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- W2357368431 abstract "Comprehensive studies were made for fluid inclusions in minerals of Dongguashan strata-bound skarn deposit. It is demonstrated that the ore forming fluid is a high temperature (350～400℃), high density (larger than 1.1 g/cm 3 ) and high salinity (13.45%～48% NaCl) hydrothermal fluid. The fluid is also characterized by obvious fractionation of REE, enriched in LREE and strong negative Eu anomaly. The ore forming process took place under relative acidic and reductive conditions. The fluid transported as isothermal process under a particularly ore forming environment. It is postulated that the ore forming fluid was suplied by both magmatic and strata sources. The Dongguashan deposit is a typical multi source of ore forming materials, multi ore forming stages and multi controllong factors strata bound skarn deposit." @default.
- W2357368431 created "2016-06-24" @default.
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- W2357368431 date "2002-01-01" @default.
- W2357368431 modified "2023-09-25" @default.
- W2357368431 title "THE CHARACTERISTICS OF ORE-FORMING FLUID OF DONGGUASHAN STARATA- BOUND SKARN Cu DEPOSIT AND ITS SIGNIFICANCE FOR DEPOSIT GENESIS" @default.
- W2357368431 hasPublicationYear "2002" @default.
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