Calculation of Peridotite Partial Melting from Thermodynamic Models of Minerals and Melts, IV. Adiabatic Decompression and the Composition and Mean Properties of Mid-ocean Ridge Basalts
By P. Asimow, M. Hirschmann, E. Stolper. 2001
195 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/a8a52f827e88b021329df7635801ff89fb53487d
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In Geophysics
- J. A. Connolly
- M. Hirschmann
- J. C. Afonso
- William L Griffin
- P. Asimow
- H. Dalton
- Manel Fernàndez
- D. L. Anderson
Citations in the corpus
- The pMELTS: A revision of MELTS for improved calculation of phase relations and major element partitioning related to partial melting of the mantle to 3 GPa (2002, methodology): “Strong near-solidus enrichments in alkalis are expected to reduce isobaric and polybaric (adiabatic) melt productivity, relative to values prevailing at higher melt fractions [ Asimow et al. , 1997, 2001; Hirsch-mann et al. , 1999b; Robinson et al. , 1998].”
- Integrated geophysical‐petrological modeling of the lithosphere and sublithospheric upper mantle: Methodology and applications (2008, background): “The third factor is more uncertain, but the changes in volume and in the solidus slope associated with the phase transition [Asimow et al., 2001; Kushiro, 2001] could in principle cause this effect.”
- Adiabat_1ph: A new public front‐end to the MELTS, pMELTS, and pHMELTS models (2005, background): “D (triangular) melting regimes [ Asimow et al. , 2001].”
- Constraints on the depths and temperatures of basaltic magma generation on Earth and other terrestrial planets using new thermobarometers for mafic magmas (2009, background): “The temperatures and pressures estimated here are comparable to those inferred from crustal thicknesses, incompatible element enrichments (e.g, Na), theoretical melting models, and geophysical constraints (Klein and Langmuir, 1987; Langmuir et al., 1992; Forsyth et al., 1998; Asimow et al., 2001).”
- A cool model for the Iceland hotspot (2005, background): “…fertility anomaly raises some interesting questions: a) The question of heat: Whereas peridotitic systems have been studied exhaustively (e.g., Asimow et al., 2001) details of how eclogite or eclogite-peridotite mixtures melt under 22 conditions of passive adiabatic upwelling are less well…”