Rupture termination at restraining bends: The last great earthquake on the Altyn Tagh Fault
Author:
Affiliation:
1. Department of Earth and Planetary Sciences; University of California; Davis California USA
2. Now at Department of Earth Sciences; University of Oxford; Oxford UK
3. Institute of Geology; China Earthquake Administration; Beijing China
Funder
NSF
NSF graduate student fellowship
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2015GL063107/fullpdf
Reference44 articles.
1. Duration of strong ground motion;Bolt;World Conference on Earthquake Engineering,1973
2. Faulting characteristics of supershear earthquakes;Bouchon;Tectonophysics,2010
3. OSL dating of offset streams across the Altyn Tagh Fault: Channel deflection, loess deposition and implication for the slip rate;Chen;Tectonophysics,2013
4. Reconstruction of the Altyn Tagh fault based on U-Pb geochronology: Role of back thrusts, mantle sutures, and heterogeneous crustal strength in forming the Tibetan Plateau;Cowgill;J. Geophys. Res.,2003
5. The Akato Tagh bend along the Altyn Tagh Fault, northwest Tibet 1: Smoothing by vertical-axis rotation and the effect of topographic stresses on bend-flanking faults;Cowgill;Geol. Soc. Am. Bull.,2004
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