Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.


Science 3 February 1967:
Vol. 155. no. 3762, pp. 579 - 581
DOI: 10.1126/science.155.3762.579

Articles

Primary Oxidation Variation and Distribution of Uranium and Thorium in a Lava Flow

N. D. Watkins 1, C. W. Holmes 2, and S. E. Haggerty 3

1 Department of Geology, Florida State University, Tallahassee
2 Colgate University, Hamilton, New York
3 Royal School of Mines, Imperial College of Science and Technology, London, S.W.7, England

An Icelandic basalt lava flow has a systematic oxidation variation, formed during the initial cooling, with a resultant maximum oxidation just below the center of the lava. The ratio of thorium to uranium shows a clear dependence on this primary oxidation variation. Between-lava comparisons of thorium and uranium may be critically dependent on the position of the samples in each lava.





To Advertise     Find Products


Science. ISSN 0036-8075 (print), 1095-9203 (online)