K-AR AGE AND SR-ND CHARACTERISTICS OF SUBALKALI BASALTS IN THE CENTRAL GEORGIAN NEOVOLCANIC REGION (GREATER CAUCASUS)

dc.contributor.authorLebedev V.A.
dc.contributor.authorChernyshev I.V.
dc.contributor.authorChugaev A.V.
dc.contributor.authorDudauri O.Z.
dc.contributor.authorVashakidze G.T.
dc.date.accessioned2024-11-09T08:38:20Z
dc.date.available2024-11-09T08:38:20Z
dc.date.issued2006
dc.description.abstractLate Cenozoic magmatism in the Greater Caucasus during the last 8.5 Ma was manifested in the Elbrus, Kazbek, and Central Georgian neovolcanic regions. In our work, we present K–Ar dates obtained for young rocks of Central Georgia, which, in turn, allowed us to determine the age of volcanism in this region and specify its role in the Neogene–Quaternary magmatic history of the Greater Caucasus. In addition, based on new Sr–Nd isotopic–geochemical and petrochemical data, we consider the petrogenesis of volcanics in this region and the problem of material source for young igneous rocks in the Greater Caucasus as a whole.
dc.identifierhttps://www.elibrary.ru/item.asp?id=13529051
dc.identifier.citationDoklady Earth Sciences, 2006, 408, 4, 657-661
dc.identifier.doi10.1134/S1028334X06040337
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/46443
dc.subjectCaucasus
dc.titleK-AR AGE AND SR-ND CHARACTERISTICS OF SUBALKALI BASALTS IN THE CENTRAL GEORGIAN NEOVOLCANIC REGION (GREATER CAUCASUS)
dc.typeСтатья

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