Climatically forced Caspian Sea level changes as it recorded in Pleistocene succession

Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12323/3275

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DC Field	Value	Language
dc.contributor.author	Aliyeva, Elmira	-
dc.contributor.author	Amirov, Elnur	-
dc.date.accessioned	2016-03-01T13:13:09Z	-
dc.date.available	2016-03-01T13:13:09Z	-
dc.date.issued	2008	-
dc.identifier.uri	http://hdl.handle.net/20.500.12323/3275	-
dc.description.abstract	Intensive orogenic movements adjacent to South Caspian basin folded areas and submersion of its central parts at the end of Pontian-beginning of Early Pliocene led to dramatic PaleoCaspian Sea level fall (from 600 to 1500 m (Reynolds, 1998)). Since that time sedimentation there took place under conditions of isolated basin temporarily connected with Black Sea in Upper Pliocene (Akchagyl). Being the largest isolated basin in the world with hyper unstable sea level regime the Caspian Sea represents the beautiful model area for studying of dynamics of sedimentary basins' development in short -term intervals.	en
dc.language.iso	en	en
dc.title	Climatically forced Caspian Sea level changes as it recorded in Pleistocene succession	en
dc.type	Article	en
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