Results 31 to 40 of about 6,423 (281)
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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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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Kuwait Journal of Science, 2023 The incident of increased seismic activity of the Merapi volcano was initiated by several tectonic earthquake phenomena. Analysis of the mechanism of tectonic earthquakes can be studied based on the combination of static stress on the rock.
Fitri Puspasari, Wahyudi
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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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Applied Sciences, 2017 The 2016 Ecuador M 7.8 earthquake ruptured the subduction zone boundary between the Nazca plate and the South America plate. This M 7.8 earthquake may have promoted failure in the surrounding crust, where six M ≥ 6 aftershocks occurred following this ...
Jianchao Wu +3 more
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Geochemistry, Geophysics, Geosystems, 2021 Slow slip events (SSEs) at subduction zones can precede large‐magnitude earthquakes and may serve as precursor indicators, but the triggering of earthquakes by slow slip remains insufficiently understood.
Vasso Saltogianni +5 more
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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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Perturbation of earthquake probability for interacting faults by static Coulomb stress changes [PDF]
Journal 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.
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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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Post-seismic fluid flow and Coulomb stress changes in a poroelastic medium [PDF]
Geophysical 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
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