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Lattice thermal conductivity of lower mantle minerals and heat flux from Earth’s core

The amount of heat flowing from Earth’s core critically determines the thermo-chemical evolution of both the core and the lower mantle. Consisting primarily of a polycrystalline aggregate of silicate perovskite and ferropericlase, the thermal boundary layer at the very base of Earth’s lower mantle r...

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Detalhes bibliográficos
Main Authors: Manthilake, Geeth M., de Koker, Nico, Frost, Dan J., McCammon, Catherine A.
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2011
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC3207700/
https://ncbi.nlm.nih.gov/pubmed/22021444
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1110594108
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