徐继山, 彭建兵, 马学军, 马润勇, 杨旭东, 封绍武, 安海波. 2012: 邢台市隆尧地裂缝发育特征及成因分析. 工程地质学报, 20(2): 160-169.
    引用本文: 徐继山, 彭建兵, 马学军, 马润勇, 杨旭东, 封绍武, 安海波. 2012: 邢台市隆尧地裂缝发育特征及成因分析. 工程地质学报, 20(2): 160-169.
    XU Jishan, PENG Jianbing, MA Xuejun, MA Runyong, YANG Xudong, FENG Shaowu, AN Haibo. 2012: CHARACTERISTIC AND MECHANISM ANALYSIS OF GROUND FISSURES IN LONGYAO,XINGTAI. JOURNAL OF ENGINEERING GEOLOGY, 20(2): 160-169.
    Citation: XU Jishan, PENG Jianbing, MA Xuejun, MA Runyong, YANG Xudong, FENG Shaowu, AN Haibo. 2012: CHARACTERISTIC AND MECHANISM ANALYSIS OF GROUND FISSURES IN LONGYAO,XINGTAI. JOURNAL OF ENGINEERING GEOLOGY, 20(2): 160-169.

    邢台市隆尧地裂缝发育特征及成因分析

    CHARACTERISTIC AND MECHANISM ANALYSIS OF GROUND FISSURES IN LONGYAO,XINGTAI

    • 摘要: 隆尧地裂缝在华北地区是典型表生灾害,不仅对地表造成了潜蚀、塌陷、张裂、错断、龟裂等地质灾害,而且给当地的农业生产、工程建设、人民生活造成严重经济损失。为揭示其成因,本文利用地质调查、监测与测量、槽探、物理勘探等方法,主要研究了隆尧地裂缝的发育特征,包括平面、剖面、深部、活动4个方面,总结了地裂缝的发育规律,最后从孕裂环境、启裂条件、破裂过程等3个方面对其成因展开分析。通过研究,本文认为:(1)隆尧地裂缝出露于十余个村镇达30km,分别向NWW、NEE方向延伸,与隆尧断裂高度一致; 其活动时间具有周期特征,可分为开启-闭合-缓变-骤变等4个时期。(2)隆尧地裂缝受控于隆尧断裂,区域内的深部构造、断裂构造、构造地貌等条件为地裂缝的形成提供了孕裂环境。孕裂过程经历了应力积累、破碎带形成2个时期。(3)断裂活动是开裂的动力基础,地下水抽采、地表水入渗是开裂的重要因素。(4)隆尧地裂缝的开裂过程具有时间和空间上的不均性。从目前的勘察和研究情况来看,隆尧地裂缝活动正处于活跃期。

       

      Abstract: The ground fissures in Longyao County are the typical surface disaster in North China region. They not only caused eroding, collapsing, extension fracturing, faulting, cracking and other geological disasters on the earth’s surface, but also caused severe economic losses in the local agricultural production, engineering construction and the lives of the people. This paper aims to reveal their genetic nature. It is based on geological investigation, monitoring and measuring, trenching, physical exploration. It studies the development characteristics of the Longyao ground fissures. They include the planes, profiles, deep and activity aspects. The paper summarizes the laws of ground fissures. Finally the ground fissure mechanism is analyzed from their crack-pregnant environment, crack-opening conditions and cracking process.the study concludes that: (1)Longyao ground fissures expose in a dozen villages of more than 30km long. They extend towards NWW and NEE which are concordant with the direction of Longyao fault system. Their periodicities are consist of opening, closing, slowly cracking and suddenly cracking periods.(2)Longyao ground fissures are controlled by the faults zone. The conditions such as deep structure, faulted structure and structural landform provide the ground fissures with crack-pregnant environment in the area. The crack-pregnant environment has through three stages: stress accumulation and fractured zone formation.(3)Faulting is the foundation of ground cracking. The groundwater exploitation and surface infiltration also are the important factors.(4)the process of Longyao ground fissures is heterogenous temporally and spatially. From the present investigation and study, the ground fissures are in active period in the area.

       

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