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Palazu Romania

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Series: GCSSEPM, GCSSEPM
Published: 01 December 2015
DOI: 10.5724/gcs.15.34.0372
EISBN: 978-1-944966-00-3
... described above, reflecting very different crustal rheologies inherited from various prerift deformational episodes, should find its counterpart in the offshore part of the conjugate Turkish margin. We speculate that the abrupt change in the rifting style across the Capidava-Ovidiu (Palazu) fault system...
Series: GSA Special Papers
Published: 01 January 2007
DOI: 10.1130/2007.2423(18)
... (km) east-west and 250–300 km north-south (Fig. 1) , located mainly in the present territories of Romania and Bulgaria. It belongs to a zone of Caledonian terranes along the SW margin of the East European craton between Denmark and the Black Sea (Fig. 1) . The term Caledonian is used here...
Series: Geological Society, London, Memoirs, Geological Society, London, Memoirs
Published: 01 January 2006
DOI: 10.1144/GSL.MEM.2006.032.01.17
EISBN: 9781862394070
... advanced in the SE part of the TESZ in Romania and Turkey, where terranes originally accreted during the Variscan Orogeny have been displaced and re-accreted to the EEC margin during the development of the peri-Tethyan margin, opening of the Black Sea and the subsequent Alpine-Carpathian Orogeny. Some...
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