Physics
Scientist
Japan Agency for Marine-Earth Science and Technology, 2-15, Natsushima-cho, Yokosuka 237-0061, Japan. for Frontier Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, Yokohama Institute of Earth Sciences, Showa-machi, 3173-25, Kanazawa, Yokohama 236-0001, Japan for Frontier Research on Earth Evolution, Japan Marine Science and Technology Center, 3173-25, Showa-machi, Kanazawa-ku, Yokohama 236-0001 Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan
Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, 3173-25 Showa-machi, Kanazawa-ku, Yokohama, 236-0001, Japan
Institute for Frontier Research on Earth Evolution, Japan Marine Science and Technology Center, 3173-25, Showa-machi, Kanazawa, Yokohama 236-0001, Japan
Frontier Reasearch Program for subduction Dynamics, Japan marine Science and Technology Center Natsushima-cho 2-15, 237-0061, Yokokosuka, Japan
Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan
Institute for Frontier Research on Earth Evolution, Japan Marine Science and Technology Center, Natsushima-cho 2-15, 237-0061, Yokosuka, Japan
Frontier Research Program for Subduction Dynamics, Japan Marine Science and Technology Center, Yokohama School of Earth Sciences, Yokohama, Japan
Marine Technology Center, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan
Institute for Frontier Research on Earth Evolution, Japan Marine Science and Technology Center, 3173-25 Showa-machi, Yokohama 236-0001, Japan
A numerical simulation of earthquake cycles along the Nankai Trough in southwest Japan: lateral variation in frictional property due to the slab geometry controls the nucleation position
A simple explanation for the occurrence of the 1911 Morgan Hill earthquake in the stress shadow of the 1906 San Francisco earthquake
A subducted oceanic ridge influencing the Nankai megathrust earthquake rupture
A subducting seamount beneath the Nankai accretionary prism off Shikoku, southwestern Japan
An anomalous spatial pattern of shear-wave splitting observed in Ocean Bottom Seismic data above a subducting seamount in the Nankai Trough
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