Low-spin ferric iron in primordial bridgmanite crystallized from a deep magma ocean

The crystallization of the magma ocean resulted in the present layered structure of the Earth’s mantle. An open question is the electronic spin state of iron in bridgmanite (the most abundant mineral on Earth) crystallized from a deep magma ocean, which has been neglected in the crystallization hist...

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Detalles Bibliográficos
Autores principales: Okuda, Yoshiyuki, Ohta, Kenji, Nishihara, Yu, Hirao, Naohisa, Wakamatsu, Tatsuya, Suehiro, Sho, Kawaguchi, Saori I., Ohishi, Yasuo
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8484549/
https://www.ncbi.nlm.nih.gov/pubmed/34593901
http://dx.doi.org/10.1038/s41598-021-98991-w

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8484549/
https://www.ncbi.nlm.nih.gov/pubmed/34593901
http://dx.doi.org/10.1038/s41598-021-98991-w

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