Near-equilibrium isotope fractionation during planetesimal evaporation.
Asteroids
Cosmochemistry
Planetesimals
composition
Journal
Icarus
ISSN: 0019-1035
Titre abrégé: Icarus
Pays: United States
ID NLM: 9890634
Informations de publication
Date de publication:
01 May 2019
01 May 2019
Historique:
entrez:
12
2
2019
pubmed:
12
2
2019
medline:
12
2
2019
Statut:
ppublish
Résumé
Silicon and Mg in differentiated rocky bodies exhibit heavy isotope enrichments that have been attributed to evaporation of partially or entirely molten planetesimals. We evaluate the mechanisms of planetesimal evaporation in the early solar system and the conditions that controled attendant isotope fractionations. Energy balance at the surface of a body accreted within ~1 Myr of CAI formation and heated from within by
Identifiants
pubmed: 30739951
doi: 10.1016/j.icarus.2019.01.012
pmc: PMC6364317
mid: NIHMS1007937
doi:
Types de publication
Journal Article
Langues
eng
Pagination
1-15Subventions
Organisme : Intramural NASA
ID : 80NSSC18K0594
Pays : United States
Déclaration de conflit d'intérêts
Declarions of interest: none
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