Brannerite from the Penn Haven Junction uranium occurrence, Carbon County, Pennsylvania

Journal of Research of the U.S. Geological Survey
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Abstract

Thorium-free brannerite has been identified in Upper Devonian uraniferous sandstone from Penn Haven Junction, Carbon County, Pa. The brannerite was located by a variation of the "Lexan" technique and is associated with galena, uraninite, and clausthalite. The angular thorium-free nature of the brannerite suggests that it formed by metamorphism of uranium-saturated leucoxene. As a result of the metamorphism some uranium may be in less soluble minerals than those found in the uranium deposits of the Western United States. For this reason, in-place leaching of the uranium may be impractical.

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Publication type Article
Publication Subtype Journal Article
Title Brannerite from the Penn Haven Junction uranium occurrence, Carbon County, Pennsylvania
Series title Journal of Research of the U.S. Geological Survey
Volume 4
Issue 6
Year Published 1976
Language English
Publisher U.S. Geological Survey
Description 2 p.
First page 715
Last page 716
Country United States
State Pennsylvania
County Carbon County
Other Geospatial Penn Haven Junction
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