摘要
在收集矿区水文地质资料的基础上,对太原组上段灰岩富水性进行分析。研究表明,宿南向斜太灰富水性最好,宿东向斜太灰富水性次之,宿南背斜西部太灰富水性最差;随着灰岩埋深的增大,太灰富水性有减小的趋势。
Based on collecting hydrogeological data of Suxian mining area, water abundance of the upper Taiyuan formation limestone was analysed. Research shows that, the water abundance of Taiyuan formation limestone is best in Su＇nan syncline,and which is better in Sudong syncline as well as the water abundance of Taiyuan formation limestone is worst in the west of Su＇nan anticline; with the increase of limestone buried depth, water abundance of Taiyuan formation limesone has a decreased trend.
出处
《煤炭技术》
CAS
北大核心
2014年第10期82-84,共3页
Coal Technology
基金
国家自然科学基金(41272278)
高等学校博士学科点专项科研基金(20123415110002)
2011年度安徽省企业发展专项资金项目(煤炭安全类)
关键词
太原组灰岩
富水性
分布特征
宿县矿区
taiyuan formation limestone
water abundance
distribution law
suxian mining area
