| Abstract: | The Westwater Canyon Member of the Upper Jurassic Morrison Formation is a relatively homogeneous, hydrologically continuous 100-m-thick sequence of massive fluvial sandstone, bounded above and below by relatively heterogeneous, hydrologically discontinuous units and has served as a primary conduit for fluids within this stratigraphic interval. Patterns of mineral-fluid reactions suggest a basinwide hydrologic regime in which warm, evolved fluids migrated up-dip from the center of the basin under the influence of a regional hydraulic head. -from Authors |
| Genre: | Article |
| ProdID: | 70014250 |
| Citation Author: | Whitney, G.; Northrop; H. R. |
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| Citation End Page: | 382 |
| Citation Issue: | 4 |
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| Citation Language: | English |
| Citation Larger Work Title: | American Journal of Science |
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| Citation Number Of Pages: | 30 |
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| Citation Publisher: | American Journal of Science |
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| Citation Search Results Text: | Diagenesis and fluid flow in the San Juan Basin, New Mexico - regional zonation in the mineralogy and stable isotope composition of clay minerals in sandstone.; 1987; Article; Journal; American Journal of Science; Whitney, G.; Northrop; H. R. |
| Citation Start Page: | 353 |
| Citation Volume: | 287 |
| Citation Year: | 1987 |
| Type: | citation/reference |
| Text: | Diagenesis and fluid flow in the San Juan Basin, New Mexico - regional zonation in the mineralogy and stable isotope composition of clay minerals in sandstone.; 1987; Article; Journal; American Journal of Science; Whitney, G.; Northrop; H. R. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| URL (DIGITAL OBJECT IDENTIFIER): | http://dx.doi.org/doi: 10.2475/ajs.287.4.353 |
| Date Other: | Thu, 1 Jan 1987 00:00 -0600 |
| Publisher: | American Journal of Science |
