Cargando…
Redox state of Earth’s magma ocean and its Venus-like early atmosphere
Exchange between a magma ocean and vapor produced Earth’s earliest atmosphere. Its speciation depends on the oxygen fugacity (fO(2)) set by the Fe(3+)/Fe(2+) ratio of the magma ocean at its surface. Here, we establish the relationship between fO(2) and Fe(3+)/Fe(2+) in quenched liquids of silicate E...
Autores principales: | Sossi, Paolo A., Burnham, Antony D., Badro, James, Lanzirotti, Antonio, Newville, Matt, O’Neill, Hugh St.C. |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
American Association for the Advancement of Science
2020
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7688334/ https://www.ncbi.nlm.nih.gov/pubmed/33239296 http://dx.doi.org/10.1126/sciadv.abd1387 |
Ejemplares similares
-
Stochastic accretion of the Earth
por: Sossi, Paolo A., et al.
Publicado: (2022) -
Investigating Magma Ocean Solidification on Earth Through Laser‐Heated Diamond Anvil Cell Experiments
por: Nabiei, Farhang, et al.
Publicado: (2021) -
A magma ocean origin to divergent redox evolutions of rocky planetary bodies and early atmospheres
por: Deng, Jie, et al.
Publicado: (2020) -
Electrical conductivity and magnetic dynamos in magma oceans of Super-Earths
por: Soubiran, François, et al.
Publicado: (2018) -
Genesis of a CO(2)-rich and H(2)O-depleted atmosphere from Earth’s early global magma ocean
por: Solomatova, Natalia V., et al.
Publicado: (2021)