Results 11 to 20 of about 969,874 (233)
Earthquake nucleation on rough faults [PDF]
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]
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]
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
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]
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]
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]
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
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
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
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

