Results 11 to 20 of about 969,874 (233)

Earthquake nucleation on rough faults [PDF]

open access: yesGeology, 2017
Earthquake nucleation is currently explained using rate and state stability analysis, which successfully models the behavior of laboratory simulated faults with constant thickness gouge layers.
Christopher W. A. Harbord   +3 more
semanticscholar   +6 more sources

Earthquake nucleation in weak subducted carbonates [PDF]

open access: yesNature Geoscience, 2016
Ocean-floor carbonate- and clay-rich sediments form major inputs to subduction zones, especially at low-latitude convergent plate margins. Therefore, knowledge of their frictional behaviour is fundamental for understanding plate-boundary earthquakes.
R. Kurzawski   +4 more
semanticscholar   +5 more sources

The Effects of Fault Roughness on the Earthquake Nucleation Process [PDF]

open access: yesJournal of Geophysical Research: Solid Earth, 2018
AbstractWe study numerically the effects of fault roughness on the nucleation process during earthquake sequences. The faults are governed by a rate and state friction law. The roughness introduces local barriers that complicate the nucleation process and result in asymmetric expansion of the rupture, nonmonotonic increase in the slip rates on the ...
Yuval Tal   +2 more
exaly   +5 more sources

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   +2 more sources

Effect of Fluid Viscosity on Earthquake Nucleation [PDF]

open access: yesGeophysical Research Letters, 2020
Injection of fluids in geo‐reservoirs can reduce the effective stresses at depth, lubricating the nearby faults, promoting slip and, potentially, earthquakes.
C. Cornelio, M. Violay
semanticscholar   +3 more sources

Frictional healing and induced earthquakes on conventionally stable faults [PDF]

open access: yesNature Communications
Conventional studies suggest that faults in the shallow subsurface resist earthquake nucleation, because their frictional strength increases as slip accelerates (i.e., velocity-strengthening friction).
Meng Li   +2 more
doaj   +2 more sources

Earthquake simulations with time-dependent nucleation and long-range interactions [PDF]

open access: yesNonlinear Processes in Geophysics, 1995
A model for rapid simulation of earthquake sequences is introduced which incorporates long-range elastic interactions among fault elements and time-dependent earthquake nucleation inferred from experimentally derived rate- and state-dependent fault ...
J. H. Dieterich
doaj   +1 more source

Earthquake Nucleation and Slip Behavior Altered by Stochastic Normal Stress Heterogeneity

open access: yesJournal of Geophysical Research - Solid Earth
In recent laboratory experiments, varying nucleation locations of accelerating slip with changing nucleation lengths were observed. Spatial variations in effective normal stress, due to the controlling influence on fault strength and fracture energy ...
Meng Li, A. Niemeijer, Y. van Dinther
semanticscholar   +2 more sources

Foreshocks and Mainshock Nucleation of the 1999 Mw 7.1 Hector Mine, California, Earthquake

open access: yesJournal of Geophysical Research: Solid Earth, 2019
Foreshocks provide valuable information on the nucleation process of an upcoming large earthquake. We applied high‐resolution similar‐waveform techniques for earthquake detection, location, and source parameter estimation to understand the space‐time ...
Nana Yoshimitsu   +2 more
exaly   +2 more sources

Nucleation and Cascade Features of Earthquake Mainshock Statistically Explored from Foreshock Seismicity

open access: yesEntropy, 2019
The relation between the size of an earthquake mainshock preparation zone and the magnitude of the forthcoming mainshock is different between nucleation and domino-like cascade models.
Masashi Kamogawa   +5 more
doaj   +2 more sources

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