论文部分内容阅读
柴达木盆地蕴藏着极为丰富的盐类资源。据钻井资料表明,盐湖形成演化过程中可以分为未成盐和成盐两个阶段。成盐阶段中具盐类沉积和碎屑沉积交替成层或混层的特征,构成许多盐类和碎屑沉积物相间的沉积韵律。粘土矿物的形成和稳定,除了基本的金属离子外,还与一定的环境相联系。通过对粘土的某些研究,认识盐湖沉积物中粘土矿物的某些特征,讨论粘土矿物在盐湖形成演化过程中的变化是有意义的。本文通过盆地内10个湖区64个样品的资料来进行讨论。所有样品均系我室历年来进行盐湖考察时
The Qaidam Basin contains extremely rich salt resources. According to drilling data shows that the formation and evolution of the Salt Lake can be divided into two stages of salt and salt into salt. Salt-forming stages are characterized by alternate layers or layers of salt deposits and detrital deposits, which constitute the depositional rhythm of many salt and clastic sediments. The formation and stability of clay minerals, in addition to the basic metal ions, but also with a certain environment. Through some research on clay and understanding some characteristics of clay minerals in salt lake sediments, it is meaningful to discuss the changes of clay minerals in the formation and evolution of salt lake. This article discusses the data from 64 samples of 10 lakes in the basin. All samples are from my room over the years when Salt Lake investigation