Journal ArticleDOI
The platinum-group chemistry and mineralogy of the UG-2 chromitite layer of the Bushveld Complex
TLDR
In this paper, the average noble metal content of the UG-2 chromitite layer is about 7 ppm; Pt is most abundant, followed by Pd, Ru, Rh, Ir, and Au, in that order.Abstract:
Individual platinum-group elements, as well as Au, Cu, and Ni, were determined in borehole cores of the UG-2 chromitite layer from different localities in the Bushveld Complex. The average noble metal content of the layer is about 7 ppm; Pt is most abundant, followed by Pd, Ru, Rh, Ir, and Au, in that order. Noble metal contents, recalculated to concentration in 100 percent sulfide, are extremely high, which raises questions regarding the distribution coefficients of noble metals in sulfide and silicate melts, and the initial concentrations of the platinum-group elements in Bushveld magmas.More than 6,000 grains of platinum-group minerals were identified qualitatively in polished sections of the ore, the most abundant species being laurite (RuS 2 ), cooperite (PtS), an unnamed Pt-Ir-Rh-Cu sulfide, braggite ([Pt, Pd, Ni]S), an unnamed Pt-Pb-Cu sulfide, vysotskite (PdS), gold, and electrum (Au, Ag) as well as intermetalloids such as Pt-Fe, Pd-Cu, Pd-Pb, and Pd-Hg. Associated base metal sulfides are mainly pentlandite, chalcopyrite, pyrrhotite, and pyrite. Variation in the platinum-group mineral assemblages can be explained by variations in the fugacity of sulfur between the various localities studied.Compositions of chromite grains show an increase of Fe (super +2) , Fe (super +3) , and Cr upward. Variations in Fe (super +3) /(Fe (super +2) + Fe (super +3) ) (laterally and vertically) may reflect variations in the prevailing fugacity of oxygen.read more
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Journal ArticleDOI
The origin of the fractionation of platinum-group elements in terrestrial magmas
TL;DR: The platinum-group elements (PGE's) when chondrite normalized, have been found to be fractionated in order of descending melting point (Os, Ir, Ru, Rh, Pt, Pd and Au) as mentioned in this paper.
Journal ArticleDOI
Ir, Ru, Pt, and Pd in basalts and komatiites: new constraints for the geochemical behavior of the platinum-group elements in the mantle
Mark Rehkämper,Mark Rehkämper,Alex N. Halliday,Alex N. Halliday,J. G. Fitton,Der-Chuen Lee,M. Wieneke,Nicholas Arndt +7 more
TL;DR: In this paper, the concentrations of the platinum-group elements (PGE) Ir, Ru, Pt, and Pd were determined in 18 mantle-derived basalts from a variety of tectonic settings and six komatiites from three locations.
Book ChapterDOI
The Use of Mantle Normalization and Metal Ratios in Discriminating between the Effects of Partial Melting, Crystal Fractionation and Sulphide Segregation on Platinum-Group Elements, Gold, Nickel and Copper: Examples from Norway
Sarah-Jane Barnes,Rognvald Boyd,A. Korneliussen,L.P. Nilsson,Morten Often,Rolf-Birger Pedersen,B. Robins +6 more
TL;DR: In this paper, the relative importance of the influence of sulphides, chromite, olivine and PGM on the distribution of noble metals, Ni and Cu in mafic and ultramafic rocks is examined.
Journal ArticleDOI
Origin of the UG2 chromitite layer, Bushveld Complex
Sisir K. Mondal,E. A. Mathez +1 more
TL;DR: In this paper, a detailed study of the silicate-rich layers immediately above and below the UG2 chromitite and another chromite layer lower in the stratigraphic section, at the top of the Lower Critical Zone, was conducted.
Journal ArticleDOI
Experimentally determined sulfide melt-silicate melt partition coefficients for iridium and palladium
TL;DR: In this article, the sulfide melt-silicate melt partition coefficients for Ir and Pd have been determined from experiments run in a piston-cylinder apparatus at 1450°C, 8 kbar and under ƒ O 2 ǫ S 2 conditions appropriate for mafic magmas.