The effect of static annealing on microstructures and crystallographic preferred orientations of quartzites experimentally deformed in axial compression and shear

By R. Heilbronner, J. Tullis. Geological Society Special Publication, 2002

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Dynamic recrystallization near the brittle-plastic transition in naturally and experimentally deformed quartz aggregates (2008, result): “…that remaining porphyroclasts approach an end orientation with increasing strain and increasing amounts of recrystallization corresponding to earlier results for axial compression and simple shear experiments (e.g. Tullis et al., 1973; Dell'Angelo and Tullis, 1989; Heilbronner and Tullis, 2002).”
Rheology of the Earth's mantle: A historical review (2010, background): “Briefly, lattice-preferred orientation is the most stable microstructure among them (e.g., Heilbronner and Tullis, 2002; Zhang and Karato, 1995), dislocation density is the most unstable microstructure (e.g., Durham et al., 1977; Karato and Ogawa, 1982) and grain-size is in between (e.g., Karato,…”