Mathematics
Logic
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National Institute of Polar Research, Tokyo, Japan
Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Kanagawa, Japan
Institute for Research on Earth Evolution, Japan Agency for Marin-Earth Science and Technology, Yokosuka, Japan
Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Japan
Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Kanagawa 237-0061, Japan
Institute for Frontier Research on Earth Evolution, Japan Marine Science and Technology Center, Yokosuka, Kanagawa 237-0061, Japan
Institute for Frontier Research on Earth Evolution, Yokosuka, 237-0061, Japan
Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan
IFREE, JAMSTEC, Kouto1-1-1, Sayo, Hyogo 679-5198, Japan
Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, Natsushima-cho, Yokosuka, Kanagawa 237-0061, Japan
Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, 2-15 Natsushima-cho, Yokosuka, Kanagawa 237-0061, Japan
Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, Kanagawa, Japan
Institute for Frontier Research on Earth Evolution, Yokosuka, Japan
Japan Marine Science and Technology Center, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan
Institute for Solid State Physics, University of Tokyo, Kashiwa 277-8581, Japan
Consortium for Advanced Radiation Sources, University of Chicago, Chicago, IL 60637, USA
Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, 2-15 Natsushima-Cho, Yokosuka-city, Kanagawa 237-0061, Japan
Institute for Research on Earth Evolution, Jamstec, Yokosuka 237-0061, Japan
Aluminous hydrous mineral δ-AlOOH as a carrier of hydrogen into the core-mantle boundary
Approach to the mineralogy of the lower mantle by a combined method of a laser-heated diamond anvil cell experiment and analytical electron microscopy
Chemical equilibrium between ferropericlase and molten iron to 134 GPa and implications for iron content at the bottom of the mantle
Determination of post-perovskite phase transition boundary in MgSiO3 using Au and MgO pressure standards
Determination of post-perovskite phase transition boundary up to 4400 K and implications for thermal structure in D″ layer
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