张德波, 谭泽新, 张欣. 2006: 东莞断陷盆地第三系地层的工程岩土特征. 工程地质学报, 14(S1): 42-46.
    引用本文: 张德波, 谭泽新, 张欣. 2006: 东莞断陷盆地第三系地层的工程岩土特征. 工程地质学报, 14(S1): 42-46.
    ZHANG Debo, TAN Zexin, ZHANG Xin. 2006: THE GEOTECHNICAL CHARACTERISTICS OF TERTIARY SYSTEM IN DONGGUAN FAULT BASIN. JOURNAL OF ENGINEERING GEOLOGY, 14(S1): 42-46.
    Citation: ZHANG Debo, TAN Zexin, ZHANG Xin. 2006: THE GEOTECHNICAL CHARACTERISTICS OF TERTIARY SYSTEM IN DONGGUAN FAULT BASIN. JOURNAL OF ENGINEERING GEOLOGY, 14(S1): 42-46.

    东莞断陷盆地第三系地层的工程岩土特征

    THE GEOTECHNICAL CHARACTERISTICS OF TERTIARY SYSTEM IN DONGGUAN FAULT BASIN

    • 摘要: 东莞断陷盆地位于广州东部,基岩为第三系红色碎屑岩,属冲洪积相沉积。其特殊的岩性组合造成盆地的基岩岩性变化无常,风化不均,软弱夹层异常发育,形成了极其复杂的工程岩土条件,给工程基础设计和施工带来了不利影响。本文根据近几年在该地区进行的工程岩土勘察实践,对其第三系地层的工程岩土特征进行研究和总结,以期为该区今后的工程建设提供参考。

       

      Abstract: Dongguan fault basin located in the east of Guangzhou, the bedrock belong to Tertiary system fragmentary rocks, it's alluvial and pluvial sediment. The rock and its weathering grade are different from here to there within basin, because of the different rock-combinations. So the development of soft-interlayer is all-pervading. In a word the rock and soil conditions are extremely complicated and bring adverse affection to engineering construction. This paper summary the characteristics of Tertiary system, according to geotechnical investigation during the past years in the basin. Our work can provide important reference for the engineering constructions in those areas.

       

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