Lithospheric thickness and upper-mantle deformation beneath the NE Tibetan Plateau inferred fromSreceiver functions andSKSsplitting measurements
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/191/3/1285/1495996/191-3-1285.pdf
Reference78 articles.
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3. Shear-wave splitting in the upper-mantle wedge above the Tonga subduction zone;Bowman;Geophys. J. R. astr. Soc.,1987
4. A ‘no-lid’ zone in the central Chang-Thang platform of Tibet: evidence from pure path phase velocity measurements of long-period Rayleigh waves;Brandon;J. geophys. Res.,1986
5. Radial anisotropy in the crust and upper mantle beneath the Qinghai-Tibet Plateau and surrounding regions;Chen;J. Asian Earth Sci.,2009
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