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Article Navigation >  Acta Sedimentologica Sinica  > 1997  >  15(S1): 51-56

Wang Jian, Sha Run, Wang Yongjin, Xiao Jiayi, Zhou Chunlin, Hu Xiaoxiao, Chen Guoxiang, Huang Xichuan. Coastal Development and Environmental Evolution in Central Part of Jiangsu Province Derived from a Long Drilling Section[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 51-56.
Citation: Wang Jian, Sha Run, Wang Yongjin, Xiao Jiayi, Zhou Chunlin, Hu Xiaoxiao, Chen Guoxiang, Huang Xichuan. Coastal Development and Environmental Evolution in Central Part of Jiangsu Province Derived from a Long Drilling Section[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 51-56.
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Coastal Development and Environmental Evolution in Central Part of Jiangsu Province Derived from a Long Drilling Section

  • 1.

    Department of Geography,Nanjing Normal University,Nanjing 210097;

  • 2.

    Engineering Planning Institute,Transportation Administration,Beijing 100000;

  • 3.

    Jiangsu Institute for Hydrogeological and Engineering-geological Inverstigation,Huaiyin 223005;

  • 4.

    Xian Institute for Loess Research,Xi'an 710054

  • Received Date: 1996-07-30
  • A 10km long section composed of 39 drilling holes in the central Jiangsu is examined to reconstruct the history of the coastaldevelopment and environmental evolution. There appears some evidences that modern tidal flat in central Jiangsu developed fromHolocene tidal sand ridges in the past centuries. A hiatus of sedimentation occurred between 20 and 10 ka BP. because of the lowerstand of sea level. Tidal flat occured in the modern coastal zone or nearshore during 30-20 ka BP.
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    [7] 王靖泰，汪品先.中国东部晚更新世以来海面升降与气候变化 的关系.地理学报，1980.35(4):299-311
    [8] 耿秀山.中国东部晚更新世以来的海水进退.海洋学报，1981.3 (1):114-130
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    [12] 李成治，李本川.苏北沿海暗沙成因的研究.海洋与湖沼.1981,12(4):321-331
    [13] 耿秀山，万延森.李善为，张誉年，徐孝诗苏北海岸带的演变过程及苏北浅滩动态模式的初步探讨.海洋学报，1983,5(1):62-71
    [14] 延森，张替年.江苏近海辐射状脊群的泥沙运动与来裸.海洋与湖沼.1985,16(5);392-399
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    [20] 耿秀山，傅命佐.江苏中南部平原淤泥滩岸的地貌特征.海岸地质与第四纪地质.1988,8(2):91-101
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  • Received:  1996-07-30

Coastal Development and Environmental Evolution in Central Part of Jiangsu Province Derived from a Long Drilling Section

  • 1. Department of Geography,Nanjing Normal University,Nanjing 210097;
  • 2. Engineering Planning Institute,Transportation Administration,Beijing 100000;
  • 3. Jiangsu Institute for Hydrogeological and Engineering-geological Inverstigation,Huaiyin 223005;
  • 4. Xian Institute for Loess Research,Xi'an 710054
  • Received Date: 1996-07-30

Abstract: A 10km long section composed of 39 drilling holes in the central Jiangsu is examined to reconstruct the history of the coastaldevelopment and environmental evolution. There appears some evidences that modern tidal flat in central Jiangsu developed fromHolocene tidal sand ridges in the past centuries. A hiatus of sedimentation occurred between 20 and 10 ka BP. because of the lowerstand of sea level. Tidal flat occured in the modern coastal zone or nearshore during 30-20 ka BP.

Wang Jian, Sha Run, Wang Yongjin, Xiao Jiayi, Zhou Chunlin, Hu Xiaoxiao, Chen Guoxiang, Huang Xichuan. Coastal Development and Environmental Evolution in Central Part of Jiangsu Province Derived from a Long Drilling Section[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 51-56.
Citation: Wang Jian, Sha Run, Wang Yongjin, Xiao Jiayi, Zhou Chunlin, Hu Xiaoxiao, Chen Guoxiang, Huang Xichuan. Coastal Development and Environmental Evolution in Central Part of Jiangsu Province Derived from a Long Drilling Section[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 51-56.
shu

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