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Initial Dissolution Behavior of Granite by Hydrothermal Solution in the Temperature Range between 200°C and 350°C
Initial Dissolution Behavior of Granite by Hydrothermal Solution in the Temperature Range between 200°C and 350°C
2003
Yi Wang
Nobuo Hirano
Noriyoshi Tsuchiya
Katsuto Nakatsuka
Nakamichi Yamasaki
Takahiro Ishida
Keywords:
Feldspar
Dissolution
Quartz
Hydrothermal circulation
Geochemistry
Geology
Atmospheric temperature range
Mineralogy
Correction
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