Mass removal and clay mineral dehydration/rehydration in carbonate-rich surface exposures of the 2008 Wenchuan Earthquake fault: Geochemical evidence and implications for fault zone evolution and coseismic slip
Article first published online: 15 FEB 2013
©2013. American Geophysical Union. All Rights Reserved.
Journal of Geophysical Research: Solid Earth
Volume 118, Issue 2, pages 474–496, February 2013
How to Cite
2013), Mass removal and clay mineral dehydration/rehydration in carbonate-rich surface exposures of the 2008 Wenchuan Earthquake fault: Geochemical evidence and implications for fault zone evolution and coseismic slip, J. Geophys. Res. Solid Earth, 118, 474–496, doi:10.1002/jgrb.50089., , , and (
- Issue published online: 16 APR 2013
- Article first published online: 15 FEB 2013
- Accepted manuscript online: 18 JAN 2013 12:00AM EST
- Manuscript Accepted: 11 JAN 2013
- Manuscript Revised: 20 DEC 2012
- Manuscript Received: 20 AUG 2012
- National Scientific Special Funding of the WFSD. Grant Number: WFSD-0009
- State Key Laboratory of Earthquake Dynamics, the China Earthquake Administration. Grant Number: LED2010A03
- National Science Foundation. Grant Number: 41102130
- Basic Scientific Funding of Chinese National Nonprofit Institutes. Grant Number: IGCEA1006
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