Petrogenesis of the ~ 3.4 Ga IOG and 2.25 Ga Malangtoli lavas of Singhbhum Craton
Relative PGE abundances attributed to sulphide and chromite fractionation
Variable mantle melting and crustal contamination controlled sulphide saturation.
Intraoceanic arc and transitional arc to rift controlled back-arc in a marginal basin.