Physics
Scientist
Institute for Study of the Earth's Interior, Okayama University, Misasa, 682-0193, Tottori-ken, Japan
In situ X-ray observation of iron using Kawai-type apparatus equipped with sintered diamond: Absence of β phase up to 44 GPa and 2100 K
Post-spinel transition in Mg2SiO4 determined by high P-T in situ X-ray diffractometry
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