Physics – Plasma Physics
Scientist
Physics
Plasma Physics
Scientist
Okayama University, Misasa, Japan
Magma Factory, Earth and Planetary Sciences, Tokyo Institute of Technology, Ookayama, Meguro-ku, Tokyo 152-8551, Japan
Department of Earth and Planetary Sciences, Tokyo Institute of Technology, 2-12-1 Ookayama, Meguro, Tokyo 152-8551, Japan
Okayama University, Japan
Department of Earth and Planetary Sciences, Magma Factory, Tokyo Institute of Technology, 2-12-1 Ookayama, Meguroku, Tokyo, Japan
Magma Factory, Department of Earth & Planetary Sciences, Tokyo Institute of Technology, 2-12-1 Ookayama Meguroku, Tokyo 152-8551, Japan
Department of Earth and Planetary Sciences, Tokyo Institute of Technology, 2-12-1 Ookayama, Meguro-ku, Tokyo 152-8551, Japan
Institute for Thermal Spring Research, Okayama University, Misasa, Tottori-ken, 682-02 Japan
Magma Factory, Earth and Planetary Sciences, Tokyo Institute of Technology, 2-12-1 Ookayama, Meguro-ku, Tokyo 153-8551, Japan
Okayama University, Misasa, Tottori, Japan
Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo, 152-8551 Japan; Institute for Research on Earth Evolution, Jamstec, 2-15 Natsushima-Cho, Yokosuka, 237-0061 Japan of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo, Japan
Magua Factory, Earth and Planetary Science Department, Tokyo Institute of Technology, 2-12-1 Ookayama, Meguroku, Tokyo 152, Japan
Earth and Planetary Sciences, Tokyo Institute of Technology, Tokyo 152, Japan
Tokyo Institute of Technology, Earth and Planetary Sciences, Tokyo, Japan Factory, Earth and Planetary Sciences, Tokyo Institute of Technology, 2-12-1 Ookayama, Meguro-ku, 152-8551, Tokyo, Japan
Controls on eruptive style for North Arch lavas
Density of MORB eclogite in the upper mantle
Effects of laser wavelength and density scalelength on absorption of ultrashort intense lasers on solid-density targets
Evidences for the terrestrial magma ocean from high-pressure melting experiments
Geochemical properties of lithospheric mantle beneath the Sino-Korea craton; evidence from garnet xenocrysts and diamond inclusions
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