Earthquake - The dynamic Coulomb stresses transmitted by seismic wave propagation.

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The dynamic Coulomb stresses transmitted by seismic wave propagation for the M=7.2 1944 earthquake on the North Anatolian fault. These were calculated by Kim Olsen (SDSU) on a Los Alamos National Laboratory supercomputer, in collaboration with Ross Stein and Serkan Bozkurt. Once the waves have dispersed, the final pattern is the static Coulomb stress change seen in the other animations.