Cargando…
Altered chemistry of oxygen and iron under deep Earth conditions
A drastically altered chemistry was recently discovered in the Fe-O-H system under deep Earth conditions, involving the formation of iron superoxide (FeO(2)Hx with x = 0 to 1), but the puzzling crystal chemistry of this system at high pressures is largely unknown. Here we present evidence that despi...
Autores principales: | Liu, Jin, Hu, Qingyang, Bi, Wenli, Yang, Liuxiang, Xiao, Yuming, Chow, Paul, Meng, Yue, Prakapenka, Vitali B., Mao, Ho-Kwang, Mao, Wendy L. |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2019
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6329810/ https://www.ncbi.nlm.nih.gov/pubmed/30635572 http://dx.doi.org/10.1038/s41467-018-08071-3 |
Ejemplares similares
-
Mineralogy of the deep lower mantle in the presence of H(2)O
por: Hu, Qingyang, et al.
Publicado: (2020) -
Evidence for oxygenation of Fe-Mg oxides at mid-mantle conditions and the rise of deep oxygen
por: Liu, Jin, et al.
Publicado: (2020) -
Stability of iron-bearing carbonates in the deep Earth’s interior
por: Cerantola, Valerio, et al.
Publicado: (2017) -
Key problems of the deep Earth
por: Mao, Ho-Kwang
Publicado: (2021) -
Iron-rich Fe–O compounds at Earth’s core pressures
por: Liu, Jin, et al.
Publicado: (2022)