2023
DOI: 10.1038/s41467-023-37063-1
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Dueling dynamics of low-angle normal fault rupture with splay faulting and off-fault damage

Abstract: Despite a lack of modern large earthquakes on shallowly dipping normal faults, Holocene Mw > 7 low-angle normal fault (LANF; dip<30°) ruptures are preserved paleoseismically and inferred from historical earthquake and tsunami accounts. Even in well-recorded megathrust earthquakes, the effects of non-linear off-fault plasticity and dynamically reactivated splay faults on shallow deformation and surface displacements, and thus hazard, remain elusive. We develop data-constrained 3D dynamic rupture models of… Show more

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Cited by 5 publications
(1 citation statement)
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“…A better understanding of the complex interaction between static and time-dependent earthquake displacements, off-fault deformation, and seismic, acoustic, and tsunami amplitudes is now possible using realistic 3D scenarios. Non-linear earthquake dynamic rupture simulations combining coseismic frictional failure on prescribed faults and seismic wave propagation are powerful tools to investigate earthquake dynamics as a consequence of the model's initial conditions (e.g., Aochi and Ulrich, 2015;Wollherr et al, 2019;Ulrich et al, 2019a;Lozos and Harris, 2020;Harris et al, 2021;Taufiqurrahman et al, 2022;Biemiller et al, 2023). Empowered by high-performance computing (Ben-Zion et al, 2022), joint earthquake-tsunami modeling is now becoming applicable for the development of (probabilistic) tsunami forecasting and early warning systems (Yamamoto, 1982;Cecioni et al, 2014;Bernard and Titov, 2015;Mei and Kadri, 2017;Gomez and Kadri, 2021;Selva et al, 2021).…”
mentioning
confidence: 99%
“…A better understanding of the complex interaction between static and time-dependent earthquake displacements, off-fault deformation, and seismic, acoustic, and tsunami amplitudes is now possible using realistic 3D scenarios. Non-linear earthquake dynamic rupture simulations combining coseismic frictional failure on prescribed faults and seismic wave propagation are powerful tools to investigate earthquake dynamics as a consequence of the model's initial conditions (e.g., Aochi and Ulrich, 2015;Wollherr et al, 2019;Ulrich et al, 2019a;Lozos and Harris, 2020;Harris et al, 2021;Taufiqurrahman et al, 2022;Biemiller et al, 2023). Empowered by high-performance computing (Ben-Zion et al, 2022), joint earthquake-tsunami modeling is now becoming applicable for the development of (probabilistic) tsunami forecasting and early warning systems (Yamamoto, 1982;Cecioni et al, 2014;Bernard and Titov, 2015;Mei and Kadri, 2017;Gomez and Kadri, 2021;Selva et al, 2021).…”
mentioning
confidence: 99%