摘要
中条山地区胡篦型铜矿床深部出现的四种特殊类型矿脉（巢），其产出地质特征表明胡篦型铜矿床中大脉状铜矿化不完全限于矿层之内，在特殊地质环境下也可形成于矿层外部。胡篦型铜矿床在热液成矿作用晚期不是一个简单的铜质迭加富集，而是经历了一个复杂的物质演变过程，且有钴组份参与了成矿，从而丰富了矿床成因的地质认识，拓宽了今后找矿思路。
There are four special kinds of ore vein which appear in deap copper deposit of Hubi type in zhongtial Mountain area. Their geological features reflect that the copper minerolization of large size of ore vein is not completely limited in the ore containing rock layers, part of which could be formed outside under special geologcal setting. The original of the deposit was not a simple copper enriched process in late hydrochermal period, owing to the element of Co taking part in the process.
出处
《矿产与地质》
1999年第6期343-347,共5页
Mineral Resources and Geology
