中国震旦系深层水成因的两种基本模式——以四川盆地和冀中拗陷为例  

TWO GENETIC MODELS OF THE DEEP GROUNDWATER IN THE SINIAN STRATA OF CHINA ——Taking Sichuan Basin and Central Hebei Depression for exampies

作　　者：汪蕴璞 王翠霞 叶思源 

出　　处：《水文地质工程地质》1989年第4期1-4,共4页Hydrogeology & Engineering Geology

摘　　要：本文在总结四川盆地、冀中拗陷震旦系深层地下水化学成分的特征和水化学场属性的基础上,从水文地质发育史的角度,划分了地下水形成的水文地质期和恢复了各期水文地质作用的主要特点,重建和再现了它们的形成过程,从而概括了深层水成因的两种基本模式。On the basis of the elementary Characteristics of the hydrochemical field and the Chemisal Compositions of deep groundwater hi Sichuan Basin and Central Hebei Depression, the hydrogeological stages of the groundwater genesis are divided, the hydrogeological processes in different stages are recovered, and two genetic models of deep groundwater are summarized, whose theoretical and practical value in the understanding of the formation of oil-gas field and also for the exploitation and utilization of the water resources in these areas are disscussed.

关 键 词：震旦纪 深层水 成因 岩溶水 沉积水 

分 类 号：P641.11[天文地球—地质矿产勘探]