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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, 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.
Czasopismo
Rocznik
Tom
Strony
319--344
Opis fizyczny
Bibliogr. 115 poz., rys.
Twórcy
autor
- Jagiellonian University, Institute of Geological Sciences, Oleandry 2a, 30-063 Kraków, Poland
autor
- Jagiellonian University, Institute of Geological Sciences, Oleandry 2a, 30-063 Kraków, Poland
autor
- Jagiellonian University, Institute of Geological Sciences, Oleandry 2a, 30-063 Kraków, Poland
autor
- Polish Geological Institute, Carpathian Branch, Skrzatów 1, 31-560 Kraków, Poland
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