摘要
作者从大量的实际水文地质钻孔资料出发,利用概率统计、二维趋势面分析、回归分析等统计方法和抽水试验资料,研究了漓江河谷区碳酸盐岩岩溶发育与分布特征,及其富水性变化,认为桂林东区土泥盆统融县组灰岩岩溶强裂发育,类似多孔含水介质。
On the basic of. abundaut hydrogcological dri- lling data, the development and distributoon of thecarbonate karst in the Lijiang River basin area andthe variation of water abundance are studied byusing probability statestics, two-dimensional trend-surface analysis, regression analysis and pumpingtest. It is suggested that the well-developed karst inthe Upper Devonian Limestone of Rongxiao Forma-tion in the Eastern Guilin area gives risc to a likilyporous water-bearing medium.
出处
《水文地质工程地质》
CAS
CSCD
北大核心
1990年第2期42-44,36,共4页
Hydrogeology & Engineering Geology
