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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| Aineistotyyppi: | Online |
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| Kieli: | englanti |
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MDPI - Multidisciplinary Digital Publishing Institute
2022
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| Linkit: | ONIX_20220111_9783036526423_986 |
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| collection | Directory of Open Access Books |
| description | 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. |
| format | Online |
| id | doab-20.500.12854ir-77155 |
| institution | Directory of Open Access Books |
| language | eng |
| publishDate | 2022 |
| publishDateRange | 2022 |
| publishDateSort | 2022 |
| publisher | MDPI - Multidisciplinary Digital Publishing Institute |
| publisherStr | MDPI - Multidisciplinary Digital Publishing Institute |
| record_format | ojs |
| spelling | doab-20.500.12854ir-771552024-03-28T03:31:36Z Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy Jung, Haemyeong Park, Munjae 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 n/a thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general thema EDItEUR::K Economics, Finance, Business and Management::KC Economics::KCV Economics of specific sectors::KCVG Environmental economics 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. 2022-01-11T13:54:06Z 2022-01-11T13:54:06Z 2021 book ONIX_20220111_9783036526423_986 9783036526423 9783036526430 https://directory.doabooks.org/handle/20.500.12854/77155 eng image/jpeg Attribution 4.0 International https://mdpi.com/books/pdfview/book/4773 https://mdpi.com/books/pdfview/book/4773 MDPI - Multidisciplinary Digital Publishing Institute 10.3390/books978-3-0365-2643-0 10.3390/books978-3-0365-2643-0 46cabcaa-dd94-4bfe-87b4-55023c1b36d0 9783036526423 9783036526430 204 Basel, Switzerland open access |
| spellingShingle | 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 n/a thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general thema EDItEUR::K Economics, Finance, Business and Management::KC Economics::KCV Economics of specific sectors::KCVG Environmental economics Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy |
| title | 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_short | 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 |
| topic | 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 n/a thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general thema EDItEUR::K Economics, Finance, Business and Management::KC Economics::KCV Economics of specific sectors::KCVG Environmental economics |
| topic_facet | 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 n/a thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general thema EDItEUR::K Economics, Finance, Business and Management::KC Economics::KCV Economics of specific sectors::KCVG Environmental economics |
| url | ONIX_20220111_9783036526423_986 |