It is well known that there are two patterns of potash deposition in lacustrine fades: " tear drop pattern " (the Dabsan saline lake is a typical example)and " bull’s eye pattern " . Potash-forming in tear drop pattern is still continuing.The 2,678 m A . S. L . lake in the middle of the Qarhan playa in the Qaidam Basin covers an area of 210 km2 , and has an average depth of 0.39 m. Its MgCh type surface brine is 280-340 g/1 in salinity and mainly consists of Na, K, Mg and Cl. As a rule, the potash deposits occur as evaporite distributed in tear drop pattern at the northern and northeastern lakeshore zones. They mostly consist of carnallite and halite, occasionally sylvite.The deposition is very unstable and controlled principally by the varying supply of deposit materials from the Golmud River in the south.The potash deposits were formed when concentration of the surface brine reached a certain degree in the main evaporating season. Their forming process followed some crystalization paths in the phase d
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机译:众所周知,湖泊中存在两种钾肥沉积:“泪滴模式”(Dabsan Saline Lake是一个典型的例子)和“牛眼图案”。在泪滴模式中形成钾肥仍在继续。2,678米A。 S. L。 Qarhan Playa中间的湖在柴达木盆地中间占地面积210平方公里,平均深度为0.39米。其MgCH型表面盐水为280-340克/ 1,主要由Na,K,Mg和Cl组成。通常,钾沉积物发生在北部和东北部湖岸区的泪滴模式中分布的蒸发岩。它们主要由碳铝酸盐和宿舍组成,偶尔斯卡维特。沉积极度不稳定,主要通过南方戈尔木河流的沉积物供应。当表面盐水浓度达到一定程度时形成钾沉积物主要的蒸发季节。它们的成形过程遵循阶段D中的一些结晶路径
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