Community‐driven code comparisons for three‐dimensional dynamic modeling of sequences of earthquakes and aseismic slip
Dynamic modeling of sequences of earthquakes and aseismic slip (SEAS) provides a self‐
consistent, physics‐based framework to connect, interpret, and predict diverse geophysical …
consistent, physics‐based framework to connect, interpret, and predict diverse geophysical …
Transient and steady‐state friction in non‐isobaric conditions
S Barbot - Geochemistry, Geophysics, Geosystems, 2024 - Wiley Online Library
The frictional properties of faults control the initiation and propagation of earthquakes and
the associated hazards. Although the ambient temperature and instantaneous slip velocity …
the associated hazards. Although the ambient temperature and instantaneous slip velocity …
On the interplay between distributed bulk plasticity and local fault slip in evolving fault zone complexity
M Abdelmeguid, MS Mia… - Geophysical Research …, 2024 - Wiley Online Library
We numerically investigate the role of plastic strain accumulation on the mechanical
response of a planar strike‐slip fault. Our models show that fault‐zone strength significantly …
response of a planar strike‐slip fault. Our models show that fault‐zone strength significantly …
[HTML][HTML] Analytical boundary integral solutions for cracks and thin fluid-filled layers in a 3D poroelastic solid in time and wavenumber domain
ER Heimisson - Journal of the Mechanics and Physics of Solids, 2024 - Elsevier
The spectral boundary integral (SBI) method has been widely employed in the study of
fractures and friction within elastic and elastodynamic media, given its natural applicability to …
fractures and friction within elastic and elastodynamic media, given its natural applicability to …
MCQsim: A multicycle earthquake simulator
Multicycle earthquake rupture simulators generate long sequences of earthquakes along
predefined fault geometries for statistical analysis of earthquake recurrence and related …
predefined fault geometries for statistical analysis of earthquake recurrence and related …
Modeling earthquake cycles and wear on rough faults with the mortar finite element method
Y Tal - Geophysical Journal International, 2023 - academic.oup.com
This paper presents a mortar-based finite element formulation for modelling earthquake
cycles and wear on rough faults governed by rate and state friction. The method allows large …
cycles and wear on rough faults governed by rate and state friction. The method allows large …
The paucity of supershear earthquakes on large faults governed by rate and state friction
C Liang, JP Ampuero… - Geophysical Research …, 2022 - Wiley Online Library
Supershear earthquakes are rare compared to their subshear counterparts, but the cause for
their paucity remains to be understood. We investigate for the first time the prevalence of …
their paucity remains to be understood. We investigate for the first time the prevalence of …
Stress heterogeneity and the onset of faulting along geometrically irregular faults
We present a two‐dimensional analytical solution for the static stress field around a rough
interlocked interface under background stresses and its applications to faulting. The solution …
interlocked interface under background stresses and its applications to faulting. The solution …
A discontinuous Galerkin method for sequences of earthquakes and aseismic slip on multiple faults using unstructured curvilinear grids
Physics-based simulations provide a path to overcome the lack of observational data
hampering a holistic understanding of earthquake faulting and crustal deformation across …
hampering a holistic understanding of earthquake faulting and crustal deformation across …
Slow slip as an indicator of fault stress criticality
V Lambert - Geophysical Research Letters, 2024 - Wiley Online Library
Fault regions inferred to be slowly slipping are interpreted to accommodate much of tectonic
plate motion aseismically and potentially serve as barriers to earthquake rupture. Here, we …
plate motion aseismically and potentially serve as barriers to earthquake rupture. Here, we …