Zhiqin X.; Jingsui Y.; Cailai W.; Haibing L.; Jianxin Z.; Xuexiang Q.; Shuguang S.; Haijun Q.
(2006)
The Qilian Caledonian orogenic belt on the north margin of the Qinghai-Tibet Plateau were formed by convergence and collision of the Alxa terrain, Qilian terrain and Qaidam terrain. The 350-km-long, WNW-ESE-trending North ...