Results 11 to 20 of about 8,208,222 (284)

Space observation and Coulomb Stress Change Modelling: application to the Izmit earthquake [PDF]

open access: yes, 2017
In 1999, the Izmit Earthquake struck Istanbul and its surroundings in northwest Turkey. It was one of the most devastating earthquakes of the twentieth century, significantly impacting on 20 million inhabitants and nearly half of the country’s industry.
Alac Barut, Ruken
openaire   +3 more sources

Coulomb Stress Analysis of the West Coast Sumatra Earthquake on Mount Imun and Mount Helatoba [PDF]

open access: yesJPFT (Jurnal Pendidikan Fisika dan Teknologi)
The island of Sumatra is a meeting area between the Indian Ocean plate in the South and the southwest edge of the Sunda Exposure, which is also the continental plate of Southeast Asia or the Eurasian Plate.
Goldberd Harmuda Duva Sinaga   +2 more
doaj   +2 more sources

Revisiting the seismic hazards of faults surrounding the 2022 Ms6.8 Luding earthquake, Sichuan, China

open access: yesGeomatics, Natural Hazards & Risk, 2023
The occurrence of the Ms6.8 Luding earthquake on 5 September 2022 filled the seismic gap in the southeastern segment of the Xianshuihe fault zone and transferred stress to the surrounding faults, which attracted much more attention to the seismic hazard.
Yujiang Li, Haoqing Liu, Cheng Yang
doaj   +1 more source

Coseismic Stress Change and Viscoelastic Relaxation after the 2008 Great Sichuan Earthquake

open access: yesApplied Sciences, 2022
Long-term stress accumulation influenced by coseismic stress changes and postseismic viscoelastic relaxation is considered critical to triggering giant earthquakes. Nevertheless, how the stress increase is interrupted by aftershocks and how it influences
Chaodi Xie   +6 more
doaj   +1 more source

Coulomb Stress Change in Ahar-Varzaghan (20121108) Earth Quakes [PDF]

open access: yes, 2021
Abstract Understanding how the movement of faults and deformation affects such as motion-induced surface stress and strain, which is very important in seismic regions. The best way to learn about the effects of fault movement is modeled. For example, the modeling of surface displacement or deformation and the amount of damage earthquake can be ...
openaire   +2 more sources

Applying the Coulomb Failure Function with an optimally oriented plane to the 2008 Mw 7.9 Wenchuan earthquake triggering [PDF]

open access: yes, 2010
The Coulomb failure function (CFF) quantitatively describes static stress changes in secondary faults near the source fault of an earthquake. CFF can be employed to monitor how static stress transfers and then shed some light on the probability of ...
Xu, C., Li, Z., Wang, J., Drummond, J.
core   +1 more source

Stress triggering of the Lushan M7. 0 earthquake by the Wenchuan Ms8. 0 earthquake

open access: yesGeodesy and Geodynamics, 2013
The Wenchuan Ms8. 0 earthquake and the Lushan M7. 0 earthquake occurred in the north and south segments of the Longmenshan nappe tectonic belt, respectively. Based on the focal mechanism and finite fault model of the Wenchuan Ms8.
Wu Jianchao   +4 more
doaj   +1 more source

The stress change of the major activity faults in the Weihe Graben after the Wenchuan earthquake

open access: yesEarthquake Research Advances, 2021
The seismicity of small earthquakes in the Weihe Graben has changed after the Wenchuan earthquake. In detail, the seismicity around the Qishan-Mazhao fault in the western Weihe Graben decreased, while the seismicity in Gaoling and Jingyang Counties in ...
Sheng Dong, Weina Yuan, Fuqiang Shi
doaj   +1 more source

Perturbation of earthquake probability for interacting faults by static Coulomb stress changes [PDF]

open access: yesJournal of Seismology, 2009
This work aims at the assessment of the occurrence probability of future earthquakes on the Italian territory, conditional to the time elapsed since the last characteristic earthquake on a fault and to the history of the following events on the neighbouring active sources.
Console, R., Murru, M., Falcone, G.
openaire   +2 more sources

Post-seismic fluid flow and Coulomb stress changes in a poroelastic medium [PDF]

open access: yesGeophysical Journal International, 2005
SUMMARY It is generally agreed that the occurrence of seismic sequences implies a kind of interaction between different fault segments. The coseismic stress transfer produced by each dislocation is the most obvious component of such an interaction. However, the time intervals elapsing between subsequent events in a sequence indicate that the coseismic ...
PIOMBO, ANTONELLO   +2 more
openaire   +1 more source

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