A new parameterization of hydrous mantle melting

By Richard F. Katz, Marc Spiegelman, C. Langmuir. 2003

984 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/02acf5c6e534ee3b022d7ef527390db6594ed0be

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In Geophysics

Citations in the corpus

GEODYNAMICS AND RATE OF VOLCANISM ON MASSIVE EARTH-LIKE PLANETS (2008, background): “In order of increasing complexity, they are those of McKenzie (1984) as extended in McKenzie & Bickle (1988) (henceforth MB88), Katz et al. (2003) (henceforth K03), and (for plate tectonic models only) Ghiorso et al. (2002), with the Smith & Asimow (2005) front-end (henceforth pMELTS).”
Evidence for multiple magma ocean outgassing and atmospheric loss episodes from mantle noble gases (2013, methodology): “96 in a magma ocean at 2053 K, the peridotite liquidus temperature at 1 bar (Katz et al., 2003), noting that the surface of a magma ocean should be at least this hot initially.”
The Role of Volatiles in Reactive Melt Transport in the Asthenosphere (2015, positive): “2, are in broad agreement with previous parameterizations of mantle melting (Katz et al., 2003, and references therein).”
A Simple Thermodynamic Model for Melting of Peridotite in the System NCFMASOCr (2015, background): “This change in melt productivity is a result of cpx exhaustion (i.e. the lherzolite to harzburgite transition), and both the position of the cusp and the slope of the curve on either side match the parameterization of Katz et al. (2003) well.”
Three-dimensional thermomechanical modeling of oceanic spreading initiation and evolution (2013, positive): “The standard (i.e. without melt extraction) volumetric degree of mantle melting M0 changes with pressure and temperature according to the parameterized batch melting model of Katz et al. (2003).”
Constraints on the depths and temperatures of basaltic magma generation on Earth and other terrestrial planets using new thermobarometers for mafic magmas (2009, background): “…fraction contour of a dry fertile lherzolite, which is the temperature and pressure at which fertile lherzolite would melt by 10% (estimated from Katz et al., 2003); assuming a slightly depleted source like the mantle source of MORBs would yield a slightly higher solidus and lower melting…”
Water, Melting, and the Deep Earth H 2 O Cycle (2006, background): “For example, estimates of Dmineral/meltH2O provide constraints for several proposed dehydration melting models (Hirth & Kohlstedt 1996, Katz et al. 2003, Aubaud et al. 2004).”