摘要
对于大冶铁矿内接触带钠化蚀变的岩石特征、钠质来源、动力机制、形成机理等作了比较系统的阐述。
This paper systematically expounds rock characteristics, ore-forming process, natrium origin and natrium alteration mechanism in contacting zones of Daye iron deposit. The relation of natriumlization, potassiumlization and skarnize is very close. It is emphasized that natriumlization is one of the important directive signs of iron mineralization.
出处
《地质与勘探》
CAS
CSCD
北大核心
2001年第6期20-24,共5页
Geology and Exploration
关键词
湖北
热液交代蚀变
三叠系
膏盐层
铁矿床
形成机理
钠化蚀变
动力机制
Hubei province, Daye iron deposit, natriumlization, hydrothermal metasomatic alteration, Triassic strata containing gypsum
