Advanced Search

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.

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

  • 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.
  • [1] 任美得,张忍顺,杨巨海,江苏王港地区淤泥质潮滩的沉积作用海洋通报,1984,3(1):40-54
    [2] 朱大奎,柯贤坤,高抒.江苏海岸潮滩沉积的研究.黄渤海海洋, 1986,4(3):20-27
    [3] 李从先,李萍淤泥质海岸的沉积和砂体.海洋与湖沼,1982, ?(1);48-59

    (4] 张国栋,王益友等.苏北琼港现代潮坪沉积.沉积学报,1984,2 (2);39-51
    [4] 任美愕(主编).江苏省海岸带和海涂资源综合调查报告.北京: 海洋出版社,1986, 66-134
    [5] 张忍顺,陈才俊等.江苏岸外沙洲演变与条子泥并陆前景研究. 北京:海洋出版社.1992,8-18
    [6] 韩桂荣,刘玉海.黄河口海区沉积物柱样中碳酸盐组分.海洋与 湖沼,1993,24(5):456-465
    [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
    [9] 刘敏厚,吴世迎,王永吉.黄海晚第四纪沉积.北京:海洋出版 社,1987
    [10] 沈承德,周明富.中国东海大陆架C14年代学及晚更新世以来海面变化.科学通报,1981,3:162-165
    [11] 王建,刘泽纯等.江苏海域13万年来海面变化定t重建及我国沿海海侵的年代及对比间题.第四纪沉积与环境变迁.东南文化杂志社,1991.,68-75
    [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
    [15] 杨长恕.琼港辐射沙脊成因探讨,海洋地质与第四纪地质.1985,5(3):35-44
    [16] 黄易杨,王文清江苏沿岸辐射状沙脊群的动力机制探讨海洋学报,1987,9(2):209-215
    [17] 赵松龄.苏北浅滩成因的级新研究.海洋地质与第四纪地质,1991,11(3):106-112
    [18] 张光威,南黄海陆架沙脊的形成与演变海洋地质与第四纪地质,1991,11(2):25-33
    [19] 杨报章,李从先.业治铮.黄海南部陆区全新世埋藏潮沙体.地理学报,1995,50(5):447-457
    [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
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(455) PDF downloads(335) Cited by()

Proportional views
Related
Publishing history
  • Received:  1996-07-30

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

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.
Reference (20)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return