Results 1 to 10 of about 2,047 (206)
Nucleation speed limit on remote fluid-induced earthquakes [PDF]
Larger earthquakes unlocked by fluids are seen globally to take a predictably longer time to begin.
Parsons, Tom +2 more
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Optimized Traffic Light System with AIC and Application to the 2021 M6.7 Yangbi Earthquake Sequence
One important question in earthquake prediction is whether a moderate or large earthquake will be followed by an even bigger one. Through temporal b-value evolution analysis, the traffic light system can be used to estimate if an earthquake is a ...
Rui Wang +8 more
doaj +1 more source
Implications of a percolation model for earthquake ‘nucleation’ [PDF]
A percolation model is applied to the explanation of some of the qualitative and quantitative aspects associated with the recent observations of earthquake ‘nucleation’. An additional assumption is introduced that nucleation starts at the critical point of percolation.
openaire +1 more source
Scientific Exploration of Induced SeisMicity and Stress (SEISMS) [PDF]
Several major fault-drilling projects have captured the interseismic and postseismic periods of earthquakes. However, near-field observations of faults immediately before and during an earthquake remain elusive due to the unpredictable nature of ...
H. M. Savage +8 more
doaj +1 more source
The elastic properties of rocks in subduction zones are indicators of the stress states and determine the critical length required for earthquake nucleation.
Hanaya Okuda +3 more
doaj +1 more source
Permeability-controlled migration of induced seismicity to deeper depths near Venus in North Texas
Migration of seismic events to deeper depths along basement faults over time has been observed in the wastewater injection sites, which can be correlated spatially and temporally to the propagation or retardation of pressure fronts and corresponding ...
Kyung Won Chang, Hongkyu Yoon
doaj +1 more source
The depth extent of the crustal seismogenic zone is closely related to the size of earthquakes. The mechanisms that control the depth of the lower transition of the seismogenic zone are important issues in seismology and disaster mitigation.
Koji Masuda +2 more
doaj +1 more source
How frictional ruptures and earthquakes nucleate and evolve
Frictional motion is mediated by rapidly propagating ruptures that detach the ensemble of contacts forming the frictional interface between contacting bodies1-7. These ruptures are similar to shear cracks. When this process takes place in natural faults, these rapid ruptures are essentially earthquakes8,9. Although fracture mechanics describe the rapid
Gvirtzman, Shahar +3 more
openaire +3 more sources
Understanding the mechanisms of crustal deformation along convergent margins is critical to identifying seismogenic structures and assessing earthquake hazards for nearby urban centers. In the southern central Andes (28–33 $$^{\circ }$$ ∘ S), differences
Jean-Baptiste Ammirati +3 more
doaj +1 more source
Off-fault deformation feedback and strain localization precursor during laboratory earthquakes
Recent large-scale seismological observations have shown that off-fault strain localization and foreshock migration could serve as an early warning of an impending earthquake. However, this process is still largely unknown.
Gabriel G. Meyer +3 more
doaj +1 more source

