Crustal structure beneath the Indochina peninsula from teleseismic receiver functions
Author:
Affiliation:
1. Department of Geological Sciences; University of Michigan; Ann Arbor; Michigan; USA
2. Institute of Geology and Geophysics; Chinese Academy of Sciences; Beijing; China
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/gl1024/2010GL044874/2010GL044874.pdf
Reference24 articles.
1. The isolation of receiver effects from teleseismic P waveforms;Ammon;Bull. Seismol. Soc. Am.,1991
2. On the non-uniqueness of receiver function inversions;Ammon;J. Geophys. Res.,1990
3. Crustal deformation of the eastern Tibetan plateau revealed by magnetotelluric imaging;Bai;Nat. Geosci.,2010
4. Upper mantle anisotropy beneath Indochina block an adjacent regions from shear-wave splitting analysis of Vietnam array data;Bai;Phys. Earth Planet. Inter.,2009
5. Moho depth determinations based on spectral ratio analysis of NORSAR long-period P waves;Berteussen;Phys. Earth Planet. Inter.,1977
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