Constitutive relationships and physical basis of fault strength due to flash heating

By N. Beeler, T. Tullis, D. Goldsby. 2008

256 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/f230fb4da928f73b0da1a8e9bb0fec69dffa6c1e

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In Geophysics

Citations in the corpus

Three‐dimensional earthquake sequence simulations with evolving temperature and pore pressure due to shear heating: Effect of heterogeneous hydraulic diffusivity (2010, background): “…and Shimamoto, 2005; Mizoguchi et al., 2006; O’Hara et al., 2006; Rempel and Rice, 2006; Rice, 2006; Sirono et al., 2006; Han et al., 2007; Mizoguchi et al., 2007; Beeler et al., 2008; Brantut et al., 2008; Noda, 2008; Fukuyama and Mizoguchi, 2010; Sulem and Famin, 2009; Sone and Shimamoto, 2009].”
Rupture dynamics and ground motion from 3‐D rough‐fault simulations (2013, background): “…¼ fw þ fLV Vð Þ fw 1þ V=Vwð Þ8 h i1=8 : (B6) [59] The above form has a strongly velocity-weakening feature such that when V ≫ Vw, fSS approaches a fully weakened friction coefficient fw, approximating experimental observations of frictional weakening at high slip speed [e.g., Beeler et al., 2008].”
The transition of dynamic rupture styles in elastic media under velocity-weakening friction (2012, background): “Dramatic velocity-weakening at high slip rates is amply supported by laboratory experiments [e.g., Tsutsumi and Shimamoto, 1997; Tullis and Goldsby, 2003; Di Toro et al., 2005; Hirose and Shimamoto, 2005] and by theoretical studies [Rice, 2006; Beeler et al., 2008].”
Inferring earthquake physics and chemistry using an integrated field and laboratory approach (2012, background): “4e40 mm, see Beeler et al., 2008), but this might be partly explained by the fact that the models assume a fully localized fault, whereas a considerable gouge layer (w100 mm thick) was observed after the experiments.”
Earthquake ruptures with thermal weakening and the operation of major faults at low overall stress levels (2009, background): “[9] Recent high speed friction experiments show that f decreases roughly as the inverse of the sliding velocity, V, for V above 0.1 m/s [Tsutsumi and Shimamoto, 1997; Tullis and Goldsby, 2003a, 2003b; Prakash and Yuan, 2004; Hirose and Shimamoto, 2005; Beeler et al., 2008].”
Earthquake Ruptures with Strongly Rate-Weakening Friction and Off-Fault Plasticity, Part 1: Planar Faults (2011, methodology): “The steady state friction coefficient used in this work features the extreme velocity-weakening response seen in recent experiments (Tsutsumi and Shimamoto, 1997; Tullis and Goldsby 2003a, 2003b; Prakash and Yuan, 2004; Di Toro et al., 2004; Hirose and Shimamoto, 2005; Beeler et al., 2008).”