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Natural Chromite Lacework Structures in Allende

Housley, R. M. (2002) Natural Chromite Lacework Structures in Allende. Meteoritics and Planetary Science, 37 (S5). A66-A66. ISSN 1086-9379. doi:10.1111/j.1945-5100.2002.tb00912.x. https://resolver.caltech.edu/CaltechAUTHORS:20140522-083021230

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Abstract

A strikingly high abundance of submicrometer chromite in Allende acid residues was discovered by Lewis et al in 1975 [1] during early efforts to isolate the carriers of anomalous inert gas components in this meteorite. Subsequent work showed that this chromite is not a significant inert gas carrier, but left its origin and significance unexplained. Housley and Clarke {2] used STEM techniques to image and analyze 20 of these chromite grains and found that they are rounded and irregular in shape and vary widely in composition.


Item Type:Article
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http://adsabs.harvard.edu/abs/2002M&PSA..37Q..66HADSArticle
http://dx.doi.org/10.1111/j.1945-5100.2002.tb00912.xDOIAbstracts
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Additional Information:© 2002 Meteoritical Society.
Issue or Number:S5
DOI:10.1111/j.1945-5100.2002.tb00912.x
Record Number:CaltechAUTHORS:20140522-083021230
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20140522-083021230
Official Citation:Natural Chromite Lacework Structures in Allende Housley, R. M. Meteoritics & Planetary Science, vol. 37, Supplement, p.A66
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:45878
Collection:CaltechAUTHORS
Deposited By: Ruth Sustaita
Deposited On:27 May 2014 16:15
Last Modified:10 Nov 2021 17:17

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