现代干盐湖晶间卤水分异成因的新观点阶段性淡化说以中国察尔汗盐湖为例

已被多数研究察尔汗盐湖的地质学者普遍运用的、原苏联学者Ｍ．Г．Ｂａлящко的干盐湖晶间卤水分异成因理论“重力垂直分异”说，并不能圆满地解释该湖晶间卤水非常复杂的分异现象。现以系统理论为指导，用数学地质方法，通过电子计算机对大量数据的处理，把全湖Ｓ３盐层晶间卤水分为８个总体，将其补给系统（一级补给系统）分为４大子系统（二级补给系统）、４０个更小的系统（三级补给系统）。在此基础上，提出了晶间卤水分异成因新观点阶段性淡化说

A NEW CONCEPT ABOUT THE MECHANISM OF DIFFERENTIATION IN THE INTERCRYSTALLINE BRINES IN MODERN PLAYAS: A HYPOTHESIS OF STAGED DESALINIZATION WITH REFERENCE TO CHAERHAN SALINE LAKE IN CHINA

How the intercrystalline brine in Chaerhan saline lake is differentiating has not yet found a reasonable explanation in the model of “gravity differentiation”, which has been accepted by most of the workers engaged in the researches on the lake. Given the fact, the present paper put forward a new viewpoint about the brine differentiation in Chaerhan, a hypothesis of stage desalinization, after the intercrystalline brine trapped in the salt layer S 3 the lake as a whole was grouped into eight populations through computer processing a great deal of data and coupling geomathematicall analysis, under direction of systematic the ory. The recharging systems of the whole lake, first order systems, were distiguished successively into four second order systems and forty order third ones.