Sedimentary Facies and Correlation of the Gallup Sandstone and Associated Formations, Northwestern New Mexico

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The Gallup Sandstone of upper Cretaceous is a regressive clastic wedge that prograded about halfway across the San Juan Basin from a probable source in southwestern Arizona.

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C.M.Molenaar ---- Roy Long, Sedimentary Facies and Correlation of the Gallup Sandstone and Associated Formations, Northwestern New Mexico, 2016-09-29, https://edx.netl.doe.gov/dataset/sedimentary-facies-and-correlation-of-the-gallup-sandstone-and-associated-formations-northwestern

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Field	Value
Last Updated	September 29, 2016, 14:35 (LMT)
Created	September 29, 2016, 14:35 (LMT)
Citation	C.M.Molenaar ---- Roy Long, Sedimentary Facies and Correlation of the Gallup Sandstone and Associated Formations, Northwestern New Mexico, 2016-09-29, https://edx.netl.doe.gov/dataset/sedimentary-facies-and-correlation-of-the-gallup-sandstone-and-associated-formations-northwestern
Netl Product	yes
Poc Email	Roy.long@netl.doe.gov
Point Of Contact	Roy Long
Program Or Project	KMD

Sedimentary Facies and Correlation of the Gallup Sandstone and Associated Formations, Northwestern New Mexico

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