朱志刚, 魏云杰, 陶连金, 王成. 2010: 北京燕家台碎裂岩体的成因机理及其工程地质意义. 工程地质学报, 18(S1): 71-75.
    引用本文: 朱志刚, 魏云杰, 陶连金, 王成. 2010: 北京燕家台碎裂岩体的成因机理及其工程地质意义. 工程地质学报, 18(S1): 71-75.
    ZHU Zhigang, WEI Yunjie, TAO Lianjin, WANG Cheng. 2010: FORMATION MECHANISM OF YANJIATAI CRACKED ROCK MASS AND ENGINEERING GEOLOGICAL SIGNIFICANCE IN BEIJING. JOURNAL OF ENGINEERING GEOLOGY, 18(S1): 71-75.
    Citation: ZHU Zhigang, WEI Yunjie, TAO Lianjin, WANG Cheng. 2010: FORMATION MECHANISM OF YANJIATAI CRACKED ROCK MASS AND ENGINEERING GEOLOGICAL SIGNIFICANCE IN BEIJING. JOURNAL OF ENGINEERING GEOLOGY, 18(S1): 71-75.

    北京燕家台碎裂岩体的成因机理及其工程地质意义

    FORMATION MECHANISM OF YANJIATAI CRACKED ROCK MASS AND ENGINEERING GEOLOGICAL SIGNIFICANCE IN BEIJING

    • 摘要: 岩石薄片鉴定和微观特征研究表明:碎裂岩体的组成以伊利石黏土为主,具有泥质结构,薄层状构造,页理发育; 区域构造特征分析说明区域构造作用对于碎裂岩体的形成具有控制作用,沿河城断裂经过挤压、引张、再挤压的反复加载-卸载过程及紫荆关沿河城断裂、房山八宝山断裂的扭动作用,形成了区内裂隙网络化,使岩体碎裂化; 岩体的正常卸荷作用和缓倾角结构面的卸荷回弹,使岩体碎裂化加剧。

       

      Abstract: Through the thin section identification and micro-characters study.Cracked rock mass are mainlyillite clay with shaly structure,thin-layer structure and joints were developed.Through the analysis of regional tectonic features,the regional tectonic process controls the formation of cracked rock mass.Yan Hecheng fault formed fracture network of the region and cracked rock mass after repeated loading-unloading process by extrusion,tension and squeeze and Zi Jing Guan fault,Fang Shan-Ba Bao Shang fault twist action.Rock mass normal unloading and gently dipping structural plane unloading rebound so that rock mass become more cracked.

       

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