Earthquake ruptures with thermal weakening and the operation of major faults at low overall stress levels

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Rupture dynamics and ground motion from 3‐D rough‐fault simulations (2013, background): “…has steady-state value equal to the normal traction Tn. [57] The RSD friction coefficient can be expressed in a regularized form [Rice, 1983, 2006; Noda et al., 2009; Dunham et al., 2011a] as f V ;cð Þ ¼ a sinh 1 V 2V0 exp c a (B3) where the evolution of state variable c follows a slip law _c ¼…”
The transition of dynamic rupture styles in elastic media under velocity-weakening friction (2012, background): “…experiments [e.g., Xia et al., 2004; Lykotrafitis et al., 2006; Lu et al., 2007] and theory [e.g., Cochard and Madariaga, 1994; Perrin et al., 1995; Beeler and Tullis, 1996; Zheng and Rice, 1998; Nielsen and Carlson, 2000; Ampuero and Ben-Zion, 2008; Noda et al., 2009; Dunham et al., 2011].”
Three‐dimensional earthquake sequence simulations with evolving temperature and pore pressure due to shear heating: Effect of heterogeneous hydraulic diffusivity (2010, methodology): “…propagation [Andrews, 2002; Noda, 2004; Cocco and Bizzarri, 2004; Andrews, 2005; Bizzarri and Cocco, 2006a, 2006b; Suzuki and Yamashita, 2006; Noda et al., 2009], the quasi‐dynamic nucleation of ruptures [Schmitt and Segall, 2008], and a long‐term cycle simulation of a spring‐slider‐ dashpot…”