摘要
大盐滩是在阿尔金山走滑大断裂的影响下形成的一个次级断陷盆地,大气降水、山区冰雪融水是区域地下水的主要补给来源。大盐滩是一个以硫酸盐矿物为主的大型钾盐类矿产地。地下卤水可以划分为晶间潜卤水层(W_1)和晶间承压卤水层(W_Ⅱ、W_Ⅲ、W_Ⅳ和W_Ⅴ)5层,大盐滩矿床晶间卤水赋存特征的研究对开发大盐滩矿产资源有着重要意义。
Formed in the influence of the Altun strike- slip fault,Kunty Salt Lake is a secondary fault basin.Atmospheric precipitation and snow melt water are the main recharge source of groundwater in the area.Kunty Salt Lake is a large potassium minerals mainly belonging sulfate type.The underground brines can be classified into the intercrystalline brine（WⅠ）and the pressurized brine（WⅡ、WⅢ、WⅣ and WⅤ）.Getting a clear picture of storage characteristics of intercrystalline brine in Kunty Salt Lake can provide a favorable technical basis for sylvite development.
出处
《盐湖研究》
CSCD
2014年第2期26-32,共7页
Journal of Salt Lake Research
基金
大盐滩钾矿补水评价(Y250101030)
关键词
大盐滩
晶间卤水
赋存特征
Kunty Salt Lake
Intercrystalline brines
Storage characteristics
