The biostratinomy of Silurian cephalopod limestone biofacies of the Prague Basin is interpreted. Two facies types are recognized. One is the result of a surface current and the other one is the effect of redeposition within the current itself in a shallower environment during storm events. Orientation of cephalopod shells in these two facies types is discussed in relation to the Prague Basin development and to phenomena like telescoping, trap-structures and geopetal structures.

Cephalopod limestone biofacies in the Silurian of the Prague Basin, Bohemia / Ferretti, Annalisa; Kriz, Jiri. - In: PALAIOS. - ISSN 0883-1351. - STAMPA. - 10:3(1995), pp. 240-253.

Cephalopod limestone biofacies in the Silurian of the Prague Basin, Bohemia

FERRETTI, Annalisa;
1995

Abstract

The biostratinomy of Silurian cephalopod limestone biofacies of the Prague Basin is interpreted. Two facies types are recognized. One is the result of a surface current and the other one is the effect of redeposition within the current itself in a shallower environment during storm events. Orientation of cephalopod shells in these two facies types is discussed in relation to the Prague Basin development and to phenomena like telescoping, trap-structures and geopetal structures.
1995
10
3
240
253
Cephalopod limestone biofacies in the Silurian of the Prague Basin, Bohemia / Ferretti, Annalisa; Kriz, Jiri. - In: PALAIOS. - ISSN 0883-1351. - STAMPA. - 10:3(1995), pp. 240-253.
Ferretti, Annalisa; Kriz, Jiri
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11380/16727
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