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    Volume 44 Issue 1
    Jan.  2019
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    Article Contents
    Zhang Yongqing, Ling Wenli, Zhang Junbo, Duan Ruichun, Ren Bangfang, Yang Hongmei, 2019. Zircon U-Pb Geochronology of the Mesozoic Volcanic Rocks from Qingshan Group in the Eastern Shandong. Earth Science, 44(1): 344-354. doi: 10.3799/dqkx.2018.337
    Citation: Zhang Yongqing, Ling Wenli, Zhang Junbo, Duan Ruichun, Ren Bangfang, Yang Hongmei, 2019. Zircon U-Pb Geochronology of the Mesozoic Volcanic Rocks from Qingshan Group in the Eastern Shandong. Earth Science, 44(1): 344-354. doi: 10.3799/dqkx.2018.337

    Zircon U-Pb Geochronology of the Mesozoic Volcanic Rocks from Qingshan Group in the Eastern Shandong

    doi: 10.3799/dqkx.2018.337
    • Received Date: 2018-05-30
    • Publish Date: 2019-01-15
    • The mesozoic volcanic rocks from the Qingshan Group are the most representative in the Shandong Province, and investigation of its genesis and forming time is very important to reveal the evolution history of the eastern North China Craton. LA-ICP-MS zircon U-Pb ages of meta-basic volcanic rocks and meta-acid volcanic rocks from the Qingshan Group in the eastern Shandong are reported in this paper. The dating results show that the ages of the meta-basic and meta-acidic volcanic rocks are 117±2 Ma (MSWD=3.2) and 116±4 (MSWD=3.5) respectively, which represent the formation time of the volcanic rocks from the Qingshan Group. Based on the synthesis of geochronology, the start and the end age of the volcanic rocks from the Qingshan Group in the eastern Shandong are younger than those in the western Shandong. The meta-basic volcanic rocks might have undergone multiple events induced by continental crustal materials both from the North China Craton and the deep subduction of the Yangtze Craton.

       

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