CAJ | 학술논문

根据兴隆庄井田的构造特点，分析了构造对奥灰的控制作用及对突水的影响，得出兴隆庄井田奥灰富水性具有从西北向东南减弱，并在其中构造发育部位加强的特点。井田内一些落差较大的断层缩小了奥灰与上覆薄层灰岩和下组煤层的间距，增加了奥灰突水的可能性。研究结果可为兴隆庄井田下组煤的安全开采提供参考。
근거흥륭장정전적구조특점，분석료구조대오회적공제작용급대돌수적영향，득출흥륭장정전오회부수성구유종서북향동남감약，병재기중구조발육부위가강적특점。정전내일사락차교대적단층축소료오회여상복박층회암화하조매층적간거，증가료오회돌수적가능성。연구결과가위흥륭장정전하조매적안전개채제공삼고。
This paper, on the basis of the structural features in Xinglongzhuang Mine Field, analyzed the control action of the structure on Ordovician limestone and its influence on water inrush, obtained the characteristics that the water abundance of Ordovician limestone weakened from northwest to southeast and strengthened in the structure developed zone. Some faults with larger throws in the mine field narrowed the distance between the Ordovician limestone and the overlying thin limestone layer and the lower group of coal seams, which increased the possibility of water inrush. The research results can provide reference for the safe-mining of the lower group of coal seams in Xinglongzhuang Mine.