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Experimental Measurement of PGE and Semi-metal Partitioning during Sulfide Melt Crystallization at Controlled fO2-fS2 Conditions

机译:fO2-fS2受控条件下硫化物熔体结晶过程中PGE和半金属分配的实验测量

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摘要

In order to better understand the behaviour of platinum-group elements (PGE) and semi-metals (SM;As,Se,Sb,Te and Bi) during the solidification of sulfide magmas,we have conducted a series of partitioning experiments between monosulfide solid solution (MSS) and sulfide melt,as well as MSS and intermediate solid solution (ISS),at fO2-fS2 close to natural conditions.We found that Re,Os,Ir,Ru and Rh are compatible in MSS,relative to sulfide melt,whereas Au,Ag,Pd,as well as the SM,are incompatible.MSS/ISS partitioning experiments reveal that Ru,Os,Ir,Rh and Re are partitioned into MSS by factors >50,whereas Pd,Pt,Ag,Au and the semi-metals partition weakly (Se,Te) to strongly (Ag,Au) into ISS.Calculated ISS/melt partition coefficients of Se and Te are close to unity while the other elements partition preferentially into the melt phase.Uniformly low MSS- and ISS-melt partition coefficients for the SM,Pt,Pd,Ag and Au will lead to enrichment of these elements in the residual sulfide liquid,possibly leading to saturation in SM-bearing accessory minerals or immiscible melts.
机译:为了更好地了解硫化岩浆凝固过程中铂族元素(PGE)和半金属(SM; As,Se,Sb,Te和Bi)的行为,我们进行了一系列单硫化物固体之间的分配实验fO2-fS2时,接近自然条件的溶液(MSS)和硫化物熔体,以及MSS和中间固溶体(ISS)。我们发现,相对于硫化物熔体,Re,Os,Ir,Ru和Rh在MSS中相容MSS / ISS分区实验表明,Ru,Os,Ir,Rh和Re被> 50的因素分配到MSS中,而Pd,Pt,Ag,Au则被分解为MSS。半金属(Se,Te)从弱(Se,Te)到强(Ag,Au)进入ISS。计算得出的ISS / Se和Te的熔体分配系数接近于1,而其他元素优先分配到熔融相。 -和ISS-SM,Pt,Pd,Ag和Au的熔体分配系数将导致这些元素在残留硫化物液体中的富集可能导致含SM的辅助矿物或不溶混的熔体饱和。

著录项

  • 来源
  • 会议地点 Guiyang(CN)
  • 作者

    Ya-Nan Liu; James Brenan;

  • 作者单位

    University of Toronto,Geology Department;

    University of Toronto,Geology Department;

  • 会议组织
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 P578.24;
  • 关键词

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