Please use this identifier to cite or link to this item: http://hdl.handle.net/1811/23570
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| V093N4_083.pdf | 2.920Mb |
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| Title: | Depositional Environments of the Pictured Cliffs Sandstone, Late Cretaceous, near Durango, Colorado |
| Creators: | Tokar, Frank J., Jr.; Evans, James E. |
| Issue Date: | 1993-09 |
| Citation: | The Ohio Journal of Science. v93, n4 (September, 1993), 83-89 |
| Abstract: | The Pictured Cliffs Sandstone was deposited in the northwestern part of the San Juan Basin (Colorado-New Mexico) during the last regression of the Cretaceous Interior Seaway. The unit is generally interpreted as deltaic or marginal marine; however, outcrops near Durango, CO, consist of repetitive sequences of hummocky stratified (HS) sandstone. Each HS sequence consists of a scoured surface overlain by hummocky-stratified, fine-grained sandstone 20-50 cm thick, overlain by ripple- to planarlaminated, bioturbated, very fine-grained sandstone to mudstone. Amalgamated HS sequences are as much as 7 m thick. |
| URI: | http://hdl.handle.net/1811/23570 |
| ISSN: | 0030-0950 |
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