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    Volume 35 Issue 6
    Jun.  2010
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    Article Navigation >  Earth Science  > 2010  >  35(6): 985-999
    ZHANG Yan-fei, LIU Jing-dang, XIAO Rong-ge, WANG Sheng-zhi, WANG Jin, BAO De-jun, 2010. The Hyalotourmalites of Houxianyu Borate Deposit in Eastern Liaoning: Zircon Features and SHRIMP Dating. Earth Science, 35(6): 985-999. doi: 10.3799/dqkx.2010.112
    Citation: ZHANG Yan-fei, LIU Jing-dang, XIAO Rong-ge, WANG Sheng-zhi, WANG Jin, BAO De-jun, 2010. The Hyalotourmalites of Houxianyu Borate Deposit in Eastern Liaoning: Zircon Features and SHRIMP Dating. Earth Science, 35(6): 985-999. doi: 10.3799/dqkx.2010.112
    shu

    The Hyalotourmalites of Houxianyu Borate Deposit in Eastern Liaoning: Zircon Features and SHRIMP Dating

    doi: 10.3799/dqkx.2010.112
    • 1.

      Liaoning Technical University, Fuxin 123000, China

    • 2.

      Liaoning Geological Survey for Chemical Industry, Jinzhou 121000, China

    • 3.

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

    • Received Date: 2010-05-15
    • Publish Date: 2010-11-01
      Abstract
    • SHRIMP zircon U-Pb dating results are firstly reported for the hyalotourmalites in Houxianyu borate deposit in order to determine its formation time. The zircons commonly have core-rim structures. Most cores show oscillatory zoning in CL and plane polarized light images, suggesting a magmatic detrital origin. The zircon without distinct structural change may represent a metamorphic origin. Magmatic detrital zircons and metamorphic zircons from three samples yield ages of 2 171-2 175 Ma and 1 894-1 906 Ma, respectively. Combined with geology and lithology, the protolith of hyalotourmalite is concluded to be the product of exhalation of submarine hot water caused by the magmatic activity with the magma derived from the depleted mantle source with crustal contamination in the cratonic rift environment, which occurred in the middle Palaeoproterozoic (2 171-2 175 Ma) and underwent the late metamorphism during a period of 1 894-1 906 Ma.

       

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