This program is associated with the article: "Constraints on the composition and temperature of LLSVPs from seismic properties of lower mantle minerals" by K. Vilella, T. Bodin, C.-E. Boukare, F. Deschamps, J. Badro, M. D. Ballmer, and Y. Li . The program calculates the properties of a large range of mineral composition. More specifically, the program writes the density of ferropericlase (Fp) and bridgmanite (Bm) as well as the molar concentration of FeO in Fp, FeO in Bm, and AlO2 in Bm. These properties allow us to calculate the density and seismic wave velocities of the rock assemblage
We calculated temperature, pressure and compositional sensitivities of seismic velocities in the low...
International audienceEquation-of-state (EOS) modeling, whereby the seismic properties of a specifie...
The physical and chemical properties of the Earth’s mantle govern the cause of natural disasters, su...
This program is associated with the article: "Constraints on the composition and temperature of LLSV...
This file contains the 79 394 successful models investigated for LLSVPs. For each model, we provide ...
Mineralogical modeling of the lower mantle critically depends on thermoelastic parameters, such as t...
[1] This study presents a new approach to quantitatively assess the relationship between the composi...
Comparison of seismic velocities in mantle minerals, under mantle conditions, with seismic data is a...
98 p.Thesis (Ph.D.)--University of Illinois at Urbana-Champaign, 2005.The sound velocities, elastici...
We test a mineral physics model of the upper mantle against seismic observations. The model is based...
Equation-of-state (EOS) modeling, whereby the seismic properties of a specified thermochemical struc...
Seismic velocities are calculated for two petrological models of the upper mantle, an olivine-rich a...
The chemical composition of Earth's lower mantle can be constrained by combining seismological obser...
This thesis focuses on interpreting geophysical and geochemical observables in terms of the thermome...
Earth’s lower mantle is the most voluminous layer of our planet, extending from approximately 670 to...
We calculated temperature, pressure and compositional sensitivities of seismic velocities in the low...
International audienceEquation-of-state (EOS) modeling, whereby the seismic properties of a specifie...
The physical and chemical properties of the Earth’s mantle govern the cause of natural disasters, su...
This program is associated with the article: "Constraints on the composition and temperature of LLSV...
This file contains the 79 394 successful models investigated for LLSVPs. For each model, we provide ...
Mineralogical modeling of the lower mantle critically depends on thermoelastic parameters, such as t...
[1] This study presents a new approach to quantitatively assess the relationship between the composi...
Comparison of seismic velocities in mantle minerals, under mantle conditions, with seismic data is a...
98 p.Thesis (Ph.D.)--University of Illinois at Urbana-Champaign, 2005.The sound velocities, elastici...
We test a mineral physics model of the upper mantle against seismic observations. The model is based...
Equation-of-state (EOS) modeling, whereby the seismic properties of a specified thermochemical struc...
Seismic velocities are calculated for two petrological models of the upper mantle, an olivine-rich a...
The chemical composition of Earth's lower mantle can be constrained by combining seismological obser...
This thesis focuses on interpreting geophysical and geochemical observables in terms of the thermome...
Earth’s lower mantle is the most voluminous layer of our planet, extending from approximately 670 to...
We calculated temperature, pressure and compositional sensitivities of seismic velocities in the low...
International audienceEquation-of-state (EOS) modeling, whereby the seismic properties of a specifie...
The physical and chemical properties of the Earth’s mantle govern the cause of natural disasters, su...