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Evidence of ^(26)Mg Excess in Hibonite from Murchison

Papanastassiou, D. A. and Wasserburg, G. J. (1980) Evidence of ^(26)Mg Excess in Hibonite from Murchison. Meteoritics, 15 (4). p. 348. ISSN 0026-1114. https://resolver.caltech.edu/CaltechAUTHORS:20131107-070750178

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Abstract

We report Mg isotopic analyses on a hibonite inclusion from Murchison (CM), named the Blue Angel for its distinct color, and discovered by R.H. Becker. Petrographic, mineralogic, and chemical information is provided in a companion abstract (Armstrong et al., 1980). Hibonite is important as it has the highest estimated condensation temperature for major element oxides (Blander and Fuchs, 1975), may have a high Al/Mg ratio, and may be chemically resistant to alteration.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://adsabs.harvard.edu/abs/1980Metic..15..348PADSArticle
ORCID:
AuthorORCID
Wasserburg, G. J.0000-0002-7957-8029
Additional Information:© 1980 Meteoritical Society. Div. Contrib. No. 3466 (359).
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Caltech Division of Geological and Planetary Sciences3466
Lunatic Asylum Lab359
Issue or Number:4
Record Number:CaltechAUTHORS:20131107-070750178
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20131107-070750178
Official Citation:Evidence of 26Mg Excess in Hibonite from Murchison Papanastassiou, D. A.; Wasserburg, G. J. Meteoritics, Vol. 15, p.348
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:42289
Collection:CaltechAUTHORS
Deposited By: Ruth Sustaita
Deposited On:07 Nov 2013 18:03
Last Modified:09 Mar 2020 13:19

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