Results 21 to 30 of about 10,317 (215)
Annals of Geophysics, 2006 We compute the static displacement, stress, strain and the Coulomb failure stress produced in an elastic medium by a finite size rectangular fault after its dislocation with uniform stress drop but a non uniform dislocation on the source.
F. Catalli, R. Console
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Earthquake Productivity Law in a Wide Magnitude Range
Frontiers in Earth Science, 2022 Earthquakes are usually followed by aftershocks. The number of aftershocks—the so-called productivity—depends on the magnitude of the earthquake. In seismic modeling it is usually assumed that the number of aftershocks is approximately the same for ...
Peter Shebalin +3 more
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Analysis of short time-space range seismicity patterns in Italy
Annals of Geophysics, 1997 In our paper we analyze the data base obtained from the observations of the Italian Seismological Network from 1975 to 1994 by using a simple algotithm to determine the rate of occurrence of seismic events condi- tioned by the occurrence of previous ...
M. Imotof +3 more
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On the Aftershocks of Oga Earthquake, May 7, 1964 [PDF]
, 2010 application/pdf紀要類 (bulletin)2640908 bytesdepartmental bulletin ...
Research Group For Aftershocks
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Mainshock-Integrated Aftershock Vulnerability Assessment of Bridge Structures
Applied Sciences, 2020 Seismic fragility analysis is often conducted to quantify the vulnerability of civil structures under earthquake excitation. In recent years, besides mainshocks, strong aftershocks have been often witnessed to induce structural damage to engineered ...
Xuan Guo, Zheyu Zhang, ZhiQiang Chen
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Frontiers in Earth Science, 2022 Strong to great earthquakes considerably weaken the structural strength of the subsurface strata and civil constructions. The occurrence of Mw ≥ 5 aftershocks further contributes to the loss of human lives and damage to property.
Harsh K. Gupta, Rajesh Rekapalli
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About the aftershocks, the Omori law, and the Utsu formula [PDF]
, 2023 After the main shock of an earthquake, a stream of aftershocks that does not subside for a long time is usually observed. Fusakichi Omori found that the frequency of aftershocks decreases hyperbolically with time. It has recently been observed that Omori'
Klain, Boris +3 more
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Regional variations in the diffusion of triggered seismicity [PDF]
, 2005 We determine the spatiotemporal characteristics of interearthquake triggering in the International Seismological Centre catalogue on regional and global scales. We pose a null hypothesis of spatially clustered, temporally random seismicity, and determine
Ian G. Main +3 more
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Earthquakes in the Shadows: Why Aftershocks Occur at Surprising Locations
The Seismic Record, 2022 For decades there has been a debate about the relative effects of dynamic versus static stress triggering of aftershocks. According to the static Coulomb stress change hypothesis, aftershocks should not occur in stress shadows—regions where static ...
Jeanne L. Hardebeck, Ruth A. Harris
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Forecasting Strong Subsequent Earthquakes in Greece with the Machine Learning Algorithm NESTORE
Entropy, 2023 Aftershocks of earthquakes can destroy many urban infrastructures and exacerbate the damage already inflicted upon weak structures. Therefore, it is important to have a method to forecast the probability of occurrence of stronger earthquakes in order to ...
Eleni-Apostolia Anyfadi +3 more
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