Journal of Jilin University(Earth Science Edition) ›› 2021, Vol. 51 ›› Issue (3): 734-748.doi: 10.13278/j.cnki.jjuese.20200218

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Tectonic Evolution of Northern Margin of Eastern North China Craton: Evidences of Middle Triassic Plutons in Faku Area, Liaoning Province

Zhang Chao1, Shi Shaoshan2, Shi Yi2, Wei Minghui2, Yang Fan2, Huan Hengfei2, Li Wenbo2, Wang Luyuan1,3   

  1. 1. School of Resources and Environmental Engineering, Shandong University of Technology, Zibo 255049, Shandong, China;
    2. Shenyang Center, China Geological Survey, Shenyang 110034, China;
    3. Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources(Jilin University), Changchun 130061, China
  • Received:2020-09-20 Online:2021-05-26 Published:2021-06-07
  • Supported by:
    Supported by the National Natural Science Foundation of China (41902234,41802238),the Project of China Geological Survey (DD20190042-02) and the Opening Foundation of Key Laboratory of Mineral Resources Evaluation in Nor-theast Asia,Ministry of Natural Resources (DBY-KF-18-11)

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Abstract: This paper reports the studies of petrography, zircon U-Pb dating,geochemistry and zircon Lu-Hf isotopic data of the Middle Triassic Fengqipu pluton and Kaolinggou pluton in Faku area in north Liaoning, Northern margin of Eastern North China craton. The LA-ICP-MS zircon U-Pb dating results show that the mean weighted ages of Middle Triassic Fengqipu pluton and Kaolinggou pluton are (241±1) Ma and (243±1) Ma, respectively. The contents of Ba and Sr of Fengqipu pluton are from 290.00×10-6 to 484.00×10-6 and from 129.00×10-6 to 338.00×10-6, respectively, and the ratios of Sr/Y and Sr/Yb are from 13.27 to 28.17 and from 117.50 to 250.28,respectively. Similar to the geochemistry of high Ba-Sr granites, the samples of Kaolinggou pluton have high Ba and Sr contents, high ratios of Sr/Y and Sr/Yb, and low Rb, Y, and Yb contents. Furthermore, the samples of Fengqipu pluton are enriched in Rb, K(LILE) and depleted in Nb, P, Ti(HFSE) and Ba(LILE), while the samples of Kaolinggou pluton are enriched in Ba, K, Sr(LILE) and depleted in Nb, P, Ti(HFSE). All the sample’s ratios of Nb/Ta and Zr/Hf range from 4.18 to 10.26, from 30.39 to 38.76, respectively, and the samples have low Ni, Co and Cr contents. Geochemecially, the source of Middle Triassic grantic rocks in Faku area was from crust. During the Middle-Late Trassic, Northern margin of Eastern North China craton was under the thickened crustal tectonic setting related to the sustainable orogeny. The Middle Triassic granitic rocks have postive εHf(t) values and 949-555 Ma of two stage model ages, indicating that the magma source of Middle Triassic granitic rocks should be partial melting products of the thickened new-proterozoic lower crust.

Key words: geochemistry, zircon U-Pb dating, Paleo-Asian Ocean, Northern margin of Eastern North China craton, Faku area

CLC Number: 

  • P595
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