摘要
本文利用店子、文登铁矿钻孔资料，分析了淄河断裂地下岩溶的发育规律和控制因素。根据抽水试验资料进行了富水性分区，发现各区的富水性与地下岩溶发育密切相关。
This paper, usins borehole data of Dianzi iron mine and Wendens iron mine, analyses the regularity and the control factors of the karst development in Zihe fracture. According to pumping experimental data it has carried out a division for the watery areas, finding that the each watery area is related to the karst development. It has the guiding significance to comprehend the karst development pathern for understanding the watery layers, for analysing hydrogeologic conditon, for predicting outflow rate of pits and for opening up a mine and water contral.
关键词
淄河断裂
店子铁矿
岩溶发育规律
富水性
岩溶
Zike fracture
the regularity of the karst development
dianzi iron mine
wendeng iron mine
watery.
