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.identifier	https://www.elibrary.ru/item.asp?id=13513992
dc.identifier.citation	Geochemistry International, 2006, 44, 7, 729-735
dc.identifier.issn	0016-7029
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46237
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.subject	lamproite
dc.subject	Sayan region
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
dc.identifier.doi	10.1134/S0016702906070093
dc.subject.age	Докембрий::Протерозой::Рифей

Files in this item

Name: Egor_06.pdf

Size: 303.0Kb

Format: PDF