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北京平原地区第四纪地质研究新进展

蔡向民, 张磊, 郭高轩, 尤世娜, 方同明, 吕金波, 梁亚楠

蔡向民, 张磊, 郭高轩, 尤世娜, 方同明, 吕金波, 梁亚楠. 北京平原地区第四纪地质研究新进展[J]. 中国地质, 2016, 43(3): 1055-1066. DOI: 10.12029/gc20160327
引用本文: 蔡向民, 张磊, 郭高轩, 尤世娜, 方同明, 吕金波, 梁亚楠. 北京平原地区第四纪地质研究新进展[J]. 中国地质, 2016, 43(3): 1055-1066. DOI: 10.12029/gc20160327
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CAI Xiang-min, ZHANG Lei, GUO Gao-xuan, YOU Shi-na, FANG Tong-ming, LV Jin-bo, LIANG Ya-nan. New Progress in the study of Quaternary geology in Beijing Plain[J]. GEOLOGY IN CHINA, 2016, 43(3): 1055-1066. DOI: 10.12029/gc20160327
Citation: CAI Xiang-min, ZHANG Lei, GUO Gao-xuan, YOU Shi-na, FANG Tong-ming, LV Jin-bo, LIANG Ya-nan. New Progress in the study of Quaternary geology in Beijing Plain[J]. GEOLOGY IN CHINA, 2016, 43(3): 1055-1066. DOI: 10.12029/gc20160327
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北京平原地区第四纪地质研究新进展

  • 1. 北京市地质调查研究, 北京 102206;

  • 2. 北京市水文地质工程地质大队, 北京 100195

基金项目: 

中国地质调查局项目(1212011301290)资助。

详细信息
    作者简介:

    蔡向民,男,1958年生,教授级高级工程师,主要从事区域地质、环境地质调查研究;E-mail:cxm5706@sohu.com。

  • 中图分类号: P534.63

New Progress in the study of Quaternary geology in Beijing Plain

  • 1. Beijing Institute of Geological Survey, Beijing 100195, China;

  • 2. Hydrogeological and Engineering Geological Party of Beijing, Beijing 100195, China

Funds: 

China Geological Survey Program (No. 1212011301290).

摘要

    摘要
  • 摘要: 北京平原地处山前冲洪积扇分布区,区内湖泊密布,河流纵横,沉积环境多样。由于第四系三维结构的复杂性,对第四系进行地层划分有一定的难度。前人根据不同的资料对北京平原第四系进行过地层划分,建立了泥河湾组、周口店组、马兰组等多个岩石地层单位。这些地层单位主要是依据沉积凹陷钻孔岩心中的孢粉、有孔虫、介形虫等化石和少量的古地磁数据划分的,实际上仍是年代地层单位。由于这些地层单位划分依据不统一,识别标志不清晰,因此难以得到广泛的共识。近十余年来,随着资料的积累和对第四系三维结构的认识提高,特别是古地磁测年技术的普及,为北京平原第四纪地层的划分奠定了基础。本文依据40余个钻孔的古地磁测试数据,初步厘定了下更新统底界、中更新统底界、上更新统底界3个等时面。依据工程地质勘察、水文地质钻孔、考古发掘和泥炭调查等资料编绘了平原区全新统等厚度图。
    Abstract: Beijing plain, located in the piedmont alluvial fan area, has lots of lakes and rivers in its administrative area. Because of the variability of sedimentary environment, the three-dimensional structure is very complex. Due to the complexity of the threedimensional structure of the Quaternary strata, the Quaternary stratigraphic division is relatively difficult to some extent. Some researcher have established the lithostratigraphic units such as Nihewan Group, Zhoukoudian Group and Malan Group based on some geological data from different sources. These stratigraphic units are mainly based on fossil pollen, foraminifera, and Ostracoda in sedimentary sag drill holes, and a small amount of paleomagnetic data, and are actually the chronostratigraphic units. Because the units are not uniform and the identification mark is not clear, it is difficult to get a broad consensus. In the past 10 years, the increase of the accumulation of data, the understanding of the three-dimensional structure of the Quaternary, and especially the popularity of the ancient magnetic prospecting technology have laid the foundation for the division of the Quaternary strata in Beijing plain. Based on paleomagnetic data from more than 40 drill holes, the authors initially established the bottom boundaries of lower, middle and upper Pleistocene series. According to the engineering geological prospecting, hydrogeological drilling, archaeological excavations and peat investigation materials, the authors compiled a Holocene isopach map for Beijing Plain.
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出版历程
  • 收稿日期:  2016-03-20
  • 修回日期:  2016-04-15
  • 网络出版日期:  2023-09-26
  • 刊出日期:  2016-06-24

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