Published July 27, 1998
| Published
Journal Article
Open
Measurement of gas-phase species during Langmuir evaporation of forsterite
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
- NAGW3337
- NASA
- 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