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Magnesium isotope evidence that accretional vapour loss shapes planetary compositions

It has long been recognised that Earth and other differentiated planetary bodies are chemically fractionated compared to primitive, chondritic meteorites and by inference the primordial disk from which they formed. An important question has been whether the notable volatile depletions of planetary b...

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Détails bibliographiques
Publié dans:Nature
Auteurs principaux: Hin, Remco C., Coath, Christopher D., Carter, Philip J., Nimmo, Francis, Lai, Yi-Jen, Pogge von Strandmann, Philip A.E., Willbold, Matthias, Leinhardt, Zoë M., Walter, Michael J., Elliott, Tim
Format: Artigo
Langue:Inglês
Publié: 2017
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Accès en ligne:https://ncbi.nlm.nih.gov/pmc/articles/PMC5624506/
https://ncbi.nlm.nih.gov/pubmed/28959965
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/nature23899
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