Reconciling metal–silicate partitioning and late accretion in the Earth

Highly siderophile elements (HSE), including platinum, provide powerful geochemical tools for studying planet formation. Late accretion of chondritic components to Earth after core formation has been invoked as the main source of mantle HSE. However, core formation could also have contributed to the...

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Detalles Bibliográficos
Autores principales: Suer, Terry-Ann, Siebert, Julien, Remusat, Laurent, Day, James M. D., Borensztajn, Stephan, Doisneau, Beatrice, Fiquet, Guillaume
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8131616/
https://www.ncbi.nlm.nih.gov/pubmed/34006864
http://dx.doi.org/10.1038/s41467-021-23137-5

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8131616/
https://www.ncbi.nlm.nih.gov/pubmed/34006864
http://dx.doi.org/10.1038/s41467-021-23137-5

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