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Chromite and Platinum-group Elements Coprecipitation by Crustal Contamination or Magma Mixing Revisited - Genetic and Exploration Implications

机译:铬铁矿和铂族群元素通过地壳污染或岩浆混合重新审查 - 遗传和勘探影响

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Traditional models employed to genetically link associated chromite and platinum-group elements have favoured crustal contamination as the primary process for inducing sulfide and oxide saturation. The association of chromite ores with crustal contamination is well established in the literature. However, in the 1970s (cf Irvine, 1973,1975), Irvine demonstrated that crustal contamination was in fact problematic as a tool for inducing chromite precipitation in mafic to ultramafic magmas. His results are re-examined here, along with some attempts to reconcile them with the effects of adding Fe to the models. It is concluded that crustal contamination is indeed problematic based on phase relationships alone. However, the role of fluids as a compensating agent is evaluated, which may explain why crustal contamination may indeed facilitate oxide and sulfide precipitation.
机译:用于基因链接相关铬铁矿和铂族组分的传统模型使地壳污染成为诱导硫化物和氧化物饱和的主要方法。铬铁矿矿石与地壳污染的结合在文献中得到了很好的成熟。然而,在20世纪70年代(CF Irvine,1973,1975)中,Irvine证明了地壳污染实际上是一种诱导乳头沉淀到超微岩浆岩浆中的铬铁矿沉淀的工具。他的结果在这里重新检查,以及一些尝试将它们与模型添加FE的效果调和它们。结论是基于单独的相位关系,地壳污染确实有问题。然而,评估流体作为补偿剂的作用,这可以解释为什么地壳污染确实有促进氧化物和硫化物沉淀。

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    《PACRIM Congress》|2015年||共6页
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    S A Prevec;

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