Low-temperature, high-stress deformation of olivine under water-saturated conditions

190 citations recorded by the source corpus.

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

Numerical modelling of spontaneous slab breakoff and subsequent topographic response (2011, background): “In subduction modelling, slabs of olivine rheology are subject to large stresses and low temperature in contrast tothe surrounding asthenosphere (Katayama and Karato, 2008).”
A thermodynamically self-consistent damage equation for grain size evolution during dynamic recrystallization (2011, background): “…regimes, other deformation mechanisms might be present like grain boundary sliding (Kohlstedt & Wang 2001; Hirth & Kohlstedt 2003; Drury 2005; Langdon 2006; Kohlstedt 2007) or Peierls mechanisms (Evans & Goetze 1979; Frost & Ashby 1982; Raterron et al. 2004; Katayama & Karato 2008; Kohlstedt 2007).”