摘要
咪霞金矿赋存在多元素高背景值下志留统薄层状蚀变板岩中,受北西向F6-1断裂及正长岩、煌斑岩控制,与多元素异常、黄铁矿化等多种围岩蚀变对应,具较好的成矿地质条件。
The Mixia Au deposit occurs in Lower Silurian thin bedded altered slate with high background value of multiple elements,which is controlled by NW fault F6-1 and syenite,lamprophyre.It is corresponding to anomaly of multiple elements and various wall rock alteration,such as pyritization,etc,which has good metallogenetic geological conditions.
引文
[1]云南省地矿局.1∶20元阳幅大鹿马幅区域地质调查报告[R].1979.
[2]云南大学数学系.地质数据变量的多元统计分析[M].昆明:云南大学出版社,1983.
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