Physics
Scientist
Department of Earth Sciences, Faculty of Science, Ehime University, Matsuyama 790, Japan
Department of Earth and Planetary Systems Science, Hiroshima University, Higashi-Hiroshima, Hiroshima 793-8526, Japan
Department of Earth and Planetary Systems Science, Hiroshima University, Higashi-Hiroshima 739-8526, Japan
Department of Earth and Planetary Systems Science, Hiroshima University, Hiroshima 739-8526, Japan
Center for High Pressure Research and Mineral Physics Institute, State University of New York at Stony Brook, Stony Brook, NY 11794-2100, USA, USLaboratoire de Structure et Propriétés de l'Etat Solide-URA CNRS 234, Université des Sciences et Technologies de Lille, 59655 Villeneuve d'Ascq Cedex, France, FRCenter for High Pressure Research and Mineral Physics Institute, State University of New York at Stony Brook, Stony Brook, NY 11794-2100, USA, USLaboratoire de Structure et Propriétés de l'Etat Solide-URA CNRS 234, Université des Sciences et Technologies de Lille, 59655 Villeneuve d'Ascq Cedex, France, FR
Dislocation microstructures in naturally deformed silicate garnets
Origin of seismic anisotropy in the D″ layer inferred from shear deformation experiments on post-perovskite phase
Plastic deformation of silicate garnetsI. High-pressure experiments
Precise determination of phase relations in pyrolite across the 660km seismic discontinuity by in situ X-ray diffraction and quench experiments
Rheological contrast between garnet and clinopyroxene in the mantle wedge: An example from Higashi-akaishi peridotite mass, SW Japan
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