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Published in 2021 at "Tectonophysics"
DOI: 10.1016/j.tecto.2021.228954
Abstract: Abstract Orthopyroxene is the second most abundant mineral in the upper mantle and, like olivine, can form crystallographic preferred orientations (CPO) during mantle deformation that may influence mantle seismic anisotropy. Here we use a compilation…
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Keywords:
seismic anisotropy;
orthopyroxene cpo;
olivine orthopyroxene;