REE DISTRIBUTION IN FLUORITE AS AN INDICATOR OF GEOLOGIC-GENETIC FEATURES OF ORE DEPOSITS RELATED TO VARIOUS MAGMATIC ASSOCIATIONS

dc.contributor.author	Kupriyanova I.I.
dc.contributor.author	Kukushkina O.A.
dc.contributor.author	Shpanov E.P.
dc.contributor.author	Matias V.V.
dc.contributor.author	Novikova M.I.
dc.contributor.author	Kuvshinova K.A.
dc.date.accessioned	2021-06-07T12:43:30Z
dc.date.available	2021-06-07T12:43:30Z
dc.date.issued	2002
dc.identifier	https://elibrary.ru/item.asp?id=13395787
dc.identifier.citation	Petrology, 2002, 10, 3, 277-297
dc.identifier.issn	0869-5911
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/28891
dc.description.abstract	The REE distribution in fluorites as an indicator of geologic-genetic features of ore deposits related to various magmatic associations was discussed. It was found that with an increase in the distance between the mineralization and the granitic massif or volcanic edifice, the relative Eu amounts in the fluorite increased and the negative anomaly gradually decreased, disappeared or even gave away to a positive anomaly. The analysis showed that when fluorites from deposits of various depths were compared, their Eu/Eu* ratio sinusoidally varied.
dc.title	REE DISTRIBUTION IN FLUORITE AS AN INDICATOR OF GEOLOGIC-GENETIC FEATURES OF ORE DEPOSITS RELATED TO VARIOUS MAGMATIC ASSOCIATIONS
dc.type	Статья

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