Results 1 to 10 of about 910 (180)

Earthquake nucleation in the lower crust by local stress amplification [PDF]

open access: yesNature Communications, 2020
This study investigates deep intracontinental earthquakes. Based on field data from exhumed lower crustal pseudotachylytes and mylonites from Lofoten, northern Norway, the authors describe a novel model of earthquake nucleation in the lower crust as a ...
L. R. Campbell   +3 more
doaj   +6 more sources

Earthquake Nucleation Along Faults With Heterogeneous Weakening Rate [PDF]

open access: yesGeophysical Research Letters, 2021
AbstractThe transition from quasistatic slip growth to dynamic rupture propagation constitutes one possible scenario to describe earthquake nucleation. If this transition is rather well understood for homogeneous faults, how the friction properties of multiscale asperities may influence the overall stability of seismogenic faults remains largely ...
Jean-François Molinari   +2 more
exaly   +9 more sources

Physical mechanisms of earthquake nucleation and foreshocks: Cascade triggering, aseismic slip, or fluid flows?

open access: yesEarthquake Research Advances
Earthquakes are caused by the rapid slip along seismogenic faults. Whether large or small, there is inevitably a certain nucleation process involved before the dynamic rupture.
Zhigang Peng, Xinglin Lei
exaly   +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

Insights on earthquake nucleation revealed by numerical simulation and unsupervised machine learning of laboratory-scale earthquake [PDF]

open access: yesScientific Reports
Understanding earthquake nucleation is vital for predicting and mitigating seismic events, saving lives, and enhancing construction practices in earthquake-prone areas.
Sheng Hua Ye   +2 more
doaj   +2 more sources

An electrochemical hypothesis of earthquakes exploring a theoretical link between radiated seismic energy and Pourbaix potential [PDF]

open access: yesScientific Reports
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 Mechanism and Rupture Dynamics of Laboratory Earthquakes at Different Loading Rates

open access: yesApplied Sciences, 2023
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

Sensitivity limits for strain detection of hypothetical remote fluid-induced earthquakes (Mw ≥ 4): a case study in Taiwan

open access: yesFrontiers in Earth Science, 2023
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

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

Earthquake Nucleation Characteristics Revealed by Seismicity Response to Seasonal Stress Variations Induced by Gas Production at Groningen

open access: yesGeophysical Research Letters, 2023
Deterministic earthquake prediction remains elusive, but time‐dependent probabilistic seismicity forecasting seems within reach thanks to the development of physics‐based models relating seismicity to stress changes. Difficulties include constraining the
Mateo Acosta   +5 more
doaj   +1 more source

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