摘要
柴达木盆地是我国最大的盐湖产业基地,大柴旦盐湖为盆地内重要的固液相硼矿床,其卤水中富含硼、锂、钾、镁、钠、溴、碘等。通过勘查大柴旦地质背景和卤水储层地质特征,分析大柴旦湖水(地表卤水)、潜卤水、承压卤水水文地质特征、水化学特征,结果表明大柴旦地区硼、锂来源于地球深部,断裂构造为导卤构造,钾、钠、镁等盐类来源于周缘花岗岩,新构造运动形成大柴旦断陷盆地接受沉积,干旱的气候条件下沉积盐类地层,随着地下水补给增加,岩盐层溶解,形成高矿化度卤水,相应的硼、钾、锂等溶解于卤水之中,形成卤水(液体硼矿)。
The Qaidam Basin is the largest industrial base in Salt Lake,and the Salt Lake Basin is an important solid-liquid boron deposit in the basin,which is rich in boron,lithium,potassium,magnesium,sodium,bromine,iodine and so on.In order to provide an important basis for the full development and application of Da Qaidam Salt Lake,through the study of dachaidan geological background,brine reservoir geological characteristics,based on the analysis of the hydrogeological and hydrochemical characteristics of the water(surface brine),buried brine and confined brine in the lake,it is considered that boron and lithium in the lake come from the deep part of the Earth,and the fault structure is a salt-conducting structure,the salts such as potassium,sodium and magnesium come from the peripheral granite,and the neotectonic movement formed the Da Qaidam faulted basin to accept the sediments,the formation of high salinity brine,the corresponding boron,potassium,lithium dissolved in the brine,the formation of brine(liquid boron ore).
作者
马鸿颖
李洪普
安永为
仇新迪
MA Hongying;LI Hongpu;AN Yongwei;QIU Xindi(Qinghai Province Key Laboratory of Exploration Research of Salt Lake Resources in Qaidam Basin,Geerm,816099,China;Qinghai Province Qaidam Qaidam Comprehensive Geological and Mineral Exploration Institute,Geerm,816099,China;Qinghai Provincial Geological Survey Institute,Xining,810016,China)
出处
《盐湖研究》
CAS
CSCD
2024年第2期54-61,共8页
Journal of Salt Lake Research
基金
青海省基金项目(2022-ZJ-734)。
关键词
卤水特征
卤水成因
液体硼矿
大柴旦盐湖
Brine characteristics
Origin of brine
Liquid Boron ore
Da Qaidam Salt Lake
