Laboratory partitioning of platinum-group elements (PGE) and gold with application to magmatic sulfide-PGE deposits

被引:171
作者
Fleet, ME [1 ]
Crocket, JH
Liu, MH
Stone, WE
机构
[1] Univ Western Ontario, Dept Earth Sci, London, ON N6A 5B7, Canada
[2] McMaster Univ, Sch Geog & Geol, Hamilton, ON L8S 4M1, Canada
[3] WMC Resources, Kambalda, WA 6442, Australia
基金
加拿大自然科学与工程研究理事会;
关键词
platinum-group element; gold; magmatic sulfide;
D O I
10.1016/S0024-4937(99)00011-0
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Apparent diversity in laboratory partitioning of platinum-group elements (PGE)-Au between (Fe,Ni)-sulfide liquid and S-saturated basaltic melt is resolved by recognizing the marked control exerted by variation in metal/S ratio of the sulfide liquid. Partition coefficients (D) increase markedly for Os, Ir and Pd and somewhat for Pt with increase in S content. In addition, the partitioning is markedly dependent on concentration of PGE-Au in the sulfide fraction, for all precious metals in metal-rich sulfide, and for Ru, Pt and Pd in relatively S-rich sulfide. Reversal of partitioning of PGE-Au is presently demonstrated for experiments with metal-rich sulfide liquids. Erratic partitioning behaviour, with anomalously high D(PGE-Au) values, is minimised by degassing starting materials. Summary D(PGE-Au) values for metal-rich sulfide liquids and near-natural PGE-Au abundances are: Os(2.2), Ir(1.8), Ru(2.4), Pt(1.4), Pd(2.9), Au(0.9)(X 10(3)) for the CCO oxygen buffer and molar Ni/(Fe + Ni) = 0.02, and Os(3.7), Ir(3.2), Ru(4.4), Pt(4.6), Pd(5.0), Au(3.0) (X 10(3)) for the IQF buffer and Ni/(Fe + Ni)= 0.12. Thus, PGE-Au would not be extensively fractionated for equilibrium between sulfide and deep mantle melts. For more S-rich sulfide liquids (WM oxygen buffer) and 100-1000 ppm in the sulfide, D(PGE-Au) values are: Os(30), Ir(26), Ru(6.4), Pt(10), Pd(17) (X 10(3)) at Ni/(Fe + Ni)= 0.36, and Os(10), Ir(51), Ru(3.5), Pt(13), Pd(25), Au (1.2) (X 10(3)) at Ni/(Fe + Ni) = 0.66. The laboratory partitioning is notably differential within the PGE-Au group, with relatively high Ds for Ir and Pd and low Ds for Ru and Au. Although separation of an early-magmatic sulfide liquid would result in significant concentration of some PGE (e.g., Ir and Pd), sulfide liquid immiscibility alone would not account for the high abundance of PGE-Au in the reef deposits of the Bushveld and Stillwater Complexes. (C) 1999 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:127 / 142
页数:16
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