刘传正, 施韬, 张明霞. 1995: 链子崖危岩体T8──T12缝段开裂变形机制的研究. 工程地质学报, 3(2): 29-41.
    引用本文: 刘传正, 施韬, 张明霞. 1995: 链子崖危岩体T8──T12缝段开裂变形机制的研究. 工程地质学报, 3(2): 29-41.
    Liu Chuanzheng, Shi Tao, Zhang Mingxia. 1995: ON THE MECHANISM OF DEFORMING-CRACKING ON THE SEGMENT OF CRACKS T8-T12 OF LIANZI CLIFF DANGEROUS ROCK BODY. JOURNAL OF ENGINEERING GEOLOGY, 3(2): 29-41.
    Citation: Liu Chuanzheng, Shi Tao, Zhang Mingxia. 1995: ON THE MECHANISM OF DEFORMING-CRACKING ON THE SEGMENT OF CRACKS T8-T12 OF LIANZI CLIFF DANGEROUS ROCK BODY. JOURNAL OF ENGINEERING GEOLOGY, 3(2): 29-41.

    链子崖危岩体T8──T12缝段开裂变形机制的研究

    ON THE MECHANISM OF DEFORMING-CRACKING ON THE SEGMENT OF CRACKS T8-T12 OF LIANZI CLIFF DANGEROUS ROCK BODY

    • 摘要: 文章通过对煤层采空区的分布、地压作用、山体开裂和近20多年来的变形等方面的综合分析,得出链子崖危岩体具有南北强拉裂、东西弱拉裂和平面反时针转动的立体开裂变形机制。据此,作者进行了有针对性的计算,为危岩体综合加固体系的建立提供了依据。

       

      Abstract: The deforming-cracking mechanisms of strong pulling-apart in south-north direction, weak pulling-apart in east-west direction ,and anticlockwise rotation on the horizontal were been recognized after analysis of distribution of coal mined-out area, geopressure action on the roof, and rock body fracturing and deformation in last twenty yeas in this article. On the above analysis,the authors made a series of calculations and applied them to engineering design for controling the Lianzi Cliff dangerous rock body.

       

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