Abstract
THE ages of lead of Earth and of meteorites are commonly based on the assumption that when these bodies were formed they contained lead of the same isotopic composition1,2. The present differences in the isotopic compositions of the lead in meteorites and also between common terrestrial lead and meteorite lead are due to radiogenic contributions from uranium and thorium since that time.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
Similar content being viewed by others
References
Patterson, C., Geochim. et Cosmochim. Acta, 10, 230 (1956).
Masuda, A., Geochim. et Cosmochim. Acta, 13, 143 (1958).
Starik, I. E., Sobotovich, E. V., Lovtsyus, G. P., Shats, M. M., and Lovtsyus, A. V., Sov. Phys. (Doklady), 134, 555 (1960).
Patterson, C., Brown, H., Tilton, G., and Inghram, M., Phys. Rev., 92, 1234 (1953).
Reed, G. W., Hamaguchi, H., and Turkevich, A., Geochim. et Cosmo-chim. Acta, 13, 248 (1958).
König, H., and Wänke, H., Z. Naturforsch., 14, a, 866 (1959).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
FIREMAN, E., FISHER, D. Uranium in the Sikhote-Alin Meteorite and its Relation to the Lead Method of Age Determination. Nature 192, 644–645 (1961). https://doi.org/10.1038/192644a0
Issue Date:
DOI: https://doi.org/10.1038/192644a0
This article is cited by
-
The radioanalytical bibliography of USA (1936–1977)
Journal of Radioanalytical Chemistry (1981)
Comments
By submitting a comment you agree to abide by our Terms and Community Guidelines. If you find something abusive or that does not comply with our terms or guidelines please flag it as inappropriate.