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Major, trace and platinum group element (PGE) geochemistry of Archean Iron Ore Group and Proterozoic Malangtoli metavolcanic rocks of Singhbhum Craton, Eastern India: Inferences on mantle melting and sulphur saturation history
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文摘

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.

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