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Asymmetric shock heating and the terrestrial magma ocean origin of the Moon
One of the difficulties of the current giant impact model for the origin of the Moon is to explain the marked similarity in the isotopic compositions and the substantial differences in the major element chemistry. Physics of shock heating is analyzed to show that the degree of heating is asymmetric...
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
The Japan Academy
2014
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| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3997809/ https://ncbi.nlm.nih.gov/pubmed/24621956 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.2183/pjab.90.97 |
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