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- W2350367073 abstract "Although Qinling lead-zinc ores belt related to hydrothermal sedimentary, Zhashan area has more special copper metallogenic background than that of Fengtai area— geological setting, basal of basis. On the basis of fluid inclusions of the Mujiazhuang copper deposit, it is showed that there were two stages of fluid evolution. The first stage is magma hydrothermal with middle temperature, middle and high salinity(CO 2)-H 2O-NaCl fluid, which homogenization temperature are 190~265oC and salinity 12.5~35.34(w t%NaCl),pressure 12.8~21.3MPa.Meanwhile, a large of three facies fluid inclusions with a salty crystal coexistence to vapour faices inclusions are discovered in the high and middle high temperature steps of homotemperature of fluid inclusions for the Mujiazhuang copper deposit. It is suggested that the mineralization fluid is over-saturation and occurring boilization and supposed that there is magma chamber in deep of mining area. The second stage is behind hydrothermal of magma with middle-high temperature, middle and high salinityH 2O-NaCl fluid, which homogenization temperature are 300~350oC and salty 7.4~41.59(w t%NaCl),pressure 10.8~19.3MPa.Boilization is an important mechanism of mineral matters precipitation.On the basis of Geochemistry of fluid inclusion(fluid composition, fluid evolution), it is approved that the mineralization fluid is from the magma water in the Mujiazhuang(the first stage), and is from the formational water and the deep-derived magma in the Mujiazhuang (the second stage). In addition, the hydrogen and oxygen isotopic data of the Mujiazhuang copper deposit supports the results." @default.
- W2350367073 created "2016-06-24" @default.
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- W2350367073 date "2005-01-01" @default.
- W2350367073 modified "2023-09-23" @default.
- W2350367073 title "Evidences of the epigenetic mineralization processand geochemical features of Mujiazhuang copper deposit" @default.
- W2350367073 hasPublicationYear "2005" @default.
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