In this work, we investigate how grain crushing and pore collapse drive the formation of localized shear zones in granular rocks. Using a Breakage Mechanics-based model—offering an efficient alternative to time-consuming or unfeasible Discrete Element simulations—enriched with a Cosserat continuum and calibrated on Bentheim sandstone, we show that fault cores evolve through coupled compaction, dilation, and permeability changes. Our results highlight the critical role of grain size evolution, grain breakage down to ultrafine particles, and solid fraction in controlling (hydro-)mechanical behavior during seismic slip.
For more details: https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2025JB033062

#Geomechanics #FaultMechanics #GranularMedia #InducedSeismicity @NickCollinsCraft @JeanSulem @ItaiEinav @European Research Council (ERC), @ENSTA







