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This study aims to understand how basaltic rocks absorb CO 2 in high-temperature alteration zones in the subseafloor, and to reconstruct hydrothermal alteration processes such as carbonatization of Archean greenstones. To this end, we conducted two laboratory experiments, simulating hydrothermal reactions between basalt (synthesized under quartz–fayalite–magnetite oxygen fugacity) and CO ...
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