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 | ||||||
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| Additional Information: | © 1991 Meteoritical Society. | ||||||
| Issue or Number: | 4 | ||||||
| Record Number: | CaltechAUTHORS:20131106-153950591 | ||||||
| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20131106-153950591 | ||||||
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| 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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