Results 231 to 240 of about 263,848 (296)

Complete Coulomb Failure Stress Changes and Stress Triggering of Yunnan Longling Earthquake Sequence

open access: closedChinese Journal of Geophysics, 2007
The complete Coulomb failure stress changes caused by the 1976 Ms73, Ms74 Yunnan Longling double main earthquakes are calculated. And dynamic and static stress triggering effects on the after earthquake sequence are studied. The results show that the second main earthquake is subjected to the triggering effect of dynamic and static Coulomb ...
Xiao-Ping Wu, Jia-Fu Hu
exaly   +6 more sources

Coseismic Coulomb failure stress changes caused by the 2017 M7.0 Jiuzhaigou earthquake, and its relationship with the 2008 Wenchuan earthquake

open access: closedScience China Earth Sciences, 2017
On August 8, 2017, a M 7.0 earthquake occurred in Jiuzhaigou County, Sichuan Province, China, resulting in significant casualties and property damage. Therefore, it is critical to identify the areas of potential aftershocks before reconstruction and re-settling people to avoid future disasters.
Bin Shan, Yong Zheng, Chengli Liu
exaly   +4 more sources

Large aftershocks triggering by Coulomb failure stress following the 2001M S=8.1 great Kunlun earthquake

open access: closedActa Seismologica Sinica, 2004
The great Kunlun earthquake occurred on Nov. 14, 2001 in Qinghai Province, China. Five large aftershocks with magnitude larger than 5.0 occurred near the Kunlun fault after main shock. Calculations of the change in Coulomb failure stress reveal that 4 of 5 large aftershocks occurred in areas with Δσf>0 (10−2–10−1 MPa) and one aftershock occurred in an ...
Ping Hao   +4 more
exaly   +5 more sources

Evolution of cumulative Coulomb failure stress in northeastern Qinghai-Xizang (Tibetan) Plateau and its effect on large earthquake occurrence

open access: closedActa Seismologica Sinica, 2007
We simulate accumulative Coulomb failure stress change in a layered Maxwell viscoelastic media in the northeastern Qinghai-Xizang (Tibetan) Plateau since 1920. Lithospheric stress/strain evolution is assumed to be driven by dislocations of large earthquakes (M≥7.0) and secular tectonic loading.
Yong-Ge Wan, Zheng-Kang Shen
exaly   +5 more sources

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