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A compositionally heterogeneous martian mantle due to late accretion
The approximately chondritic estimated relative abundances of highly siderophile elements (HSE) in the bulk martian mantle suggest that these elements were added after Mars’ core formed. The shergottite-nakhlite-chassigny (SNC) meteorites imply an average mantle Pt abundance of ≈3 to 5 parts per bil...
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| Publicado en: | Sci Adv |
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| Autores principales: | , , |
| Formato: | Artigo |
| Lenguaje: | Inglês |
| Publicado: |
American Association for the Advancement of Science
2020
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| Materias: | |
| Acceso en línea: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7015684/ https://ncbi.nlm.nih.gov/pubmed/32095525 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.aay2338 |
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