LEADER 03929nam 2200889z- 450 001 9910557369903321 005 20231214133250.0 035 $a(CKB)5400000000042192 035 $a(oapen)https://directory.doabooks.org/handle/20.500.12854/77155 035 $a(EXLCZ)995400000000042192 100 $a20202201d2021 |y 0 101 0 $aeng 135 $aurmn|---annan 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 10$aLattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy 210 $aBasel, Switzerland$cMDPI - Multidisciplinary Digital Publishing Institute$d2021 215 $a1 electronic resource (204 p.) 311 $a3-0365-2642-0 311 $a3-0365-2643-9 330 $aThe 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. 606 $aResearch & information: general$2bicssc 606 $aEnvironmental economics$2bicssc 610 $amicrostructural evolution 610 $alattice preferred orientation 610 $aolivine in A?heim 610 $aamphibole 610 $aseismic anisotropy 610 $aseismic velocity 610 $aolivine-rich eclogite 610 $aWestern Gneiss Region 610 $aglaucophane 610 $aepidote 610 $adeformation experiment 610 $asimple shear 610 $adislocation glide 610 $acataclastic flow 610 $aspinel peridotite xenoliths 610 $adeformation microstructures 610 $apetrogenesis 610 $amantle heterogeneity 610 $aBaekdusan volcano 610 $aIce 610 $amicrostructure 610 $acrystallographic preferred orientation (CPO) 610 $aStyx Glacier 610 $aelectron backscatter diffraction (EBSD) 610 $aVal Malenco 610 $aserpentinized peridotite 610 $atectonic evolution 610 $adeformation 610 $astrain localization 610 $aphyllite 610 $amuscovite 610 $achlorite 610 $aretrograded eclogite 610 $atopotactic growth 610 $areflection coefficient 610 $aomphacite 610 $asubduction zone 610 $alattice-preferred orientation 610 $aXitieshan eclogite 610 $alawsonite 610 $atwin 610 $ablueschist 610 $acrystal preferred orientation 615 7$aResearch & information: general 615 7$aEnvironmental economics 700 $aJung$b Haemyeong$4edt$01311909 702 $aPark$b Munjae$4edt 702 $aJung$b Haemyeong$4oth 702 $aPark$b Munjae$4oth 906 $aBOOK 912 $a9910557369903321 996 $aLattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy$93030547 997 $aUNINA