Physics – Geophysics
Scientist
Physics
Geophysics
Scientist
Department of Mineralogy, Petrology, and Economic Geology, Tohoku University, Sendai, Japan
Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University, Sendai 980-8578, Japan; V.S. Sobolev Institute of Geology and Mineralogy, SB RAS, Novosibirsk, 630090, Russia
Institute of Mineralogy, Petrology and Economic Geology, Faculty of Sciences, Tohoku University, Aoba-ku, 980-8578, Sendai, Japan
Institute of Mineralogy, Petrology and Economic Geology, Faculty of Science, Tohoku University, Sendai, Japan
Institute of Mineralogy, Petrology, and Economic Geology, Tohoku University, Sendai 980-8578, Japan
Institute of Mineralogy, Petrology and Economic Geology, Faculty of Science, Tohoku University, Aoba-ku, Sendai 980-8578, Japan
Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University, Sendai 980-8578, Japan; Geophysical Laboratory, Carnegie Institution of Washington, 5251 Broad Branch Rd. NW, Washington, DC 20015, USA
Institute of Mineralogy, Petrology and Economic Geology, Faculty of Science, Tohoku University, Aoba-ku, 980-8578, Sendai, Japan
Institute of Mineralogy, Petrology and Economic Geology, Tohoku University, 980-8578, Sendai, Japan
Faculty of Science, Institute of Mineralogy, Petrology and Economic Geology, Tohoku University, Aza Aoba Aramaki, Sendai 980-8578, Japan
Absence of density crossover between basalt and peridotite in the cold slabs passing through 660 km discontinuity
Hydrous solidus of CMAS-pyrolite and melting of mantle plumes at the bottom of the upper mantle
In situ X-ray diffraction study of post-spinel transformation in a peridotite mantle: Implication for the 660-km discontinuity [rapid communication]
In situ X-ray diffraction study of the effect of water on the garnet perovskite transformation in MORB and implications for the penetration of oceanic crust into the lower mantle
Melting relations of hydrous pyrolite in CaO-MgO-Al2O3-SiO2-H2O system at the transition zone pressures
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