DEPOSITION SETTINGS ON THE CONTINENTAL SHELF OF THE EAST SIBERIAN SEA

dc.contributor.author	Dudarev O.V.
dc.contributor.author	Semiletov I.P.
dc.contributor.author	Charkin A.N.
dc.contributor.author	Botsul A.I.
dc.date.accessioned	2024-10-27T02:28:40Z
dc.date.available	2024-10-27T02:28:40Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13516221
dc.identifier.citation	Doklady Earth Sciences, 2006, 409, 6, 1000-1005
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46234
dc.description.abstract	The spacious continental shelf of the East Siberian Sea (ESS) is of particular interest primarily due to its formation in settings of periglacial lithogenesis. This region is characterized by the universal development of Pleistocene permafrost rocks (PFR). The presence of thick veins of relict ice enclosed in these sequences determined the dependence of the coastal shelf cryolithozone PFR on the thermal and hydrodynamic impact.
dc.title	DEPOSITION SETTINGS ON THE CONTINENTAL SHELF OF THE EAST SIBERIAN SEA
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06060389

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