化工矿产地质2015，Vol.37Issue(3)：163-167,5.
吉布提阿萨勒(ASSAL)盐湖的卤水钾盐矿床赋存特征
OCCURRENCE CHARACTERISTICS OF BRINE POTASH DEPOSIT AT ASSAL SALT LAKE, DJIBOUTI
赵玉海 1商朋强 1李博昀 1刘星旺1
作者信息
- 1. 中化矿山总局地质研究院,河北涿州 072754
- 折叠
摘要
Abstract
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.关键词
吉布堤/阿萨勒盐湖/钾盐矿/湖表盐水矿/晶间卤水矿/石盐矿Key words
The Republic of Djibouti/Assal salt lake/potash minerals/surface lake/brine minerals/intercrystalline brine minerals/rock salt分类
天文与地球科学引用本文复制引用
赵玉海,商朋强,李博昀,刘星旺..吉布提阿萨勒(ASSAL)盐湖的卤水钾盐矿床赋存特征[J].化工矿产地质,2015,37(3):163-167,5.
