A Spectral Boundary‐Integral Method for Faults and Fractures in a Poroelastic Solid: Simulations of a Rate‐and‐State Fault With Dilatancy, Compaction, and Fluid Injection-Reference-Cited by-同舟云学术

A Spectral Boundary‐Integral Method for Faults and Fractures in a Poroelastic Solid: Simulations of a Rate‐and‐State Fault With Dilatancy, Compaction, and Fluid Injection

Published:2022-08-31 Issue:9 Volume:127 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Heimisson Elías Rafn¹²^ORCID,Liu Shengduo³,Lapusta Nadia²³^ORCID,Rudnicki John⁴^ORCID

Affiliation:

1. Swiss Seismological Service ETH Zurich Zurich Switzerland

2. Division of Geological and Planetary Sciences California Institute of Technology Pasadena CA USA

3. Division of Engineering and Applied Science California Institute of Technology Pasadena CA USA

4. Department of Civil and Environmental Engineering and Department of Mechanical Engineering Northwestern University Evanston IL USA

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/10.1029/2022JB024185

Reference78 articles.

1. Earthquake nucleation on rate and state faults – Aging and slip laws

2. Dynamic simulations of slip on a smooth fault in an elastic solid

3. Critical evaluation of state evolution laws in rate and state friction: Fitting large velocity steps in simulated fault gouge with time‐, slip‐, and stress‐dependent constitutive laws

4. The evolution of rock friction is more sensitive to slip than elapsed time, even at near-zero slip rates

5. Fluid-induced aseismic fault slip outpaces pore-fluid migration

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