| Abstract: | Tabular-type uranium deposits occur as tabular, originally subhorizontal bodies entirely within reduced fluvial sandstones of Late Silurian age or younger. This paper proposes that belts of tabular-type uranium deposits formed in areas of mixed local and regional groundwater discharge shortly after deposition of the host sediments. The general characteristics of tabular-type uranium deposits indicate that their essential feature was the formation at a density-stratified ground-water interface in areas of local and regional ground-water discharge. Reconstruction of the paleohydrogeology is the key to understanding the formation of these deposits. Geologic ground-water controls that favor discharge, such as the pinch-out of major aquifers, are also favorable for uranium ore. The combination of topographic and geologic features that both cause discharge is most favorable for ore deposition. -from Author |
| Genre: | Article |
| ProdID: | 70016826 |
| Citation Author: | Sanford, R. F. |
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| Citation End Page: | 2055 |
| Citation Issue: | 8 |
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| Citation Language: | English |
| Citation Larger Work Title: | Economic Geology |
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| Citation Number Of Pages: | 15 |
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| Citation Search Results Text: | A new model for tabular-type uranium deposits; 1992; Article; Journal; Economic Geology; Sanford, R. F. |
| Citation Start Page: | 2041 |
| Citation Volume: | 87 |
| Citation Year: | 1992 |
| Type: | citation/reference |
| Text: | A new model for tabular-type uranium deposits; 1992; Article; Journal; Economic Geology; Sanford, R. F. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Wed, 1 Jan 1992 00:00 -0600 |
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