THE GLACIAL HISTORY OF THE BARENTS AND KARA SEA REGION

dc.contributor.author	Svendsen J.I.
dc.contributor.author	Mangerud J.
dc.contributor.author	Gataullin V.
dc.contributor.author	Polyak L.
dc.date.accessioned	2022-09-02T03:33:56Z
dc.date.available	2022-09-02T03:33:56Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=17810312
dc.identifier.citation	Developments in Quaternary Science, 2004, 2, Part 1, 369-378
dc.identifier.issn	1571-0866
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38605
dc.description.abstract	The Barents and Kara seas, fringing the northern rim of the Eurasian continent, cover one of the widest continental shelves in the world. Geological investigations reveal that this vast area has been repeatedly affected by major glaciations during the Quaternary (e.g. Elverhøi et al., 1998a). From time to time the ice sheets expanded onto the Russian Lowland blocking the north-flowing rivers on the continent.
dc.title	THE GLACIAL HISTORY OF THE BARENTS AND KARA SEA REGION
dc.type	Статья

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