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Fast accretion of the Earth with a late Moon-forming giant impact
Constraints on the formation history of the Earth are critical for understanding of planet formation processes. (182)Hf-(182)W chronometry of terrestrial rocks points to accretion of Earth in approximately 30 Myr after the formation of the solar system, immediately followed by the Moon-forming giant...
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| Hlavní autoři: | , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
National Academy of Sciences
2011
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| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3203782/ https://ncbi.nlm.nih.gov/pubmed/22006299 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1108544108 |
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