Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4683795 | Geodesy and Geodynamics | 2011 | 5 Pages |
Abstract
:Trapped waves in the Qingchuan fault zone were observed at Muyu near the northeastern end of the fractured zone of the Wenchuan Ms8. 0 earthquake. The results indicate a fault-zone width of about 200 m and a great difference in physical property of the crust on different sides of the fault. The inferred location of crustal changes is consistent with land-form boundary on the surface.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Lai Xiaoling, Sun Yi,