Fig. 7From: Shear strain concentration mechanism in the lower crust below an intraplate strike-slip fault based on rheological laws of rocks a Surface heat flow for simulation of interplate (broken line) and intraplate (solid line) strike-slip faults. b Enlarged view of the fault core, the sharp peak above the fault (\(x = {\sim}0\)) was created by fault frictional heatingBack to article page