SECONDARY MELT INCLUSIONS IN OLIVINE FROM UNALTERED KIMBERLITES OF THE UDACHNAYA-EAST PIPE, YAKUTIA

dc.contributor.author	Golovin A.V.
dc.contributor.author	Sharygin V.V.
dc.contributor.author	Pokhilenko N.P.
dc.contributor.author	Mal'kovets V.G.
dc.contributor.author	Sobolev N.V.
dc.contributor.author	Kolesov B.A.
dc.date.accessioned	2022-01-16T05:05:33Z
dc.date.available	2022-01-16T05:05:33Z
dc.date.issued	2003
dc.description.abstract	In the central part of the Udachnaya-East kimberlite pipe situated in the Daldyn–Alakit district of the Yakutian kimberlite province, unique (in the high degree of its preservation) kimberlitic rock with abundant olivine, which did not undergo serpentinization, was found at a depth of 350–650 m. This kimberlite can be regarded as a reference primary rock that retained all features of the deep-seated melt [1].
dc.identifier	https://www.elibrary.ru/item.asp?id=13444147
dc.identifier.citation	Doklady Earth Sciences, 2003, 388, 1, 93-96
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34352
dc.title	SECONDARY MELT INCLUSIONS IN OLIVINE FROM UNALTERED KIMBERLITES OF THE UDACHNAYA-EAST PIPE, YAKUTIA
dc.type	Статья

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