| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4693059 | Tectonophysics | 2011 | 10 Pages |
Abstract
⺠We calculated the velocity and stress fields of the studied region. ⺠We numerically simulated the rupture process of the 2008 Wenchuan earthquake. ⺠The movement and Coulomb failure stress (CFS) changes on boundary faults in the Qinghai-Tibet Plateau were calculated. ⺠The maximum deviation reaches 1.5 m on Wenchuan seismogenic fault. ⺠The maximum change of CFS reaches about 0.2 MPa at both ends of the Wenchuan seismogenic fault.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Zuan Chen, Banghui Lin, Wuming Bai, Xu Cheng, Yunsheng Wang,