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Volume 29 Issue 2
Mar 2018
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Xiaocheng Zhao, Wenxiao Zhou, Dong Fu, Bo Huang, Mengchun Ge. Isotope Chronology and Geochemistry of the Lower Carboniferous Granite in Xilinhot, Inner Mongolia, China. Journal of Earth Science, 2018, 29(2): 280-294. doi: 10.1007/s12583-017-0942-2
Citation: Xiaocheng Zhao, Wenxiao Zhou, Dong Fu, Bo Huang, Mengchun Ge. Isotope Chronology and Geochemistry of the Lower Carboniferous Granite in Xilinhot, Inner Mongolia, China. Journal of Earth Science, 2018, 29(2): 280-294. doi: 10.1007/s12583-017-0942-2

Isotope Chronology and Geochemistry of the Lower Carboniferous Granite in Xilinhot, Inner Mongolia, China

doi: 10.1007/s12583-017-0942-2
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  • Corresponding author: Wenxiao Zhou, zhouwenxiao@cug.edu.cn
  • Received Date: 25 Jan 2016
  • Accepted Date: 15 Sep 2016
  • Publish Date: 01 Apr 2018
  • Geochronological and geochemical analyses were performed on K-feldspar granites and monzonitic granites from the Xilinhot area, Inner Mongolia, China. Zircon U/Pb ages indicate that the two types granites were emplaced during the Lower Carboniferous. The K-feldspar granites (332 Ma) have the typical A-type granite characteristics of a post-collision setting. The monzonitic granites have an emplacement age of 323 Ma. Zircon εHf values of the former range from +12.8 to +14.2, with an average TDM2 of 453 Ma. The latter have lower zircon εHf values, ranging from +5.4 to +10.7, with an average TDM2 of 798 Ma. The strong, positive εHf values of the zircon indicate that both sets of samples are from a juvenile crust formed in an oceanic crust subduction stage, although the monzonitic granite may have undergone a hybridization of crustal materials. These results indicate a younger post orogenic event. The Paleo-Asian Ocean had closed before the Early Carboniferous and the Xilinhot area started its post-orogenic evolution with an extensional tectonic environment during the Early Carboniferous.

     

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