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- W2391097389 abstract "Through the contrast study of petrography,micro thermometry and laser Raman ingredient analysis of fluid inclusion,this paper has verified the basic nature of ore-forming fluid(temperature,salinity and ingredient)in daqiaowu uranium deposit,discussed the origin of the ore-forming fluid with its structure character and geology-geochemistry character.The testing results indicats that ore-forming temperature of this deposit is between 200℃and 250℃ in main metallogenetic period,which belongs to middle temperature hydrothermal.The ore-forming fluids are of middle-high salinity and rich in valatility suchas CO2,H2,CH4.To sum up,the deposit mineralization process should be affected by the deep fluid primarily,and the ore-forming fluid is mainly the mantle fluid." @default.
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- W2391097389 date "2009-01-01" @default.
- W2391097389 modified "2023-09-23" @default.
- W2391097389 title "Geological-geochemical evidence for deep fluid action in Daqiaowu uranium deposit, Zhejiang province" @default.
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