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The fate of sulfide during decompression melting of peridotite - implications for sulfur inventory of the MORB-source depleted upper mantle
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We modeled the fate of S and Cu during decompression melting of peridotite. Hotter mantle produces higher FeO⁎FeO⁎ partial melts and consumes sulfide faster. Primitive MORBs are likely mixture of sulfide-undersaturated and -saturated melts. 100–200 ppm S in the mantle source can satisfy both S and Cu of primitive MORBs.

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