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Hydrogen isotopic evidence for early oxidation of silicate Earth
The Moon-forming giant impact extensively melts and partially vaporizes the silicate Earth and delivers a substantial mass of metal to Earth’s core. The subsequent evolution of the magma ocean and overlying atmosphere has been described by theoretical models but observable constraints on this epoch...
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| Publicado en: | Earth Planet Sci Lett |
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| Autores principales: | , , |
| Formato: | Artigo |
| Lenguaje: | Inglês |
| Publicado: |
2019
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| Materias: | |
| Acceso en línea: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7939044/ https://ncbi.nlm.nih.gov/pubmed/33688096 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1016/j.epsl.2019.115770 |
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