supported by National Natural Science Foundation of China (Grant No. 40772126);Guangxi Natural Science Foundation Key Projects Funds (Grant No. 2010XNSFD13001);Guangxi Largescale Geologic and Mineral Investigation Project (Grant No. [2010]130);Guangxi Graduate Innovative Education Fund (Grant No. 2009105960818M01)
The Guposhan-Huashan batholith was emplaced during transition from Tethysian tectonic regime to Pacific tectonic regime in the Middle-Late Jurassic. The regional EW-striking Yishan-Quannan basement deep fault zone, as...