摘要
吉林省西部平原新近系碎屑岩含水层是地下水主要开采层,本文主要对西部平原新近系碎屑岩控水机理分析探讨。
The aquifer of the Neogene system detrital rock in the western plain, Jilin Province is a main exploitation stratum. The paper studied the control water mechanism in the study area.
出处
《吉林地质》
2009年第1期72-74,共3页
Jilin Geology
关键词
碎屑岩沉积
构造环境
沉积特征
新构造运动
富水性
detrital rock sedimentation
structural setting
sedimentary characteristics
neotectonic motion
water abundance
