杨军, 李伟, 单联君. 2006: 广州西部上白垩统黄花岗段的岩溶现象与成因分析. 工程地质学报, 14(S1): 38-41.
    引用本文: 杨军, 李伟, 单联君. 2006: 广州西部上白垩统黄花岗段的岩溶现象与成因分析. 工程地质学报, 14(S1): 38-41.
    YANG Jun, LI Wei, SHAN Lianjun. 2006: ANALYSIS THE CAUSE OF UPPER CHALK KARST PHENOMENA IN HUANGHUAGANG AREA OF WEST GUANGZHOU. JOURNAL OF ENGINEERING GEOLOGY, 14(S1): 38-41.
    Citation: YANG Jun, LI Wei, SHAN Lianjun. 2006: ANALYSIS THE CAUSE OF UPPER CHALK KARST PHENOMENA IN HUANGHUAGANG AREA OF WEST GUANGZHOU. JOURNAL OF ENGINEERING GEOLOGY, 14(S1): 38-41.

    广州西部上白垩统黄花岗段的岩溶现象与成因分析

    ANALYSIS THE CAUSE OF UPPER CHALK KARST PHENOMENA IN HUANGHUAGANG AREA OF WEST GUANGZHOU

    • 摘要: 广州西部上白垩统黄花岗段存在岩溶现象,钻孔见洞率4%~40%,其发育程度主要受灰岩分布、构造活动、地层剥蚀带以及地下水动力作用的控制。其岩溶特征是溶洞规模相对小、层数相对少、80%以上无充填、洞顶之上常存在软塑状全风化岩带,无溶沟溶槽伴生。由于区内的岩溶地质现象分布极其不均,对此,本文就工程建设的适宜性与基础选择问题进行了专门评述,以期对该地区的工程建设有参考作用。

       

      Abstract: Upper Chalk Karst is exist in Huanghuagang area of west Guangzhou, the probability of water-eroded cave existing in one drill is 4 to 40 percent, the factors main affecting developing degree of the water-eroded cave include the distributing of limestone, the acting of conformation, the denudation of stratum and the dynamical action of ground water. the dimensions of it is smaller, the layers is less, nothing fill in 80 percent of it, existing the whole airslake soft plasticity stone strap above the water-eroded cave, no accompany by the karren and solution groove, all of these are the characters of the Upper Chalk Karst. Considering the distribution of the Upper Chalk Karst is very misproportion, therefore, the feasibility of engineering construction and the selection of base foundation are specially discussed in this paper, the result is hoped to have some reference to the engineering construction in this area.

       

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