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What is Thermodynamic Model of Mantle Melts about?
This study tests a thermodynamic melting model on various mantle compositions to understand the major element signatures of mantle melts, particularly focusing on pyroxenite melting. The model effectively reproduces experimental melt compositions and suggests that ferropicrites, high-FeO primitive melts, originate from partial melting of silica-deficient pyroxenite at elevated mantle temperatures. The findings indicate that lithological heterogeneity, possibly from recycled oceanic crust, is present in cont
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- a1982919845
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- EN