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YANG Fu-xin, LI Wei-min, CHEN Dai, et al. Discussion on the Deposit Features and Genetic Characteristics of Vanadium-Titanium Magnetite Ore in Xiaohongshan, Western Inner Mongolia[J]. Northwestern Geology, 2010, 43(3): 66-74.
Citation: YANG Fu-xin, LI Wei-min, CHEN Dai, et al. Discussion on the Deposit Features and Genetic Characteristics of Vanadium-Titanium Magnetite Ore in Xiaohongshan, Western Inner Mongolia[J]. Northwestern Geology, 2010, 43(3): 66-74.
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Discussion on the Deposit Features and Genetic Characteristics of Vanadium-Titanium Magnetite Ore in Xiaohongshan, Western Inner Mongolia

  • 1.

    Institute of 203 Nuclear Research, Xianyang 712000, Shanxi, China

  • 2.

    The Nuclear Industry Geological Bureau of Qinghai Province, Xining 81008, Qinghai, China

  • 3.

    Qinghai Senyuan Mining Co. Ltd, Xining 810001, Qinghai, China

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  • Received Date: November 16, 2009
  • Revised Date: November 16, 2009
  • Published Date: September 04, 2010
    Graphical Abstract
    • Abstract
  • Xiaohongshan and Damiao vanadium and ilmenite deposits in the Tianshan mountains-Yinshan belts in the similar latitude.The early Hercynian gabbro rock is the main mine body.The consistent income-based distribution of vanadium-titanium magnetite is shown mostly in the surface,and in the deep is the magma-shaped like layered sub-vanadium-titanium magnetite output.The ore body is stable and rich.The magnetite and ilmenite ore minerals are mainly symbiotic elements such as vanadium,which is a magma-differentiation and segregation-penetration superpo sition compound type of vanadium-titanium magnetite,and a new type of type between Panzhihua and Damiao V-Ti magnetite-type ore-forming charact eristics.the discovery of This type of mineralization has a certain scientific significance for the similar types of vanadium-titanium magnetite.
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