FLUORITE AS AN INDICATOR OF INTERNAL ZONING AND ORE POTENTIAL OF RARE METAL GRANITES OF THE ORLOVSKOE TANTALUM DEPOSIT, EASTERN TRANSBAIKALIA

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dc.contributor.author Kukushkina O.A.
dc.contributor.author Matias V.V.
dc.date.accessioned 2022-07-20T06:12:19Z
dc.date.available 2022-07-20T06:12:19Z
dc.date.issued 2004
dc.identifier https://www.elibrary.ru/item.asp?id=13456740
dc.identifier.citation Geochemistry International, 2004, 42, 7, 641-655
dc.identifier.issn 0016-7029
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/38292
dc.description.abstract This study is devoted to accessory fluorite in granites of the Western Massif of the Khangilai pluton, eastern Transbaikalia. This mineral is widespread in Ta-Nb-bearing granites of the Orlovskoe ore deposit. Tantalum-bearing and barren phases of the granites, as well as their varieties with different concentrations of major and ore elements, were sampled at the ore deposit. Fluorite from these samples was studied by photoluminescene, thermoluminescence, EPR, neutron activation, and spectral analysis. Specific features were determined for fluorite from Ta-bearing and barren granites of various intrusive phases and zones of the deposit differing in major-element chemistry and ore potential. The reliability of the conclusions was verified by criteria of nonparametric statistics.
dc.title FLUORITE AS AN INDICATOR OF INTERNAL ZONING AND ORE POTENTIAL OF RARE METAL GRANITES OF THE ORLOVSKOE TANTALUM DEPOSIT, EASTERN TRANSBAIKALIA
dc.type Статья


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