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    Volume 34 Issue 1
    Jan.  2009
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    Article Navigation >  Earth Science  > 2009  >  34(1): 179-188
    YANG Sai-hong, WU Yuan-bao, LIU Xiao-chi, WANG Jing, PENG Min, JIAO Wen-fang, 2009. U-Pb Ages of Detrital Zircon from Meta-Sedimentary Rock from the Huwan Shear Zone, Western Dabie Terrain and Their Geological Significance. Earth Science, 34(1): 179-188.
    Citation: YANG Sai-hong, WU Yuan-bao, LIU Xiao-chi, WANG Jing, PENG Min, JIAO Wen-fang, 2009. U-Pb Ages of Detrital Zircon from Meta-Sedimentary Rock from the Huwan Shear Zone, Western Dabie Terrain and Their Geological Significance. Earth Science, 34(1): 179-188.
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    U-Pb Ages of Detrital Zircon from Meta-Sedimentary Rock from the Huwan Shear Zone, Western Dabie Terrain and Their Geological Significance

    • 1.

      State Key Laboratory of Geological Processes and Mineral Resources, Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China

    • 2.

      MOE Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China

    • Received Date: 2008-10-21
    • Publish Date: 2009-01-25
      Abstract
    • The Huwan high-pressure (HP) metamorphic zone is a key region to investigate the evolution process and timing of the Qinling-Dabieshan-Sulu orogenic belt. However, the timing of eclogite-facies metamorphism in this zone has not been well constrained. In order to constrain the time of eclogite-facies metamorphism, zircons from a metasediment sample HXD98-9 near Xiongdian were selected for LA-ICPMS U-Pb dating and trace element analysis. Metamorphic zircons are characterized by weak or none zoning, low Th/U ratios, low and/or flat HREE patterns, and an insignificantly negative Eu anomaly. These reflect that the metamorphc zircons crystallized with the presence of garnet and the absence of plagioclase feldspar, which occurred in eclogite-facies conditions. The weighted mean 206Pb/238U age of 310±3 Ma for these metamorphic zircons is thus the best estimated age of the eclogite-faeies metamorphism in this HP metamorphic zone. Three groups of U-Pb age were obtained from the inherited magmatic zircons, ranging of (400±5 Ma)-(419±5Ma), (426±5Ma)-(449±5Ma), and (496±5 Ma)-(524±7 Ma), respectively. One inherited grain has a U-Pb age of 580.7±7.3 Ma. These indicate that the inherited zircons were mostly derived from southern part of the North China block, while some from the Yangtze block.

       

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