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Dating and Nd, Sr, O Isotope Studies of the Chaganhundi Granite

周有勤, 王银喜

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Abstract

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. The

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What this paper is about

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. The

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Available abstract

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. The

Key concepts: Greisen, Geology, Geochemistry, Mineralization (soil science), Crust, Chlorite, Quartz, Granitic rock

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