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- W2112503764 abstract "[1] We have measured hydrogen partition coefficients between nominally anhydrous minerals (olivine, pyroxenes) and basaltic melts in 13 hydrous melting experiments performed at upper mantle P-T conditions (1–2 GPa and 1230–1380°C). Resulting liquids have 3.1–6.4 wt.% H2O and average mineral/melt partition coefficients as follows: DHol/melt = 0.0017 ± 0.0005 (n = 9), DHopx/melt = 0.019 ± 0.004 (n = 8), and DHcpx/melt = 0.023 ± 0.005 (n = 2). Mineral/mineral partition coefficients are DHol/opx = 0.11 ± 0.01 (n = 4), DHol/cpx = 0.08 ± 0.01 (n = 2) and DHcpx/opx = 1.4 ± 0.3 (n = 1). These measurements confirm that water behaves similarly to Ce during mantle melting (DHperidotite/melt is ∼0.009). For mantle water concentrations of 50–200 ppm, the onset of melting is 5–20 km deeper than the dry solidus, less than previous estimates." @default.
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- W2112503764 date "2004-01-01" @default.
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- W2112503764 title "Hydrogen partition coefficients between nominally anhydrous minerals and basaltic melts" @default.
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- W2112503764 doi "https://doi.org/10.1029/2004gl021341" @default.
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