THE PARATETHYS AT THE END OF THE EARLY-MIDDLE MIOCENE AND ITS RELATIONS WITH SURROUNDING BASINS

dc.contributor.author	Goncharova I.A.
dc.contributor.author	Shcherba I.G.
dc.date.accessioned	2020-12-23T08:29:05Z
dc.date.available	2020-12-23T08:29:05Z
dc.date.issued	1997
dc.identifier	https://elibrary.ru/item.asp?id=13258118
dc.identifier.citation	Stratigraphy and Geological Correlation, 1997, , 3, 299-304
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/21145
dc.description.abstract	The Paratethys cyclic development (Andrusov, 1961; Nevesskaya et al., 1986) determined the main trend in investigating the composition and evolution of its biota, its hydrology, paleogeography, and tectonics. Each cycle was marked by changes from marine to semimarine and brackish conditions. Incidentally, each subsequent cycle with marine or semimarine regime became increasingly shorter, while the brackish stage became, on the contrary, progressively longer (Nevesskaya et al., 1986).
dc.subject	Miocene	en
dc.title	THE PARATETHYS AT THE END OF THE EARLY-MIDDLE MIOCENE AND ITS RELATIONS WITH SURROUNDING BASINS
dc.type	Статья
dc.subject.age	Cenozoic::Neogene::Miocene	en
dc.subject.age	Кайнозой::Неоген::Миоцен	ru

Files in this item

Files	Size	Format	View
There are no files associated with this item.