Shear heating during distributed fracturing and pulverization of rocks

We provide estimates of temperature changes produced in fault damage zones during brittle deformation associated with distributed cracking and pulverization. In contrast to localized faulting accompanied by signifi cant frictional weakening, the relatively high friction coeffi cient on the multitudinous small cracks generated in the fracturing process can lead to signifi cant shear heating. Simple calculations with parameter values constrained by laboratory experiments and simulations indicate that the temperature can increase during the generation of rock damage and pulverization by 100 C or more. The results can help explain signatures of elevated temperature observed in geometrically complex fault zone sections with signifi cant rock damage and regions with broad distributed deformation.