Published July 1992
| Published
Journal Article
Open
Isotopic Analysis of Os and Re with negative thermal ion mass spectrometry and application to the age and evolution of iron meteorites
Abstract
The ^(187)Re-^(187)Os isotope system has long been recognized as a method by which the age of iron meteorites can be directly determined (Herr et al., 1961). Pioneering work by Luck and Allègre (1983) established a whole-rock isochron for iron meteorites and the results were used to determine indirectly the half-life of ^(187)Re.
Additional Information
© 1992 Meteoritical Society. This work was supported by NASA, Grant NAG 9-43. Contribution No. 779.Attached Files
Published - 1992Metic__27__212C.pdf
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Additional details
- Eprint ID
- 42305
- Resolver ID
- CaltechAUTHORS:20131107-131452047
- NAG 9-43
- NASA
- Created
-
2013-11-08Created from EPrint's datestamp field
- Updated
-
2020-03-09Created from EPrint's last_modified field
- Other Numbering System Name
- Lunatic Asylum Lab
- Other Numbering System Identifier
- 779