CENOZOIC UPPER MANTLE PLUMES IN EAST SIBERIA AND CENTRAL MONGOLIA AND SUBDUCTION OF THE PACIFIC PLATE

dc.contributor.author	Zorin Yu.A.
dc.contributor.author	Turutanov E.Kh.
dc.contributor.author	Kozhevnikov V.M.
dc.contributor.author	Rasskazov S.V.
dc.contributor.author	Ivanov A.V.
dc.date.accessioned	2024-11-02T11:07:49Z
dc.date.available	2024-11-02T11:07:49Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13520495
dc.identifier.citation	Doklady Earth Sciences, 2006, 409, 5, 723-726
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46351
dc.description.abstract	According to petrological and geochemical data, Cenozoic alkali basalts of East Siberia and Central Mongolia are related to mantle plumes. Analysis of geophysical data made it possible to outline tails of these plumes [3, 4] that are apparently confined to the upper mantle [4]. Calculations show that the upper and lower boundaries of plume tails can be located at 150–200 and 420–660 km, respectively.
dc.subject	plumes
dc.title	CENOZOIC UPPER MANTLE PLUMES IN EAST SIBERIA AND CENTRAL MONGOLIA AND SUBDUCTION OF THE PACIFIC PLATE
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06050096

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