MULTIPLE MAGMA SOURCES FOR THE PERALKALINE GRANITOIDS AND RELATED ROCKS OF THE KHALDZAN BUREGTE GROUP OF MASSIFS, WESTERN MONGOLIA: ISOTOPIC (NEODYMIUM, STRONTIUM, AND OXYGEN) AND GEOCHEMICAL DATA

dc.contributor.author	Kovalenko V.I.
dc.contributor.author	Yarmolyuk V.V.
dc.contributor.author	Kozlovskii A.M.
dc.contributor.author	Kovach V.P.
dc.contributor.author	Sal'nikova E.B.
dc.contributor.author	Kotov A.B.
dc.contributor.author	Khanchuk A.I.
dc.date.accessioned	2022-11-03T10:21:04Z
dc.date.available	2022-11-03T10:21:04Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13451537
dc.identifier.citation	Petrology, 2004, 12, 6, 497-518
dc.identifier.issn	0869-5911
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/39335
dc.description.abstract	The Khaldzan Buregte group of alkaline massifs was formed during seven intrusive phases and is confined to a large dike belt within Early Caledonian island-arc ophiolite and normal granite cutting the ophiolite. The uranium isotopic composition of the rock of the massif varies from +5 to +9. With respect to the ratio of compatible and incompatible trace element, the source of the alkaline rocks vary from those OIB. A two stage model was propose for the formation of khaldzan Bburgte group of alkaline massifs.
dc.title	MULTIPLE MAGMA SOURCES FOR THE PERALKALINE GRANITOIDS AND RELATED ROCKS OF THE KHALDZAN BUREGTE GROUP OF MASSIFS, WESTERN MONGOLIA: ISOTOPIC (NEODYMIUM, STRONTIUM, AND OXYGEN) AND GEOCHEMICAL DATA
dc.type	Статья

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