Results 11 to 20 of about 71,394 (292)
Aftershock triggering by complete Coulomb stress changes [PDF]
Journal of Geophysical Research: Solid Earth, 2002 We examine the correlation between seismicity rate change following the 1992, M7.3, Landers, California, earthquake and characteristics of the complete Coulomb failure stress (CFS) changes (ΔCFS(t)) that this earthquake generated. At close distances the time‐varying “dynamic” portion of the stress change depends on how the rupture develops temporally ...
Debi Kilb, Joan Gomberg, Paul Bodin
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ARAH PENYEBARAN STRESS COULOMB PADA BATUAN AKIBAT GEMPABUMI KAIRATU 26 SEPTEMBER 2019 [PDF]
Wahana Fisika: Jurnal Penelitian Fisika dan Terapannya, 2020 Penelitian ini bertujuan untuk mengetahui arah penyebaran stress batuan yang diakibatkan oleh gempabumi Kairatu dan diduga memiliki keterkaitan dengan kejadian gempabumi yang terjadi setelahnya.
Harti Umbu Mala, Juliany N. Mohamad
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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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Analysis of Seismicity Level and Coulomb Stress Changes in the Central Sulawesi Region in 1996-2022
Jurnal Fisika Flux, 2023 Central Sulawesi is an area that is prone to earthquakes. The movement of the Palu Koro Fault is the trigger for most of the destructive earthquakes in the Central Sulawesi region.
Lailatul Husna Lubis +2 more
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Coulomb Stress Change in Ahar-Varzaghan (20121108) Earth Quakes [PDF]
, 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 ...
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Geomatics, 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
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Coseismic Stress Change and Viscoelastic Relaxation after the 2008 Great Sichuan Earthquake
Applied 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
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Stress triggering of the Lushan M7. 0 earthquake by the Wenchuan Ms8. 0 earthquake
Geodesy 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
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The stress change of the major activity faults in the Weihe Graben after the Wenchuan earthquake
Earthquake 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
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Coulomb Ordering in Anderson-Localized Electron Systems [PDF]
, 2002 We consider an electron system under conditions of strong Anderson localization, taking into account interelectron long-range Coulomb repulsion.
Kovtun, H. A. +2 more
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