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-Reference-Cited by-同舟云学术

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

Published:2013-02 Issue:2 Volume:118 Page:474-496
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Chen Jianye¹²,Yang Xiaosong¹,Ma Shengli¹,Spiers Christopher J.²

Affiliation:

1. State Key Laboratory of Earthquake Dynamics, Institute of Geology; China Earthquake Administration; Beijing China

2. HPT Laboratory, Department of Earth Sciences; Utrecht University; The Netherlands

Funder

National Scientific Special Funding of the WFSD

State Key Laboratory of Earthquake Dynamics, the China Earthquake Administration

National Science Foundation

Basic Scientific Funding of Chinese National Nonprofit Institutes

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/jgrb.50089/fullpdf

Reference86 articles.

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2. Textural evidence for recent co-seismic circulation of fluids in Nojima fault zone;Boullier;Awaji Island, Japan, Tectonophysics,2004

3. Stick-slip as a mechanism for earthquakes;Brace;Science,1966

4. High-velocity frictional properties of a clay-bearing fault gouge and implications for earthquake mechanics;Brantut;J. Geophys. Res.,2008

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