摘要
榆神府矿区具供水意义的含水层为萨拉乌苏组和烧变岩,均位于煤系地层上部及浅部,在分析烧变岩水文地质条件基础上,主张在烧变岩带建立供水水源地,是解决近期矿区供水既经济可行又可靠的技术途径。
The effective aquifers in Yushenfu coal mining area are Salawusu Formation and fritted rock that settled on the upper part of coal and shallow of strata. Based on the analysis of fritted rock＇s hydro - geological condition, it is pointed out that establishment of wa- ter supply base in fritted rock zone is the economical and reliable way to solve the water problem in mines in＇ the near future.
出处
《陕西煤炭》
2005年第4期20-21,17,共3页
Shaanxi Coal
关键词
烧变岩
地下水
水源地
榆神府矿区
fritted rock
groundwater
water supply base
Yushenfu coal mining area.
