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Sulfide is a ubiquitous phase in the mantle (Alard et al., 2011) and an important repository for sulfur and geochemically and economically important chalcophile metals, which plays a pivotal role in the partitioning behaviors of PGE, Cu, and Ni (Mungall & Brenan, 2014;Patten et al., 2013). Understanding the factors that control the fate of sulfide phases in the partially molten mantle is of fundamental importance in exploring the recycling of sulfur and chalcophile elements among different geochemical reservoirs (

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