RARE-EARTH ELEMENTS AND THE GENESIS OF ORE MINERALIZATION AT THE KALGUTINSKOE TUNGSTEN ORE FIELD, GORNYI ALTAI

dc.contributor.author	Ivanova G.F.
dc.contributor.author	Kolesov G.M.
dc.contributor.author	Karpukhina V.S.
dc.contributor.author	Cherkasova E.V.
dc.date.accessioned	2024-11-09T08:38:13Z
dc.date.available	2024-11-09T08:38:13Z
dc.date.issued	2006
dc.description.abstract	Rare-earth elements (REE) are widely used as indicators of the conditions under which rocks and minerals were produced. This paper reports the results of our study of REE in granites and minerals from quartz zones with ore mineralization and the principal parameters under which these minerals were formed at the Kalgutinskoe ore field, which is located in the south-eastern part of the Gornyi Altai Range, within the Charysh–Terekta tectono–stratigraphic zone.
dc.identifier	https://www.elibrary.ru/item.asp?id=13526822
dc.identifier.citation	Geochemistry International, 2006, 44, 5, 508-515
dc.identifier.doi	10.1134/S0016702906050089
dc.identifier.issn	0016-7029
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46416
dc.subject	Kalgutinskoe ore field
dc.subject	Gornyi Altai
dc.title	RARE-EARTH ELEMENTS AND THE GENESIS OF ORE MINERALIZATION AT THE KALGUTINSKOE TUNGSTEN ORE FIELD, GORNYI ALTAI
dc.type	Статья

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