摘要
云南金顶铅锌矿床是我国超大型铅锌矿床,矿床的形成是多因素相互作用的结果。依据矿床地球化学特征、铅同位素特征等,以成矿溶液的形成为研究对象,探讨了矿床成矿物质来源,在结合矿区构造特征,对矿液的运移模式进行了研究,并总结出了早、中、晚三期矿液运移特征。
The Jinding Pb-Zn deposit is a superlarge Pb-Zn deposit in China. It resulted from interaction of multiple factors. The present paper makes an approach to its ore material source, ore fluids migration patterns and ore genesis based on geochemical and Pb isotopic composition and our fluids.
出处
《四川地质学报》
2016年第3期414-417,共4页
Acta Geologica Sichuan
关键词
铅锌矿
成矿物质
运移模式
金顶
Pb-Zn deposit
ore material source
ore fluid
migration pattern
Jinding
