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.
出处
《矿物学报》
CAS
CSCD
北大核心
1992年第4期372-379,T001,共9页
Acta Mineralogica Sinica
关键词
高岭石
长石
成因
kaolinite
feldspar
residual layer collection
dynamic transformation
Kuangdong
