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以江西武山铜矿为例,研究了硫化物矿石在氧化过程中稀土元素的地球化学行为. 硫化物在氧化成为铁帽的过程中,稀土元素的迁移能力不强,大部分停留在硫化物矿石的氧化残余物中. 在这个过程中,稀土元素的模式发生了系统的改变: 铁帽的轻重稀土比值低于原生硫化物矿石的轻重稀土比值;铁帽中出现了Ce的负异常. 硫化物矿石在氧化成为铁帽的过程中,Eu异常基本没有发生改变.

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