CHLORIDE-CARBONATE NODULES IN KIMBERLITES FROM THE UDACHNAYA PIPE: ALTERNATIVE APPROACH TO THE EVOLUTION OF KIMBERLITE MAGMAS

dc.contributor.author	Kamenetsky V.S.
dc.contributor.author	Kamenetsky M.B.
dc.contributor.author	Sharygin V.V.
dc.contributor.author	Golovin A.V.
dc.date.accessioned	2024-11-02T11:07:44Z
dc.date.available	2024-11-02T11:07:44Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13521946
dc.identifier.citation	Geochemistry International, 2006, 44, 9, 935-940
dc.identifier.issn	0016-7029
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46334
dc.description.abstract	In the studying kimberlites, special attention was given to one aspect of the evolution of kimberlite magmas in mantle and crustal conditions: the entrapment of country rocks and interaction with them. Nodules in kimberlites (peridotites, eclogites, metamorphic and sedimentary rocks, as well as diamondiferous rocks) are usually used to estimate physicochemical and structural conditions in the subcontinental lithosphere, the properties of kimberlite magma, and the crystallization conditions of diamonds.
dc.subject	Udachnaya pipe
dc.title	CHLORIDE-CARBONATE NODULES IN KIMBERLITES FROM THE UDACHNAYA PIPE: ALTERNATIVE APPROACH TO THE EVOLUTION OF KIMBERLITE MAGMAS
dc.type	Статья
dc.identifier.doi	10.1134/S0016702906090084

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