| Abstract: | Apparently, several pulses of salt flowed into the diapir between about 2-3 and 0.25Myr ago, and the diapir may still be active. The rising salt diapir impeded the flow of ancestral Fisher Creek, causing deposition of more than 125m of basin-fill sediments, and eventually diverted the creek down Cottonwood graben to the Dolores River about 0.25Myr ago. Onion Creek has eroded headward from the Colorado River, through both the diapir and the basin-fill sediments, and is about to capture Fisher Creek, restoring the original drainage course. -from Author |
| Genre: | Article |
| ProdID: | 70011255 |
| Citation Author: | Colman, S. M. |
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| Citation End Page: | 243 |
| Citation Issue: | 4 |
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| Citation Language: | English |
| Citation Larger Work Title: | Geology |
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| Citation Number Of Pages: | 4 |
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| Citation Search Results Text: | Influence of the Onion Creek salt diapir on the late Cenozoic history of Fisher Valley, southeastern Utah.; 1983; Article; Journal; Geology; Colman, S. M. |
| Citation Start Page: | 240 |
| Citation Volume: | 11 |
| Citation Year: | 1983 |
| Type: | citation/reference |
| Text: | Influence of the Onion Creek salt diapir on the late Cenozoic history of Fisher Valley, southeastern Utah.; 1983; Article; Journal; Geology; Colman, S. M. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sat, 1 Jan 1983 00:00 -0600 |
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