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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
引用本文:张永双,曲永新,胡绍祥.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[J].工程地质学报(英文版),1999,7(2):154-160.
作者姓名:张永双  曲永新  胡绍祥
作者单位:1.中国科学院地质研究所工程地质力学开放研究实验室,北京100029;
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。

关 键 词:断陷盆地    煤矿    层滑带    再变形分析    巷道支护
收稿时间:1998-01-10
修稿时间:1998-01-10

DEVELOPMENT CHARACTERISTICS OF SEAM-SLIDING ZONE IN FAULTED BASIN AND AHALYSIS OF ITS REPEATED REDEFORMATION IN UNDERGROUND MINING
Institution:1.Institute of Geology, Chinese Academia of Sciences, Beiji ng 100029;2.Shandong Institute of Mining and Technology, Tai’an 271019
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.
Keywords:Faulting  depression  basin  Coal mine  Seam  sliding z one  Repeated  deformation analysis  Roadway supporting  
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