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.
引文
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