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- W2365960876 abstract "The Hunan-Guangxi region is a region of Mesozic-Cenozoic tectono-magmatic activization. Uranium mineralization is evidently controlled by the activization of this age and characterized by a specific mineralization series and association of deposit types. Uraniferous hosts are various, but the mineralization took place in the same period and under the same tectonic condition. Uranium was enriched by polystage, polysource and porygenesis. Based on this, a built-up and progressively enriched model of mineralization was put forward. It is considered that the formation of economic uranium deposits proceeded from primary enrichment prior to and during ore formation to multiple-enrichment during deuterogene. It was a constantly built-up and progressively enriched course from early to late. In the last part of the article, some targets for future survey and exploration are suggested." @default.
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- W2365960876 date "1985-01-01" @default.
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- W2365960876 title "SOME CHARACTERISTICS OF URANIUM MINERALIZATION IN THE HUNAN-GUANGXI REGION" @default.
- W2365960876 hasPublicationYear "1985" @default.
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