Melting and defect transitions in FeO up to pressures of Earth’s core-mantle boundary

The high-pressure melting curve of FeO controls key aspects of Earth’s deep interior and the evolution of rocky planets more broadly. However, existing melting studies on wüstite were conducted across a limited pressure range and exhibit substantial disagreement. Here we use an in-situ dual-techniqu...

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Detalles Bibliográficos
Autores principales: Dobrosavljevic, Vasilije V., Zhang, Dongzhou, Sturhahn, Wolfgang, Chariton, Stella, Prakapenka, Vitali B., Zhao, Jiyong, Toellner, Thomas S., Pardo, Olivia S., Jackson, Jennifer M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2023
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10643405/
https://www.ncbi.nlm.nih.gov/pubmed/37957142
http://dx.doi.org/10.1038/s41467-023-43154-w

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10643405/
https://www.ncbi.nlm.nih.gov/pubmed/37957142
http://dx.doi.org/10.1038/s41467-023-43154-w

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