supported by the China National Science Foundation (Grant No: 40572113);China national key basic research program for earlier stage study (Grant No: 2005CCA05600)
The intraplate uplift of the Qinghai-Tibet Plateau took place on the basis of breakup and assembly of the Precambrian supercontinent, and southward ocean-continent transition of the Proto-, Paleo-, Meso- and Neo-Tethy...