Nichols, R. H., Jr. and Grimley, R. T. and Wasserburg, G. J.
(1998)
Measurement of gas-phase species during Langmuir evaporation of forsterite.
Meteoritics and Planetary Science, 33
(S4).
A115-A116.
ISSN 1086-9379.
https://resolver.caltech.edu/CaltechAUTHORS:20140716-144324335
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Abstract
Forsterite, the most abundant mineral in meteorites, forms at high temperatures often associated with nebular processes. It evaporates congruently, and its equilibrium evaporation is rather well understood [e.g.]. For these reasons, in part, many recent studies have focused on the
more difficult kinetics of the free (Langmuir or nonequilibrium) evaporation of this mineral.
| Item Type: | Article |
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| Additional Information: | © 1998 The Meteoritical Society. Article first published online: 4 Feb 2010. Supported by NASA grant NAGW3337 (GJW).
Div. Cont. 8519 (999). |
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| Funders: | | Funding Agency | Grant Number |
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| NASA | NAGW3337 |
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| Other Numbering System: | | Other Numbering System Name | Other Numbering System ID |
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| Caltech Division of Geological and Planetary Sciences | 8519 | | Lunatic Asylum Lab | 999 |
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| Issue or Number: | S4 |
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| Record Number: | CaltechAUTHORS:20140716-144324335 |
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| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20140716-144324335 |
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| Official Citation: | (1998), Abstracts. Meteoritics & Planetary Science, 33: A7–A172. doi: 10.1111/j.1945-5100.1998.tb01327.x |
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| Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. |
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| ID Code: | 47273 |
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| Collection: | CaltechAUTHORS |
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| Deposited By: |
Ruth Sustaita
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| Deposited On: | 16 Jul 2014 23:32 |
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| Last Modified: | 09 Mar 2020 13:19 |
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