DISTRIBUTION OF THE THICKNESS OF QUATERNARY SEDIMENTS AND PRINCIPAL FEATURES OF THE PRE-VALDAI SURFACE IN THE WHITE SEA

dc.contributor.author	Tarasov G.A.
dc.contributor.author	Shlykova V.V.
dc.date.accessioned	2024-10-27T02:28:48Z
dc.date.available	2024-10-27T02:28:48Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13518436
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 8, 1225-1228
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46266
dc.description.abstract	Friable sediments of different glacial and interglacial epochs are abundant in the White Sea and adjacent land areas influenced by Pleistocene glaciations. Numerous studies carried out in neighboring areas of the Kola and Kanin peninsulas and Karelia provide grounds to conclude that glacial–periglacial sediments epresent a substantial constituent of Quaternary sequences. Most of the land areas surrounding the White Sea have been studied thoroughly. Detailed paleogeographic maps of the region were compiled, and analysis of its Late Cenozoic evolution was presented based on generalization of the available geomorphological, lithofacies, and geological–geophysical data.
dc.subject	Quaternary
dc.title	DISTRIBUTION OF THE THICKNESS OF QUATERNARY SEDIMENTS AND PRINCIPAL FEATURES OF THE PRE-VALDAI SURFACE IN THE WHITE SEA
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06080149
dc.subject.age	Cenozoic::Quaternary
dc.subject.age	Кайнозой::Четвертичная

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