HETEROGENEITY OF AR AND SR INITIAL ISOTOPIC COMPOSITION IN THE COEXISTING MINERALS FROM MIOCENE HYPABYSSAL GRANITOIDS IN THE CAUCASIAN MINERAL WATERS REGION

dc.contributor.author	Lebedev V.A.
dc.contributor.author	Chernyshev I.V.
dc.contributor.author	Avdeenko A.S.
dc.contributor.author	Nosova A.A.
dc.contributor.author	Dokuchaev A.Ya.
dc.contributor.author	Oleinikova T.I.
dc.contributor.author	Gol'tsman Yu.V.
dc.date.accessioned	2024-10-27T02:28:36Z
dc.date.available	2024-10-27T02:28:36Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13514473
dc.identifier.citation	Doklady Earth Sciences, 2006, 410, 7, 1070-1074
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46217
dc.description.abstract	Late Miocene subalkaline granite magmatism in the Caucasian Mineral Waters (CMW) region is related to the first stage of Late Cenozoic magmatic activity in the Caucasian segment of the Alpine foldbelt. The young age and presence of uranium mineralization, as well as other factors including easy availability, promoted detailed study of these intrusions in geological, mineralogical, petrographical, geochemical, and physicochemical aspects.
dc.subject	Caucasus
dc.subject	Miocene
dc.title	HETEROGENEITY OF AR AND SR INITIAL ISOTOPIC COMPOSITION IN THE COEXISTING MINERALS FROM MIOCENE HYPABYSSAL GRANITOIDS IN THE CAUCASIAN MINERAL WATERS REGION
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06070154
dc.subject.age	Cenozoic::Neogene::Miocene
dc.subject.age	Кайнозой::Неоген::Миоцен

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