Complex, multilayered azimuthal anisotropy beneath Tibet: evidence for co-existing channel flow and pure-shear crustal thickening
Author:
Funder
Science Foundation Ireland
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/210/3/1823/19194672/ggx266.pdf
Reference164 articles.
1. Azimuthal anisotropy beneath southern Africa from very broad-band surface-wave dispersion measurements;Geophys. J. Int.,2012
2. The structure and dynamics of the lithosphere beneath Tibet from seismic surface-wave analysis,2013
3. Tibetan and Indian lithospheres in the upper mantle beneath Tibet: evidence from broadband surface-wave dispersion;Geochem. Geophys. Geosyst.,2013
4. Shear-velocity structure, radial anisotropy and dynamics of the Tibetan crust;Geophys. J. Int.,2014
5. Intraplate deformation of the Indian subcontinent;Geophys. Res. Lett.,2008
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