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The Frontier Formation and equivalent sediments were deposited in, or on the margins of, a shallow sea which covered the Western Interior region during the Cenomanian and Turonian stages of the Late Cretaceous. Most of the oil production at the Salt Creek field is from lenticular sand bodies in the Frontier. These sand bodies are interpreted as offshore bars.
This record provided courtesy of AGI/GeoRef.
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K. Lee, M. R. Gani, G. A. McMechan, J. P. Bhattacharya, S. L. Nyman, and X. Zeng Three-dimensional facies architecture and three-dimensional calcite concretion distributions in a tide-influenced delta front, Wall Creek Member, Frontier Formation, Wyoming AAPG Bulletin, February 1, 2007; 91(2): 191 - 214. [Abstract] [Full Text] [PDF]
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K. Lee, X. Zeng, G. A. McMechan, C. D. Howell Jr., J. P. Bhattacharya, F. Marcy, and C. Olariu A ground-penetrating radar survey of a delta-front reservoir analog in the Wall Creek Member, Frontier Formation, Wyoming AAPG Bulletin, September 1, 2005; 89(9): 1139 - 1155. [Abstract] [Full Text] [PDF]
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Lowstand Deltas in the Frontier Formation, Powder River Basin, Wyoming: Implications for Sequence Stratigraphic Models AAPG Bulletin, February 1, 2001; 85(2): 261 - 294.
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