摘要
本文通过对平顶山地区水文地质循环中氢、氧同位素组成分布及地下水-岩作用过程的分析,识别了矿区地下水流系统,并对岩溶发育规律进行了初步研究。
This paper deals with the isotopic composition of hydrogen and oxygen in hydrogeology cycle and water-rock interaction in Pingdingshan area, based which the groundwater flow systems are recognized and the rules governing karst development is preliminarily studied.
出处
《水文地质工程地质》
CAS
CSCD
北大核心
1992年第4期16-19,共4页
Hydrogeology & Engineering Geology
