A SUBMARINE FAN IN THE AMUNDSEN BASIN, ARCTIC OCEAN

dc.contributor.author	Kristoffersen Y.
dc.contributor.author	Sorokin M.Y.
dc.contributor.author	Jokat W.
dc.contributor.author	Svendsen O.
dc.date.accessioned	2022-10-01T05:54:57Z
dc.date.available	2022-10-01T05:54:57Z
dc.date.issued	2004
dc.identifier	https://elibrary.ru/item.asp?id=13470946
dc.identifier.citation	Marine Geology, 2004, 204, 3-4, 317-324
dc.identifier.issn	0025-3227
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38851
dc.description.abstract	Seismic reflection data from drifting ice stations and an icebreaker survey document the presence of a submarine fan along the east flank of the Lomonosov Ridge in the Amundsen Basin, Arctic Ocean. The fan extends from a source area at the North Greenland and Canadian Arctic continental margin to the North Pole. The fan probably developed in response to the combined effect of increased glacial sediment input during the Plio^Pleistocene and topographically confined transport of glacial debris in the deep sea passage between Lincoln Sea margin and the southern end of the Lomonosov Ridge. 4 2004 Elsevier B.V. All rights reserved.
dc.subject	Arctic Ocean
dc.subject	Amundsen Basin
dc.subject	bottom features
dc.subject	submarine fan
dc.subject	glaci-marine sedimentation
dc.title	A SUBMARINE FAN IN THE AMUNDSEN BASIN, ARCTIC OCEAN
dc.type	Статья

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