Member

IIDAKA, Takashi Professor Center for Integrated Disaster Information Research Office: ERI-1-405 TEL: +81-3-5841-5804 FAX: +81-3-5689-7234 E-mail: HP:
Research Field Seismology for disaster prevention, Observational Seismology Current Research Japan is one of the active regions because Pacific and Philippine Sea plates are descending beneath the island arc. Many earthquakes occur in Japan. Our group is working on seismic studies for the prevention and mitigation of disasters. Research of crustal and mantle structures in this region is very important to understand the cause of earthquake and dynamics of subduction zones. Our group is working on the research to reveal the dynamics of the subduction zones and island arc regions by seismic observations considering tectonic background. Representative Publications 1. Iidaka, T., T. Igarashi, A. Hashima, A. Kato, T. Iwasaki, The Research Group for the Joint Seismic Observations at the Nobi Area, Receiver function images of the distorted Philippine Sea Slab contact with the continental crust: implications for generation of the 1891 Nobi earthquake (Mj 8.0), Tectonophys., 717, 41–50, 2017. 2. Iidaka, T., E. Kurashimo, T. Iwasaki1, R. Arai, A. Kato, H. Katao, F. Yamazaki, The Research Group for the 2007 Atotsugawa Fault Seismic Expedition, Large heterogeneous structure beneath the Atotsugawa Fault, central Japan, revealed by seismic refraction and reflection experiments, Tectonophysics, 657，144–154，doi:10.1016/j.tecto.2015.06.031，2015 3. Iidaka, T., J. Muto, K. Obara, T. Igarashi and B. Shibazaki, Trench-parallel crustal anisotropy along the trench in the fore-arc region of Japan, Geophys. Res. Lett., DOI: 10.1002/2013GL058359, 2014.

IIDAKA, Takashi

Professor
Center for Integrated Disaster Information Research

Office: ERI-1-405
TEL: +81-3-5841-5804
FAX: +81-3-5689-7234
E-mail:
HP:

Research Field

Seismology for disaster prevention, Observational Seismology

Current Research

Japan is one of the active regions because Pacific and Philippine Sea plates are descending beneath the island arc. Many earthquakes occur in Japan. Our group is working on seismic studies for the prevention and mitigation of disasters. Research of crustal and mantle structures in this region is very important to understand the cause of earthquake and dynamics of subduction zones. Our group is working on the research to reveal the dynamics of the subduction zones and island arc regions by seismic observations considering tectonic background.

Representative Publications

1. Iidaka, T., T. Igarashi, A. Hashima, A. Kato, T. Iwasaki, The Research Group for the Joint Seismic Observations at the Nobi Area, Receiver function images of the distorted Philippine Sea Slab contact with the continental crust: implications for generation of the 1891 Nobi earthquake (Mj 8.0), Tectonophys., 717, 41–50, 2017.
2. Iidaka, T., E. Kurashimo, T. Iwasaki1, R. Arai, A. Kato, H. Katao, F. Yamazaki, The Research Group for the 2007 Atotsugawa Fault Seismic Expedition, Large heterogeneous structure beneath the Atotsugawa Fault, central Japan, revealed by seismic refraction and reflection experiments, Tectonophysics, 657，144–154，doi:10.1016/j.tecto.2015.06.031，2015
3. Iidaka, T., J. Muto, K. Obara, T. Igarashi and B. Shibazaki, Trench-parallel crustal anisotropy along the trench in the fore-arc region of Japan, Geophys. Res. Lett., DOI: 10.1002/2013GL058359, 2014.