Coseismic stress variation and numerical analysis of 2011 Japan-Honshu 9.0 earthquake

Using hybrid hypersingular integral equation-Lattice Boltzmann method [1], [2], [3], the 2011 Japan-Honshu 9.0 earthquake coseismic stress tensor has been explored. A hypothesis based on slip elastic bound back and transient elastic-dynamic ultra low frequency shock plates assumes has been proposed and chaos phenomena in the results has been explained by using this hypothesis.