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KONG Weiqiong, DING Shuhong, FAN Xinxiang, et al. Geology and Genesis of the Shuanglong Iion Deposit in the Western Section of North Qilian Mountains[J]. Northwestern Geology, 2017, 50(1): 50-62.
Citation: KONG Weiqiong, DING Shuhong, FAN Xinxiang, et al. Geology and Genesis of the Shuanglong Iion Deposit in the Western Section of North Qilian Mountains[J]. Northwestern Geology, 2017, 50(1): 50-62.
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Geology and Genesis of the Shuanglong Iion Deposit in the Western Section of North Qilian Mountains

  • 1. Fourth Institute of Geological and Mineral Exploration of Gansu Provincial Bureau of Geology and Mineral Resources, Jiuquan 735000, Gansu, China;

  • 2. Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MLR, Xi'an Institute of Geology and Mineral Resources, Xi'an 710054, Shaanxi, China

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  • Received Date: October 07, 2016
  • Revised Date: November 01, 2016
  • Available Online: July 28, 2022
  • Published Date: March 04, 2017
    Graphical Abstract
    • Abstract
  • The Shuanglong iron deposit is located in the Kawa iron ore-concentrated area in the western section of North Qilian Mountains, which is the other important sedimentary-metamorphic iron deposit after the Jingtieshan iron deposit found within the polymetallicmetallogenic belt in the western section of North Qilian Mountains. The Shuanglong iron deposit was occurred in shallow sedimentary clastic sedimentary rocks of Changchengian Huashugou Formation. The orebodies are mostly developed as the stratiform shapes, while their distribution and occurrence were controlled by the ore-bearing strata, and their thickness vary with the ones of wall rocks. The iron ores have fine-grained structure, banded structure, low grade with great range, showing the characteristics of sedimentary-metamorphic iron ore. After discussing the genesis of this deposit, the Shuanglong iron deposit has been classified as the sedimentary-metamorphic iron deposit that related with submarine exhalative process, and the metallogenic model of this deposit has been established.
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