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Cited by 351

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Hydrogen partition coefficients between nominally anhydrous minerals and basaltic melts

Aubaud, Cyril, Hauri, Erik H., Hirschmann, Marc M.·2004·Geophysical Research Letters

Abstract

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.% H 2 O 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.

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Metadata

Authors
Aubaud, C., Hauri, E. H., & Hirschmann, M. M.
Venue
Geophysical Research Letters
Published
2004-10
Volume
31
Issue
20
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2112503764
Cited by
351
References
25
FWCI
9.56
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Hydrogen partition coefficients between nominally anhydrous minerals and basaltic melts. https://app.cochat.ai/papers/10.1029/2004gl021341
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Aubaud, C., Hauri, E. H., & Hirschmann, M. M. (2004). Hydrogen partition coefficients between nominally anhydrous minerals and basaltic melts. Geophysical Research Letters. https://doi.org/10.1029/2004gl021341

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