Results 1 to 10 of about 3,201,141 (296)

Dynamic restrengthening and fault heterogeneity explain megathrust earthquake complexity [PDF]

open access: yesNature Communications
Megathrusts host Earth’s largest earthquakes. Understanding the physical conditions controlling their rupture dynamics is critical for assessing seismic and tsunami hazards.
Jeremy Wing Ching Wong   +2 more
doaj   +2 more sources

Dynamic Rupture Simulation Reproduces Spontaneous Multifault Rupture and Arrest During the 2016 Mw 7.9 Kaikoura Earthquake

open access: yesGeophysical Research Letters, 2018
The 2016 Kaikoura (New Zealand) earthquake is characterized as one of the most complex multifault rupture events ever observed. We perform dynamic rupture simulations to evaluate to what extent relatively simple forward models accounting for realistic ...
Ryosuke Ando, Yoshihiro Kaneko
doaj   +2 more sources

Dynamic Rupture Process of the 2023 Mw 7.8 Kahramanmaraş Earthquake (SE Türkiye): Variable Rupture Speed and Implications for Seismic Hazard

open access: yesGeophysical Research Letters, 2023
We considered various non‐uniformities such as branch faults, rotation of stress field directions, and changes in tectonic environments to simulate the dynamic rupture process of the 6 February 2023 Mw 7.8 Kahramanmaraş earthquake in SE Türkiye.
Zijia Wang   +5 more
doaj   +2 more sources

On the nonlinear dynamics of rupture [PDF]

open access: yesNonlinear Processes in Geophysics, 1998
Abstract. The rupture on a fault resulting in an earthquake is clearly a complex process. In order to better understand this process the continuum version of the slider-block model has been considered in some detail. In particular, the role of a cohesive breakaway zone is considered.
Ockendon, H., Turcotte, D. L.
openaire   +5 more sources

The Dynamics of Elongated Earthquake Ruptures [PDF]

open access: yesJournal of Geophysical Research: Solid Earth, 2019
AbstractThe largest earthquakes propagate laterally after saturating the fault's seismogenic width and reach large length‐to‐width ratiosL/W. Smaller earthquakes can also develop elongated ruptures due to confinement by heterogeneities of initial stresses or material properties. The energetics of such elongated ruptures is radically different from that
Ampuero, Jean-Paul, Weng, Huihui
openaire   +5 more sources

Asymmetric Topography Causes Normal Stress Perturbations at the Rupture Front: The Case of the Cajon Pass

open access: yesGeophysical Research Letters, 2021
We use 3D dynamic rupture simulations to discover a previously un‐described effect of asymmetric topography on the earthquake process. With the Cajon Pass along the San Andreas Fault as an example, we find that asymmetric topography generates an ...
Christodoulos Kyriakopoulos   +2 more
doaj   +1 more source

Gel rupture during dynamic swelling

open access: yesSoft Matter, 2021
A complex, three-stage fracture process is described for hydrogels, resulting in material failure. This process is markedly different than that observed in brittle materials, and we describe how this process varies with network architecture.
Kelsey-Ann Leslie   +5 more
openaire   +3 more sources

Dynamic earthquake rupture in the lower crust [PDF]

open access: yesScience Advances, 2019
A lower crustal earthquake is initiated by dynamic rupturing with fragmentation of wall rock that precedes frictional melting.
Petley-Ragan, Arianne   +5 more
openaire   +6 more sources

The Dynamics of Unlikely Slip: 3D Modeling of Low‐Angle Normal Fault Rupture at the Mai'iu Fault, Papua New Guinea

open access: yesGeochemistry, Geophysics, Geosystems, 2022
Despite decades‐long debate over the mechanics of low‐angle normal faults (LANFs) dipping less than 30°, many questions about their strength, stress, and slip remain unresolved.
J. Biemiller, A.‐A. Gabriel, T. Ulrich
doaj   +1 more source

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