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2019 Vol. 52, No. 4
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LIN Zhongyang, ZHAO Xudong, JIN Xianglong, PAN Shaojun, GU Mingguang. 2019. Palaeoenvironmental Evolution and Multi-stratigraphic Division and Correlation of Yangtze River Delta Plain since Pleistocene: Evidence from BZK03 Borehole. Northwestern Geology, 52(4): 115-126.
Citation: LIN Zhongyang, ZHAO Xudong, JIN Xianglong, PAN Shaojun, GU Mingguang. 2019. Palaeoenvironmental Evolution and Multi-stratigraphic Division and Correlation of Yangtze River Delta Plain since Pleistocene: Evidence from BZK03 Borehole. Northwestern Geology, 52(4): 115-126.
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Palaeoenvironmental Evolution and Multi-stratigraphic Division and Correlation of Yangtze River Delta Plain since Pleistocene: Evidence from BZK03 Borehole

  • 1. College of Marine Science and Technology, China University of Geosciences, Wuhan 430074, Hubei, China;

  • 2. Zhejiang Institute of Geological Survey, Hangzhou 311203, Zhejiang, China;

  • 3. The Key Laboratory of Submarine Geoscience, Second Institute of Oceanography, MNR, Hangzhou 310012, Zhejiang, China

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Received Date:  26 December 2018
Revised Date:  16 April 2019
    Abstract
  • Based on the analysis of sediment isotope dating, sporopollen assemblages, microfossils, grain size and magnetism of the samples from BZK03 borehole in the Yangtze River Delta plain, this paper discusses the sedimentary environment evolution, sedimentary facies and paleoclimate characteristics since Pleistocene, and then the Quaternary multi-stratigraphic division and correlation framework of the borehole has been established. The results show that, from bottom to top, the samples of drilled holes are weathered siltstone of Cretaceous Quxian Formation and Quaternary sedimentary strata of Jiaxing Formation, Qiangang Formation, Dongpu Formation, Ningbo Formation and Zhenhai Formation. Sporopollen assemblages can be divided into 18 sporopollen zones. According to the cycle law of warm, humid, cold, dry paleoclimate cycles, BZK03 borehole shows that there are 6 paleoclimate cycles in this region. In line with lithologic stratification, sedimentary environment and paleoclimate, the division and correlation of borehole multiple strata reveals that 144.6~198.5m is Jiaxing Formation strata with alternating fluvial and fluvial-lacustrine sedimentary environments in early Pleistocene, and there are two climatic cycles. 88.3~144.6m is the Qiangang Formation stratum of Middle Pleistocene fluvio lacustrine face-fluvial face-fluvio lacustrine face-fluvial face sedimentary environment, including two climatic cycles. 16.6~88.3m is late Pleistocene deposition, and the sedimentary environment is the Ningbo Formation of fluvial-littoral-fluvial-tidal-fluvial facies and the Dongpu Formation of estuarine-neritic facies, including two climatic cycles. 0~16.6m is Zhenhai Formation stratum of fluvial-lacustrine-shallow-fluvial-tidal flat sedimentary environment.
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