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

Xiaocheng Zhao; Wenxiao Zhou; Dong Fu; Bo Huang; Mengchun Ge

doi:10.1007/s12583-017-0942-2

Volume 29 Issue 2

Mar 2018

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Journal of Earth Science > 2018 > 29(2): 280-294.

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

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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

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

doi: 10.1007/s12583-017-0942-2

1.
Geotechnical & Structural Engineering Research Center, Shandong University, Jinan 250061, China
2.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China
3.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

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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

Abstract

Abstract

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 ε_Hf values of the former range from +12.8 to +14.2, with an average T_DM2 of 453 Ma. The latter have lower zircon ε_Hf values, ranging from +5.4 to +10.7, with an average T_DM2 of 798 Ma. The strong, positive ε_Hf 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.
- Lower Carboniferous granite,
- Paleo-Asian Ocean,
- Lu-Hf isotope,
- Xilinhot,
- Inner Mongolia

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References(67)

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