C. Arson

Seismicity migration from fluid injection: Laboratory experiments and numerical models illuminate volume-driven versus pressure-diffusion-driven migration

23 Fluid injection into the subsurface can induce seismicity by reactivating shear rupture, which 24 typically produces larger earthquake magnitudes than tensile rupture. In laboratory shear 25 rupture experiments, pressurization of the entire fault is often limited because large unconfined 26 samples allow fluid to le...