CO 2 geological sequestration (CGS) into deep saline formations is promoted as a key technology to reduce the loading of anthropogenic greenhouse gases into the atmosphere to mitigate global warming (Bachu, 2003;IPCC, 2005;Lackner, 2003;U.S. DOE, 2015). During and post-injection of supercritical CO 2 (ScCO 2 ), existing faults or pressure-induced fractures in the confining caprock of the storage formation pose a potential leakage risk of formation brine and CO 2 (Celia et al.