HISTORY OF HOLOCENE SEDIMENTATION IN THE SOUTHERN KARA SEA

dc.contributor.author	Levitan M.A.
dc.contributor.author	Krupskaya V.V.
dc.contributor.author	Sedykh E.M.
dc.contributor.author	Bourtman M.V.
dc.contributor.author	Demina L.L.
dc.contributor.author	Chudetsky M.Yu.
dc.date.accessioned	2022-09-28T05:54:16Z
dc.date.available	2022-09-28T05:54:16Z
dc.date.issued	2004
dc.identifier	https://elibrary.ru/item.asp?id=13464819
dc.identifier.citation	Lithology and Mineral Resources, 2004, 39, 6, 566-579
dc.identifier.issn	0024-4902
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38817
dc.description.abstract	Two bottom sediment cores (BP00-23/7 and BP00-7/6) recovered from the Yenisei transect in the southern Kara Sea are described. Data on their grain size composition, clay and heavy mineral assemblages, and distribution of a large group of chemical elements are presented. Radiocarbon dates based on AMS C-14 method suggest the Holocene age of sediments in the cores. Literature data on physical properties and foraminifers have also been analyzed. The facies affiliation of the lithostratigraphic subdivisions has been unraveled. History of the Yenisei River runoff in the Holocene has been reconstructed on the basis of different indicators.
dc.subject	Holocene
dc.title	HISTORY OF HOLOCENE SEDIMENTATION IN THE SOUTHERN KARA SEA
dc.type	Статья
dc.subject.age	Cenozoic::Quaternary::Holocene
dc.subject.age	Кайнозой::Четвертичная::Голоцен	ru

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