Modeling Crystallographic Preferred Orientation of Olivine Polycrystals Deformed in Diffusion Creep Regime, and Implications for Seismic Anistropy in the Upper Mantle.
Modeling Crystallographic Preferred Orientation of Olivine Polycrystals Deformed in Diffusion Creep Regime, and Implications for Seismic Anistropy in the Upper Mantle.
