摘要
研究了山西省兴县铝土岩中的主要元素和微士元素的富集规律及与下伏基岩的关系，认为该铝土岩是由下伏碳酸盐岩和页岩风化而形成的。
The abundances of major and trace elements in bauxite and their relations with the underlyingbasement rocks are studied in this paper. It is concluded that the bauxite was formed as a result of weathering of underying carbonate rocks and shales.
出处
《地质地球化学》
CSCD
北大核心
1997年第2期41-44,共4页
Geology-Geochemistry
