Experimental constraints on Pt, Pd and Au partitioning and fractionation in silicate melt-sulfide-oxide-aqueous fluid systems at 800 °C, 150 MPa and variable sulfur fugacity

We have performed experiments to constrain the effect of sulfur fugacity (fS(2)) and sulfide saturation on the fractionation and partitioning behavior of Pt, Pd and Au in a silicate melt-sulfide crystal/melt-oxide-supercritical aqueous fluid phase-Pt-Pd-Au system. Experiments were performed at 800 degrees C, 150 MPa, with oxygen fugacity (fO(2)) fixed at approximately the nickel-nickel oxide buffer (NNO). Sulfur fugacity in the experiments was varied five orders of magnitude from approximately log fS(2) = 0 to log fS(2) = -5 by using two different sulfide phase assemblages. Assemblage one consisted initially of chalcopyrite plus pyrrhotite and assemblage two was loaded with chalcopyrite plus bornite. At run conditions pyrrhotite transformed compositionally to monosulfide solid solution (mss), chalcopyrite to intermediate solid solution (iss), and in assemblage two chalcopyrite and bornite formed a sulfide melt. Run-product silicate glass (i.e., quenched silicate melt) and crystalline materials were analyzed by using both electron probe microanalysis and laser ablation inductively coupled plasma mass spectrometry. The measured concentrations of Pt, Pd and Au in quenched silicate melt in runs with log fS(2) values ranging from approximately 0.0 to -5.0 do not exhibit any apparent dependence on fS(2). The measured Pt, Pd and Au concentrations in mss do vary as a function of fS(2). The measured Pt, Pd and Au concentrations in iss do not appear dependent on fS(2). The data suggest that fS(2), working in concert with fO(2), via the determinant role that these variables play in controlling the magmatic sulfide phase assemblage and the solubility of Pt, Pd and Au as lattice bound components in magmatic sulfide phases, is a controlling factor on the budgets of Pt, Pd and Au during the evolution of magmatic systems.