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PGE mineralization in the Zhubu mafic intrusion: implications for the origin of the reef-type PGE deposits

机译:在珠博·迈克斯入侵中的PGE矿化:对珊瑚礁型PGE沉积物的起源的影响

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@@The origin of reef-type PGE deposits remains controversial (Maier, 2005). For example, the Merensky Reef of the Bushveld, there are two kinds of models to explain its formation. The first is that the PGE are mainly concentrated by primary magmatic sulfides by many researchers (Barnes and Maier, 2002; Cawthorn and Boerst, 2006; Cawthorn et al., 2002; Viljoen, 1999); the second is PGE could have been precipitated from late magmatic or hydrothermal fluid (Boudreau, 2008; Boudreau and Meurer, 1999; Willmore et al., 2000). The first model is also called "top-loaded", it has no explanations about the role played by the volatiles in the ore formations (Boudreau, 2008); the second is also called "bottom-loaded". However, this model is not consistent with the observations that there is no evidence of PGE depletion below the reefs whereas the rocks above the reefs tend to be highly depleted in PGE (Barnes and Maier, 1999). Therefore, new model is needed to explain all the controversies.
机译:@@的珊瑚礁型PGE存款的起源仍然存在争议(Maier,2005)。例如,BUSHVELD的Merensky Reef,有两种模型来解释其形成。首先是PGE主要由许多研究人员(Barnes和Maier,2002; Cawthorn和Boest,2006; Cawthorn等,2002; Viljoen,1999)的主要魔法硫化物主要集中。第二个是PGE可以从晚期岩岩或水热流体(Boudreau,2008; Boudreau和Meurer,1999; Willmore等,2000)中沉淀出来。第一个模型也被称为“最大加载”,它没有关于矿石在矿石中挥发物(Boudreau,2008)所扮演的角色的解释;第二个也被称为“底部加载”。然而,该模型与礁石下方没有PGE耗尽的观察结果,而珊瑚礁上方的岩石倾向于在PGE(Barnes和Maier,1999)中高度耗尽。因此,需要新模型来解释所有争议。

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