ORIGIN OF BOTTOM SEDIMENTS RECOVERED ALONG THE GEOTRAVERSE ARCTIC-2000 IN THE ARCTIC OCEAN (MENDELEEV RISE AREA)

dc.contributor.author	Kaban'kov V.Ya.
dc.contributor.author	Andreeva I.A.
dc.contributor.author	Ivanov V.N.
dc.date.accessioned	2022-07-18T00:48:59Z
dc.date.available	2022-07-18T00:48:59Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13448555
dc.identifier.citation	Doklady Earth Sciences, 2004, 399, 8, 1088-1090
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38188
dc.description.abstract	The analysis of the data on the geotraverse Arctic-2000 shows that the bottom sediments of the Mendeleev Rise and associated basins are derived from local source. The inference that has been about their relation to ice-rafting is inconsistent with many facts. This argument is also indirectly supported by the absence of rocks typical of Greenland and the Arctic Archipelago in the studied sediments. The composition and texture of large rock fragments and fossil inclusions in them imply that the sediments were derived from the platform-type provenance and the continental nature of the Mendeleev Rise.
dc.title	ORIGIN OF BOTTOM SEDIMENTS RECOVERED ALONG THE GEOTRAVERSE ARCTIC-2000 IN THE ARCTIC OCEAN (MENDELEEV RISE AREA)
dc.type	Статья

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