03929nam 2200889z- 450 991055736990332120231214133250.0(CKB)5400000000042192(oapen)https://directory.doabooks.org/handle/20.500.12854/77155(EXLCZ)99540000000004219220202201d2021 |y 0engurmn|---annantxtrdacontentcrdamediacrrdacarrierLattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic AnisotropyBasel, SwitzerlandMDPI - Multidisciplinary Digital Publishing Institute20211 electronic resource (204 p.)3-0365-2642-0 3-0365-2643-9 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.Research & information: generalbicsscEnvironmental economicsbicsscmicrostructural evolutionlattice preferred orientationolivine in Åheimamphiboleseismic anisotropyseismic velocityolivine-rich eclogiteWestern Gneiss Regionglaucophaneepidotedeformation experimentsimple sheardislocation glidecataclastic flowspinel peridotite xenolithsdeformation microstructurespetrogenesismantle heterogeneityBaekdusan volcanoIcemicrostructurecrystallographic preferred orientation (CPO)Styx Glacierelectron backscatter diffraction (EBSD)Val Malencoserpentinized peridotitetectonic evolutiondeformationstrain localizationphyllitemuscovitechloriteretrograded eclogitetopotactic growthreflection coefficientomphacitesubduction zonelattice-preferred orientationXitieshan eclogitelawsonitetwinblueschistcrystal preferred orientationResearch & information: generalEnvironmental economicsJung Haemyeongedt1311909Park MunjaeedtJung HaemyeongothPark MunjaeothBOOK9910557369903321Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy3030547UNINA