Vertical coherence of deformation in lithosphere in the eastern Himalayan syntaxis using GPS, Quaternary fault slip rates, and shear wave splitting data
Author:
Affiliation:
1. China Earthquake Administration; Institute of Geophysics; Beijing China
2. Department of Earth, Atmospheric, and Planetary Sciences; Purdue University; West Lafayette Indiana USA
Funder
China Seismic Array Data Management Center
NSF
LMF and National Natural Science Foundation of China
China National Special Fund for Earthquake Scientific Research in Public Interest
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2015GL064568/fullpdf
Reference53 articles.
1. Lithospheric thickness of the Chinese Continent;An;Phys. Earth Planet. Inter.,2006
2. Independent active microplate tectonics of northeast Asia from GPS velocities and block modeling;Apel;Geophys. Res. Lett.,2006
3. Intraplate deformation of the Indian subcontinent;Banergee;Geophys. Res. Lett.,2008
4. Reconciling lithospheric deformation and lower crustal flow beneath central Tibet;Bendick;Geology,2007
5. Geodetic evidence for a low slip rate in the Altyn Tagh fault system;Bendick;Nature,2000
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