Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy
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, grai...
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Jung, Haemyeong edt Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy Basel, Switzerland MDPI - Multidisciplinary Digital Publishing Institute 2021 1 electronic resource (204 p.) text txt rdacontent computer c rdamedia online resource cr rdacarrier 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. English Research & information: general bicssc Environmental economics bicssc microstructural evolution lattice preferred orientation olivine in Åheim amphibole seismic anisotropy seismic velocity olivine-rich eclogite Western Gneiss Region glaucophane epidote deformation experiment simple shear dislocation glide cataclastic flow spinel peridotite xenoliths deformation microstructures petrogenesis mantle heterogeneity Baekdusan volcano Ice microstructure crystallographic preferred orientation (CPO) Styx Glacier electron backscatter diffraction (EBSD) Val Malenco serpentinized peridotite tectonic evolution deformation strain localization phyllite muscovite chlorite retrograded eclogite topotactic growth reflection coefficient omphacite subduction zone lattice-preferred orientation Xitieshan eclogite lawsonite twin blueschist crystal preferred orientation 3-0365-2642-0 3-0365-2643-9 Park, Munjae edt Jung, Haemyeong oth Park, Munjae oth |
language |
English |
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eBook |
author2 |
Park, Munjae Jung, Haemyeong Park, Munjae |
author_facet |
Park, Munjae Jung, Haemyeong Park, Munjae |
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HerausgeberIn Sonstige Sonstige |
title |
Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy |
spellingShingle |
Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy |
title_full |
Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy |
title_fullStr |
Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy |
title_full_unstemmed |
Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy |
title_auth |
Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy |
title_new |
Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy |
title_sort |
lattice-preferred orientation and microstructures of minerals and their implications for seismic anisotropy |
publisher |
MDPI - Multidisciplinary Digital Publishing Institute |
publishDate |
2021 |
physical |
1 electronic resource (204 p.) |
isbn |
3-0365-2642-0 3-0365-2643-9 |
illustrated |
Not Illustrated |
work_keys_str_mv |
AT junghaemyeong latticepreferredorientationandmicrostructuresofmineralsandtheirimplicationsforseismicanisotropy AT parkmunjae latticepreferredorientationandmicrostructuresofmineralsandtheirimplicationsforseismicanisotropy |
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(CKB)5400000000042192 (oapen)https://directory.doabooks.org/handle/20.500.12854/77155 (EXLCZ)995400000000042192 |
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Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy |
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