Physics
Scientist
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; School of Earth and Space Science, Peking University, Beijing 100871, China
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, Japan
Correction to “P-V-T relations of the MgSiO3 perovskite determined by in situ X-ray diffraction using a large-volume high-pressure apparatus”
P-V-T relations of wadsleyite determined by in situ X-ray diffraction in a large-volume high-pressure apparatus
Phase relations of CaAl4Si2O11 at high-pressure and high-temperature with implications for subducted continental crust into the deep mantle
Pressure generation and investigation of the post-perovskite transformation in MgGeO3 by squeezing the Kawai-cell equipped with sintered diamond anvils
Thermal expansion of forsterite at high pressures determined by in situ X-ray diffraction: The adiabatic geotherm in the upper mantle
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