The Eocene Green River Formation was deposited in two large Eocene saline lakes, Lake Uinta in the Uinta and Piceance Basins and Lake Gosiute in the Greater Green River Basin. Here we will discuss mass-movement deposits in just the Piceance Basin part of Lake Uinta.
Citation Information
| Publication Year | 2015 |
|---|---|
| Title | Mass-movement deposits in the lacustrine Eocene Green River Formation, Piceance Basin, western Colorado |
| DOI | 10.3133/ofr20151044 |
| Authors | Ronald C. Johnson, Justin E. Birdwell, Michael E. Brownfield, Tracey J. Mercier |
| Publication Type | Report |
| Publication Subtype | USGS Numbered Series |
| Series Title | Open-File Report |
| Series Number | 2015-1044 |
| Index ID | ofr20151044 |
| Record Source | USGS Publications Warehouse |
| USGS Organization | Central Energy Resources Science Center |
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Ronald C Johnson (Former Employee)
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