TY - BOOK ID - 133456185 TI - Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy AU - Jung, Haemyeong AU - Park, Munjae PY - 2021 PB - Basel, Switzerland MDPI - Multidisciplinary Digital Publishing Institute DB - UniCat KW - Research & information: general KW - Environmental economics KW - microstructural evolution KW - lattice preferred orientation KW - olivine in Åheim KW - amphibole KW - seismic anisotropy KW - seismic velocity KW - olivine-rich eclogite KW - Western Gneiss Region KW - glaucophane KW - epidote KW - deformation experiment KW - simple shear KW - dislocation glide KW - cataclastic flow KW - spinel peridotite xenoliths KW - deformation microstructures KW - petrogenesis KW - mantle heterogeneity KW - Baekdusan volcano KW - Ice KW - microstructure KW - crystallographic preferred orientation (CPO) KW - Styx Glacier KW - electron backscatter diffraction (EBSD) KW - Val Malenco KW - serpentinized peridotite KW - tectonic evolution KW - deformation KW - strain localization KW - phyllite KW - muscovite KW - chlorite KW - retrograded eclogite KW - topotactic growth KW - reflection coefficient KW - omphacite KW - subduction zone KW - lattice-preferred orientation KW - Xitieshan eclogite KW - lawsonite KW - twin KW - blueschist KW - crystal preferred orientation KW - n/a KW - olivine in Åheim UR - https://www.unicat.be/uniCat?func=search&query=sysid:133456185 AB - The lattice-preferred orientation (LPO) of minerals is important for interpreting seismic anisotropy, which occurs in the Earth’s crust and mantle, and for understanding the internal structure of the deep interior of the Earth. The characterization of microstructures, including LPO, grain size, grain shape, and misorientation, is important to determine the deformation conditions, deformation histories, kinematics, and seismic anisotropies in the crust and mantle The articles in this Special Issue prove that studies of LPO and microstructures of minerals and rocks are a major research area and provide a foundation for interpreting seismic anisotropy in the crust, mantle, and subduction zones. Therefore, the authors hope that this Special Issue encompassing recent advances in the measurement of LPOs of different minerals under various tectonic settings will be a fundamental and valuable resource for the readers and researchers interested in exploring the deformation conditions of minerals and rocks, as well as the interpretation of seismic anisotropy in the crust, mantle, and subduction zones. ER -