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机构地区:[1]云南省有色地质勘查院滇南院,个旧661400 [2]云南省有色地质勘查局,昆明650051
出 处:《地质与勘探》2004年第5期33-38,共6页Geology and Exploration
基 金:中国地质调查局项目(编号:200010200112)资助。
摘 要:云南金平龙脖河铜矿区,除铜外还伴有金、铁矿化,东矿带目前累计估算铜资源量已达100万t,具有矿床埋藏较浅、规模大、品位高、矿石质量好、交通便利、容易开采的特点,矿床受地层岩性、构造、海相中基性火山岩等因素控制特征明显,属海相火山块状硫化物型铜矿床,是云南三江南段找矿有较大突破的区带。Besides copper, there are gold and iron mineralizations in the Longbohe copper deposit, Yunnan provinces. It is estimated that total Cu recourse can reach one million ton in the east belt. The ores have characters of shallow buried, large scale, high quality, transport facility, and easy mining. The deposit is obviously controlled by strata lithology, structure, and marine intermediate-basic volcanic rocks, and belong to submarine volcanic-hosted massive sulfide copper deposit. The discovery of the deposit is a big breakthrough in the southern Sanjiang area of Yunnan province.
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