THE TARKHANIAN-KARAGANIAN STAGE IN DEVELOPMENT OF THE EUXINIAN-CASPIAN BASIN (EASTERN PARATETHYS). PART 1: TARKHANIAN

dc.contributor.author	Goncharova I.A.
dc.contributor.author	Khondkarian S.O.
dc.contributor.author	Shcherba I.G.
dc.date.accessioned	2021-02-20T08:09:41Z
dc.date.available	2021-02-20T08:09:41Z
dc.date.issued	2001
dc.identifier	https://elibrary.ru/item.asp?id=13374889
dc.identifier.citation	Stratigraphy and Geological Correlation, 2001, 9, 5, 508-522
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/25243
dc.description.abstract	Evolution of the Euxinian-Caspian basin (Eastern Paratethys since the Oligocene) during the Tarkhanian (terminal early-initial middle Miocene) is considered, and its interrelations with the Alpine-Carpathian (Western Paratethys), Central Iranian, and East Mediterranean basins are discussed. The article includes the map of current distribution of Chokrakian deposits and their continental analogues, and the paleogeographic map for the Chokrakian time, where geological history of the Transcaspian region, Paleo-Don delta area, and Caucasus region are anew interpreted. Supplementary palinspastic profiles illustrate the peculiar morphology and bathymetry of the Chokrakian basin.
dc.subject	Euxinian-Caspian basin
dc.subject	Tarkhanian
dc.subject	Miocene
dc.title	THE TARKHANIAN-KARAGANIAN STAGE IN DEVELOPMENT OF THE EUXINIAN-CASPIAN BASIN (EASTERN PARATETHYS). PART 1: TARKHANIAN
dc.type	Статья
dc.subject.age	Cenozoic::Neogene::Miocene	en
dc.subject.age	Кайнозой::Неоген::Миоцен	ru

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