Published July 27, 1998
| Published
Journal Article
Open
Measurement of gas-phase species during Langmuir evaporation of forsterite
Chicago
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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.
Additional Information
© 1998 The Meteoritical Society. Article first published online: 4 Feb 2010. Supported by NASA grant NAGW3337 (GJW). Div. Cont. 8519 (999).Attached Files
Published - Wasserburg_1998pA115.pdf
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Additional details
- Eprint ID
- 47273
- DOI
- 10.1111/j.1945-5100.1998.tb01327.x
- Resolver ID
- CaltechAUTHORS:20140716-144324335
- NASA
- NAGW3337
- Created
-
2014-07-16Created from EPrint's datestamp field
- Updated
-
2021-11-10Created from EPrint's last_modified field
- Other Numbering System Name
- Lunatic Asylum Lab
- Other Numbering System Identifier
- 999