DEEP GEODYNAMICS AND MANTLE PLUMES: THEIR ROLE IN THE FORMATION OF THE CENTRAL ASIAN FOLD BELT

dc.contributor.author	Yarmolyuk V.V.
dc.contributor.author	Kovalenko V.I.
dc.date.accessioned	2022-02-17T11:03:52Z
dc.date.available	2022-02-17T11:03:52Z
dc.date.issued	2003
dc.identifier	https://elibrary.ru/item.asp?id=13443556
dc.identifier.citation	Petrology, 2003, 11, 6, 504-531
dc.identifier.issn	0869-5911
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/35491
dc.description.abstract	The role of geodynamics and mantle plumes in the formation of the Central Asian Fold Belt is discussed. The isotopic geochemical study demonstrates that the mantle plumes were derived from moderately depleted and enriched mantle reservoirs. Participation of these sources in the magma formation is believed to be related to the domination of one cell mantle convection. The paleogeographic reconstruction show that the Northern Asian Mantle Hot Fields is comparable with the modern African-Atlantic hot superplumes.
dc.title	DEEP GEODYNAMICS AND MANTLE PLUMES: THEIR ROLE IN THE FORMATION OF THE CENTRAL ASIAN FOLD BELT
dc.type	Статья

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