Abstract:<p>Bleached rocks are commonly formed from CO<sub>2</sub>-saturated water leakage to the surface. It could provide opportunities to understand the mechanisms and controlling factors associated with injected and sequestrated CO<sub>2</sub> leakages as well as fluid flow in the subsurface. In this study, we investigated the various bleaching patterns and their related structures in order to understand the characteristics of fluid-flow migratio… Show more
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