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    Volume 40 Issue 10
    Oct.  2015
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    Article Navigation >  Earth Science  > 2015  >  40(10): 1723-1740
    Zhu Weina, Wang Yitian, Wang Chunlong, Zhang Bing, Zhang Licheng, Ren Yi, Xiao Yanhong, Yuan Yanchao, Hu Xiangbo, 2015. Magnetite Composition and Its Genetic Significance of the Songhu Iron Deposit in the Western Tianshan, Xinjiang, NW China. Earth Science, 40(10): 1723-1740. doi: 10.3799/dqkx.2015.155
    Citation: Zhu Weina, Wang Yitian, Wang Chunlong, Zhang Bing, Zhang Licheng, Ren Yi, Xiao Yanhong, Yuan Yanchao, Hu Xiangbo, 2015. Magnetite Composition and Its Genetic Significance of the Songhu Iron Deposit in the Western Tianshan, Xinjiang, NW China. Earth Science, 40(10): 1723-1740. doi: 10.3799/dqkx.2015.155
    shu

    Magnetite Composition and Its Genetic Significance of the Songhu Iron Deposit in the Western Tianshan, Xinjiang, NW China

    doi: 10.3799/dqkx.2015.155
    • 1.

      School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

    • 2.

      Key Laboratory of Metallogeny and Mineral Assessment of Ministry of Land and Resources, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China

    • 3.

      Xinjiang Research Centre for Mineral Resources, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China

    • 4.

      University of Chinese Academy of Sciences, Beijing 100049, China

    • 5.

      No.7 Geological Party, Xinjiang Bureau of Geology and Mineral Resources, Wusu 833300, China

    • 6.

      China Water Resources Beifang Investigaiton, Design and Research Co. Ltd., Tianjin 300222, China

    • Received Date: 2014-12-11
    • Publish Date: 2015-10-15
      Abstract
    • The Songhu iron deposit located in the middle Awulale Fe-Cu metallogenic belt of Western Tianshan. The minralization of Songhu iron deposit included two metallogenic periods which could be further subdivided into six metallogenic stages, i. e., sulfide-k-feldspar stage, hematite-calcite-chlorite stage, magnetite-chlorite-k-feldspar stage(early stage of magnetite), magnetite-sulfide stage(late stage of magnetite), calcite-chalcopyrite stage and supergene period. In order to analyze the characteristics and causes of its components, Electron microprobe analyses show that the magnetites formed in early stage were rich in FeOT and poor in TiO2, Al2O3, MgO, MnO, which are similar to those of contact-metasomatic deposits. High content of SiO2 suggests that the formation of early magnetite was associated with acidic magmatic hydrothermal system. Late magnetite stage was the main minralization stage which was widely superimposed on ores formed during the early stage. Magnetites have lower content of FeOT and higher content of TiO2, MnO, V2O3, MgO, Al2O3. Both ternary plot of TiO2-Al2O3-MgO and Ca+Al+Mn vs. Ti+V discriminant diagram suggest that late magnetites were the product of hydrothermal mineralization. Considering the geological features of ore deposit, we infer that late magnetites are formed in the late magmatic activity or period of inactivity with the participation of sea water.

       

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