摘要
青海省茫崖镇大浪滩盆地盐矿位于矿产资源丰富的柴达木盆地西北部,区域范围内绝大部分地区分布新生界地层,只在西北部阿尔金山地区有前新生界地层出露。区内沉积厚度较大,地质构造复杂,岩浆活动由加里东期至燕山期均有分布。针对大浪滩盆地盐矿区域水文地质特征分析探讨。
Yanlangtan Basin salt deposit in Yuya Town of Qinghai Province is located in the northwestern part of Qaidam Basin, which is rich in mineral resources. The vast area of the area is distributed in the Cenozoic strata.Only the pre-Cenozoic strata will be exposed in Altun Mountains in the northwest. The sedimentary thickness in the area is large and the geological structure is complex. The magmatic activity is distributed from Caledonian to Yanshanian. The hydrogeological characteristics of the salt mines in Dalangtan Basin are analyzed.
作者
陈金牛
董启伟
范增林
刘溪溪
岳鑫
仇新迪
CHEN Jinniu;DONG Qiwei;FAN Zenglin;LIU Xixi;YUE Xin;QIU Xindi(Qaidam Comprehensive Geology and Mineral Exploration Institute,Golmud,Qinghai 816000,China)
出处
《中国锰业》
2018年第5期113-116,共4页
China Manganese Industry
基金
青海省茫崖镇大浪滩东北部深层卤水钾盐矿普查项目(2013630002)
关键词
大浪滩盆地
盐矿
区域地质
水文地质
Dalangtan Basin
Salt mine
Regional geology
Hydrogeology