Influence of Shear Heating and Thermomechanical Coupling on Earthquake Sequences and the Brittle‐Ductile Transition
Author:
Affiliation:
1. Department of Geophysics Stanford University Stanford CA USA
2. Now at Department of Geology University of Maryland College Park MD USA
3. Institute for Computational and Mathematical Engineering Stanford University Stanford CA USA
Funder
U.S. Geological Survey
National Science Foundation
Southern California Earthquake Center
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020JB021394
Reference142 articles.
1. A domain decomposition approach to implementing fault slip in finite-element models of quasi-static and dynamic crustal deformation
2. A Physics-Based Rock Friction Constitutive Law: Steady State Friction
3. The Brittle‐Ductile Transition Predicted by a Physics‐Based Friction Law
4. Earthquake cycle simulations with rate-and-state friction and power-law viscoelasticity
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