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...
Supported by the National Key Project for Basic Research of China (Grant No. 2002CB412610);National Key Project for New-round National Resource Investiga-tions (Grant No. 200210200001);pre-National 973 Project (Grant No. 2005CCA05600)
In situ zircon U-Pb ages for the recently discovered Zhunuo porphyry copper deposit in the western part of the Gangdese metallogenic belt in Tibet were determined by sensitive high-resolution ion mi-croprobe(SHRIMP) ....