摘要
对矿区基底O1灰岩的溶隙、溶孔、溶洞进行综合分析,得出矿区的岩溶形态和岩溶发育程度特征。对研究奥陶系灰岩岩溶含水层的发育分布特征、富水特征及其地下水运移规律具有重要意义。
The basal 01 limestone mining area of the gap, solution pores were analyzed comprehensively. It was concluded that the morphology and degree of rock dissolve development characteristics in mining area, which was of great significance in studying the distribution of the ordovician limestone rock dissolve aquifer characteristics, the characteristic of rich water and groundwater migration.
出处
《煤炭与化工》
CAS
2013年第8期4-6,共3页
Coal and Chemical Industry
关键词
蔚县
奥陶系
岩溶
发育规律
Yuxian
ordovician
rock dissolve
development law