Crystallographic-preferred-orientation of (Mg,Fe)SiO3-bridgmanite : implications for the mantle dynamics in the lower mantle

Noriyoshi Tsujino1,2, Yu Nishihara3, Daisuke Yamazaki4, Yusuke Seto5, Yuji Higo1 and Eiichi Takahashi6, (1)Japan Synchrotron Radiation Research Institute, Hyogo, Japan, (2)Yale University, Geology & Geophysics, New Haven, CT, United States, (3)Ehime University, Geodynamics Research Center, Matsuyama, Japan, (4)Okayama University, Institute for Planetary Materials, Okayama, Japan, (5)Kobe University, Faculty of Science, Kobe, Japan, (6)Tokyo Institute of Technology, Tokyo, Japan
Back to: Atomic to Planetary Scales: Multiscale Understanding of Planetary Dynamics II