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DU Wei, TANG Zhongli, DU Yuliang, et al. Reserch on Mineralization characters and Prospecting of the Xiarihamu Magematic Ni-Cu Sufide Deposit[J]. Northwestern Geology, 2017, 50(3): 180-186.
Citation: DU Wei, TANG Zhongli, DU Yuliang, et al. Reserch on Mineralization characters and Prospecting of the Xiarihamu Magematic Ni-Cu Sufide Deposit[J]. Northwestern Geology, 2017, 50(3): 180-186.
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Reserch on Mineralization characters and Prospecting of the Xiarihamu Magematic Ni-Cu Sufide Deposit

  • 1. School of Earth Science and Resources, Chang'an University, Xi'an 710054, Shaanxi, China;

  • 2. Laboratory of Mineralization and Dynamics, Chang'an University, Xi'an 710054, Shaanxi, China;

  • 3. Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, Shaanxi, China

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  • Received Date: February 11, 2017
  • Revised Date: June 11, 2017
  • Available Online: July 28, 2022
  • Published Date: September 04, 2017
    Graphical Abstract
    • Abstract
  • The Xiarihamu super-large nickel deposit is located in the middle part of the western segment of the East Kunlun orogenic belt. Submassive-massive, sideronitic and disseminated sulfide ores are dominant in the orebody. The former type is formed by deep liquating injected magmaalong the early-formed weak tectonic zone or fracture penetration. The latter two types are formed by liquation and fractional crystallization of mantle-derived magma, which are occurred in peridotite and pyroxenite. It is an effective way for prospecting prospect to understand mineralization enrichment regularity according to the diagenesis mineralization and ore-controlling factors.
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    • References (26)
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