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,...
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Other Authors: | , |
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Format: | Electronic Book Chapter |
Language: | English |
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Basel, Switzerland
MDPI - Multidisciplinary Digital Publishing Institute
2021
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Online Access: | DOAB: download the publication DOAB: description of the publication |
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DOAB: download the publicationDOAB: description of the publication
3rd Floor Main Library
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A1234.567 |
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Copy 1 | Available |