Modeling Earth materials from crustal to lower mantle conditions: A transferable set of interaction potentials for the CMAS system
A fully flexible ionic interaction model (Aspherical Ion Model, AIM) is presented and applied to various relevant minerals and melts of the Ca-Mg-Al-Si-O (CMAS) system. The model reproduces accurately lattice parameters and thermoelastic properties of minerals in a wide range of compositions. Furthe...
Main Authors: | Jahn, S, Madden, P |
---|---|
Formato: | Journal article |
Idioma: | English |
Publicado em: |
2007
|
Registos relacionados
-
Earth's Earliest Phaneritic Ultramafic Rocks: Mantle Slices or Crustal Cumulates?
Por: Jiawei Zuo, et al.
Publicado em: (2022-12-01) -
Plume-lithosphere interaction : geochemical evidence from upper mantle and lower crustal xenoliths from the Kerguelen Islands
Por: Hassler, Deborah Renee, 1961-
Publicado em: (2010) -
Transformations and Decomposition of MnCO3 at Earth’s Lower Mantle conditions
Por: EGLANTINE BOULARD, et al.
Publicado em: (2016-12-01) -
On the Processes of Heat Transfer in Earth's Mantle
Por: H. A. LUBIMOVA
Publicado em: (1961-06-01) -
Improved CMAS corrosion resistance of rare earth niobates by high-entropy and composite design
Por: Liujia Tian, et al.
Publicado em: (2024-07-01)