A tensorially generalised version of the Terracotta clay model, specialised to direct shear, yields a friction law for fault gouges whose rate-and-state, dilational, and thickness-dependent behaviour is validated against clay-gouge experiments.
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Hydrodynamics of fault gouges from constitutive modelling to the physics of friction
A tensorially generalised version of the Terracotta clay model, specialised to direct shear, yields a friction law for fault gouges whose rate-and-state, dilational, and thickness-dependent behaviour is validated against clay-gouge experiments.