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    中国百强科技报刊

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    Volume 45 Issue 7
    Jul.  2020
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    Zheng Ning, Li Tingdong, Ding Xiaozhong, Liu Yanxue, Cheng Muwei, 2020. The Cambrian Terreneuvian-Series 2 Sedimentary Environment of Central-Southern Area of Hunan and Jiangxi. Earth Science, 45(7): 2629-2649. doi: 10.3799/dqkx.2020.018
    Citation: Zheng Ning, Li Tingdong, Ding Xiaozhong, Liu Yanxue, Cheng Muwei, 2020. The Cambrian Terreneuvian-Series 2 Sedimentary Environment of Central-Southern Area of Hunan and Jiangxi. Earth Science, 45(7): 2629-2649. doi: 10.3799/dqkx.2020.018

    The Cambrian Terreneuvian-Series 2 Sedimentary Environment of Central-Southern Area of Hunan and Jiangxi

    doi: 10.3799/dqkx.2020.018
    • Received Date: 2020-02-13
    • Publish Date: 2020-07-15
    • In order to solve the dispute-"deep sea" or "shallow sea" about the Cambrian Terreneuvian-Series 2 sedimentary environment of central-southern area of Hunan and Jiangxi, this paper further analyzed sedimentary environment such as paleo-water depth by investigating the petrological characteristics, radiolarian distribution and lithofacies of eight sections for these strata. According to the investigation, suspected radiolarians found in Loudi, Shaoyang, Hengyang and Pingxiang areas were deposited in the basin center and the source of Si in these strata are biogenic. Horizontal beddings representing weak hydrodynamic force are developed in central and southern parts of Hunan and Jiangxi; the average value of Td of the greywacke is 5.94; the average value of δ30Si is 0.1‰; five types of lithofacies and three types of lithofacies associations (middle fan subfacies of submarine fan, outer fan subfacies of submarine fan, and continental rise subfacies). Taking major element, trace element and REE contents into consideration, we think that the sea water of the central-southern area of Hunan and Jiangxi was stagnant; the study area was a continental slope-rise with a bathyal environment in the Cambrian Terreneuvian-Series 2, relatively shallow in the southeast.

       

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