| Abstract: | The ratio of ground-water outflow to inflow (flux ratio) in hydrologically open basins is as important in determining the mineralogy and thicknesses of evaporite deposits as the solute composition of the inflow water. Attainment of steady state flux ratios permits large thicknesses of two or three minerals to form rather than thin veneers of many minerals. -from Authors |
| Genre: | Article |
| ProdID: | 70015875 |
| Citation Author: | Wood, W. W.; Sanford, W. E. |
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| Citation End Page: | 1235 |
| Citation Issue: | 6 |
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| Citation Language: | English |
| Citation Larger Work Title: | Economic Geology |
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| Citation Number Of Pages: | 10 |
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| Citation Search Results Text: | Ground-water control of evaporite deposition; 1990; Article; Journal; Economic Geology; Wood, W. W.; Sanford, W. E. |
| Citation Start Page: | 1226 |
| Citation Volume: | 85 |
| Citation Year: | 1990 |
| Type: | citation/reference |
| Text: | Ground-water control of evaporite deposition; 1990; Article; Journal; Economic Geology; Wood, W. W.; Sanford, W. E. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Mon, 1 Jan 1990 00:00 -0600 |
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