PROBLEMS OF THE CAUCASUS PALEOLAND EXISTENCE DURING THE OLIGOCENE-MIOCENE TIME

dc.contributor.author	Kholodov V.N.
dc.contributor.author	Nedumov R.I.
dc.date.accessioned	2020-11-30T07:42:22Z
dc.date.available	2020-11-30T07:42:22Z
dc.date.issued	1996
dc.identifier	https://elibrary.ru/item.asp?id=13240806
dc.identifier.citation	Stratigraphy and Geological Correlation, 1996, , 2, 181-190
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/19971
dc.description.abstract	This paper considers the litho-facial environments that existed in the Caucasus region during the Oligocene and Miocene. The analyzed distribution patterns of reef deposits, evaporites, rock slide and avalanche facies, coal deposits, and paleoflora provided, in addition to denudation chronology, the basis to argue that the Caucasus orogen of that time existed as an island, actively influencing the sedimentation in adjacent basins.
dc.subject	Oligocene	en
dc.subject	Miocene	en
dc.title	PROBLEMS OF THE CAUCASUS PALEOLAND EXISTENCE DURING THE OLIGOCENE-MIOCENE TIME
dc.type	Статья
dc.subject.age	Cenozoic::Paleogene::Oligocene	en
dc.subject.age	Cenozoic::Neogene::Miocene	en
dc.subject.age	Кайнозой::Неоген::Миоцен	ru
dc.subject.age	Кайнозой::Палеоген::Олигоцен	ru

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