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Cited by 386

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The importance of water to oceanic mantle melting regimes

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Asimow, P. D., Langmuir, C. H.·2003·Nature

Abstract

The formation of basaltic crust at mid-ocean ridges and ocean islands provides a window into the compositional and thermal state of the Earth's upper mantle. But the interpretation of geochemical and crustal-thickness data in terms of magma source parameters depends on our understanding of the melting, melt-extraction and differentiation processes that intervene between the magma source and the crust. Much of the quantitative theory developed to model these processes has neglected the role of water in the mantle and in magma, despite the observed presence of water in ocean-floor basalts. Here we extend two quantitative models of ridge melting, mixing and fractionation to show that the addition of water can cause an increase in total melt production and crustal thickness while causing a decrease in mean extent of melting. This may help to resolve several enigmatic observations in the major- and trace-element chemistry of both normal and hotspot-affected ridge basalts.

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Metadata

Authors
Asimow, P. D., & Langmuir, C. H.
Venue
Nature
Published
2003-02
Volume
421
Issue
6925
Pages
815-820
ISSN
  • 0028-0836 (ISSN-L)
  • 1476-4687
OpenAlex
W2135595053
Cited by
386
References
26
FWCI
23.00
Type
journal article
Language
en
Open access
green

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CoChat. (2026). Citation check: The importance of water to oceanic mantle melting regimes. https://app.cochat.ai/papers/10.1038/nature01429
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Asimow, P. D., & Langmuir, C. H. (2003). The importance of water to oceanic mantle melting regimes. Nature. https://doi.org/10.1038/nature01429

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