Grain size evolution and the rheology of ductile shear zones: from laboratory experiments to postseismic creep

By L. Montési, G. Hirth. 2003

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Microstructural Evidence for Grain Size Sensitive Deformation Mechanisms in Naturally Deformed Peridotites (2002, unknown): “, [39]).”
Implications of grain size evolution on the seismic structure of the oceanic upper mantle (2008, background): “…to stress (e.g., 41 Twiss, 1977; Karato et al., 1980; van der Wal, 1993), more recent studies have proposed models 42 in which grain size evolution is also sensitive to temperature and strain rate (de Bresser et al., 43 2001; Hall & Parmentier, 2003; Montési & Hirth, 2003; Austin & Evans, 2007).”
A thermodynamically self-consistent damage equation for grain size evolution during dynamic recrystallization (2011, background): “Various models have however discussed the possible interactions between large scale deformation and grain size evolution (Kameyama et al. 1997; Braun et al. 1999; Montési & Hirth 2003; Bercovici & Ricard 2005).”
Mechanisms for the generation of plate tectonics by two-phase grain-damage and pinning (2012, background): “, 1998; Furusho and Kanagawa, 1999) has prompted much activity in exploring grain-size shear-localizing feedback mechanisms (e.g., Kameyama et al., 1997; Braun et al., 1999; Montési and Hirth, 2003).”