TECTONIC POSITION AND ORIGIN OF VOLCANOSEDIMENTARY ROCKS OF THE POLYARNYI UPLIFT (SOUTH ANYUI SUTURE, WESTERN CHUKOTKA)

dc.contributor.author	Sokolov S.D.
dc.contributor.author	Tuchkova M.I.
dc.contributor.author	Bondarenko G.E.
dc.contributor.author	Leyer P.
dc.date.accessioned	2024-10-27T02:28:44Z
dc.date.available	2024-10-27T02:28:44Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13516491
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 8, 1199-1203
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46249
dc.description.abstract	The South Anyui Suture (SAS) resulted from the closure of a past oceanic basin and subsequent collision between the North American and North Asian continents. Many geological aspects of this essential tectonic element of Mesozoides in Northeast Russia remain unclear so far. This concerns, first, the problem of the existence period of the paleoceanic basin. In this connection, the structural position, age, and origin of relatively widespread volcanosedimentary rocks are very important issues.
dc.subject	South Anyui Suture
dc.subject	Chukotka
dc.title	TECTONIC POSITION AND ORIGIN OF VOLCANOSEDIMENTARY ROCKS OF THE POLYARNYI UPLIFT (SOUTH ANYUI SUTURE, WESTERN CHUKOTKA)
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06080071

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