| Abstract: | The Schwartzwalder uranium deposit was formed during Laramide uplift from groundwaters enriched in ore elements leached from the Proterozoic metavolcanic and metasedimentary host-rocks. Contributions from an unseen intrusive or from Phanerozoic sedimentary rocks are inconsistent with the data. Two stages of alteration and three stages of vein mineralization are related to evolution of CO2, in part episodically.-G.J.N. |
| Genre: | Article |
| ProdID: | 70014867 |
| Citation Author: | Wallace, A. R.; Whelan, J. F. |
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| Citation End Page: | 888 |
| Citation Issue: | 4 |
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| Citation Language: | English |
| Citation Larger Work Title: | Economic Geology |
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| Citation Number Of Pages: | 17 |
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| Citation Search Results Text: | The Schwarzwalder uranium deposit, III: alteration, vein mineralization, light stable isotopes, and genesis of the deposit.; 1986; Article; Journal; Economic Geology; Wallace, A. R.; Whelan, J. F. |
| Citation Start Page: | 872 |
| Citation Volume: | 81 |
| Citation Year: | 1986 |
| Type: | citation/reference |
| Text: | The Schwarzwalder uranium deposit, III: alteration, vein mineralization, light stable isotopes, and genesis of the deposit.; 1986; Article; Journal; Economic Geology; Wallace, A. R.; Whelan, J. F. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Wed, 1 Jan 1986 00:00 -0600 |
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