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    Volume 46 Issue 4
    Apr.  2021
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    Liu Hao, Deng Xin, Jin Xinbiao, Zeng Qingluan, Xu Daliang, Zhang Weifeng, Peng Lianhong, 2021. Lower Ordovician Stratigraphic Sequence in Jingshan-Zhongxiang Area at Northern Margin of Yangtze and Regional Correlation. Earth Science, 46(4): 1359-1373. doi: 10.3799/dqkx.2020.146
    Citation: Liu Hao, Deng Xin, Jin Xinbiao, Zeng Qingluan, Xu Daliang, Zhang Weifeng, Peng Lianhong, 2021. Lower Ordovician Stratigraphic Sequence in Jingshan-Zhongxiang Area at Northern Margin of Yangtze and Regional Correlation. Earth Science, 46(4): 1359-1373. doi: 10.3799/dqkx.2020.146

    Lower Ordovician Stratigraphic Sequence in Jingshan-Zhongxiang Area at Northern Margin of Yangtze and Regional Correlation

    doi: 10.3799/dqkx.2020.146
    • Received Date: 2020-04-22
    • Publish Date: 2021-04-15
    • The characteristics of the Lower Ordovician in the Jingshan-Zhongxiang area are significantly different from those in the Three Gorges and southern Suizhou. Therefore, correlation of lithostratigraphy and biostratigraphy between them is helpful to understanding the paleogeograpghy as well as the geological evolution during the Early Ordovician in the northern margin of the Yangtze platform. Based on detailed study on the lithostratigraphy and the fossil assemblage, the Wenxiakou Formation and Zhongxiang Formation of the Lower Ordovician are established. The Wenxiakou Formation consists predominantly of flat pebble limestone, oolitic limestone and bioclastic limestone, which belongs to shoal facies of platform margin to shallow shelf facies. According to the fossils such as gastropods, cephalopods and brachiopods, this formation is confirmed as a deposition from Middle-Late Tremadocian to Early Florian, which is underlain conformably by the Loushanguan Formation. This succession can be correlated to the Nanjinguan Formation, Fenxiang Formation and Honghuayuan Formation in Three Gorges area, and can also be compared with the bottom of Gaojiawan Formation in southern Suizhou area. The Zhongxiang Formation is characterized by grey or dark grey shales with some siltstones and lenticular bioclastic limestone and is assumed to have been deposited in the neritic continental shelf zone. Based on the abundant fossils such as brachiopods, trilobites, crinoid stems, graptolite and cephalopods, this formation is considered to be formed at the age of Floian and has a conformable contact with the Wenxiakou and Dawan formations. It can be compared with the lowest part to Dawan Formation in Three Gorges and the middle-upper part of the Gaojiawan Formation in southern Suizhou, respectively.

       

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