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Economic Geology; May 1965; v. 60; no. 3; p. 477-484
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Radioactive disequilibrium studies in sandstone, Powder River Basin, Wyoming, and Slick Rock District, Colorado

J. N. Rosholt, M. Tatsumoto, and J. R. Dooley

Relationship between uranium daughters Th-230 and Pa-231 and parent uranium indicates that uranium has migrated from concave toward convex boundary in rolls. U-234 has been preferentially leached from Powder River basin ore for at least 100,000 years.

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JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
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