摘要
大浪滩盆地是柴达木盆地西部的一个次级盆地,以新生界沉积为主,蕴藏着丰富的盐类矿产资源。本文从卤水钾矿的分布上、含钾卤水地层的岩性、水文地质、水化学及主要组份含量方面论述了大浪滩盆地深层松散岩类孔隙卤水的赋存特征。
Dalangtan Basin is a secondary basin in the west of Chaidamu Basin. It is dominated by the neozoic deposits and is rich in salt mineral resources.This paper, from the brine potassium ore distribution, the stratigraphic lithology, hydrogeological, brine potassium in chemistry and the content of main components of water basin, discusses the occurrence characteristics of pore brine in the deep loose rocks in Dalangtan Basin.
作者
王新民
Wang Xinmin(liangsu Yangtzer River Geological Exploration Institution, Nanjing Jiangsu, 21004)
出处
《中国井矿盐》
CAS
2018年第4期14-17,共4页
China Well and Rock Salt
关键词
卤水钾矿
孔隙
赋存特征
Brine potassium mine
pore
occurrence characteristics