PETROLOGICAL FEATURES OF OLIVINE-PHLOGOPITE LAMPROITES OF THE SAYAN REGION: EVIDENCE FROM SR-ND ISOTOPE AND ICP-MS TRACE-ELEMENT DATA

dc.contributor.author	Egorov K.N.
dc.contributor.author	Solov'eva L.V.
dc.contributor.author	Men'shagin Yu.V.
dc.contributor.author	Maslovskaya M.N.
dc.contributor.author	Sekerin A.P.
dc.contributor.author	Bankovskaya E.V.
dc.contributor.author	Kovach V.P.
dc.date.accessioned	2024-10-27T02:28:41Z
dc.date.available	2024-10-27T02:28:41Z
dc.date.issued	2006
dc.description.abstract	The only occurrence of Middle Riphean diamondiferous magmatism in the Siberian Craton is the diamondiferous lamproites of the Sayan region, which are located in the Ingashi River basin, a right tributary of the Oka River, in its middle reaches. The lamproites form a series of vein bodies and together with local halos of indicator minerals compose the Ingashi lamproite field, ~30 km long and 5–8 km wide.
dc.identifier	https://www.elibrary.ru/item.asp?id=13513992
dc.identifier.citation	Geochemistry International, 2006, 44, 7, 729-735
dc.identifier.doi	10.1134/S0016702906070093
dc.identifier.issn	0016-7029
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46237
dc.subject	lamproite
dc.subject	Sayan region
dc.subject.age	Докембрий::Протерозой::Рифей
dc.title	PETROLOGICAL FEATURES OF OLIVINE-PHLOGOPITE LAMPROITES OF THE SAYAN REGION: EVIDENCE FROM SR-ND ISOTOPE AND ICP-MS TRACE-ELEMENT DATA
dc.type	Статья

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