A unified description of localization for application to large-scale tectonics

By L. Montési, Maria T. Zuber. 2002

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Initiation of localized shear zones in viscoelastoplastic rocks (2006, background): “It is important to note that in this work we ignore many effects, such as the presence of weak and/or hydrated minerals, grain size reduction, strain rate weakening and power law rheology [Montesi and Zuber , 2002].”
Organized melt, seismic anisotropy, and plate boundary lubrication (2010, background): “…including shear heating [e.g., Fleitout and Froidevaux, 1980; Regenauer‐Lieb and Yuen, 1998], grain size reduction [e.g., Kameyama et al., 1997; Montesi and Zuber, 2002; Precigout et al., 2007], diking [e.g., Buck, 2004, 2006], water weakening and infiltration [e.g., Regenauer‐Lieb et al.,…”
A thermodynamically self-consistent damage equation for grain size evolution during dynamic recrystallization (2011, background): “In simple shear experiments, this happens when the derivative of deviatoric stress τ with respect to strain-rate ̇ is negative (Bercovici 1993; Montési & Zuber 2002).”