Journal of Jilin University(Earth Science Edition) ›› 2016, Vol. 46 ›› Issue (6): 1769-1780.doi: 10.13278/j.cnki.jjuese.201606114

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Geochemical Characteristics and Implication for Provenance of Upper Permian Linxi Formation Clastic Rocks in Solonker Area, Inner Mongolia

Li Fulai1,2, Xiao Fei3, Meng Fanchao1,2, Ren Zeying4   

  1. 1. College of Geosciences, China University of Petroleum(East China), Qingdao 266580, Shandong, China;
    2. Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, Shandong, China;
    3. School of Energy Resources, China University of Geosciences, Beijing 100083, China;
    4. Dongsheng Group CO. LTD. of Shengli Oilfield, Dongying 257000, Shandong, China
  • Received:2016-05-15 Online:2016-11-26 Published:2016-11-26
  • Supported by:
    Supported by National Natural Science Foundation of China(41202075) and Fundamental Research Funds for the Central Universities(15CX05007A)

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Abstract: The provenanceof the Linxi Formation in Solonker area was greatly influenced by the closure of the Paleo-Asian Ocean occurred in the Late Paleozoic. A comprehensive analysis of the element geochemical characteristics of the clastic rock has been done to study the source rock types and the tectonic setting of the Linxi Formation in the Solonker area. The major elements compositions indicated that the early sediments was of low weathering degree from the first depositional cycle and the latter sediments was of moderate weathering degree from the first depositional cycle or recycled deposition, and the igneous rock was the primary source rock. The trace elements and rare earth elements characteristics demonstrated a dissected magmatic arc dominated tectonic setting for the source rock of Linxi Formation. The intermediate and alkaline igneous rocks from the upper crust were the primary source rocks, with lower content of sedimentary rock. The indicator (Gd/Yb)n showed the early sediments was from the Archean alkaline igneous rocks. Comprehensive analysis showed that the provenances of the Linxi Formation were jointly derived from the north margin of the North China plate in the south and the Sonid Zuoqi-Xilinhot-sourthern Xiwuqi magma arc in the north.

Key words: geochemical, provenance, tectonic setting, Linxi Formation, Solonker area

CLC Number: 

  • P588.21
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