Inelastic Dilation Causes Coseismic Fault Depressurization

This paper is significant because it highlights the importance of considering inelastic dilation, a phenomenon often overlooked in hydromechanical models, in understanding coseismic pore pressure changes near faults. The study's findings align with field observations and suggest that incorporating inelastic effects is crucial for accurate modeling of groundwater behavior during earthquakes. The research has implications for understanding fault mechanics and groundwater management.