THE LATITE TYPE OF LATE COLLISIONAL GRANITOIDS (NORTHERN CAUCASUS): GEOCHEMICAL AND MINERALOGICAL FEATURES

dc.contributor.author	Sazonova L.V.
dc.contributor.author	Dokuchaev A.Ya.
dc.contributor.author	Nosova A.A.
dc.contributor.author	Gurbanov A.G.
dc.date.accessioned	2022-01-14T04:15:15Z
dc.date.available	2022-01-14T04:15:15Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13437469
dc.identifier.citation	Doklady Earth Sciences, 2003, 393, 8, 1192-1195
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34306
dc.description.abstract	Using ICP-MS technique, investigated are granitoids of Caucasus Mineralnye Vody (GCMV) present in Miocene-Holocene volcanism development area, as well as composition of their mineral components (using EM and electron probing methods). GCMV composition fields are presented. The calculated high degree of enrichment with fluorine confirms belonging of GCMV to high-potassium rocks of late orogenic periods of folded series development. Geochemical characteristics of rocks, minerals' parageneses and composition indicate GCMV belonging to the latite type, whose final differentiation product may be lithium-fluorine granites.
dc.title	THE LATITE TYPE OF LATE COLLISIONAL GRANITOIDS (NORTHERN CAUCASUS): GEOCHEMICAL AND MINERALOGICAL FEATURES
dc.type	Статья

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