Modeling Sequences of Earthquakes and Aseismic Slip (SEAS) in Elasto‐Plastic Fault Zones With a Hybrid Finite Element Spectral Boundary Integral Scheme-Reference-Cited by-同舟云学术

Modeling Sequences of Earthquakes and Aseismic Slip (SEAS) in Elasto‐Plastic Fault Zones With a Hybrid Finite Element Spectral Boundary Integral Scheme

Published:2022-12 Issue:12 Volume:127 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Abdelmeguid Mohamed¹^ORCID,Elbanna Ahmed¹

Affiliation:

1. Department of Civil and Environmental Engineering University of Illinois at Urbana‐Champaign Urbana IL USA

Funder

National Science Foundation

U.S. Department of Energy

U.S. Geological Survey

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/10.1029/2022JB024548

Reference115 articles.

1. A domain decomposition approach to implementing fault slip in finite-element models of quasi-static and dynamic crustal deformation

2. Sequences of seismic and aseismic slip on bimaterial faults show dominant rupture asymmetry and potential for elevated seismic hazard

3. A Novel Hybrid Finite Element‐Spectral Boundary Integral Scheme for Modeling Earthquake Cycles: Application to Rate and State Faults With Low‐Velocity Zones

4. Off‐Fault Damage Characterization During and After Experimental Quasi‐Static and Dynamic Rupture in Crustal Rock From Laboratory P Wave Tomography and Microstructures

5. A three‐dimensional hybrid finite element — spectral boundary integral method for modeling earthquakes in complex unbounded domains

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2. On the Interplay Between Distributed Bulk Plasticity and Local Fault Slip in Evolving Fault Zone Complexity;Geophysical Research Letters;2024-07-26

3. Rupture Jumping and Seismic Complexity in Models of Earthquake Cycles for Fault Stepovers with Off-Fault Plasticity;Bulletin of the Seismological Society of America;2024-02-21

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