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This study investigates the behavior of platinum-group elements (PGEs) and gold during magmatic differentiation in Hawaiian tholeiites. The research finds that PGE and Au concentrations remain relatively constant in these basalts, contrasting with the strong fractionation observed in mid-ocean ridge basalts (MORBs). The authors suggest that oversaturation of sulfur and the separation of sulfides from magmas are necessary to explain the observed concentrations of PGEs and Au in Hawaiian tholeiites.

Author

no2owl977

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EN