东滩矿断层活化对3煤顶板突水的影响  

Influence of fault activation on water inrush from roof of Coal Bed 3 in Dongtan Mine

作　　者：冯恩杰 付民强 

机构地区：[1]兖矿集团公司东滩煤矿,山东邹城273512

出　　处：《煤田地质与勘探》2004年第4期33-36,共4页Coal Geology & Exploration

摘　　要：兖州矿区东滩煤矿二叠纪 3(3上)煤层与其顶部侏罗纪红层的间距约 6 0～ 2 2 0m。回采过程中多数工作面未发生红层突水 ,或水量较小 ;4 30 8和 14 30 1工作面却发生了红层突水 ,且水量较大。分析认为 :采动影响使工作面内断层活化 ,增大了冒裂带高度 ,从而导通红层含水层所致 ,最后提出了防治红层突水的建议。The distance between Triassic age Coal Bed 3 and Jurassic age red bed is about 60～220 m in Dongtan Mine,Yanzhou mining area.Generally in mining process no water inrush or less water from roof red bed,but in Nos 4308 and 14301 mining faces occur water inrush and the water yield is relatively large.The analysis results indicated that the mining operation caused the fault to activate and the height of caving zone to increase,connecting the red bed aquifer.At last,schemes are suggested to control water inrush from red bed.

关 键 词：冒裂带 红层突水 断层活化 东滩煤矿 

分 类 号：P641.4[天文地球—地质矿产勘探]