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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