Φορτώνει......
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...
Αποθηκεύτηκε σε:
| Κύριοι συγγραφείς: | , , , |
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| Μορφή: | Artigo |
| Γλώσσα: | Inglês |
| Έκδοση: |
National Academy of Sciences
2011
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| Θέματα: | |
| Διαθέσιμο Online: | 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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