摘要
本文通过对多处以火山碎屑岩或沉积岩为容矿岩石的块状硫化物型矿床上方岩矿石样品中铅同位素组成特征的研究，总结了不同成因类型矿床铅同位素组成模式及与成矿元素异常之间的关系，指出对于系统采集的岩矿石样品，铅同位素组成能较好的反映成矿环境和成矿作用，对异常起到定性评价作用。
The study of lead isotope features and minor element components of known massive sulfide deposits shows that the isotope model and systematic rock & ore samples can reflect the mineralization evironments and metallogenic process, and can be used to qualitatively assess the geochemical anomaly.
出处
《矿产勘查》
1994年第6期349-354,共6页
Mineral Exploration
