*Kazuki Matsuyama 1,2, Miki Tasaka3, Lars N. Hansen4, Katsuyoshi Michibayashi1,5, Takehiko Hiraga6
(1. Department of Earth and Planetary Sciences, GSES, Nagoya University, 2. Géosciences Montpellier, Université de Montpellier, CNRS, Montpellier, France, 3. Department of Geoscience, Faculty of Science, Shizuoka University, 4. Department of Earth and Environmental Sciences, University of Minnesota Twin Cities, Minneapolis, MN, USA, 5. Volcanoes and Earth's Interior Research Center, IMG, JAMSTEC, 6. Earthquake Research Institute, The University of Tokyo)
Keywords:Crystallographic preferred orientations, Olivine, Deformation mechanism, Seismic anisotropy