The End of Paleogene White River Group Deposition in Wyoming and Nebraska, USA: A Distal Record of the Collapse and Emplacement of the Markagunt Gravity Slide at 23 Ma
The late Paleogene White River Group is a post-Laramide sedimentary succession that occurs within Laramide intermontane basins and atop some basement-cored uplifts. Detrital zircon U-Pb dates of tuffaceous sandstones from the uppermost White River Group in eastern Wyoming and western Nebraska yield...
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| Médium: | Artigo |
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MDPI AG
2026-04-01
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| Edice: | Geosciences |
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| On-line přístup: | https://www.mdpi.com/2076-3263/16/5/174 |
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