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- W2360449153 abstract "The Tangjiaping Mo deposit in Henan Province is located in the Dabie orogenic belt.In quartz three types of fluid inclusions can be observed,namely CO2-rich(bearing) fluid inclusions,aqueous solution fluid inclusions and daughter -crystal -bearing fluid inclusions,based on the petrography,microthermometric measurement and Laser Raman microprobe analysis.The homogenization temperatures vary from 126.7° C to 472.1°C,the calculated fluid salinities cluster in two ranges,i.e.,(0.18-14.21) wt% NaCl.eqv and(33.10-54.37) wt% NaCl.eqv,with densities changing from 0.38 to 1.21 g/cm3.Daughter minerals,mainly halite and metallic sulfide,can be recognized in fluid inclusions.The homogenization temperature and salinity of fluid inclusions reduce gradually outward from the center of ore-forming porphyry system.From early to late the fluid system evolved from and high temperature and high salinity to low temperature,and low salinity;and the trapped pressure reduced,indicating the mineralization depth became shallower gently.The Re-Os isotopic model ages of molybdenite are between 113 Ma and 118 Ma,about 10 Ma later than the crystalline age of the Tangjiaping granite porphyry.The ore-system was formed in waning stage extension setting of the inter-continental collision between Yangtze Block and North China Block." @default.
- W2360449153 created "2016-06-24" @default.
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- W2360449153 date "2008-01-01" @default.
- W2360449153 modified "2023-09-23" @default.
- W2360449153 title "Hydrothermal metallogeny of the Tangjiaping molybdenum deposit,Henan Province" @default.
- W2360449153 hasPublicationYear "2008" @default.
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