根据大量地质资料揭示了山东良庄井田地质构造的发育特征,其断裂构造具有分区性、方向性、垂向分层性、成带性等特点,并推断井田内发育有滑动构造。探讨了该井田地质构造发育规律对矿井突水的影响,着重分析了滑动构造对矿井突水的作用。研究表明,断裂构造的分区性、方向性、垂向分层性、成带性及滑动构造对矿井突水有不同程度的影响。
Based on a great deal of geological data,we studied the geological tectonic features of Liangzhuang mine.Study shows that fault has the fallowing features such as regionalization,vertical stratification,direction,zonation,and gravity gliding structures are inferred in the mine.We also discuss the influence of geological structural development on water outburst with emphasis on the action of gliding structures on water outburst in the mine.