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Low viscosity of the Earth’s inner core

The Earth’s solid inner core is a highly attenuating medium. It consists mainly of iron. The high attenuation of sound wave propagation in the inner core is at odds with the widely accepted paradigm of hexagonal close-packed phase stability under inner core conditions, because sound waves propagate...

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Détails bibliographiques
Publié dans:Nat Commun
Auteurs principaux: Belonoshko, Anatoly B., Fu, Jie, Bryk, Taras, Simak, Sergei I., Mattesini, Maurizio
Format: Artigo
Langue:Inglês
Publié: Nature Publishing Group UK 2019
Sujets:
Accès en ligne:https://ncbi.nlm.nih.gov/pmc/articles/PMC6554349/
https://ncbi.nlm.nih.gov/pubmed/31171778
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-019-10346-2
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