| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4696295 | Marine and Petroleum Geology | 2009 | 5 Pages |
Abstract
The Colgate Member of the Fox Hills Formation in Montana is an exact correlative of the Whitemud, and kaolinization of the Colgate is due to the same sea level fall from the International Boundary to central North Dakota. The age correlates to the sea level cycle marking the base of supercycle TA-1, and the short duration indicates that this sea level cycle was glacioeustatic.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
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Authors
J.F. Lerbekmo,