The crust in northern Xinjiang intensely moved about during the Middle Hercynian, which formed a large area of granitoid. In the south of Alataw Mountain, granitic bodies such as Kongwusayi, Wulasitan, Zuluhong, Kazib...The crust in northern Xinjiang intensely moved about during the Middle Hercynian, which formed a large area of granitoid. In the south of Alataw Mountain, granitic bodies such as Kongwusayi, Wulasitan, Zuluhong, Kazibieke and Chaganhundi are distributed along the Bole W-Sn mineralization belt from east to west, of which the Zuluhong, Kazibieke and Chaganhundi granitic bodies in the west sector are directly related to W-Sn mineralizations of quartz vein type, greisen type and chlorite type in this area.展开更多
基金Project supported by Youth Science Foundation of the University of Science and Technology of China
文摘The crust in northern Xinjiang intensely moved about during the Middle Hercynian, which formed a large area of granitoid. In the south of Alataw Mountain, granitic bodies such as Kongwusayi, Wulasitan, Zuluhong, Kazibieke and Chaganhundi are distributed along the Bole W-Sn mineralization belt from east to west, of which the Zuluhong, Kazibieke and Chaganhundi granitic bodies in the west sector are directly related to W-Sn mineralizations of quartz vein type, greisen type and chlorite type in this area.
