Results 31 to 40 of about 5,166,941 (333)

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

Broadband Dynamic Rupture Modeling With Fractal Fault Roughness, Frictional Heterogeneity, Viscoelasticity and Topography: The 2016 Mw 6.2 Amatrice, Italy Earthquake

open access: yesGeophysical Research Letters, 2022
Advances in physics‐based earthquake simulations, utilizing high‐performance computing, have been exploited to better understand the generation and characteristics of the high‐frequency seismic wavefield.
T. Taufiqurrahman   +5 more
semanticscholar   +1 more source

The Role of Background Stress State in Fluid‐Induced Aseismic Slip and Dynamic Rupture on a 3‐m Laboratory Fault

open access: yesJournal of Geophysical Research: Solid Earth, 2022
Fluid injection stimulates seismicity far from active tectonic regions. However, the details of how fluids modify on‐fault stresses and initiate seismic events remain poorly understood.
S. Cebry, Chun‐Yu Ke, G. Mclaskey
semanticscholar   +1 more source

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

open access: yesJournal of Geophysical Research: Solid Earth, 2020
Elastic strain energy released during shear failure in rock is partially spent as fracture energy Γ to propagate the rupture further. Γ is dissipated within the rupture tip process zone, and includes energy dissipated as off‐fault damage, Γoff ...
F. Aben, N. Brantut, T. Mitchell
semanticscholar   +1 more source

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

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

Dynamic nucleation as a cascade-up of earthquakes depending on rupture propagation velocity

open access: yesEarth, Planets and Space, 2023
Earthquake dynamic rupture requires a nucleation process to provide sufficient energy to overcome the fracture energy. Large earthquakes may occur via a cascading rupture process, which includes many triggering processes that cascade from small to large ...
Kansuke Uemura, Satoshi Ide, Hideo Aochi
doaj   +1 more source

Single-Molecule Rupture Dynamics on Multidimensional Landscapes [PDF]

open access: yesPhysical Review Letters, 2010
We explore emergent effects of multidimensionality of the free energy landscape on single-molecule kinetics under constant force. The proposed minimal model reveals the existence of a spectrum of unusual scenarios for the force-dependent lifetime, all of which are shown to occur on a free energy landscape with a single transition state.
Suzuki, Yohichi, Dudko, Olga K.
openaire   +2 more sources

Rupture-dependent breakdown energy in fault models with thermo-hydro-mechanical processes [PDF]

open access: yesSolid Earth, 2020
Substantial insight into earthquake source processes has resulted from considering frictional ruptures analogous to cohesive-zone shear cracks from fracture mechanics.
V. Lambert, N. Lapusta, N. Lapusta
doaj   +1 more source

Dilatancy-induced fluid pressure drop during dynamic rupture: Direct experimental evidence and consequences for earthquake dynamics [PDF]

open access: yesEarth and Planetary Science Letters, 2019
Fluid pressure and flow in the crust is a key parameter controlling earthquake physics. Since earthquake slip is linked to spatio-temporal localisation of deformation, it is expected that the localised fluid pressure around the fault plane could ...
N. Brantut
semanticscholar   +1 more source

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