Brannerite from the Penn Haven Junction uranium occurrence, Carbon County, Pennsylvania
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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.
Study Area
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 |
Google Analytic Metrics | Metrics page |