Fig. 6From: Shear strain concentration mechanism in the lower crust below an intraplate strike-slip fault based on rheological laws of rocksTemperature anomaly produced by shear and frictional heating versus depth and distance from the fault for models a W1E, b D1E and c W30E after 3 Myr of fault sliding. “\(\times\)” shows the location of maximum temperature increase; numbers indicate the magnitude of maximum temperature increaseBack to article page