The structure of the mantle transition zone and its implications for mantle upwelling beneath the central Tibetan plateau from triplicated P-waveforms modeling
Author:
Funder
National Natural Science Foundation of China
Publisher
Elsevier BV
Reference51 articles.
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4. Small 660-km seismic discontinuity beneath Tibet implies resting ground for detached lithosphere;Chen;J. Geophys. Res. Solid Earth,2007
5. Cenozoic Mg-rich potassic rocks in the Tibetan Plateau: geochemical variations, heterogeneity of subcontinental lithospheric mantle and tectonic implications;Chen;J. Asian Earth Sci.,2012
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