ECLOGITIC INCLUSIONS IN DIAMONDS: EVIDENCE OF COMPLEX MANTLE PROCESSES OVER TIME

dc.contributor.author	Taylor L.A.
dc.contributor.author	Snyder G.A.
dc.contributor.author	Sobolev V.N.
dc.contributor.author	Crozaz G.
dc.contributor.author	Yefimova E.S.
dc.contributor.author	Sobolev N.V.
dc.date.accessioned	2020-12-01T08:34:52Z
dc.date.available	2020-12-01T08:34:52Z
dc.date.issued	1996
dc.identifier	https://elibrary.ru/item.asp?id=13247191
dc.identifier.citation	Earth and Planetary Science Letters, 1996, , 3, 535-551
dc.identifier.issn	0012-821X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/19993
dc.description.abstract	The first ion-probe trace element analyses of clinopyroxene-garnet pairs both included within diamonds and from the eclogite host xenoliths are reported; these diamondiferous eclogites are from the Udachnaya and Mir kimberlite pipes, Yakutia, Russia. The major and trace element analyses of these diamond-inclusion and host-rock pairs are compared in order to determine the relative ages of the diamonds, confirm or deny genetic relationships between the diamonds and the eclogites, evaluate models of eclogite petrogenesis, and model igneous processes in the mantle before, during, and after diamond formation.
dc.title	ECLOGITIC INCLUSIONS IN DIAMONDS: EVIDENCE OF COMPLEX MANTLE PROCESSES OVER TIME
dc.type	Статья

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