Abstract
The lattice-preferred orientation (LPO) of minerals is important for interpreting seismic anisotropy [...]
Highlights
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The lattice-preferred orientation (LPO) of minerals is important for interpreting seismic anisotropy [1,2,3,4,5], which occurs in the Earth’s crust and mantle [6,7], and for understanding the internal structure of the deep interior of the Earth [6,7,8]
LPOs develop in minerals in the crust, mantle, and subduction zones [1,2], where the rocks are deformed under high pressure and temperature [1,2,3,4,5]
Summary
Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations. The lattice-preferred orientation (LPO) of minerals is important for interpreting seismic anisotropy [1,2,3,4,5], which occurs in the Earth’s crust and mantle [6,7], and for understanding the internal structure of the deep interior of the Earth [6,7,8]. LPOs develop in minerals in the crust, mantle, and subduction zones [1,2], where the rocks are deformed under high pressure and temperature [1,2,3,4,5].
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