GEOCHEMISTRY AND FORMATION CONDITIONS OF RARE-METAL GRANITES WITH VARIOUS FLUORINE-BEARING MINERALS (FLUORITE, TOPAZ, AND CRYOLITE)

Antipin V.S.; Savina E.A.; Mitichkin M.A.

dc.contributor.author	Antipin V.S.
dc.contributor.author	Savina E.A.
dc.contributor.author	Mitichkin M.A.
dc.date.accessioned	2024-11-09T08:38:14Z
dc.date.available	2024-11-09T08:38:14Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13526879
dc.identifier.citation	Geochemistry International, 2006, 44, 10, 965-975
dc.identifier.issn	0016-7029
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46422
dc.description.abstract	A comparative geochemical study of rare-metal granitoids with various fluorine-bearing minerals (fluorite, topaz, and cryolite) was carried out. It was shown that these rocks correspond to both plumasitic and agpaitic geochemical types. The fluorite-, topaz-, and cryolite-bearing granites of these geochemical types are distinctly different in geochemical parameters and the character of magmatic evolution. These differences are related to the composition of initial magmas and their sources. Rare-metal granitoids with fluorine-bearing minerals compose small massifs, stocks, and dike swarms. Their formation is independent of the composition and age of the country rocks or geologic structures where they occur. © Pleiades Publishing, Inc. 2006.
dc.title	GEOCHEMISTRY AND FORMATION CONDITIONS OF RARE-METAL GRANITES WITH VARIOUS FLUORINE-BEARING MINERALS (FLUORITE, TOPAZ, AND CRYOLITE)
dc.type	Статья
dc.identifier.doi	10.1134/S0016702906100028