Physics
Scientist
Earthquake Research Institute, Tokyo University, Tokyo, Japan
Earthquake Research Institute, University of Tokyo 1-1-1, Yayoi, Bunkyo-ku, Tokyo 113-0032, Japan
Earthquake Research Institute, University of Tokyo, Yayoi 1-1-1, Bunkyo-ku, Tokyo 113-0032, Japan. ; Seismological Laboratory, University of California at Berkeley 215 McCone Hall, Berkeley, CA 94720-4760, USA Research Institute, University of Tokyo, Yayoi 1-1-1, Bunkyo-ku, Tokyo 113-0032, Japan. ; Seismological Laboratory, 215 McCone Hall, University of California, Berkeley, CA 94720-4760, USA
Tokyo Univ., Tokyo, Japan
Graduate School of Science and Technology, Chiba University, Chiba, Japan
Earthquake Research Institute, Tokyo University, Yayoi 1-1-1, Bunkyo-ku, Tokyo 113-0032, Japan.
Department of Earth and Planetary Physics, Faculty of Science, Tokyo University, Hongo 7-3-1, Bunkyo-ku, Tokyo, 113-0033, Japan.
Earthquake Research Institute, University of Tokyo, Yayoi 1-1-1, Bunkyo-ku, Tokyo 113-0032, Japan
Earthquake Research Institute, University of Tokyo, Tokyo, Japan
Akita Prefectural University, Department of Electronic and Information Systems, 84-4 Tsuchiya-Ebinokuchi, Yurihonjo, 015-0055, Japan Tokyo, Japan
Department of Earth and Planetary Science, Graduate School of Science, University of Tokyo, Tokyo, Japan
Department of Earth and Planetary Physics, Faculty of Science, Tokyo University, Hongo 7-3-1, Bunkyo-ku, Tokyo, Japan
Earthquake Research Institute, University of Tokyo, Bunkyo-ku, Tokyo 113-0032, Japan
Earthquake Research Institute, The University of Tokyo, 1-1-1 Yayoi, Bunkyo-ku, Tokyo 113-0032, Japan.
TMA / Norcal, Richmond, CA.
3D effects of sharp boundaries at the borders of the African and Pacific Superplumes: Observation and modeling
A low-velocity conduit throughout the mantle in the robust component of a tomography model
A new method for computing highly accurate DSM synthetic seismograms
A strategy of detection of the lunar core using a single seismic station
Accurate numerical methods for solving the elastic equation of motion for arbitrary source locations
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