Wasserburg, G. J. and Hayden, R. J. (1955) Time Interval between Nucleogenesis and the Formation of Meteorites. Nature, 176 (4472). pp. 130-131. ISSN 0028-0836. doi:10.1038/176130b0. https://resolver.caltech.edu/CaltechAUTHORS:20221129-216858600.1
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Abstract
While determining the radiogenic argon-40 content of the Beardsley chondritic meteorite, a mass spectrometric search for xenon-129 produced by decay of iodine-129 was made. The total amount of xenon which was observed was 5 × 10⁻⁹ c.c. (s.t.p.) from a 29.86-gm. meteorite sample. Within the limits of experimental error, this xenon had a normal isotopic composition. The ratio of xenon to argon-36 was in essential agreement with that found in air, indicating that this xenon was due to atmospheric contamination. Since a 30 per cent increase in the abundance of xenon-129 over that observed in normal xenon would have been observable, this indicates that radiogenic xenon-129 was present in this meteorite to less than 1.3 × 10⁻¹¹ c.c. (s.t.p.)/gm. H. E. Suess and M. G. Inghram (personal communication) have suggested that if the meteorites had been formed soon after the formation of the elements, they would contain an excess of xenon-129 due to decay of iodine-129.
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| Additional Information: | We thank Prof. M. G. Inghram and Prof. H. C. Urey for several stimulating discussions. This work was performed in part under the auspices of the U.S. Atomic Energy Commission. | |||||||||
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| Issue or Number: | 4472 | |||||||||
| DOI: | 10.1038/176130b0 | |||||||||
| Record Number: | CaltechAUTHORS:20221129-216858600.1 | |||||||||
| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20221129-216858600.1 | |||||||||
| Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. | |||||||||
| ID Code: | 118096 | |||||||||
| Collection: | CaltechAUTHORS | |||||||||
| Deposited By: | Tony Diaz | |||||||||
| Deposited On: | 07 Dec 2022 19:04 | |||||||||
| Last Modified: | 07 Dec 2022 19:04 |
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