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BAO Qing-zhong, WANG Hong, SHA De-ming, et al. Study on the geochemical characteristics of ore-forming fluid inclusion of Dashankou gold deposit in Xinjiang[J]. Northwestern Geology, 2003, 36(2): 43-49.
Citation: BAO Qing-zhong, WANG Hong, SHA De-ming, et al. Study on the geochemical characteristics of ore-forming fluid inclusion of Dashankou gold deposit in Xinjiang[J]. Northwestern Geology, 2003, 36(2): 43-49.
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Study on the geochemical characteristics of ore-forming fluid inclusion of Dashankou gold deposit in Xinjiang

  • 1.

    Institute of Resources and Civil engineering, Northeast University, Shenyang 110004, China;Shenyang Institute of Geology and Mineral Recourses, Shenyang 110033, China

  • 2.

    No.3 Geology Brigade, Bureau of Geology and Mineral Resources of Xinjiang, korla 841000, China

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  • Received Date: January 04, 2003
  • Revised Date: April 28, 2003
  • Published Date: June 04, 2003
    Graphical Abstract
    • Abstract
  • The characteristics of fluid inclusion in Dashankou gold deposit, Xinjiang, belong to K+-Na+-SO42--Cl--CO2 type.The salinity and density are all low degree.The ore-forming temperature of No.1 stage is 219.92℃ with pressure 22.14×105 Pa, and the main ore-forming stage is 298.28℃ with pressure 27.98×105 Pa.Thus the deposit belongs to low-middle temperature system.The fluid origenates mainly from magmatic water, or may be mixed with a small quatity of other source of waters.The gold deposit belongs to poor-sulfide type gold deposit and is controled by shear zone.
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    • References (5)
  • 鲍庆中,王宏,沙德铭,等. 新疆和静县大山口金矿床地质特征及其与穆龙套金矿床的对比[J]. 贵金属地质,2000,9(4):200-205.
    栾世伟,陈尚迪,曹殿春,等. 金矿床地质及找矿方法[M]. 成都: 四川科学技术出版社,1987.
    刘斌,沈昆. 流体包裹体热力学[M]. 北京:地质出版社,1999.
    刘斌,朱思林,沈昆. 流体包裹体热力学参数计算软件及算例[M]. 北京:地质出版社,2000.
    L.J.Drew, et. al.,Geology and structural evolution of Muruntau gold deposit, Kyzylkum Desert,Uzbekistan[J]. Ore Geology Reviews, 1996, No. 11, 175-196.
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