摘要
通过钾盐矿床与晶间卤水分异特征及成因的分析对比,认为晶间卤水分异的过程也就是钾盐矿床形成的过程。胶结浸染状固体矿形成于晶间卤水分异初期的浓缩阶段,改造于分异后期的淡化阶段;晶间卤水矿和层状固体矿形成于淡化阶段。
This paper considers that the potash salt deposit formated with the intercrystalline brine differentiation through analysing and comparing characteristics and mechanism of the potash salt deposit and the intercrystalline brine differentiation. Sideronitic and disseminated solid deposit formated in condensed stage that is in the early part of intercrystalline brine differentiation,was transformed in the desalination stage that is in the later part of the differentiation. The intercrystalline brine deposit and stratiform solid deposit formated in the desalination stage.
出处
《盐湖研究》
CSCD
1996年第2期64-69,共6页
Journal of Salt Lake Research
关键词
盐湖
钾盐矿床
晶间卤水分异
成因关系
卤水
Qarhan Salt Lake, Potash salt, Intercrystalline brine differentiation, Mechanismrelation.