Earth Science Frontiers ›› 2020, Vol. 27 ›› Issue (4): 282-293.DOI: 10.13745/j.esf.sf.2020.4.42

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Sedimentary characteristics of the pre-Nanhua epi-metamorphic rock series in southern Anhui Province and the tectono-paleogeographic implications

HAN Yao1,2(), ZHANG Chuanheng2,*(), LI Liyang3, JIANG Xianqiang2, LIU Zihui2   

  1. 1. Shandong Geological Environmental Monitoring Station, Jinan 250014, China
    2. China University of Geosciences(Beijing), Beijing 100083, China
    3. Fourth Detachment of Gold Headquarters of China Armed Police Force, Liaoyang 111000, China
  • Received:2019-08-20 Revised:2020-04-08 Online:2020-07-25 Published:2020-07-25
  • Contact: ZHANG Chuanheng

Abstract:

The pre-Nanhua epi-metamorphic stratum in southern Anhui Province is an important part of the Jiangnan oregenic belt. Based on the sedimentary study of the Huansha and Niuwu formations, we can identify turbidite and deep sea-bathyal facies that both belong to the active type of sedimentary formation. Our research revealed that the sedimentary environment of the Huansha Formation reflects a shallow-deep sequence, while the Niuwu Formation features an upward-shallowing sequence. The sedimentary diffusion of the Huansha and upper Niuwu formations is northward directed, suggesting the provenances for the two formations must be from the south. Ternary plots of the sandstone point-count data showed that the Huansha and upper Niuwu formations were plotted in the magmatic-arc and recycled orogen fields, respectively. Combined with the geochemical research on granite intrusion in the Niuwu Formation, we conclude that the proto-basin of the Huansha Formation is back-arc basin, whereas the lower and upper Niuwu formations are marginal sea and peripheral foreland basins, respectively.

Key words: Huansha Formation, Niuwu Formation, sedimentary geology, Jiangnan orogen belt, tectono-paleogeography

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