CHARACTERISTICS OF THE GRAIN-SIZE COMPOSITION OF DEEP-WATER OCEANIC SEDIMENTS

Sval'nov V.N.; Alekseeva T.N.

dc.contributor.author	Sval'nov V.N.
dc.contributor.author	Alekseeva T.N.
dc.date.accessioned	2024-12-22T03:47:48Z
dc.date.available	2024-12-22T03:47:48Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13517007
dc.identifier.citation	Lithology and Mineral Resources, 2006, 41, 3, 201-214
dc.identifier.issn	0024-4902
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/47041
dc.description.abstract	The grain-size composition of nonlithified sediments in the Indian, Pacific, and Atlantic oceans is studied. Grain-size features of the major lithogenetic types of deep-water sediments are determined. The genetic interpretation of results obtained is given. Trends of the fractionation of sandy-silty and pelitic materials in pelagic zones of sedimentation basins are revealed. © Pleiades Publishing, Inc. 2006.
dc.title	CHARACTERISTICS OF THE GRAIN-SIZE COMPOSITION OF DEEP-WATER OCEANIC SEDIMENTS
dc.type	Статья
dc.identifier.doi	10.1134/S0024490206030011