Astronomy and Astrophysics – Astronomy
Scientist
Astronomy and Astrophysics
Astronomy
Scientist
Earthquake Research Institute, University of Tokyo, 1-1-1 Yayoi, Bunkyo-ku, Tokyo, 113-0032, Japan tokyo.ac.jp tokyo.ac.jp for Research on Earth Evolution, JAMSTEC, Yokosuka 237-0061, Japan
Yokohama City University, Department of Physics, Kanazawa-ku, Yokohama 236 Japan
Nagoya University, Japan
Institute for Research on Earth Evolution, Independent Administrative Institution, Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan
Japan Agency for Marine Earth Science and Technology, Yokohama, Japan
Department of Earth Sciences, Nagoya University, Chikusa, Nagoya 464, Japan
Institute for Research on Earth Evolution, JAMSTEC, 2-15 Natsushima-cho, Yokosuka, Japan. of Earth Sciences, Nagoya University, Chikusa, Nagoya 464 Japan
Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan
Japan Agency of Marine-Earth Science and Technology, Natsushima 2-15, Yokosuka 237-0061, Japan
University of Tokyo, Tokyo, Japan
Department of Physics, Yokohama City University, Mutsuura, Kanazawa-ku, Yokohama Japan
Nagoya Univ., Japan
Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Kanagawa 237-0061, Japan
Institute For Research on Earth Evolution, Japan Agency of Marine-Earth Science and Technology, 2-15 Natsushima-cho, Yokosuka, Kanagawa 237-0061, Japan
Department of Earth Sciences, Nagoya University, Chikusa, Nagoya Japan
Earthquake Research Institute, University of Tokyo, Yayoi 1-1-1, Bunkyo-ku, Tokyo 113-0032, Japan for Frontier Research on Earth Evolution, JAMSTEC, Yokosuka, Japan. ; Earthquake Research Institute, University of Tokyo, Tokyo, Japan
Geophysical Institute, University of Tokyo, Japan
Institute for Research on Earth Evolution, Independent Administrative Institution, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan
Department of Earth Sc
A joint interpretation of electromagnetic and seismic tomography models suggests the mantle transition zone below Europe is dry
A seismological constraint on the depth of basalt-eclogite transition in a subducting oceanic crust
A self-organized model of earthquakes with constant stress drops and the b-value of 1
Background Love and Rayleigh waves simultaneously generated at the Pacific Ocean floors
DEGREE-2 Pattern of Attenuation Structure in the Upper Mantle from Apparent Complex Frequency Measurements of Fundamental Spheroidal Modes
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