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...

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Detalles Bibliográficos
Autores principales: Melwani Daswani, Mohit, Vance, Steven D., Mayne, Matthew J., Glein, Christopher R.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2021
Materias:
Research Letter
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

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9286408/
https://www.ncbi.nlm.nih.gov/pubmed/35865189
http://dx.doi.org/10.1029/2021GL094143

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