贵州沙子岭煤矿断裂构造特征及其对矿井充水条件的控制  

The characteristics of the Shaziling colliery faulted structure in Guizhou and its control of the filling water conditions of mine

作　　者：张斌[1] 沈大兴[1] 梁龙[1] 谭海英[1] 

机构地区：[1]贵州省地质矿产勘查开发局106地质大队,贵州遵义563000

出　　处：《有色金属文摘》2015年第3期63-65,共3页Nonferrous Metals Abstract

摘　　要：本文重点研究沙子岭煤矿的充水途径。该煤矿充水主要受大型边界断裂构造控制。通过野外调查及工程揭露,查清了几条边界断层的性质、断距、上下盘岩性组合、导水及富水性等。因此今后矿山的重点防水部位应为这3条断层带附近,应留设好防水墙。This paper emphasized on the study of the water filling ways of mine. After analyzing, it found out that water filling of colliery was mainly controlled by the large boundary faulted structure. It also made clear several boundary faults＇ nature, fault throw, transmissibility, watery as well as the lithology association of upper and lower sides and others through field investi- gation and engineering revelation. Thus, in the future, the waterproof wall should be built around the three faulted zone, which is the key waterproof area.

关 键 词：断裂构造 矿井充水 水文地质特征 沙子岭煤矿 

分 类 号：TD745[矿业工程—矿井通风与安全]