Valence and spin states of iron are invisible in Earth’s lower mantle

Heterogeneity in Earth’s mantle is a record of chemical and dynamic processes over Earth’s history. The geophysical signatures of heterogeneity can only be interpreted with quantitative constraints on effects of major elements such as iron on physical properties including density, compressibility, a...

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Detalhes bibliográficos
Publicado no:Nat Commun
Main Authors: Liu, Jiachao, Dorfman, Susannah M., Zhu, Feng, Li, Jie, Wang, Yonggang, Zhang, Dongzhou, Xiao, Yuming, Bi, Wenli, Alp, E. Ercan
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group UK 2018
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Article
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC5876394/
https://ncbi.nlm.nih.gov/pubmed/29599446
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-03671-5
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