关于长石→高岭石动态形成过程的讨论  

A DISCUSSION ON THE DYNAMIC PROCESS OF KAOLINIZATION OF FELDSPAR

作　　者：张实[1] 张惠芬[1] 

机构地区：[1]中国科学院地球化学研究所,广州510640

出　　处：《矿物学报》1992年第4期372-379,T001,共9页Acta Mineralogica Sinica

摘　　要：在对广东几个地区高岭土、高岭石研究的基础上,从结构的观点出发,详细分析讨论了风化过程中长石→高岭石转变的动力学机制,建立了高岭石形成的长石结构动态转化模型,并以此解释了高岭土矿床以及高岭石的某些特征和现象。On the basis of the study of kaolin and kaolinite from several locations of Guangdong Province, a detailed discussion has been made of the dynamic mechanism of feldspar→kaolinite transformation. A model of 'dynamic transformation of feldspar structure' is presented to describe the process of kaolinization, and to characterize the kaolin and kaolinite.

关 键 词：高岭石 长石 成因 

分 类 号：P578.964[天文地球—矿物学]