Depositional patterns and stratal relationships on the distal margins of a foreland basin: Middle Jurassic Gypsum Spring and lower Sundance Formations, Bighorn Basin, WY
Depositional patterns and stratal relationships in the Middle Jurassic Gypsum Spring and lower Sundance Formations were influenced by a combination of paleotopographic highs and eustatic changes in the eastern Bighorn Basin. Most of these highs are of tectonic origin related to an island arc collisi...
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| Format: | Others |
| Language: | en_US |
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Wichita State University
2013
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| Online Access: | http://hdl.handle.net/10057/5595 |