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宁夏中卫晚石炭世沉积相分析与古环境重建

谢小平,  王永栋,  沈焕庭

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文章导航 > 沉积学报  > 2004 >  22(1): 19-28
谢小平, 王永栋, 沈焕庭. 宁夏中卫晚石炭世沉积相分析与古环境重建[J]. 沉积学报, 2004, 22(1): 19-28.
引用本文: 谢小平, 王永栋, 沈焕庭. 宁夏中卫晚石炭世沉积相分析与古环境重建[J]. 沉积学报, 2004, 22(1): 19-28.
shu
XIEXiao ping, WANGYong dong, SHENHuan ting. Facies Analysis and Sedimentary Environment Reconstruction of the Late Carboniferous in Zhongwei,Ningxia[J]. Acta Sedimentologica Sinica, 2004, 22(1): 19-28.
Citation: XIEXiao ping, WANGYong dong, SHENHuan ting. Facies Analysis and Sedimentary Environment Reconstruction of the Late Carboniferous in Zhongwei,Ningxia[J]. Acta Sedimentologica Sinica, 2004, 22(1): 19-28.
shu

宁夏中卫晚石炭世沉积相分析与古环境重建

  • 1.

    华东师范大学河口海岸国家重点实验室 山东曲阜 273165;

  • 2.

    中国科学院南京地质古生物研究所 南京 210008;

  • 3.

    华东师范大学河口海岸国家重点实验室 上海 200062;

  • 4.

    曲阜师范大学地理系 上海 200062

详细信息
    作者简介:

    谢小平,男,1966年出生,在读博士,沉积学

  • 中图分类号: P512.2

Facies Analysis and Sedimentary Environment Reconstruction of the Late Carboniferous in Zhongwei,Ningxia

  • 1.

    State Key Laboratory of Estuarine and Coastal Science Research, Eastern China Normal University, Shanghai 200062;

  • 2.

    Department of Geography, Qufu Normal University, QufuShandong 273165;

  • 3.

    Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008

    摘要
  • 摘要: 宁夏中卫地处北祁连加里东褶皱带东段,出露有连续而发育完好的晚石炭世海陆交互相含煤地层。根据岩性、颜色、粒度分析、沉积相标志、地球化学特征以及结合古生物化石资料,对中卫下河沿地区晚石炭世红土洼组、羊虎沟组和太原组的沉积相进行了分析研究,确立并划分出泻湖、潮坪、支间湾河口坝、滨海沼泽及三角洲平原等沉积相。在此基础上,结合本地区的古地理背景对宁夏中卫的晚石炭世的古沉积环境进行了重建。
    Abstract: The Late Carboniferous marine and non marine alternating deposits are well developed and outcropped in Xiaheyan of Zhongwei County, Ningxia Hui Autonomous Regionnorthwest China, including the Hongtuwa, Yanghugou and Taiyuan Formations. The facies analysis and sedimentary environment evolution are investigated in this study based on evidences of lithology, color, granularity analysis, facies indicator, geochemical data as well as fossil fauna and flora and Spore Pollen assemblages. Five facies are recognized including lagoon, tide flat, distributary bay estuarine sandbar, seashore and lowland marsh and tidal plainas well. In addition, the palaeogeographical background and sedimentary environmental evolution in Zhongwei of Ningxia are revealed and reconstructed based upon comparisons of the sedimentary characteristics with adjacent regions, including Eastern Sector of North Qilian, Ordos Basin and Taiyuan area of Northern China.
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    • 参考文献(23)
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    [23] Huang Baochun, Yo-ichiro Otofuji, Zhu Rixiang,et al. Paleomagnetism of Carboniferous sediments in the Hexi Corridor: its origin and tectonic implications.Earth and Planetary Science Letters,2001,194:135～149
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  • 收稿日期:  2002-09-24
  • 修回日期:  2002-12-17
  • 刊出日期:  2004-03-10

目录

    宁夏中卫晚石炭世沉积相分析与古环境重建

    • 1. 华东师范大学河口海岸国家重点实验室 山东曲阜 273165;
    • 2. 中国科学院南京地质古生物研究所 南京 210008;
    • 3. 华东师范大学河口海岸国家重点实验室 上海 200062;
    • 4. 曲阜师范大学地理系 上海 200062
      • 作者简介:

      谢小平,男,1966年出生,在读博士,沉积学

    • 收稿日期: 2002-09-24
    • 修回日期: 2002-12-17
    • 刊出日期: 2004-03-10

    • 中图分类号: P512.2

    摘要: 宁夏中卫地处北祁连加里东褶皱带东段,出露有连续而发育完好的晚石炭世海陆交互相含煤地层。根据岩性、颜色、粒度分析、沉积相标志、地球化学特征以及结合古生物化石资料,对中卫下河沿地区晚石炭世红土洼组、羊虎沟组和太原组的沉积相进行了分析研究,确立并划分出泻湖、潮坪、支间湾河口坝、滨海沼泽及三角洲平原等沉积相。在此基础上,结合本地区的古地理背景对宁夏中卫的晚石炭世的古沉积环境进行了重建。

    English Abstract

    谢小平, 王永栋, 沈焕庭. 宁夏中卫晚石炭世沉积相分析与古环境重建[J]. 沉积学报, 2004, 22(1): 19-28.
    引用本文: 谢小平, 王永栋, 沈焕庭. 宁夏中卫晚石炭世沉积相分析与古环境重建[J]. 沉积学报, 2004, 22(1): 19-28.
    shu
    XIEXiao ping, WANGYong dong, SHENHuan ting. Facies Analysis and Sedimentary Environment Reconstruction of the Late Carboniferous in Zhongwei,Ningxia[J]. Acta Sedimentologica Sinica, 2004, 22(1): 19-28.
    Citation: XIEXiao ping, WANGYong dong, SHENHuan ting. Facies Analysis and Sedimentary Environment Reconstruction of the Late Carboniferous in Zhongwei,Ningxia[J]. Acta Sedimentologica Sinica, 2004, 22(1): 19-28.
    shu

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