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BIANXiao-wei, ZHU Hai-ping, JIWen-hua, et al. The Discovery of Qingbaikouan Plutonite inT axorgan, Xinjiang,and Evidence from Zircon LA-ICP-MS U-Pb Dating of Intrusive Rock.[J]. Northwestern Geology, 2013, 46(1): 22-31.
Citation: BIANXiao-wei, ZHU Hai-ping, JIWen-hua, et al. The Discovery of Qingbaikouan Plutonite inT axorgan, Xinjiang,and Evidence from Zircon LA-ICP-MS U-Pb Dating of Intrusive Rock.[J]. Northwestern Geology, 2013, 46(1): 22-31.
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The Discovery of Qingbaikouan Plutonite inT axorgan, Xinjiang,and Evidence from Zircon LA-ICP-MS U-Pb Dating of Intrusive Rock.

  • 1.

    China University of Geosciences, Beijing,100083,China Shaanxi Geological Survey, Xi′an,710065,China

  • 2.

    China University of Geosciences, Beijing,100083

  • 3.

    Xi′an Institute of Geology and Mineral Resources, Xi′an, 710054, China

  • 4.

    Xinjiang Bureau of Geology and Mineral Resources, Urumqi 830000,China

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  • Published Date: March 04, 2013
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    • Abstract
  • In the period of 1∶50000 field mapping, precambrian strata was distinguished from theLower Paleozoic strata,intruding the Neoproterozoic tonalite pluton. In situ zircon U-Pb LA-ICP-MS dating on the tonalite pluton zircons yielded an age of the 855±14 Ma and 836±12Ma,representing the tonalite pluton intruding age and being the only Neoproterozoic age in Karakorumbelt,which is important in studying of Karakorum Precambrian geological evolution.
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