摘要
本文主要通过对抚松大营铅锌矿床同位素特征的研究,讨论了成矿物质来源、成矿流体性质、岩浆活动对成矿作用的影响,从而证明矿床成因属沉积—热液叠加型层控矿床。
This paper principally describes the sources of ore—forming materials, the properties of sulfur origin and ore—forming fluid, and effects of magmatism on mineralization through the investigation of the features of isotopes in the deposit, indicating that the origin of the deposit is a sedimentary hydrothermal superimposed-stratabound ore deposit.
出处
《吉林地质》
1990年第3期27-33,共7页
Jilin Geology
