摘要
本文论述了氢、氧同位素作为高岭土矿成因类型地球化学指标的意义.根据氢、氧同位素数据,我国浙闽沿海地区高岭土矿床主要可分为热液蚀变型和风化作用型两大类.其成矿溶液以大气降水为主.
This paper discusses significance of stable hydrogen and oxygen isotopic geochcmical sign for type of kaoline deposits origin. Based on data of hydrogen and exygen isotope, kaoline deposits in coastal Zhejiang and Fugian, China, can mainly be classified into two types of hydrothermal alteration and weathering. Meteoric water is main compoment in the ore-forming fluids.
出处
《火山地质与矿产》
1992年第3期63-71,共9页
Volcanology & Mineral Resources
关键词
高岭土矿床
氢
氧
同位素
成因
Koaline deposit, hydrogen and oxygen isotope, genetic type.
