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富二氧化碳(CO_2)的水很久以来就引起人们的关注。White(1957)首先提出含碳酸盐的岩石在地壳深处通过变质作用产生富CO_2的水。CO_2似乎是地表逸出物中最显著的变质组分,它或是以气体形式逸出,或是以大量的重碳酸盐溶于水中。在研究加里福尼亚州圣安德烈斯断层中发
Carbon dioxide (CO2) water has drawn much attention for a long time. White (1957) first proposed carbonate-bearing rocks to produce CO2-rich water through metamorphism deep in the crust. CO 2 appears to be the most prominent metamorphic component of the earth’s surface discharge, either as a gas or as heavy bicarbonate in water. Made in the study of the San Andres Fault in California