Geochemistry of water in aquifers and confining units of the Northern Great Plains in parts of Montana, North Dakota, South Dakota, and Wyoming
Professional Paper
1402-F
By: J.F. Busby, B. A. Kimball, J. S. Downey, and K. D. Peter
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Abstract
The geochemistry of water in five aquifers and two confining units in the Williston Basin of the Northern Great Plains is similar and is controlled by halite dissolution. In areas outside the Williston Basin ground-water is fresh and controlled by the solution chemistry of carbonate and sulfate minerals.
Suggested Citation
Busby, J., Kimball, B.A., Downey, J.S., Peter, K.D., 1995, Geochemistry of water in aquifers and confining units of the Northern Great Plains in parts of Montana, North Dakota, South Dakota, and Wyoming: U.S. Geological Survey Professional Paper 1402, p. F1-F146; 2 plates in pocket, https://doi.org/10.3133/pp1402F.
ISSN: 2330-7102 (online)
| Publication type | Report |
|---|---|
| Publication Subtype | USGS Numbered Series |
| Title | Geochemistry of water in aquifers and confining units of the Northern Great Plains in parts of Montana, North Dakota, South Dakota, and Wyoming |
| Series title | Professional Paper |
| Series number | 1402 |
| Chapter | F |
| DOI | 10.3133/pp1402F |
| Year Published | 1995 |
| Language | ENGLISH |
| Description | p. F1-F146; 2 plates in pocket |