Article ID Journal Published Year Pages File Type
4683795 Geodesy and Geodynamics 2011 5 Pages PDF
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.

Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
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