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Isotopic Analysis of Os and Re with negative thermal ion mass spectrometry and application to the age and evolution of iron meteorites

Creaser, R. A. and Papanastassiou, D. A. and Wasserburg, G. J. (1992) Isotopic Analysis of Os and Re with negative thermal ion mass spectrometry and application to the age and evolution of iron meteorites. Meteoritics, 27 (3). p. 212. ISSN 0026-1114. https://resolver.caltech.edu/CaltechAUTHORS:20131107-131452047

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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.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://adsabs.harvard.edu/abs/1992Metic..27..212CADSArticle
ORCID:
AuthorORCID
Wasserburg, G. J.0000-0002-7957-8029
Additional Information:© 1992 Meteoritical Society. This work was supported by NASA, Grant NAG 9-43. Contribution No. 779.
Funders:
Funding AgencyGrant Number
NASANAG 9-43
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Lunatic Asylum Lab779
Issue or Number:3
Record Number:CaltechAUTHORS:20131107-131452047
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20131107-131452047
Official Citation:Isotopic Analysis of OS and RE with Negative Thermal Ion Mass Spectrometry and Application to the Age and Evolution of Iron Meteorites Creaser, R. A.; Papanastassiou, D. A.; Wasserburg, G. J. Meteoritics, vol. 27, no. 3, volume 27, page 212 Publication Date: 07/1992
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:42305
Collection:CaltechAUTHORS
Deposited By: Ruth Sustaita
Deposited On:08 Nov 2013 15:41
Last Modified:09 Mar 2020 13:19

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