Platinum-group element geochemistry of the Panjal Traps: constraints on mantle melting and implications for mineral exploration
AbstractForty-two volcanic rocks of the Panjal Traps were analyzed for platinum-group elements (PGE) to investigate magma genesis, high-temperature behaviour, and exploration potential of these elements. The PGE data exhibit substantial variability and show no systematic relation to their low-Ti or high-Ti affinity. Instead, the basalts can be subdivided into PGE-undepleted (group 1) that has ∑PGE > 10 ppb and Cu/Pd < 30000, and PGE-depleted, that consists of a subgroup showing limited (group 2A) or substantial depletion in IPGE relative to Ni (group 2B). The group 1 samples indicate a S-undersaturated history whereas the group 2 samples might have different origins in terms of S-saturation. Fractionation of a tiny amount of sulfide melts (0.075 to 0.1%) from a representative group 1 sample accounts for the chalcophile element patterns observed in the group 2B samples. The relatively high Cu/Pd, unfractionated Ni/Ir, and low PGE abundances observed in the group 2A samples cannot be explained by equilibration of an immiscible sulfide melt alone, and probably requires decomposition of residual sulfides into sulfide melt and a mss in the mantle restite. Our results question the notion that the coexistence of PGE-undepleted and PGE-depleted magmas are prospective in the exploration of magmatic Ni-Cu-(PGE) sulfide mineralization.