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Abstract The geochemical behaviors of hydrogen and oxygen isotopes in the hydrothermal system and their inherent relationship with the water / rock exchange are discussed in this paper. In addition to the temperature conditions, the effective W / R ratio is another factor controlling the changes in H and O isotope compositions of the altered rock and hydrothermal water. Besides, the application and geological significance of the water‐rock exchange theory are also discussed in the light of the H and O isotope compositions and their variation characteristics of the mineralizing hydrothermal water and altered rocks from several mineral deposits. Finally, a brief evolutional model of H and O istotope compositions of meteoric and magmatic hydrothermal waters in a hydrothermal system is given.
Acta Geologica Sinica (English Edition) – Wiley
Published: Dec 1, 1992
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