首页> 外文期刊>Economic geology and the bulletin of the Society of Economic Geologists >Segregation and Fractionation of Magmatic Ni-Cu-PGE Sulfides in the Western Jinchuan Intrusion, Northwestern China: Insights from Platinum Group Element Geochemistry
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Segregation and Fractionation of Magmatic Ni-Cu-PGE Sulfides in the Western Jinchuan Intrusion, Northwestern China: Insights from Platinum Group Element Geochemistry

机译:西北金川侵入岩中岩浆状Ni-Cu-PGE硫化物的分离与分馏:铂族元素地球化学的启示

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The Jinchuan Ni-Cu-(PGE) deposit is one of the world's largest magmatic sulfide deposits. Recent studies have suggested that the Jinchuan intrusion originally comprised two individual intrusions, the Eastern and the Western intrusions. The Western intrusion consists of an Upper and a Lower unit. The Upper unit is largely free of sulfides with wealdy disseminated sulfides only at the base of the unit; these sulfides are characterized by moderate Cu/Pd ratios of 5,500 to 14,900 and relatively high PGE tenors (PGE in 100% sulfides) in the range of 510 to 1,000 ppb Ir_(sul), 420 to 1,200 ppb Ru_(sul), and 2,900 to 8,000 ppb Pd_(sul). Disseminated, net-textured and minor massive sulfides in the Lower unit comprise the No. 24 orebody, the third largest at Jinchuan. The disseminated ores have remarkably high Cu/Pd ratios (24,200-85,600) and low PGE tenors in the range of 120 to 560 ppb Ir_(sul), 100 to 480 ppb Ru_(sul), and 430 to 3,600 ppb Pd_(sul). The net-textured and massive ores contain high IPGE contents (240-820 ppb Ir_(sul) and 170-630 ppb Ru_(sul)) and Ni/Cu ratios (1.7-11.3), low Pd/Ru ratios (0.53-3.1), and exhibit significant Pt depletion (<300 ppb Pt_(sul)). Additionally, small Cu-rich orebodies occur at the base of the No. 24 orebody or in small intrusions within footwall schists, marbles, and granites beneath the Western intrusion. The Cu-rich sulfides have very low IPGE tenors (1.9-16 ppb Ir_(sul) and 6.4-21 ppb Ru_(sul)), and Ni/Cu ratios (0.3-2.8), high Pd/Ru ratios (37.3-378), and highly variable Pt_(sul) between 43 and 11,000 ppb. The PGE geochemistry and model calculations indicate that the disseminated sulfides of the Upper and Lower units segregated from PGE-undepleted and -depleted parental magmas, respectively. The PGE-depleted magma had undergone a minor amount of earlier sulfide liquid extraction at depth. Furthermore, this PGE-depleted parental magma had slightly higher PGE contents than the magma from which the sulfides of the Nos. 1 and 2 orebodies in the Eastern intrusion segregated. The significant variations in base and precious metal ratios of the net-textured and massive sulfide ores are attributed to fractionation of the sulfide melts that formed these ores. This led to both migration of the residual Cu-rich sulfide melts away from the early-formed monosulfide solid solution (mss) to form Cu-rich ores as well as back intrusion of the Cu-rich ores into the mss. The negative Pt anomalies of the net-textured and massive sulfides resulted from preferential extraction of Pt into the Cu-rich residual melts due to the presence of As, Te, and Bi.
机译:金川镍铜(PGE)矿床是世界上最大的岩浆硫化物矿床之一。最近的研究表明,金川入侵最初包括两个单独的入侵,即东方入侵和西方入侵。西方入侵包括一个上层单元和一个下层单元。上部单元基本上不含硫化物,仅在单元的底部富散布了硫化物。这些硫化物的特征是中等的Cu / Pd比为5,500至14,900,并且具有较高的PGE期限(PGE在100%硫化物中),范围为510至1,000 ppb Ir_(sul),420至1,200 ppb Ru_(sul)和2,900至8,000 ppb Pd_(sul)。下层单元中散布的,网状的和少量的块状硫化物构成金矿第三大的24号矿体。散布的矿石具有很高的Cu / Pd比(24,200-85,600)和低的PGE色标,范围在120至560 ppb Ir_(sul),100至480 ppb Ru_(sul)和430至3,600 ppb Pd_(sul)范围内。网状和块状矿石包含​​高IPGE含量(240-820 ppb Ir_(sul)和170-630 ppb Ru_(sul))和Ni / Cu比(1.7-11.3),低Pd / Ru比(0.53-3.1) ),并表现出显着的Pt损耗(<300 ppb Pt_(sul))。此外,富含铜的小型矿体出现在24号矿体的底部或西部侵入体下的底盘片岩,大理石和花岗岩中的小型侵入体中。富含铜的硫化物具有非常低的IPGE强度(1.9-16 ppb Ir_(sul)和6.4-21 ppb Ru_(sul)),Ni / Cu比(0.3-2.8),高Pd / Ru比(37.3-378) ),并且Pt_(sul)在43到11,000 ppb之间变化很大。 PGE地球化学和模型计算表明,上部和下部单元的散布硫化物分别与PGE未缺失和耗尽的母岩浆分离。 PGE贫化的岩浆在深度处经历了少量的早期硫化物液体萃取。此外,这种贫化了PGE的母岩浆的PGE含量比东部侵入岩中1号和2号矿体的硫化物分离出的岩浆略高。净织构和块状硫化矿石的贱金属和贵金属比的显着变化归因于形成这些矿石的硫化物熔体的分馏。这不仅导致残留的富铜硫化物熔体从早期形成的一硫化物固溶体(mss)迁移而形成富铜矿石,而且导致富铜矿石向后侵入mss。由于存在As,Te和Bi,Pt优先提取到富Cu残留熔体中,导致网状硫化物和块状硫化物的Pt负异常。

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