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A Metamorphic Origin for Europa's Ocean
Europa likely contains an iron‐rich metal core. For it to have formed, temperatures within Europa reached [Formula: see text] 1250 K. Going up to that temperature, accreted chondritic minerals — for example, carbonates and phyllosilicates — would partially devolatilize. Here, we compute the amounts...
| Autores principales: | , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
John Wiley and Sons Inc.
2021
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9286408/ https://www.ncbi.nlm.nih.gov/pubmed/35865189 http://dx.doi.org/10.1029/2021GL094143 |