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Early volatile depletion on planetesimals inferred from C–S systematics of iron meteorite parent bodies

During the formation of terrestrial planets, volatile loss may occur through nebular processing, planetesimal differentiation, and planetary accretion. We investigate iron meteorites as an archive of volatile loss during planetesimal processing. The carbon contents of the parent bodies of magmatic i...

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Detalles Bibliográficos
Autores principales: Hirschmann, Marc M., Bergin, Edwin A., Blake, Geoff A., Ciesla, Fred J., Li, Jie
Formato: Online Artículo Texto
Lenguaje:English
Publicado: National Academy of Sciences 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8020667/
https://www.ncbi.nlm.nih.gov/pubmed/33753516
http://dx.doi.org/10.1073/pnas.2026779118

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