| 西台吉乃尔盐湖地下卤水的赋存特征 |
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| 引用本文： | 高东林,马海州,张西营,韩凤清,周笃珺.西台吉乃尔盐湖地下卤水的赋存特征[J].盐湖研究,2006,14(2):1-6. |
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| 作者姓名： | 高东林 马海州 张西营 韩凤清 周笃珺 |
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| 作者单位： | 中国科学院青海盐湖研究所,青海,西宁,810008 |
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| 摘 要： | 西台吉乃尔盐湖属于柴达木盆地构造分区茫崖坳陷中的一里坪凹陷区,位于柴达木盆地东部三湖(台吉乃尔湖、涩聂湖和达布逊湖)沉降区的西端,接受来自昆仑山北坡的那陵格勒河补给。此盐湖是以卤水锂矿物为主,并伴生钾、硼、镁等多种组分的大型矿产地,水化学类型属于硫酸盐型硫酸镁亚型。地下卤水划分为晶间潜卤水(WⅠ)、孔隙潜卤水(WⅡ-1)和晶间承压卤水(WⅡ-2)三层。
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| 关 键 词： | 柴达木盆地 盐湖 地下水 |
| 文章编号： | 1008-858X(2006)02-0001-06 |
| 修稿时间： | 2005年12月21 |
Storage Characteristics of Ground Brines of West Taijinar Salt Lake |
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| GAO Dong-lin,MA Hai-zhou,ZHANG Xi-ying,HAN Feng-qing,ZHOU Do-jun.Storage Characteristics of Ground Brines of West Taijinar Salt Lake[J].Journal of Salt Lake Research,2006,14(2):1-6. |
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| Authors: | GAO Dong-lin MA Hai-zhou ZHANG Xi-ying HAN Feng-qing ZHOU Do-jun |
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| Abstract: | Belonging to the Yiliping depression of the Mangya sink,the west Taijinar Lake is located in the western region of the three lakes(West Taijinar Lake,East Taijinar Lake,and Senie Lake).The lake water is replenished by the Nalinggele River,which originates from the north of the Kunlun Mountain.This lake is characterized as a large mineral reserve of brines containing remarkable amount of lithium associated with other components like potassium,boron and magnesium.The hydrochemistry of the brines are of the magnesium sulfate sub-type.The underground brines can be classified into the latent intercrystalline brine(WI),the latent cavity brine(WⅡ-1),and the pressurized brine(WⅡ-2) |
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| Keywords: | Qaidam Basin Salt lake Ground brine |
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