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LI Jing, DONG Wang-cang, GUO Li-hong, et al. The Ore Control Factors and the Ore-prospecting Indicators of the Jianchaling Nickel Ore in Shaanxi Province[J]. Northwestern Geology, 2014, 47(3): 54-61.
Citation: LI Jing, DONG Wang-cang, GUO Li-hong, et al. The Ore Control Factors and the Ore-prospecting Indicators of the Jianchaling Nickel Ore in Shaanxi Province[J]. Northwestern Geology, 2014, 47(3): 54-61.
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The Ore Control Factors and the Ore-prospecting Indicators of the Jianchaling Nickel Ore in Shaanxi Province

  • 1. Shaanxi Center of Geological Survey, Xi'an 710016, China;

  • 2. No.2 Comprehensive Geophysical Prospecting Team of Shaanxi Bureau of Geology and Mineral Resources, Xi'an 710016, China

More Information
  • Received Date: October 21, 2013
  • Revised Date: June 16, 2014
  • Available Online: July 28, 2022
  • Published Date: September 04, 2014
    Graphical Abstract
    • Abstract
  • Lying in the Mianxian-Lueyang suture zone, Jianchaling nickel ore-forming belt locates inside the Jinjiahe-Tiantaishan Mn-P-Ni prospecting area in a subzone of Mn-P-Cr-Ni-Au mineralization of Mianxian-Lueyang Hercynian-Indosinian ophiolite rock; the origin of the deposit belongs to magmatic liquation-hydrothermal alteration. The main rock is the Proterozoic metamorphic ultrabasic rock, and early nickel-bearing ultrabasic main rock which was later transformed by acidic rocks is the basic metallogenic place. On the whole, the deposit is a large low-grade nickel sulfide ore deposit, associated with low-grade cobalt. By analyzing the ore geotectonic location, the rock body characteristics and the ore body characteristics, the ore control factors and ore-prospecting indicators are concluded. It is believed that the mineralization is controlled by the magnesium ultrabasic rock and the structural fracture zone, and the intermediate-acidic intrusive rock provided the reforming thermal dynamic power for the magnesium ultrabasic rock.
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    • References (30)
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