摘要
龙脖河铜矿区东矿带铜矿资源量已达大型规模,其含矿母岩为一套深海相变钠质(含铜)基性火山岩,岩石学、岩石化学特征与大红山铜矿区火山岩相似,成矿地质环境相同,推测其深部可能还赋存有大型块状硫化物型铜铁矿床,是较具找矿潜力的地区。
The scale of the known copper ore reserve in east ore zone of Longbohe copper ore field has already been a large one. Its ore bearing host rock is a series of deepsea phase metasodic (copper bearing) basic volcanic rocks. The lithological and rock chemical characteristics are similar to that of the volcanic rocks in Dahongshan copper ore field and the metallogenic environment is alike. Therefore it is suggested that there are large scale of massive sulfide copper and iron deposits in deep part with a great exploration potential.
出处
《矿产与地质》
2003年第4期526-529,共4页
Mineral Resources and Geology
