断陷盆地层滑带的发育特征及矿山开发条件下的再变形分析

    DEVELOPMENT CHARACTERISTICS OF SEAM SLIDING ZONE IN FAULTED BASIN AND AHALYSIS OF ITS REPEATED REDEFORMATION IN UNDERGROUND MINING

    • 摘要: 层滑带在华北断陷盆地中具有普遍性,是影响地下矿山工程围岩稳定的重要因素之一。本文以鲁西矿区为例,阐述了断陷盆地层滑带的发育特征及其形成机制,进行了开挖、运营条件下层滑带再变形分析,并指出了层滑带发育区巷道设计及维护中应注意的某些问题。

       

      Abstract: Seam sliding zones are commonly found in faulted depression basins in Nor th China and become the important factors influencing the stability of their s urrounding rockmass in underground miningworkings. Taking mining areas in weste rn Shandong as examples, this paper discusses development characteristics of sea m sliding zone and its formation mechanism, analyses its repeated deformation u nder the conditions of excavation and operation, and points out some problems to which should be paid attention during roadway designing and maintaining near th e seam sliding zone.

       

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