Lattice-preferred orientation of amphibole, chlorite, and olivine found in hydrated mantle peridotites from Bjørkedalen, southwestern Norway, and implications for seismic anisotropy
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DOI: 10.1016/j.tecto.2018.11.011
Abstract: Abstract Understanding lattice-preferred orientations (LPOs) of olivine is important in the study of seismic anisotropy and mantle flow of the upper mantle in the earth. Although olivine is the major mineral of the upper mantle,… read more here.
Keywords: hydrated mantle; seismic anisotropy; olivine; amphibole chlorite ... See more keywords