Physics – Condensed Matter – Materials Science
Scientist
Physics
Condensed Matter
Materials Science
Scientist
Institute of Mineralogy, Petrology and Economic Geology, Faculty of Science, Tohoku University, Aramakiaza-Aoba, Aoba-ku, Sendai, 980-8578 Japan, Sendai, 081 980-8578 Japan of Earth and Planetary Materials Science, Tohoku University, Japan
Dept. Earth Space Science, Osaka University, Toyonaka, Japan; and Space Science, Osaka University, Toyonaka, Japan; of Earth and Planetary Materials Science, Tohoku University, Sendai 9808578, Japan
Tohoku University, 6-3 Aramaki Aoba, Aoba, Sendai, MYG 980-8578, Japan of Earth and Planetary Material Sciences, Tohoku University, Aramaki, Aoba-ku, Sendai, 980-8578, Japan University, Aramaki, Aoba-ku, Sendai, 980-8578, Japan of Mineralogy, Petrology and Economic Geology, Tohoku University, Sendai, Japan
Bayerisches Geoinstitut, Universität Bayreuth, Universitätsstrasse 30, Bayreuth, 95440 Germany
Department of Earth and Planetary Material Sciences, Tohoku University, Sendai, Japan Geoinstitut, Universität Bayreuth, Universitätsstrasse 30, Bayreuth, 95447 Germany
Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University, Sendai, 980-8578, Japan
Institute of Mineralogy, Petrology and Economic Geology, Tohoku University, Sendai, Japan
Bayerisches Geointitut, Universität Bayreuth, 95444 Bayreuth, Germany
Department of Earth and Planetary Materials Science, Tohoku University, Aoba-ku Aramaki Aoba, Sendai 980-8578, Japan; Department of Earth and Space Science, Osaka University, 1-1 Machikaneyama-cho, Toyonaka, Osaka 560-0043, Japan
Department of Earth Science, School of Science, Tohoku University, Sendai, Japan
Department of Earth and Planetary Material Sciences, Tohoku University, 6-3 Aoba, Ara
A breakthrough toward wafer-size epitaxial graphene transfer
Boundary pressure of inter-connection of Fe-Ni-S melt in olivine based on in-situ X-ray tomography: Implication to core formation in asteroids
Compositional effect on the dihedral angle between olivine and Fe-S liquid up to 20 GPa: Possibility of percolative core formation
Density and structure of basaltic magma under high pressure and high temperature
Effect of hydrogen on the melting temperature of FeS at high pressure: Implications for the core of Ganymede
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