Off-fault deformation feedback and strain localization precursor during laboratory earthquakes [PDF]
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
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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.
Zuowei Wu
openalex +2 more sources
An electrochemical hypothesis of earthquakes exploring a theoretical link between radiated seismic energy and Pourbaix potential [PDF]
Earthquakes are measured using well-defined seismic parameters such as seismic moment ( $$M_o$$ ), moment magnitude ( $$M_w$$ ), and released elastic energy (E).
Atanu Das, Sankar Prasad Bag
doaj +2 more sources
Nucleation and early seismic propagation of small and large events in a crustal earthquake model [PDF]
N. Lapusta, J. R. Rice
openalex +3 more sources
Different earthquake nucleation conditions revealed by stress drop and b-value mapping in the northern Chilean subduction zone. [PDF]
Folesky J.
europepmc +3 more sources
Nucleation Mechanism and Rupture Dynamics of Laboratory Earthquakes at Different Loading Rates
The loading rate of tectonic stress is not constant during long-term geotectonic activity and significantly affects the earthquake nucleation and fault rupture process. However, the mechanism underlying the loading rate effect is still unclear.
Gongcheng Wu +3 more
doaj +1 more source
Capturing and quantifying the timing of remotely triggered earthquakes and understanding the physical processes responsible for this delay represent major challenges in earthquake forecasting.
Alexandre Canitano
doaj +1 more source
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 +1 more source
Stochastic Properties of Static Friction [PDF]
The onset of frictional motion is mediated by rupture-like slip fronts, which nucleate locally and propagate eventually along the entire interface causing global sliding.
Albertini, Gabriele +3 more
core +3 more sources
We conducted fluid injection experiments on cylindrical low‐permeability granite samples with a critically stressed sawcut fault at local injection rates of 0.2 and 0.8 mL/min and confining pressures of 31 and 61 MPa.
Yinlin Ji +4 more
doaj +1 more source

