The Frontier Formation and mid- Cretaceous orogeny in the foreland of southwestern Wyoming
Mountain Geologist
By: E. Allen Merewether
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Abstract
Tectonism in SW Wyoming and adjoining areas, and fluctuations of sea level in the central USA during the mid-Cretaceous are represented by the regional stratigraphy of the Frontier Formation. The Frontier consists mainly of clastic rocks that were deposited in marine and nonmarine environments during latest Albian, Cenomanian, Turonian, and Coniacian time. -from Author
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | The Frontier Formation and mid- Cretaceous orogeny in the foreland of southwestern Wyoming |
| Series title | Mountain Geologist |
| Volume | 20 |
| Issue | 4 |
| Year Published | 1983 |
| Language | English |
| Publisher | Rocky Mountain Association of Geologists |
| Contributing office(s) | Central Energy Resources Science Center |
| Description | 18 p. |
| First page | 121 |
| Last page | 138 |
| Country | United States |
| Other Geospatial | Southwestern Wyoming |
| Google Analytic Metrics | Metrics page |