Vertically Resolved Magma Ocean–Protoatmosphere Evolution: H(2), H(2)O, CO(2), CH(4), CO, O(2), and N(2) as Primary Absorbers

The earliest atmospheres of rocky planets originate from extensive volatile release during magma ocean epochs that occur during assembly of the planet. These establish the initial distribution of the major volatile elements between different chemical reservoirs that subsequently evolve via geologica...

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Detalles Bibliográficos
Autores principales: Lichtenberg, Tim, Bower, Dan J., Hammond, Mark, Boukrouche, Ryan, Sanan, Patrick, Tsai, Shang‐Min, Pierrehumbert, Raymond T.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2021
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7988593/
https://www.ncbi.nlm.nih.gov/pubmed/33777608
http://dx.doi.org/10.1029/2020JE006711

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7988593/
https://www.ncbi.nlm.nih.gov/pubmed/33777608
http://dx.doi.org/10.1029/2020JE006711

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