Abstract
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, Magura, Pieniny, Valais and Ceahlau-Severins oceans. The Magura Ocean occupied the more northern position in the Alpine-Carpathian arc. During the Late Cretaceous-Paleogene tectono-sedimentary evolution the Magura Ocean was transformed into several (Magura, Dukla, Silesian, sub-Silesian and Skole) basins and intrabasinal source area ridges now incorporated into the Outer Western Carpathians.
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Oszczypko, N., ͆lączka, A., Oszczypko-Clowes, M., & Olszewska, B. (2015). Where was the Magura Ocean? Acta Geologica Polonica, 65(3), 319–344. https://doi.org/10.1515/agp-2015-0014
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