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
|
PDF
- Published Version
See Usage Policy. 199kB |
Use this Persistent URL to link to this item: https://resolver.caltech.edu/CaltechAUTHORS:20131106-153950591
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: |
| ||||||
| ORCID: |
| ||||||
| 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 |
Repository Staff Only: item control page
