摘要
鹅头厂含铜铁矿床对位于康滇地轴中部 ,矿体受地层、岩性、构造、火山岩和次火山岩控制。分为三个矿群。矿石的矿物组成简单。矿石以富铁、含铜、高硫、高磷为特点。成矿地球化学研究显示出热水成矿特点 ,属火山热水沉积—次火山热液改造成因。
The Etouchang copper bearing iron ore deposit locates in the middle part of the Kangdiang axial and is controlled by strata, lithology, structure, volcanic rocks and sub-volcanic rocks. The deposit can be divided into three ore body's groups. The ores contain high iron, sulfur and phosphorus and copper. Metallogenic geochemistry researching results shows a hot water mineralization and the volcanic thermal water sedimentary and sub-volcanic thermal water reformation genesis. The north part of the mine is prospect for searching ores in tongchangqin.
出处
《矿产与地质》
2004年第6期537-540,共4页
Mineral Resources and Geology
基金
云南省国土资源厅"云南省国有矿山资源接替"
云南省改革与发展委员会"云南省有色金属资源接替"项目资助
关键词
含铜铁矿床
找矿前景
地质特征
成因
Copper bearing iron ore deposit, ore mineralogy, Genesis, Searching prospect