Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (4): 941-964.doi: 10.13278/j.cnki.jjuese.20170145

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Late Mesozoic Thermal Upwelling-Extension Structure and Its Dynamics Background in Eastern Shandong Province

Song Mingchun1, Li Jie2, Li Shiyong3, Ding Zhengjiang4, Tan Xianfeng5, Zhang Zhaolu6, Wang Shijin7   

  1. 1. Shandong Provincial Bureau of Geology & Mineral Resources/Shandong Provincial Engineering Research Center for Geological Prospecting, Jinan 250013, China;
    2. College of Resources, Hebei University of Geosciences, Shijiazhuang 050031, China;
    3. Shandong Institute of Geophysical and Geochemical Exploration, Jinan 250013, China;
    4. No.8 Shandong Provincial Exploration Institute of Geology and Mineral Resources, Rizhao 276826, Shandong, China;
    5. Lunan Institute of Geology and Engineering Investigation of Shandong, Jining 272100, Shandong, China;
    6. College of Resources and Environmental Engineering, Shandong University of Technology, Zibo 255000, Shandong, China;
    7. Shandong Institute of Geological Survey, Jinan 250013, China
  • Received:2017-05-28 Online:2018-07-26 Published:2018-07-26
  • Supported by:
    Supported by R&D Program of Shandong Province(2017CXGC1604)and Taishan Scholar Special Project Funds (ts201511076)

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Abstract: In order to understand the Late Mesozoic tectonic-magmatic-mineralization and its dynamic background in the eastern Shandong Province, the authors analyzed the spatial distribution, assemblage characteristics, genetic types, formation times and sequences, geochemical evolution, and tectonic environment of the Late Mesozoic intrusive rocks. The intrusive rocks are mainly composed of Jurassic continental crust-remelted type granites, Cretaceous crust-mantle mixed granites, Cretaceous alkali granites, and Cretaceous vein rocks. From early to late period of magma activities, the intrusive rocks evolved from the high potassium calc-alkaline series to the shoshonite series, from the high Ba-Sr granites to the low Ba-Sr granites, from the no or weak positive Eu anomalies to the higher Eu negative anomalies, and from the S type granites to I and A type granite. The strong magmatism and various magmatic rock types indicate the occurrence of mantle-crust interaction. It is considered that the eastern Shandong was in a strong tensional tectonic background in Early Cretaceous, and the crust uplifted significantly with large-scale magmatic activities in the period of 140-110 Ma. According to a detailed research of the types, properties and control factors of the faulted basin, volcanism, metamorphic core complex and fault systems, the large-scale extensional structure was formed in 130-98 Ma. Further, the authors points out that the Cretaceous tectono-magmatic combination constituted the thermal upwelling-extension structure in the eastern Shandong province,which was the product of the combined effect of the Yanshannian intracontinental orogeny and the subduction of the Pacific plate. The lithosphere delamination, crust thinning and craton destruction were underlying causes of the Early Cretaceous thermal upwelling-extension structure, which provided the favorable conditions for the large-scale metallogenesis in the eastern Shandong Province.

Key words: thermal upwelling-extension structure, Late Mesozoic, magmatic activity, crustal uplift, Yanshan movement, eastern Shandong Province

CLC Number: 

  • P548
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