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Heavy iron isotope composition of iron meteorites explained by core crystallization

Similar to Earth, many large planetesimals in the Solar System experienced planetary-scale processes such as accretion, melting, and differentiation. As their cores cooled and solidified, significant chemical fractionation occurred due to solid metal-liquid metal fractionation. Iron meteorites -- co...

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Detalles Bibliográficos
Autores principales: Ni, Peng, Chabot, Nancy L., Ryan, Caillin J., Shahar, Anat
Formato: Online Artículo Texto
Lenguaje:English
Publicado: 2020
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7500481/
https://www.ncbi.nlm.nih.gov/pubmed/32952605
http://dx.doi.org/10.1038/s41561-020-0617-y