摘要
阐述了临涣矿区开采前、后新生界底部含水层的水化学特征及其形成作用；提出了底含水化学成因模式。对矿井底含突水水源的准确判断及井筒破裂原因分析具有积极意义。
The hydrochemical characteristics of the floor aquifer of KeinozQic before and after development in Linhuan mining area and their origin are described in detail. The hydrochemical forming model is presented. These are important for the forecast of water--inrush of the floor aquifer and the analysis of shaft fracturing.
出处
《煤田地质与勘探》
CAS
CSCD
北大核心
1994年第4期37-41,共5页
Coal Geology & Exploration
关键词
水化学
含水层
成因
临涣矿区
ydrochemistry
aquifer
genesis
Linhuan mining area
