BASIC MAGMATISM IN THE GEOLOGICAL HISTORY OF THE ELBRUS NEOVOLCANIC AREA, GREATER CAUCASUS: EVIDENCE FROM K-AR AND SR-ND ISOTOPE DATA

dc.contributor.author	Lebedev V.A.
dc.contributor.author	Bubnov S.N.
dc.contributor.author	Chernyshev I.V.
dc.contributor.author	Gol'tsman Yu.V.
dc.date.accessioned	2024-10-23T07:15:59Z
dc.date.available	2024-10-23T07:15:59Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13511327
dc.identifier.citation	Doklady Earth Sciences, 2006, 406, 1, 37-40
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46155
dc.description.abstract	The age and genesis of basic rocks in the magmatic evolutionary series are of principal significance for regions with predominant acid, mainly crustal volcanism. The appearance of basic volcanic rocks in the rhyolite–dacite volcanic sequences is usually a sensitive indicator of a change in the conditions of magma generation, the involvement of different mantle and/or crustal reservoirs, or a change in the geotectonic and geodynamic settings of the volcanic activity. This is evident from the abundance of Neogene–Quaternary acid and moderately acid volcanism in the Elbrus neovolcanic area, Greater Caucasus.
dc.subject	Elbrus
dc.subject	Greater Caucasus
dc.title	BASIC MAGMATISM IN THE GEOLOGICAL HISTORY OF THE ELBRUS NEOVOLCANIC AREA, GREATER CAUCASUS: EVIDENCE FROM K-AR AND SR-ND ISOTOPE DATA
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06010107

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