肖凡;王敏芳;姜楚灵;杨武胜;

• 1:中国地质大学资源学院
• 2:中国地质大学地质过程与矿产资源国家重点实验室
• 3:长沙矿冶研究院有限责任公司

摘要(Abstract)：

香山含铜镍矿岩体位于东天山北部的土墩-图拉尔根镁铁-超镁铁岩带中段,受康古尔塔格-黄山深大断裂控制,为由辉长岩、辉橄岩、细粒辉长岩和钛铁辉长岩组成的复式岩体。香山铜镍矿床岩石铂族元素总量(∑PGE)变化范围为0.74×10-9～2.82×10-9,矿石∑PGE变化范围为20.64×10-9～148.99×10-9,PPGE(Pd、Pt)和IPGE(Ru、Ir、Os)之间分异均较弱,二者具有相似PGE原始地幔标准化配分曲线形式。香山铜镍矿床原生岩浆w(MgO)下限值为4.97%,源于亏损型地幔,PGE丰度较高,母岩浆为高镁玄武质岩浆,PGE处于亏损状态且亏损的原因是发生了硫化物熔体不混溶作用,引发硫饱和的机制为地壳物质同化混染作用,以及橄榄石、辉石和基性斜长石等矿物的结晶分离作用。

关键词(KeyWords)： 香山;铜镍矿床;PGE;硫化物熔离作用

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金面上项目(41272097),国家自然科学基金青年科学基金(40902026);; 中国地质调查局计划项目(1212011085466);; 地质过程与矿产资源国家重点实验室开放课题(GPMR201006);; 中央高校基本科研业务费专项资金(CUG120702)

作者(Author): 肖凡;王敏芳;姜楚灵;杨武胜;

Email:

DOI:

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