Numerical simulation of co-seismic deformation of 2011 Japan Mw9. 0 earthquake

Co-seismic displacements asaociated with the Mw9. 0 earthquake on March 11, 2011 in Japan are numerically simulated on the basis of a fmite-fault dislocation model with PSGRN/PSCMP software. Compared with the inland GPS observation, 90% of the computed eastward, northward and vertical displacements have residuals less than 0. 10 m, suggesting that the simulated results can he, to certain extent, used to demonstrate the co-seismic deformation in the near field. In this model, the maximum eastward displacement increases from 6 m along the coast to 30 m near the epicenter, where the maximum southward displacement is 13 m. The three-dimensional display shows that the vertical displacement reaches a maximum uplift of 14. 3 m, which is comparable to the tsunami height in the near-trench region. The maximum subsidence is 5. 3 m.