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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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| Autors principals: | , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
National Academy of Sciences
2011
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| Matèries: | |
| Accés en línia: | 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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