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.
American Journal of Science
By: C. Gene Whitney and H. R. Northrop
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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
Suggested Citation
Whitney, C.G., Northrop, H.R., 1987, 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.: American Journal of Science, v. 287, no. 4, p. 353-382, https://doi.org/10.2475/ajs.287.4.353.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | 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. |
| Series title | American Journal of Science |
| DOI | 10.2475/ajs.287.4.353 |
| Volume | 287 |
| Issue | 4 |
| Year Published | 1987 |
| Language | English |
| Publisher | American Journal of Science |
| Description | 30 p. |
| First page | 353 |
| Last page | 382 |