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Economic Geology; July 1964; v. 59; no. 4; p. 570-585
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Isotopic fractionation of uranium related to roll features in sandstone, Shirley Basin, Wyoming

J. N. Rosholt, E. N. Harshman, W. R. Shields, and E. L. Garner

Permeable ore sands are deficient in U-234, whereas altered sands adjoining are enriched. U-234 formed in situ from U-238 after ore deposition is unstable chemically because it is a disintegration product, and ground water movements can produce fractionation by acting selectively on this new U-234.

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JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
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