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    中国百强科技报刊

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    Volume 43 Issue 9
    Sep.  2018
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    Article Contents
    Zhao Xiaoming, An Zhihui, Qiu Xiaofei, Wu Nianwen, Wei Yunxu, Hu Kun, Zhao Yuxi, 2018. A New Understanding of the 'Macaoyuan Group' in North Kongling Area of Yangtze Craton. Earth Science, 43(9): 3324-3336. doi: 10.3799/dqkx.2018.565
    Citation: Zhao Xiaoming, An Zhihui, Qiu Xiaofei, Wu Nianwen, Wei Yunxu, Hu Kun, Zhao Yuxi, 2018. A New Understanding of the "Macaoyuan Group" in North Kongling Area of Yangtze Craton. Earth Science, 43(9): 3324-3336. doi: 10.3799/dqkx.2018.565

    A New Understanding of the "Macaoyuan Group" in North Kongling Area of Yangtze Craton

    doi: 10.3799/dqkx.2018.565
    • Received Date: 2017-12-02
    • Publish Date: 2018-09-15
    • The "Macaoyuan Group" in Kongzihe-Zhangcunping area, regarded as the sole sediment of Qingbaikou Period in North Kongling area, plays an important role to understanding the convergence and cracking of Rodinia Supercontinent. Here, new petrology, sedimentology, and detrital zircon chronology studies are conducted on 12 sections in Kongzihe-Zhangcunping area. The "Macaoyuan Group" is similar with the Nantuo Formation in the distribution and gravel features. The U-Pb ages of detridal zircon indicate the "Macaoyuan Group" is younger than 786 Ma, and the Nantuo Formation is constrained between 657 Ma and 635 Ma. The new findings indicate that the diamictite of "Macaoyuan Group" in North Kongling area is Neoproterozoic tillite, most likely time-equivalent to the Nantuo Formation. The sediment provenance is from the Kongling Group, Shennongjia Group and Huangling granite.

       

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