摘要
本文通过对铜陵地区含硫化物矿床氧化带地质特征,氧化带中金(银)的活化迁移、沉淀富集、成矿机制的研究,为在长江中下游及我国南方地区寻找铁帽型金(银)矿床,指明了方向,并对评价原生矿床提供了依据。
This paper studies the characteristics of the oxidation zone in the gold-bearing sulfide de- posit in the Tongling area, which include the mobilization migration, precipitation enrichment, metal- logenetic mechanism and ore-prospecting in the discovery of iron cap type gold (silver) deposit and the evaluation of primary deposit in South China.
出处
《安徽地质》
1992年第3期28-36,共9页
Geology of Anhui
基金
国家自然科学基金
关键词
含金硫化物矿床
氧化带
赋存状态
活化迁移
沉淀富集
找矿方向
gold-bearing sulfide deposit
oxidation zone
state of occurrence
mobilization migration
precipitation enrichment
orientation of ore prospecting.
