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Melting of iron determined by X-ray absorption spectroscopy to 100 GPa

Temperature, thermal history, and dynamics of Earth rely critically on the knowledge of the melting temperature of iron at the pressure conditions of the inner core boundary (ICB) where the geotherm crosses the melting curve. The literature on this subject is overwhelming, and no consensus has been...

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Publicado en:Proc Natl Acad Sci U S A
Autores principales: Aquilanti, Giuliana, Trapananti, Angela, Karandikar, Amol, Kantor, Innokenty, Marini, Carlo, Mathon, Olivier, Pascarelli, Sakura, Boehler, Reinhard
Formato: Artigo
Lenguaje:Inglês
Publicado: National Academy of Sciences 2015
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Acceso en línea:https://ncbi.nlm.nih.gov/pmc/articles/PMC4593125/
https://ncbi.nlm.nih.gov/pubmed/26371317
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1502363112
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