Fig. 10From: Shear strain concentration mechanism in the lower crust below an intraplate strike-slip fault based on rheological laws of rocksShear strain rate for models a W1E, b W1C, d D1E and e D1C. c Linear model deformed by diffusion creep has a constant grain size of 215 \(\upmu \mathrm{m}\) (minimum grain size of model W1E)Back to article page