摘要
本文通过对阿希金矿近矿蚀变岩的详细研究,探讨该矿床主要的蚀变类型以及蚀变与矿化的时空关系;并根据多种分析资料查明本区蚀变类型中存在伊利石化,为确定成矿深度、温度及矿床成因类型提供了重要依据。
Through a detailed study of altered rocks near orebody in the Axi glod ore deposits, this paper investigates the major alteration type and the time-space relationship between alteration and mineralization. Also,the existence of illitization(clayization)in the ore area is first presented according to several kinds of analytic data,which provides important evidence for the determination of ore-forming depth, temperature and genetic type of this ore deposits.
出处
《矿物岩石》
CAS
CSCD
1993年第4期57-67,共11页
Mineralogy and Petrology
关键词
金矿床
蚀变岩
伊利石
类型
Axi gold ore deposits
alteration type
alteration zone
illite
