CAJ | 학술논문

吉布堤阿萨勒(Assal)盐湖卤水钾盐矿床由其东南部的湖表卤水矿和西北部的晶间卤水矿两部分构成.二者水力联系密切.通过对湖表及晶间卤水分异特征等综合分析表明钾质来源于与之有断裂通道相通的浓缩海水、湖下及湖缘存在的热泉以及周边富钾玄武岩通过季节性河流水的不断补给有关.盐湖演化时间相对较短,具明显的海相成因特点.
길포제아살륵(Assal)염호서수갑염광상유기동남부적호표서수광화서북부적정간서수광량부분구성.이자수력련계밀절.통과대호표급정간서수분이특정등종합분석표명갑질래원우여지유단렬통도상통적농축해수、호하급호연존재적열천이급주변부갑현무암통과계절성하류수적불단보급유관.염호연화시간상대교단,구명현적해상성인특점.
The brine potash deposit at Assal salt lake, is composed of two parts which have close relationship with each other, they are the southeastern surface brine minerals and northwestern intercrystalline brine minerals. Some analysis on differentiation characteristics of surface and intercrystalline brine shows that, the potassium come from concentrated seawater which has the communicant broken channel and hot spring which is located under or nearby the lake as well as the nonperennial river water which had transferred through thek-rich basalt. The Assal salt lake evolve short with obvious feature of marine facies formation.