ISL OpenIR  > 青海盐湖研究所知识仓储
南极洲万达盐湖中硼的分布和停留时间
于昇松; William J.Green
1991-03-02
Source Publication科学通报
Issue4Pages:280-283
Abstract<正> 万达盐湖位于南极横断山脉的赖特谷(77°32′S、161°31′E).湖呈东西向延伸,北、南两侧分别与阿斯加德和欧林巴斯山的高岩墙相接.湖区是由粗玄岩覆盖的、被煌斑岩侵入的中生代及古生代的花岗岩系组成.现代万达湖长5.6km、宽1.Skm,西侧最大水深68.8m.湖水面终年被厚4m的冰层所覆盖,冰面海拔123m. 万达湖是一典型的双季回水湖,湖水分两层,54m深以上水为淡水层,54m以下为卤水
Keyword 化跃层 停留时间
Language中文
Document Type期刊论文
Identifierhttp://ir.isl.ac.cn/handle/363002/1500
Collection青海盐湖研究所知识仓储
Recommended Citation
GB/T 7714
于昇松,William J.Green. 南极洲万达盐湖中硼的分布和停留时间[J]. 科学通报,1991(4):280-283.
APA 于昇松,&William J.Green.(1991).南极洲万达盐湖中硼的分布和停留时间.科学通报(4),280-283.
MLA 于昇松,et al."南极洲万达盐湖中硼的分布和停留时间".科学通报 .4(1991):280-283.
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