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Oxygen isotopic evidence for accretion of Earth’s water before a high-energy Moon-forming giant impact
The Earth-Moon system likely formed as a result of a collision between two large planetary objects. Debate about their relative masses, the impact energy involved, and the extent of isotopic homogenization continues. We present the results of a high-precision oxygen isotope study of an extensive sui...
| Autores principales: | , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
American Association for the Advancement of Science
2018
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5873841/ https://www.ncbi.nlm.nih.gov/pubmed/29600271 http://dx.doi.org/10.1126/sciadv.aao5928 |