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    中国百强科技报刊

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    Volume 45 Issue 3
    Mar.  2020
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    Article Contents
    Fang Huaibin, Li Kaiwen, Liu Kun, Guo Jungong, Wang Xiaojuan, Zhao Huan, 2020. U-Pb Dating and Geological Significance of Detrital Zircons from the Nanwan Formation, Zhenping County, East Qinling Mountains. Earth Science, 45(3): 815-828. doi: 10.3799/dqkx.2019.062
    Citation: Fang Huaibin, Li Kaiwen, Liu Kun, Guo Jungong, Wang Xiaojuan, Zhao Huan, 2020. U-Pb Dating and Geological Significance of Detrital Zircons from the Nanwan Formation, Zhenping County, East Qinling Mountains. Earth Science, 45(3): 815-828. doi: 10.3799/dqkx.2019.062

    U-Pb Dating and Geological Significance of Detrital Zircons from the Nanwan Formation, Zhenping County, East Qinling Mountains

    doi: 10.3799/dqkx.2019.062
    • Received Date: 2019-02-28
    • Publish Date: 2020-03-15
    • The East Qinling Mountains, located at the junction of the Qinling Orogenic Belt and the Dabie Orogenic Belt, had undergone complex tectonic evolution, and plays an important role in understanding the collision of the North China Block and the Yangtze Block. The Nanwan Formation plays an important role in understanding the tectonic process of the East Qinling Mountains, however, few studies have been done to analyze the regional differences in material composition. In this paper, the LA-ICP-MS U-Pb geochronology analyses of the detrital zircons from the Nanwan Formation in the Wanghuolou, Zhenping County, East Qinling, show that the zircon age peaks are mainly concentrated in 2 757-2 500 Ma, 2 500-2 400 Ma, 2 150-1 800 Ma, 1 800-1 700 Ma, 1 520-1 165 Ma, 1 100-1 000 Ma, 1 000-880 Ma, 840-630 Ma and 550-471 Ma, respectively. The original rock material is mainly from the North China Block and the North Qinling Orogenic Belt and South Qinling Orogenic Belt. There are some differences among the age peaks and material composition of the Nanwan Formation in Zhenping County, the Liuling Group in the Qinling Mountains, the Nanwan Formation in the Xinyang area, and the Foziling Group in the North Dabie Orogenic Belt. Therefore, further studies should be carried out to evaluate whether the four can be compared.

       

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