Physics – Condensed Matter – Materials Science
Scientist
Physics
Condensed Matter
Materials Science
Scientist
Geodynamics Research Center, Ehime University, Matsuyama 790-8577, Japan
Geodynamics Research Center, Ehime University, Matsuyama, Japan
Geodynamics Research Center, Ehime University, Bunkyo-cho 2-5, Matsuyama, Ehime, 790-8577, Japan
Research School of Earth Sciences, The Australian National University, Canberra, A.C.T. 2601 Australia
Geodynamics Research Center, Ehime University, Matsuyama, Ehime 790-8577, Japan Research Center, Ehime University, 2-5 Bunkyo-cho, Matsuyama 790-8577, Japan
Geodynamics Research Center, Ehime University, Bunkyo-cho 2-5, Matsuyama 790-8577, Japan
Geodynamic Research Center, Ehime University, Matsuyama 790-8577, Japan
Department of Earth Sciences, Faculty of Science, Nagoya University, Nagoya 464 Japan
Geodynamics Research Center, Ehime University, 2-5 Bunkyo-cho, Matsuyama, Ehime 790-8577, Japan
Geodynamics Research Center, Ehime University, Matsuyama, 790-8577 Ehime, Japan
Geodynamics Research Center, Ehime University, Matsuyama, Ehime, Japan
Hokkaido University, Sapporo, Japan
Australian National University, Canberra, Australia
Research School of Earth Sciences, Australian National University, Canberra, A.C.T. 2001 Australia
Research School of Earth Sciences, Australian National University, Canberra, A.C.T. 2601 Australia
Department of Earth Sciences, Ehime University, Matsuyama 790, Japan
Research School of Earth Sciences, Australian National University, Canberra A.C.T. 2601 Australia
Earth and Planetary Sciences, Tokyo Institute of Technology, 2-12-1 Ookayama, Meguro-ku, Tokyo 152, Japan
Ehime Univ., Matsuyama, Japan
A new high-pressure form of KAlSi3O8 under lower mantle conditions
Amorphization of Serpentine at High Pressure and High Temperature
An experimental investigation of the pyroxene-garnet transformation in a pyrolite composition and its bearing on the constitution of the mantle
An experimental study of the garnet-perovskite transformation in the system MgSiO3-Mg3Al2Si3O12
Change of olivine a-axis alignment induced by water: Origin of seismic anisotropy in subduction zones
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