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Hydrogen and Oxygen Isotope Fractionation Mechanism in the Hydrothermal System and Its Geologic Significance 被引量:1
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作者 Chen Zhensheng Zhang Ligang Yichang Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences, Yichang, Hubei Jiang Minxi 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 1992年第4期397-409,共13页
The geochemical behaviors of hydrogen and oxygen isotopes in the hydrothermal system and their inher-ent relationship with the water / rock exchange are discussed in this paper In addition to the temperature con-ditio... The geochemical behaviors of hydrogen and oxygen isotopes in the hydrothermal system and their inher-ent relationship with the water / rock exchange are discussed in this paper In addition to the temperature con-ditions, the effective W / R ratio is another factor controlling the changes in H and O isotope compositions ofthe altered rock and hydrothermal water. Besides, the application and geological significance of the water-rockexchange theory are also discussed in the light of the H and O isotope compositions and their variation charac-teristics of the mineralizing hydrothermal water and altered rocks from several mineral deposits. Finally, abrief evolutional model of H and O istotope compositions of meteoric and magmatic hydrothermal waters in ahydrothermal system is given. 展开更多
关键词 hydrothermal system isotope fractionation mechanism water/rock exchnage effective W/R ratio evolutional model
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