Coseismic surface-ruptures and crustal deformations of the 2008 Wenchuan earthquake Mw7.9, China
Version of Record online: 4 JUN 2009
Copyright 2009 by the American Geophysical Union.
Geophysical Research Letters
Volume 36, Issue 11, June 2009
How to Cite
2009), Coseismic surface-ruptures and crustal deformations of the 2008 Wenchuan earthquake Mw7.9, China, Geophys. Res. Lett., 36, L11303, doi:10.1029/2009GL037971., , , and (
- Issue online: 4 JUN 2009
- Version of Record online: 4 JUN 2009
- Manuscript Accepted: 28 APR 2009
- Manuscript Revised: 24 APR 2009
- Manuscript Received: 28 FEB 2009
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|grl25891-sup-0002-fs01.jpg||image/pjpeg||281K||Figure S1. Coseismic thrust-fault scarps cut through 2-year-old buildings with maximum vertical offsets of approximately 5 m at Bajiaomiao.|
|grl25891-sup-0003-fs02.jpg||image/pjpeg||178K||Figure S2. Coseismic thrust-fault scarps on the road with vertical offsets of 4.5 m were traced on strath terraces and extended to mountains at Qingping.|
|grl25891-sup-0004-fs03.jpg||image/pjpeg||1674K||Figure S3. Left-lateral rupture with dip-slip components resulting in elevated irrigation canals with horizontal 2.8 m and vertical 1.5 m at Xiaoyudong.|
|grl25891-sup-0005-fs04.jpg||image/pjpeg||4420K||Figure S4. Simulated interferograms projected using the actual local angles of incidence for each track as done with Figure 1.|
|grl25891-sup-0006-fs05.jpg||image/pjpeg||5482K||Figure S5. Difference between the observed and the simulated interferograms.|
|grl25891-sup-0007-fs06.jpg||image/pjpeg||178K||Figure S6. Details of the slip distribution for the bi-fault model A-A′, A-A″, and B-B′ shown in Figure 4.|
|grl25891-sup-0008-ts01.txt||plain text document||0K||Table S1. Fault parameters of the Bi-fault model in the inversion analysis.|
|grl25891-sup-0009-t01.txt||plain text document||1K||Tab-delimited Table 1.|
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