Geophysical evidence for an enriched molten silicate layer above Mars’s core

The detection of deep reflected S waves on Mars inferred a core size of 1,830 ± 40 km (ref. (1)), requiring light-element contents that are incompatible with experimental petrological constraints. This estimate assumes a compositionally homogeneous Martian mantle, at odds with recent measurements of...

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Detalles Bibliográficos
Autores principales: Samuel, Henri, Drilleau, Mélanie, Rivoldini, Attilio, Xu, Zongbo, Huang, Quancheng, Garcia, Raphaël F., Lekić, Vedran, Irving, Jessica C. E., Badro, James, Lognonné, Philippe H., Connolly, James A. D., Kawamura, Taichi, Gudkova, Tamara, Banerdt, William B.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2023
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10600000/
https://www.ncbi.nlm.nih.gov/pubmed/37880437
http://dx.doi.org/10.1038/s41586-023-06601-8

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10600000/
https://www.ncbi.nlm.nih.gov/pubmed/37880437
http://dx.doi.org/10.1038/s41586-023-06601-8

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