Thermodynamics of mantle minerals - II. Phase equilibria
By L. Stixrude, C. Lithgow‐Bertelloni. 2011
572 citations recorded by the source corpus.
Subfields: Biomedical Engineering, Geophysics
View Paper: https://www.semanticscholar.org/paper/cd009aaf502163a7a7d8039f739e0370b58482cd
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In Biomedical Engineering
In Geophysics
- L. Stixrude
- C. Lithgow‐Bertelloni
- J. A. Connolly
- Hans-Peter Bunge
- Bernhard S. A. Schuberth
- J. Ritsema
- J. C. Afonso
- William L Griffin
Citations in the corpus
- Can we constrain the interior structure of rocky exoplanets from mass and radius measurements (2015, unknown): “Mineral equations of state and parameters are as given by Stixrude & Lithgow-Bertelloni (2005, 2011).”
- High Accuracy Mantle Convection Simulation through Modern Numerical Methods. II: Realistic Models and Problems (2017, methodology): “…and the initial temperature profile follows an adiabat of 1613 K computed with the material properties that are provided by the Per-ple X software [Connolly(2005)] based on a database of mineral properties [Stixrude & Lithgow-Bertelloni(2011)], overall a method similar to [Nakagawa et al.(2009)].”
- 3‐D multiobservable probabilistic inversion for the compositional and thermal structure of the lithosphere and upper mantle. I: a priori petrological information and geophysical observables (2013, background): “…uncertainty can be estimated based on the discrepancies between predictions from different thermodynamic [Holland and Powell, 1998 (revised 2002); Stixrude and Lithgow-Bertelloni, 2011], hybrid [Afonso et al., 2008], and mineral physics methods [Schutt and Lesher, 2006] for identical compositions.”
- Geophysics of Chemical Heterogeneity in the Mantle (2012, methodology): “Computed with HeFESTo (Stixrude & Lithgow-Bertelloni 2011). phase in these regions is stishovite, except near the base of the mantle where calcium-rich silicate perovskite becomes faster.”
- Reconciling dynamic and seismic models of Earth's lower mantle: The dominant role of thermal heterogeneity (2012, methodology): “The thermodynamic compilation used (Stixrude and Lithgow-Bertelloni, 2011) predicts that outside of the post-perovskite stability field, basaltic material is significantly faster in shear wave velocity and slightly faster in compressional wave velocity, when compared to a pyrolite (Fig.”