF THE PRUSKE UNIT IN THE WESTERN PART OF THE PIENINY KLIPPEN BELT. In Geologica Carpathica, vol. 45, no.4, pp. 211-223. 1335-0552.

APA:

Aubrecht, R., Ozvoldova, L. (1994). MIDDLE JURASSIC–LOWER CRETACEOUS DEVELOPMENT OF THE PRUSKE UNIT IN THE WESTERN PART OF THE PIENINY KLIPPEN BELT. Geologica Carpathica, 45(4), 211-223. 1335-0552.