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Low thermal conductivity of iron-silicon alloys at Earth’s core conditions with implications for the geodynamo

Earth’s core is composed of iron (Fe) alloyed with light elements, e.g., silicon (Si). Its thermal conductivity critically affects Earth’s thermal structure, evolution, and dynamics, as it controls the magnitude of thermal and compositional sources required to sustain a geodynamo over Earth’s histor...

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Bibliografski detalji
Izdano u:Nat Commun
Glavni autori: Hsieh, Wen-Pin, Goncharov, Alexander F., Labrosse, Stéphane, Holtgrewe, Nicholas, Lobanov, Sergey S., Chuvashova, Irina, Deschamps, Frédéric, Lin, Jung-Fu
Format: Artigo
Jezik:Inglês
Izdano: Nature Publishing Group UK 2020
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Online pristup:https://ncbi.nlm.nih.gov/pmc/articles/PMC7335046/
https://ncbi.nlm.nih.gov/pubmed/32620830
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-020-17106-7
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