Geological record of thermal pressurization and earthquake instability of subduction thrusts

Abstract

During an earthquake, fault strength decreases with slip over the slip-weakening distance, D c, to a residual strength. The estimation of D c is crucial for the evaluation of fault instability during earthquakes; however, it has been difficult to determine D c from natural faults. We found geological evidence of thermal pressurization from the on-land analog of a subduction thrust exhumed from seismogenic depths; thermal pressurization was indicated by the fluidization of comminuted material and increase in the volume of fluid inclusions by frictional heating. Numerical analysis of thermal pressurization with the constraints on the thickness of the seismic slip zone, the temperature range of frictional heating, and ambient conditions of subduction thrusts indicates that the D c of subduction thrusts ranges from 0.03 to 0.22 m, which is independent of initial pore-fluid pressure on subduction thrusts. The short D c associated with the effect of thermal pressurization on subduction thrusts indicates the occurrence of rapid stress relief and high radiated energy during subduction earthquakes.