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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...
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| Vydáno v: | Sci Adv |
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| Hlavní autoři: | , , , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
American Association for the Advancement of Science
2018
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5873841/ https://ncbi.nlm.nih.gov/pubmed/29600271 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.aao5928 |
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