Housley, R. M. (1986) On the Relationship Between CAI Evolution and Chondrule Formation. Meteoritics, 21 (4). p. 400. ISSN 0026-1114. https://resolver.caltech.edu/CaltechAUTHORS:20140115-100155727
|
PDF
- Published Version
See Usage Policy. 85kB |
Use this Persistent URL to link to this item: https://resolver.caltech.edu/CaltechAUTHORS:20140115-100155727
Abstract
The relationship in time and space between CAl formation on the one hand, and chondrule formation on the other is not well understood. It appears that at least compact, coarse-grained CAl were once largely molten. They must have been very depleted in volatiles at that time. However, as now found in Allende they show extensive alteration to volatile rich minerals such as nepheline and sodalite. I have previously argued, partly on the basis of the ubiquitous presence of these volatile rich minerals also in chondrules and matrix, that this alteration probably took place on the Allende parent body (Housley, 1985).
| Item Type: | Article | ||||||
|---|---|---|---|---|---|---|---|
| Related URLs: |
| ||||||
| Additional Information: | © 1986 Meteoritical Society. | ||||||
| Issue or Number: | 4 | ||||||
| Record Number: | CaltechAUTHORS:20140115-100155727 | ||||||
| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20140115-100155727 | ||||||
| Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. | ||||||
| ID Code: | 43377 | ||||||
| Collection: | CaltechAUTHORS | ||||||
| Deposited By: | Tony Diaz | ||||||
| Deposited On: | 29 Jan 2014 20:24 | ||||||
| Last Modified: | 03 Oct 2019 06:07 |
Repository Staff Only: item control page
