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Palabras clave – provistas por la editorial

microstructural evolution; lattice preferred orientation; olivine in Åheim; amphibole; seismic anisotropy; seismic velocity; olivine-rich eclogite; Western Gneiss Region; glaucophane; epidote; deformation experiment; simple shear; dislocation glide; cataclastic flow; spinel peridotite xenoliths; deformation microstructures; petrogenesis; mantle heterogeneity; Baekdusan volcano; Ice; microstructure; crystallographic preferred orientation (CPO); Styx Glacier; electron backscatter diffraction (EBSD); Val Malenco; serpentinized peridotite; tectonic evolution; deformation; strain localization; phyllite; muscovite; chlorite; retrograded eclogite; topotactic growth; reflection coefficient; omphacite; subduction zone; lattice-preferred orientation; Xitieshan eclogite; lawsonite; twin; blueschist; crystal preferred orientation; n/a