An experimental study at one atmospheric pressure was carried out with basalts of the Deccan Traps and black shale as a contaminant to assess the potentiality of the platinum group elements (PGEs) in the contaminated magma. The experiments involved 10%, 15% and 20% black shale as contaminants to understand the incremental concentration in the PGEs. The results show that Pd, Pt, Ru, Rh, Ir and Os substantially rise in the contaminated melt. Though the quantitative increase in the PGE content owing to contamination is evident, the increase is case-specific and related to the degree of black shale contamination, e.g. for Pt, Ru and Pd, 20% contamination yields maximum enrichment, whereas, for Rh and Ir, the maximum increment is obtained for 10% contamination; Os gives most significant increase for 15% contamination. Black shale contaminationleads to the sulfide supersaturation of the basaltic magma and the formation of the PGE-rich sulfide liquid due to immiscibility. The present experimental study revealed a significant role of black shale as a crustal contaminant for the flood basalt and consequent PGE enrichment in the contaminated magma. The findings of this study are important for the other Large Igneous Provinces of the world as well.
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