DE DE GRUYTER Acta Geologica Polonica, Vol. 65 (2015), No. 3, pp. 319–344 OPEN DOI: 10.1515/agp-2015-0014 G Where was the Magura Ocean? NESTOR OSZCZYPKO1, ANDRZEJ ŚLĄCZKA1, MARTA OSZCZYPKO-CLOWES1 and BARBARA OLSZEWSKA2 1Jagiellonian University, Institute of Geological Sciences, Oleandry 2a, 30-063 Kraków, Poland; 2Polish Geological Institute, Carpathian Branch, Skrzatów 1, 31-560 Kraków, Poland;
[email protected];
[email protected],
[email protected] ABSTRACT: Oszczypko, N., Ślączka, A., Oszczypko-Clowes, A. and Olszewska, B. 2015. Where was the Magura Ocean. Acta Geologica Polonica, 65 (3), 319–344. Warszawa. In the Late Jurassic to Early Cretaceous palaeogeography of the Alpine Tethys the term Ocean is used for dif- ferent 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 in- corporated into the Outer Western Carpathians. Key words: Cenozoic, Outer Western Carpathians; Palaeogeography; Intrabasinal ridges; Basin development. INTRODUCTION time, terms such as the Magura Basin, Magura Nappe or the Magura Superunit are commonly used. Some- The term Magura Ocean, understood as the east- times, the Magura Ocean and the Magura Basin are ern prolongation of the Ligurian – Piedmont and Pen- used interchangeably, causing confusion of their con- ninic Ocean (eg. Puglisi 2009; 2014), is often used in cepts. Whereas the terms Magura Basin and Magura the palaeogeographic and palaeotectonic reconstruc- Nappe are sufficiently well-defined, the spatial and tions of the Outer Western Carpathians (Channell and temporal coverage of the Magura Ocean has not been Kozur 1997).