Physics
Scientist
Department of Material Physics, Faculty of Engineering Sciences, Osaka University, Toyonaka, Osaka Japan
Institute for Thermal Spring Research, Okayama University, Okayama, Japan
Institute for Thermal Spring Research, Okayama University, Misasa, Tottori-ken 682-02 Japan
Okayama University, Misasa, Japan
Institute for Thermal Spring Research, Okayama University Tottori-ken 682-02 Japan
University of Tokyo, Tokyo, Japan
Institute for Study of the Earth's Interior, Okayama University, Misasa, Japan
Institute for Study of the Earth's Interior, Okayama University, Japan
Institute for Study of the Earth's Interior, Okayama University, Misasa, Tottori-ken 682-0193, Japan
Institute for Study of the Earth's Interior, Okayama University, Misasa, Tottori 682-0.193, Japan
Institute for Study of the Earth's Interior, Okayama University, Misasa, 682-0193, Tottori, Japan
Okayama Univ., Misasa, Japan
Okayama University, Japan
Institute for Study of the Earth's Interior, Okayama University, Misasa, 682-0193, Tottori-ken, Japan
Institute for Study of the Earth's Interior, Okayama University, Yamada 827, Misasa, Tottori 682-0193, Japan
Department of Earth and Space Sciences, State University of New York, Stony Brook, NY 11794 USA
Okayama University, Tottori, Japan
Institute for Thermal Spring Research, Okayama University, Misasa, Tottori, Japan
Institute for Study of the Earth's Interior, Okayama University, Misasa, Tottori-ken 682-0193, Japan; Department of Geology, Peking University, Beijing 100871, China
Institute for Study of the Earth's Interior, Okayama University, Misasa, Tottori 682-02, Japan
Institute for Thermal Spring Research, Okayama University, Misasa, Tottori-ken, 682-02 Japan
A new 6-axis apparatus to squeeze the Kawai-cell of sintered diamond cubes
Adiabatic temperature profile in the mantle
Aseismicity in the lower mantle by superplasticity of the descending slab
Behaviour of noble gases during dehydration processes in the subducting oceanic crust
Correction to “P-V-T relations of the MgSiO3 perovskite determined by in situ X-ray diffraction using a large-volume high-pressure apparatus”
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