Published December 1984
| Published
Journal Article
Open
Mg Isotopic studies of Leoville "compact" type a CAI
Chicago
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Abstract
One long-standing problem in the application of Al-Mg isotopic systematics to the chronology of CAI is the enigmatic Mg isotopic record of hibonite. Hibonite (ideally, CaAI_(12)O_(19)) is one of the first major element bearing phases to appear in the condensation sequence [1] and occurs as a major constituent only in CAI whose bulk composition is considerably more refractory than Allende Type Bl CAI.
Additional Information
© 1984 Meteoritical Society. Article first published online: 15 Jun 2012.Attached Files
Published - Wasserburg_1984p244.pdf
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Additional details
- Eprint ID
- 44152
- DOI
- 10.1111/j.1945-5100.1984.tb00840.x
- Resolver ID
- CaltechAUTHORS:20140305-101511796
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2014-03-05Created from EPrint's datestamp field
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2021-11-10Created from EPrint's last_modified field