Well-resolved variations in the formation ages for Ca–Al-rich inclusions in the early Solar System

Recent whole-rock magnesium-isotopic data for calcium-aluminum-rich inclusions (CAIs) in chondrite meteorites indicate that the primary nebular fractionation of aluminum from magnesium, probably by condensation, occurred within

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Bibliographic Details
Published in:Earth and planetary science letters 2012-05, Vol.331-332, p.43-54
Main Authors: MacPherson, G.J., Kita, N.T., Ushikubo, T., Bullock, E.S., Davis, A.M.
Format: Article
Language:English
Subjects:
26Al
Age
Aluminum
calcium–aluminum-rich inclusions
Chronology
early Solar System
Fractionation
Magnesium
Meteorites
Solar system
Spreads
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Description
Summary:Recent whole-rock magnesium-isotopic data for calcium-aluminum-rich inclusions (CAIs) in chondrite meteorites indicate that the primary nebular fractionation of aluminum from magnesium, probably by condensation, occurred within
ISSN:0012-821X
1385-013X
DOI:10.1016/j.epsl.2012.03.010