Abstract:Extraction of sulfides from the partially molten mantle is vital to
elucidate the cycling of metal and sulfur elements between different
geochemical circles but has not been investigated systematically. Using
laboratory experiments and theoretical calculations, this study
documents systematical variations in lithologies and compositions of
silicate minerals and melts, which are approximately consistent with the
results of the thermodynamically-constrained model. During a
melt-peridotite reaction, the dissoluti… Show more
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