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Trace element partitioning within Mesosiderite clasts

Kennedy, A. K. and Stewart, B. W. and Hutcheon, I. D. and Wasserburg, G. J. (1991) Trace element partitioning within Mesosiderite clasts. Meteoritics, 26 (4). p. 356. ISSN 0026-1114 . https://resolver.caltech.edu/CaltechAUTHORS:20131106-153950591

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Abstract

Mesosiderites are polymict silicate and metal breccias resulting from magmatic differentiation, brecciation, metal-silicate mixing, and metamorphic recrystallization in early planetary bodies. Petrographic and trace element studies have documented the great diversity of differentiated silicates, with eucritic basalt, gabbroic cumulate and diogenite clasts and trace element disequilibrium between phases (1-4).


Item Type:Article
Related URLs:
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http://adsabs.harvard.edu/abs/1991Metic..26R.356KADSArticle
ORCID:
AuthorORCID
Wasserburg, G. J.0000-0002-7957-8029
Additional Information:© 1991 Meteoritical Society.
Issue or Number:4
Record Number:CaltechAUTHORS:20131106-153950591
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20131106-153950591
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:42285
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:07 Nov 2013 00:51
Last Modified:03 Oct 2019 05:57

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