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- W2350486575 abstract "The harzburgites from Huinan are not residues of partial melting of large degree in the mantle, because they have anomalously high HREE abundance and peculiar secondarily recrystallized texture, when compared to the normal residual harzburgites. Instead, they likely resulted from melt-mantle reaction through clinopyroxene dissolution and olivine precipitation. The convex-upward REE pattern suggests that these samples were in equilibrium with melts with basaltic composition at high melt/rock ratio. The presence of melts/fluids enhanced the grain growth in peridotites, giving rise to the formation of secondarily recrystallized texture, typical of the Huinan harzburgites. The formation of the Huinan harzburgites was probably related to thermo-chemical erosion of the lithosphere mantle by upwelling asthenosphere. These reactive harzburgites were further affected by metasomatism involving carbonate or volatile-rich small volume silicate melts." @default.
- W2350486575 created "2016-06-24" @default.
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- W2350486575 date "2003-01-01" @default.
- W2350486575 modified "2023-09-23" @default.
- W2350486575 title "“Reactive” harzburgite xenoliths from Huinan, Jilin province and their implications for deep dynamic processes." @default.
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