Results 1 to 10 of about 424 (109)

Short-Term Foreshocks as Key Information for Mainshock Timing and Rupture: The Mw6.8 25 October 2018 Zakynthos Earthquake, Hellenic Subduction Zone. [PDF]

open access: yesSensors (Basel), 2020
Significant seismicity anomalies preceded the 25 October 2018 mainshock (Mw = 6.8), NW Hellenic Arc: a transient intermediate-term (~2 yrs) swarm and a short-term (last 6 months) cluster with typical time-size-space foreshock patterns: activity increase,
Papadopoulos GA   +4 more
europepmc   +2 more sources

The Relevance of Foreshocks in Earthquake Triggering: A Statistical Study

open access: yesEntropy, 2019
An increase of seismic activity is often observed before large earthquakes. Events responsible for this increase are usually named foreshock and their occurrence probably represents the most reliable precursory pattern.
Lucilla de Arcangelis   +2 more
exaly   +3 more sources

Seismic and Aseismic Fault Slip During the Initiation Phase of the 2017 M W = 6.9 Valparaíso Earthquake. [PDF]

open access: yesGeophys Res Lett, 2021
Transient deformation associated with foreshocks activity has been observed before large earthquakes, suggesting the occurrence of a detectable preseismic slow slip during the initiation phase.
Caballero E   +5 more
europepmc   +2 more sources

On catching the preparatory phase of damaging earthquakes: an example from central Italy. [PDF]

open access: yesSci Rep, 2023
How, when and where large earthquakes are generated remain fundamental unsolved scientific questions. Intercepting when a fault system starts deviating from its steady behavior by monitoring the spatio-temporal evolution and dynamic source properties of ...
Picozzi M   +3 more
europepmc   +2 more sources

Foreshock properties illuminate nucleation processes of slow and fast laboratory earthquakes. [PDF]

open access: yesNat Commun, 2023
Understanding the connection between seismic activity and the earthquake nucleation process is a fundamental goal in earthquake seismology with important implications for earthquake early warning systems and forecasting.
Bolton DC   +3 more
europepmc   +2 more sources

A laboratory perspective on accelerating preparatory processes before earthquakes and implications for foreshock detectability. [PDF]

open access: yesNat Commun
Dynamic failure in the laboratory is commonly preceded by many foreshocks which accompany premonitory aseismic slip. Aseismic slip is also thought to govern earthquake nucleation in nature, yet, foreshocks are rare. Here, we examine how heterogeneity due
Goebel THW   +4 more
europepmc   +2 more sources

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

open access: yesSci Rep
Understanding earthquake nucleation is vital for predicting and mitigating seismic events, saving lives, and enhancing construction practices in earthquake-prone areas.
Ye SH, Lui SKY, Young RP.
europepmc   +2 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

Compound electron acceleration at planetary foreshocks. [PDF]

open access: yesNat Commun
Shock waves, the interface of supersonic and subsonic plasma flows, are the primary region for charged particle acceleration in multiple space plasma systems, including Earth’s bow shock, which is readily accessible for in-situ measurements.
Shi X   +4 more
europepmc   +2 more sources

On the Patterns and Scaling Properties of the 2021–2022 Arkalochori Earthquake Sequence (Central Crete, Greece) Based on Seismological, Geophysical and Satellite Observations

open access: yesApplied Sciences, 2022
The 27 September 2021 damaging mainshock (Mw6.0) close to Arkalochori village is the strongest earthquake that was recorded during the instrumental period of seismicity in Central Crete (Greece).
Filippos Vallianatos   +5 more
doaj   +1 more source

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