Japan Geoscience Union Meeting 2014

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Symbol S (Solid Earth Sciences) » S-SS Seismology

[S-SS31_30PM1] Comprehensive approach to the intraplate earthquakes

Wed. Apr 30, 2014 2:15 PM - 4:00 PM 502 (5F)

Convener:*Norio Shigematsu(Active Fault and Earthquake Research Center, Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology), Aitaro Kato(Earthquake Research Institute, University of Tokyo), Takuya NISHIMURA(Disaster Prevention Research Institute, Kyoto University), Chair:Takuya NISHIMURA(Disaster Prevention Research Institute, Kyoto University), Haruo Horikawa(Active Fault and Earthquake Research Center, National Institute for Advanced Science and Technology)

3:45 PM - 4:00 PM

[SSS31-P05_PG] Modeling the viscoelastic deformation of the NE Japan arc after the 2011 Tohoku-oki earthquake

3-min talk in an oral session

*Bunichiro SHIBAZAKI1, Yoshihiko NAKAI1, Jun MUTO2, Takeshi IINUMA3 (1.International Institute of Seismology and Earthquake Engineering, Building Research Institute, 2.Department of Earth Sciences, Tohoku University, 3.International Research Institute of Disaster Science, Tohoku University)

Keywords:2011Tohoku-oki earthquake, NE Japan arc, Viscoelastic deformation

The rheological structure of the Northeastern Japan arc crust and the upper mantle is heterogeneous along and transverse to the arc. Shibazaki et al. (2014) developed a model of the stress state of the Northeastern Japan island-arc crust using a finite element method with viscoelasticity and elastoplasticity. They reproduced several elongated low-stress regions transverse to the arc with viscous deformation that corresponds to hot fingers (high-temperature regions in the mantle wedge). The viscous relaxation process after the 2011 Tohoku-oki earthquake could be affected by the existence of low-viscosity regions caused by hot fingers. A three-dimensional (3D) finite element model was developed to investigate the viscoelastic deformation processes with heterogeneous viscosity distribution after the 2011 Tohoku-oki earthquake. The model considers the realistic crustal and mantle structures, viscoelasticity (Maxwell or Burgurs rheology), and coseismic fault slip distribution obtained by Iinuma et al. (2012). For simplicity, only the elastic crust and viscoelastic mantle structure were considered. The westward movement near the trench and eastward movement in the inland region due to viscoelastic relaxation were reproduced, which are consistent with the observations. We also consider the local low viscosity region in the Northeastern Japan arc crust. In this case, extensional viscous strain concentrates on this region. We report the numerical results that take into account the realistic 3D heterogeneous viscosity distribution in the crust and the upper mantle beneath the Northeastern Japan island arc.