| 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 |
| Genre: | Article |
| ProdID: | 70012070 |
| Citation Author: | Merewether, E. A. |
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| Citation End Page: | 138 |
| Citation Issue: | 4 |
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| Citation Language: | English |
| Citation Larger Work Title: | Mountain Geologist |
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| Citation Number Of Pages: | 18 |
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| Citation Search Results Text: | The Frontier Formation and mid- Cretaceous orogeny in the foreland of southwestern Wyoming.; 1983; Article; Journal; Mountain Geologist; Merewether, E. A. |
| Citation Start Page: | 121 |
| Citation Volume: | 20 |
| Citation Year: | 1983 |
| Type: | citation/reference |
| Text: | The Frontier Formation and mid- Cretaceous orogeny in the foreland of southwestern Wyoming.; 1983; Article; Journal; Mountain Geologist; Merewether, E. A. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sat, 1 Jan 1983 00:00 -0600 |
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