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秘鲁Cerro Fierro铁铜矿地质特征及成因分析

Geological Characteristics and Ore-controlling Factors of Cerro Fierro Iron-Copper deposit in Peru
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摘要 Cerro Fierro铁铜矿位于秘鲁中上侏罗统海岸基岩I-O-C-G成矿带上,矿体总体赋存于闪长岩类的断裂构造带中,矿床成因为热液充填型矿床,属于铁氧化物-铜-金(IOCG)型矿床系统的一个组成部分。 Cerro Fierro iron-copper deposit is located in the Upper-Middle Jurassic I-O-C-G coastal belt in Peru.Ore bodies generally occur in the fault structural zone of diorite.The genesis of the deposit is hydrothermal filling deposit,which is a part of the iron oxide-copper-gold(IOCG)deposit system.
作者 金文强 JIN Wen-qiang(Tianjin North China Geological Exploration Bureau,Tianjin 300170,China)
机构地区 天津华北地质勘查局
出处 《世界有色金属》 2019年第8期97-98,共2页 World Nonferrous Metals
关键词 地质特征 控矿因素 矿床成因 铁铜矿 秘鲁 Geological characteristics Ore-controlling factors Genesis of ore deposits Iron copper deposit Peru
分类号 P618.41 [天文地球—矿床学]
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世界有色金属
2019年 第8期

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