Influence of phase transformations on lateral heterogeneity and dynamics in Earth's mantle
By L. Stixrude, C. Lithgow‐Bertelloni. 2007
138 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/5b5810c548498fc03d201a45d23844ba92f79ed7
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In Geophysics
- L. Stixrude
- C. Lithgow‐Bertelloni
- Hans-Peter Bunge
- Bernhard S. A. Schuberth
- J. Ritsema
- J. Huw Davies
- S. Goes
- David Rhodri Davies
Citations in the corpus
- Equation of state and phase diagram of FeO (2011, methodology): “We fixed the parameters V0 (McCammon and Liu, 1984), "0 (Stixrude and Lithgow-Bertelloni, 2007), and q, finding a good fit to the data for q = 0.”
- Reconciling dynamic and seismic models of Earth's lower mantle: The dominant role of thermal heterogeneity (2012, background): “…phase transformation causes a sharp increase in shear wave velocity (e.g. Wookey et al., 2005; Ammann et al., 2010; Stixrude and LithgowBertelloni, 2011) and topography on this phase boundary produces local velocity gradients of greater than 10% per 100 km (Stixrude and Lithgow-Bertelloni, 2007).”
- Thermodynamics of mantle minerals - II. Phase equilibria (2011, methodology): “These terms have been called the ‘metamorphic’ contributions to thermodynamic properties and appear only in multiphase, multicomponent systems and for processes that are sufficiently slow for chemical equilibrium to be maintained (Stixrude & Lithgow-Bertelloni 2007).”
- Thermodynamics of silicate liquids in the deep Earth (Invited) (2009, background): “the T0=1600 K isentrope (Stixrude and Lithgow-Bertelloni, 2007) and a lower thermal boundary layer that reaches a temperature of 4100 K at the core–mantle boundary”
- Geophysics of Chemical Heterogeneity in the Mantle (2012, background): “…∂ ln X ∂T ) P = ( ∂ ln X ∂T ) P, n + ( ∂ ln X ∂ n ) P,T ( ∂ n ∂T ) P , (2) where X is a property of the aggregate such as density or velocity, T is temperature, P is pressure, and n is the vector specifying the amounts of all end-member species of all phases (Stixrude & Lithgow-Bertelloni 2007).”