Off-fault plasticity and earthquake rupture dynamics: 1. Dry materials or neglect of fluid pressure changes

By E. L. Templeton, J. Rice. 2008

170 citations recorded by the source corpus.

Subfields: Geophysics, Mechanics of Materials

View Paper: https://www.semanticscholar.org/paper/63acd804304b71569cc6f0ae7f96db93acda69fc

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In Geophysics

In Mechanics of Materials

Citations in the corpus

Rupture dynamics and ground motion from 3‐D rough‐fault simulations (2013, methodology): “…1952], allowing off-fault plastic strain to relax what would otherwise be unphysically high stress concentrations in the dynamic process around the rupture tip [Andrews, 2005; Ben-Zion and Shi, 2005; Templeton and Rice, 2008] and the roughness slopes [Duan and Day, 2008; Dunham et al., 2011b].”
Dynamics, Radiation, and Overall Energy Budget of Earthquake Rupture With Coseismic Off‐Fault Damage (2019, methodology): “…determine CpII , we used the closeness to failure dMC , which indicates the safety of the initial stress state to the failure of the material represented by the ratio of the radius of the Mohr’s circle to the distance to the Mohr-Coulomb criteria (see also –13– Templeton and Rice, 2008).”
Earthquake Ruptures with Strongly Rate-Weakening Friction and Off-Fault Plasticity, Part 1: Planar Faults (2011, methodology): “Others have simply employed the rate-independent form and acknowledged that localization in their numerical solutions was limited by the employed grid spacing (Duan and Day, 2008; Templeton and Rice, 2008; Viesca et al., 2008).”
The transition of dynamic rupture styles in elastic media under velocity-weakening friction (2012, background): “The “relative strength” S (sometimes also referred to as “seismic ratio” [Templeton and Rice, 2008; Kaneko and Lapusta, 2010]) describes the strength of the material relative to the dynamic stress drop [Das and Aki, 1977b], and provides a measure of the closeness of the initial stress to the failure”