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Partially melted kyanite eclogite from the Roberts Victor Mine, South Africa
Authors: --- ---
Year: 1969 Publisher: Washington : Smithsonian Institution Press,

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Eclogite.


Book
Eclogite facies rocks
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ISBN: 0216926874 0412020718 9780216926875 Year: 1990 Publisher: Glasgow London New York Blackie Chapman and Hall

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Eclogite --- Eklogite


Dissertation
Pétrologie des nodules d'éclogites dans le Massif des Maures (Var, France)
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Year: 2002

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Dissertation
Pétrologie des nodules d'éclogites dans le Massif des Maures (Var, France)
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Year: 2002

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Blueschists and eclogites
Authors: ---
ISBN: 0813711649 9780813711645 Year: 1986 Volume: 164 Publisher: Boulder : Geological Society of America,

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Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy
Authors: ---
Year: 2021 Publisher: Basel, Switzerland MDPI - Multidisciplinary Digital Publishing Institute

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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.


Book
Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy
Authors: ---
Year: 2021 Publisher: Basel, Switzerland MDPI - Multidisciplinary Digital Publishing Institute

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Abstract

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.


Book
Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy
Authors: ---
Year: 2021 Publisher: Basel, Switzerland MDPI - Multidisciplinary Digital Publishing Institute

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Abstract

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.

Keywords

Research & information: general --- Environmental economics --- 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 --- 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

Shale-slate metamorphism in southern Appalachians
Author:
ISBN: 0444422641 1322256969 1483289850 9780444422644 0444415629 9780444415622 0444891455 9780444891457 Year: 1984 Volume: 10 Publisher: Amsterdam New York Elsevier

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