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Geochemistry of ore-forming fluids and geological significance of the Kuoerzhenkuola gold field in Xinjiang, China
作者姓名:SHEN Ping  SHEN Yuanchao  LIU Tiebing  LI Guangming & ZENG Qingdong Institute of Geology and Geophysics  Chinese Academy of Sciences  Beijing  China
作者单位:SHEN Ping,SHEN Yuanchao,LIU Tiebing,LI Guangming & ZENG Qingdong Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China
基金项目:国家"305"科技攻关项目
摘    要:The Kuoerzhenkuola gold field (including the Kuo- erzhenkuola and the Buerkesidai gold deposits), lo- cated 68 km east of Jimunai County in northern Xing- jiang, China, is an important component of the Sawuer gold belt which is the eastward extending part of the Zarma-Sawur gold-copper belt in Kazakhstan. Some studies are concerned with the geology of the gold ores1―3], the associated volcanic rocks4], radiogenic isotope5―8], and the ore-forming environment8]. Most researchers inferr…


Geochemistry of ore-forming fluids and geological significance of the Kuoerzhenkuola gold field in Xinjiang, China
SHEN Ping,SHEN Yuanchao,LIU Tiebing,LI Guangming & ZENG Qingdong Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing ,China.Geochemistry of ore-forming fluids and geological significance of the Kuoerzhenkuola gold field in Xinjiang, China[J].Science in China(Earth Sciences),2005,48(11).
Authors:SHEN Ping  SHEN Yuanchao  LIU Tiebing  LI Guangming  ZENG Qingdong
Institution:Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
Abstract:The Kuoerzhenkuola gold field (including the Kuoerzhenkuola and the Buerkesidai gold deposits) is the most important one in the Sawuer gold belt, northern Xinjiang, China. Iso-topic studies including D, O, He, C, S, Pb and Sr reveal that the ore-forming fluids of the Kuo-erzhenkuola and the Buerkesidai deposits shared the same source: the water of ore fluids was magmatic water and minor meteoric water; the mineralizers and ore materials derived mainly from mantle beneath the island arc, and partially from crust. The ore-forming fluids of two depos-its are a mixture of mantle-derived fluids incorporated by crust-derived fluid, and meteoric water. Based on these results, combined with the consideration of the tectonic setting and geological features, we suggest that the two gold deposits in the Kuoerzhenkuola gold field, Sawur gold belt share the same genesis, and are volcanogenic hydrothermal gold deposits occurring in the same caldera.
Keywords:ore-forming fluids  inclusions  isotope  volcanogenic late-stage hydrothermal gold deposits  Kuoerzhen- kuola gold field  
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