U-Pb Geochronology, Elemental and Sr-Nd Isotopic Geochemistry of the Houyaoyu Granite Porphyries:Implication for the Genesis of Early Cretaceous Felsic Intrusions in East Qinling

Xiaohu He; Hong Zhong; Zhifang Zhao; Shucheng Tan; Weiguang Zhu; Siqi Yang; Wenjun Hu; Zhong Tang; Congfa Bao

doi:10.1007/s12583-018-0788-2

Volume 29 Issue 4

Jul 2018

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Journal of Earth Science > 2018 > 29(4): 920-938.

Xiaohu He, Hong Zhong, Zhifang Zhao, Shucheng Tan, Weiguang Zhu, Siqi Yang, Wenjun Hu, Zhong Tang, Congfa Bao. U-Pb Geochronology, Elemental and Sr-Nd Isotopic Geochemistry of the Houyaoyu Granite Porphyries:Implication for the Genesis of Early Cretaceous Felsic Intrusions in East Qinling. Journal of Earth Science, 2018, 29(4): 920-938. doi: 10.1007/s12583-018-0788-2

Citation:

Xiaohu He, Hong Zhong, Zhifang Zhao, Shucheng Tan, Weiguang Zhu, Siqi Yang, Wenjun Hu, Zhong Tang, Congfa Bao. U-Pb Geochronology, Elemental and Sr-Nd Isotopic Geochemistry of the Houyaoyu Granite Porphyries:Implication for the Genesis of Early Cretaceous Felsic Intrusions in East Qinling. Journal of Earth Science, 2018, 29(4): 920-938. doi: 10.1007/s12583-018-0788-2

Citation:

Xiaohu He, Hong Zhong, Zhifang Zhao, Shucheng Tan, Weiguang Zhu, Siqi Yang, Wenjun Hu, Zhong Tang, Congfa Bao. U-Pb Geochronology, Elemental and Sr-Nd Isotopic Geochemistry of the Houyaoyu Granite Porphyries:Implication for the Genesis of Early Cretaceous Felsic Intrusions in East Qinling. Journal of Earth Science, 2018, 29(4): 920-938. doi: 10.1007/s12583-018-0788-2

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U-Pb Geochronology, Elemental and Sr-Nd Isotopic Geochemistry of the Houyaoyu Granite Porphyries:Implication for the Genesis of Early Cretaceous Felsic Intrusions in East Qinling

doi: 10.1007/s12583-018-0788-2

1.
Department of Geology, School of Resource Environment and Earth Science, Yunnan University, Kunming 650091, China
2.
State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
3.
University of Chinese Academy of Sciences, Beijing 100049, China
4.
Kunming University of Science and Technology, Kunming 650093, China
5.
Institute of Yunnan Geology Survey, Kunming 650051, China

More Information

Corresponding author: Hong Zhong
Received Date: 03 Mar 2018
Accepted Date: 07 Jun 2018
Publish Date: 01 Aug 2018

Abstract

Abstract

The Early Cretaceous Houyaoyu granite porphyries are located in the south margin of the North China Craton. Field observations, petrography, geochronology, major and trace elemental and Sr-Nd isotopic compositions are reported to elucidate the genesis of the Houyaoyu granite porphyries. SIMS zircon U-Pb analyses for the Houyaoyu granite porphyries yield two concordant ages of 133.2±2.3 (2σ) and 131±1.1 (2σ) Ma, respectively. Major and trace elemental compositions indicate that these porphyries are high-K I-type granites with high contents of SiO₂, K₂O, Rb, U, Pb, low Nb, Ta, Ti, and P. Initial ⁸⁷Sr/⁸⁶Sr ratios range from 0.708 3 to 0.709 7, and ε_Nd(t) values range from -9.13 to -12.3, with corresponding two-stage depleted-mantle Nd model ages (T_2DM) varying from 1.57 to 1.91 Ga. This suggests that the Houyaoyu granite porphyries were predominantly derived from ancient lower conti-nental crust, with minor involvement of mantle-derived components. On the basis of the tectonic evolu-tion of the Qinling Orogen and geochemical characteristics of the Houyaoyu granite porphyries, it is proposed that they were formed in an extensional tectonic setting related to lithospheric destruction of the North China Craton, and produced Mo and Pb-Zn mineralization in East Qinling Orogen.
- East Qinling,
- granite porphyries,
- ancient lower continental crust,
- destruction of North China Craton

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References(120)

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