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Buoyancy and Structure of Volatile‐Rich Silicate Melts
The early Earth was marked by at least one global magma ocean. Melt buoyancy played a major role for its evolution. Here we model the composition of the magma ocean using a six‐component pyrolite melt, to which we add volatiles in the form of carbon as molecular CO or CO(2) and hydrogen as molecular...
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| Опубликовано в: : | J Geophys Res Solid Earth |
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| Главные авторы: | , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
John Wiley and Sons Inc.
2021
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| Предметы: | |
| Online-ссылка: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7900987/ https://ncbi.nlm.nih.gov/pubmed/33680690 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1029/2020JB021045 |
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