Universal nucleation length for slip-weakening rupture instability under nonuniform fault loading
By K. Uenishi, J. Rice. 2003
251 citations recorded by the source corpus.
View Paper: https://www.semanticscholar.org/paper/47612b8f927fefe6f7cdf61b96a5310e866bd228
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Citations in the corpus
- Earthquake source characteristics from dynamic rupture with constrained stochastic fault stress (2007, methodology): “Our results on nucleation agree well with and extend earlier studies based on the same assumption [e.g., Campillo and Ionescu, 1997; Favreau et al., 2002; Uenishi and Rice, 2003; Ampuero and Vilotte, 2003].”
- Characterization of nucleation during laboratory earthquakes (2013, background): “…Favreau et al., 1999]: Lc = ˇ Dc 0 (fs – fd) (3) where fs and fd are the static and dynamic friction coefficients, Dc is the critical weakening distance, is the shear modulus, and the ˇ is a nondimensional coefficient of the order ˇ = 1.158 [Campillo and Ionescu, 1997; Uenishi and Rice, 2003].”
- Conditions governing the occurrence of supershear ruptures under slip-weakening friction (2007, methodology): “Studies by Campillo and Ionescu [1997] and Favreau et al. [1999], later generalized by Uenishi and Rice [2003] , examined the stability of cracks developing under slipweakening conditions.”
- Earthquake Initiation From Laboratory Observations and Implications for Foreshocks (2019, background): “Definitions based on different friction equations have been shown to be equivalent under some special conditions (Garagash & Germanovich, 2012; Uenishi & Rice, 2003).”
- Macroscopic Asymmetry of Dynamic Rupture on a Bimaterial Interface With Velocity- Weakening Friction (2006, background): “For instance, when nucleation is driven by tectonic loading near a stress concentration (Uenishi & Rice 2003), the slipping patch is expected to reach a critical state very slowly.”