Induced seismicity is an inherent risk associated with geologic carbon storage (GCS) in deep rock formations that could contain undetected faults prone to failure. Modeling‐based risk assessment has been implemented to quantify the potential of injection‐induced seismicity, but typically simplified multiscale geologic features or neglected multiphysics coupled mechanisms because of the uncertainty in field data and computational cost of field‐scale simulations, which may limit the reliable prediction of seismic hazard caused by industrial‐scale CO2 storage. The degree of lateral continuity of the stratigraphic interbedding below the reservoir and depth‐dependent fault permeability can enhance or inhibit pore‐pressure diffusion and corresponding poroelastic stressing along a basement fault. This study presents a rigorous modeling scheme with optimal geological and operational parameters needed to be considered in seismic monitoring and mitigation strategies for safe GCS.

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