Journal
ACTA GEOLOGICA POLONICA
Volume 65, Issue 3, Pages 319-344Publisher
POLSKA AKAD NAUK, POLISH ACAD SCIENCES, UNIV WARSAW, GEOLOGY DEPT
DOI: 10.1515/agp-2015-0014
Keywords
Cenozoic; Outer Western Carpathians; Palacogeography; Intrabasinal ridges; Basin development
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In the Late Jurassic to Early Cretaceous palaeogeography of the Alpine Tethys the term Ocean is used for different parts of these sedimentary areas: eg. Ligurian - Piedmont and Penninic, Niagara, Pieniny Valais and Ceahlau-Severins oceans. The Niagara Ocean occupied the more northern position in the Alpine-Carpathian arc. During the Late Cretaceous-Paleogene tectono-sedimentary evolution the Niagara Ocean was transformed into several (Niagara, Dukla, Silesian, sub-Silesian and Skole) basins and intrabasinal source area ridges now incorporated into the titer Western Carpathians.
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