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陕西安塞城区基岩崩塌主控构造因素分析

王虎, 郭怀军, 王益民, 薛强, 王凯, 查显锋, 王晓勇, 孙萍萍, 程秀娟. 陕西安塞城区基岩崩塌主控构造因素分析[J]. 中国地质灾害与防治学报, 2022, 33(3): 51-60. doi: 10.16031/j.cnki.issn.1003-8035.2022.03-06
引用本文: 王虎, 郭怀军, 王益民, 薛强, 王凯, 查显锋, 王晓勇, 孙萍萍, 程秀娟. 陕西安塞城区基岩崩塌主控构造因素分析[J]. 中国地质灾害与防治学报, 2022, 33(3): 51-60. doi: 10.16031/j.cnki.issn.1003-8035.2022.03-06
WANG Hu, GUO Huaijun, WANG Yimin, XUE Qiang, WANG Kai, ZHA Xianfeng, WANG Xiaoyong, SUN Pingping, CHENG Xiujuan. Analysis on the main structural factors controlling rockfalls in downtown of Ansai, Shaanxi Province[J]. The Chinese Journal of Geological Hazard and Control, 2022, 33(3): 51-60. doi: 10.16031/j.cnki.issn.1003-8035.2022.03-06
Citation: WANG Hu, GUO Huaijun, WANG Yimin, XUE Qiang, WANG Kai, ZHA Xianfeng, WANG Xiaoyong, SUN Pingping, CHENG Xiujuan. Analysis on the main structural factors controlling rockfalls in downtown of Ansai, Shaanxi Province[J]. The Chinese Journal of Geological Hazard and Control, 2022, 33(3): 51-60. doi: 10.16031/j.cnki.issn.1003-8035.2022.03-06

陕西安塞城区基岩崩塌主控构造因素分析

  • 基金项目: 中国地质调查局地质调查项目(DD20189270;DD20211398)
详细信息
    作者简介: 王 虎(1983-),男,甘肃张掖人,硕士,工程师,主要研究方向为岩石地层。E-mail:whu_xa2020@163.com
    通讯作者: 郭怀军(1990-),男,陕西延安人,硕士,工程师,主要研究方向为新生代地质与环境。E-mail:guohj03@163.com
  • 中图分类号: P642.21

Analysis on the main structural factors controlling rockfalls in downtown of Ansai, Shaanxi Province

More Information
  • 安塞区主城区范围内的基岩地层发育一以延河为枢纽线、走向约330°的背斜构造,在基岩地层中普遍发育走向与褶皱轴面平行(320°~340°)和垂直(40°~60°)两个方位的两组张性节理,还发育有两组与褶皱轴斜交的共轭剪切节理,第一组共轭剪切节理面走向为近南北(0°~10°)和近东西(80°~90°),第二组共轭剪切节理面走向为100°~120°和200°~210°。上述基岩中发育的、不同走向的多组节理面对研究区内具相同走向分布特征的崩塌结构控制面的发育有较强控制作用。第一组共轭剪节理中走向近东西(80°~90°)的节理面控制着研究区内发育程度最高的崩塌结构控制面,它与区内岩质崩塌的发育相关程度最高;其次是两组张性节理面分别控制着走向相同且发育程度较高的两组岩质崩塌结构控制面,第二组共轭剪节理面则控制着区内发育程度相对较低的、走向与共轭节理面相同的两组崩塌结构控制面。

  • 加载中
  • 图 1  安塞主城区地理位置及灾害地质图

    Figure 1. 

    图 2  安塞区内出露的砂—泥岩组合

    Figure 2. 

    图 3  安塞区主城区东西向地层结构剖面图

    Figure 3. 

    图 4  圆柱状褶皱中发育的节理、破裂,小型断层及缝合面构造[31]

    Figure 4. 

    图 5  安塞区基岩地层中所发育节理的特征

    Figure 5. 

    图 6  安塞区主城区内岩质崩塌相对基覆界面位置图

    Figure 6. 

    图 7  安塞区阳庄崩塌灾害点现场示意图及剖面图

    Figure 7. 

    图 8  贾家洼崩塌露头示意图及剖面图

    Figure 8. 

    图 9  基岩节理产状赤平投影及走向分布图

    Figure 9. 

    图 10  基岩节理赤平投影极点密度与玫瑰花分析图

    Figure 10. 

    图 11  崩塌结构控制面极射赤平投影分析结果

    Figure 11. 

    图 12  崩塌控制结构面赤平投影及走向统计分析图

    Figure 12. 

    表 1  安塞主城区基岩中所发育节理的参数及特征

    Table 1.  Parameters and characteristics of joints developed in bedrock of ansai urban

    序号走向/(°)倾角/(°)性质发育程度
    1320~34074~89纵节理(张性节理)
    240~6075~90横节理(张性节理)较高
    30~1083~90第一组共轭剪切节理较高
    480~9077~85
    5100~12075~85第二组共轭剪切节理一般
    6200~21080~85
    下载: 导出CSV
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出版历程
收稿日期:  2022-02-22
修回日期:  2022-05-12
录用日期:  2022-05-13
刊出日期:  2022-06-25

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