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.