EPOCHS OF FORMATION, GEODYNAMIC SETTING, AND SOURCES OF RARE-METAL MAGMATISM IN CENTRAL ASIA

dc.contributor.author	Kovalenko V.I.
dc.contributor.author	Yarmolyuk V.V.
dc.contributor.author	Vladykin N.V.
dc.contributor.author	Ivanov V.G.
dc.contributor.author	Kovach V.P.
dc.contributor.author	Kozlovsky A.M.
dc.contributor.author	Kostitsyn Yu.A.
dc.contributor.author	Kotov A.B.
dc.contributor.author	Sal'nikova E.B.
dc.date.accessioned	2021-06-07T12:43:30Z
dc.date.available	2021-06-07T12:43:30Z
dc.date.issued	2002
dc.identifier	https://elibrary.ru/item.asp?id=13395786
dc.identifier.citation	Petrology, 2002, 10, 3, 199-221
dc.identifier.issn	0869-5911
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/28890
dc.description.abstract	The epochs of formation, geodynamic setting and sources of rare-metal magmatism in Central Asia were discussed. It was found that in the late paleozoic-early mesozoic epoch, intraplate activity persisted but the area of intraplate magmatism probably decreased owing to the descent of cold lithospheric material into the superplume region. The process of Asiam plume degradation was found to continued in the late mesozoic and attained the maximum in the early cenozoic.
dc.title	EPOCHS OF FORMATION, GEODYNAMIC SETTING, AND SOURCES OF RARE-METAL MAGMATISM IN CENTRAL ASIA
dc.type	Статья

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