Evidence for oxygenation of Fe-Mg oxides at mid-mantle conditions and the rise of deep oxygen

As the reaction product of subducted water and the iron core, FeO(2) with more oxygen than hematite (Fe(2)O(3)) has been recently recognized as an important component in the D” layer just above the Earth's core-mantle boundary. Here, we report a new oxygen-excess phase (Mg, Fe)(2)O(3+)(δ) (0 &l...

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Detalles Bibliográficos
Autores principales: Liu, Jin, Wang, Chenxu, Lv, Chaojia, Su, Xiaowan, Liu, Yijin, Tang, Ruilian, Chen, Jiuhua, Hu, Qingyang, Mao, Ho-Kwang, Mao, Wendy L
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Oxford University Press 2020
Materias:
EARTH SCIENCES
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8288346/
https://www.ncbi.nlm.nih.gov/pubmed/34691604
http://dx.doi.org/10.1093/nsr/nwaa096

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8288346/
https://www.ncbi.nlm.nih.gov/pubmed/34691604
http://dx.doi.org/10.1093/nsr/nwaa096

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