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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Detalles Bibliográficos
Autores principales: Liu, Jiachao, Dorfman, Susannah M., Zhu, Feng, Li, Jie, Wang, Yonggang, Zhang, Dongzhou, Xiao, Yuming, Bi, Wenli, Alp, E. Ercan
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5876394/
https://www.ncbi.nlm.nih.gov/pubmed/29599446
http://dx.doi.org/10.1038/s41467-018-03671-5

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5876394/
https://www.ncbi.nlm.nih.gov/pubmed/29599446
http://dx.doi.org/10.1038/s41467-018-03671-5

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