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A new parameterization of hydrous mantle melting

Open access
Katz, Richard F., Spiegelman, Marc, Langmuir, Charles H.·2003·Geochemistry, Geophysics, Geosystems

Abstract

Modeling of melt formation and transport in all tectonic settings requires the inclusion of water, since water has large effects on mantle solidi as well as physical properties of liquids. To facilitate the inclusion of water in melting models this paper presents a new parameterization for melt fraction as a function of pressure, temperature, water content and modal cpx, based on knowledge gained from recent advances in the fields of thermodynamic modeling as well as experimental investigations of peridotite melting and hydrous equilibria. The parameterization is computationally efficient and can be modified easily as better experimental data become available. We compare it to other published parameterizations and test it in simple calculations of adiabatic decompression melting (mid‐ocean ridge) and hydrous melting (subduction zone).

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Metadata

Authors
Katz, R. F., Spiegelman, M., & Langmuir, C. H.
Venue
Geochemistry, Geophysics, Geosystems
Published
2003-09
Volume
4
Issue
9
ISSN
1525-2027 (ISSN-L)
OpenAlex
W1821593081
Cited by
1,061
References
2
FWCI
7.56
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: A new parameterization of hydrous mantle melting. https://app.cochat.ai/papers/10.1029/2002gc000433
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Katz, R. F., Spiegelman, M., & Langmuir, C. H. (2003). A new parameterization of hydrous mantle melting. Geochemistry, Geophysics, Geosystems. https://doi.org/10.1029/2002gc000433

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