TRANSGRESSIVE AND REGRESSIVE SEISMIC FADES OF THE DANUBE DEEP-SEA PALEOFAN

dc.contributor.author	Moskalenko V.N.
dc.date.accessioned	2021-02-16T10:48:35Z
dc.date.available	2021-02-16T10:48:35Z
dc.date.issued	2001
dc.identifier	https://elibrary.ru/item.asp?id=13366305
dc.identifier.citation	Stratigraphy and Geological Correlation, 2001, 9, 2, 204-211
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/24989
dc.description.abstract	Based on the seismostratigraphic analysis and geological interpretation of seismic profiling data, three marker surfaces corresponding to structural unconformities and erosion events are defined in the area of the Danube and Dnieper deep-sea fans in the Black Sea continental slope. It is established that sedimentary complexes concurrent to Quaternary glaciations correspond to three main phases in the Black Sea regressions and transgressions.
dc.subject	Danube
dc.subject	Dnieper
dc.subject	Black Sea continental slope
dc.subject	Quaternary
dc.title	TRANSGRESSIVE AND REGRESSIVE SEISMIC FADES OF THE DANUBE DEEP-SEA PALEOFAN
dc.type	Статья
dc.subject.age	Cenozoic::Quaternary	en
dc.subject.age	Кайнозой::Четвертичная	ru

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