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Published July 1992 | Version 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

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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.

Additional Information

© 1992 Meteoritical Society. This work was supported by NASA, Grant NAG 9-43. Contribution No. 779.

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Published - 1992Metic__27__212C.pdf

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42305
Resolver ID
CaltechAUTHORS:20131107-131452047

Related works

Describes
http://adsabs.harvard.edu/abs/1992Metic..27..212C (URL)

Funding

NASA
NAG 9-43

Dates

Created
2013-11-08
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Updated
2020-03-09
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Lunatic Asylum Lab
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779