Laboratory Constraints and Models of Pressure, Hydrate, and Stability in Shallow Mississippi Canyon Sediments (MC 855), Deepwater Gulf of Mexico

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Fluid pressure and stress history influence hydrate and slope stability. Shallow water flows (SWF) document shallow (<1000 m below seafloor, mbsf) overpressure in the Gulf of Mexico, but pore pressure observations in shallow silt/clay are rare.

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Dugan, Brandon1, Jack Germaine2, William Winters1, Peter Flemings3 ---- Roy Long, Laboratory Constraints and Models of Pressure, Hydrate, and Stability in Shallow Mississippi Canyon Sediments (MC 855), Deepwater Gulf of Mexico, 2016-09-29, https://edx.netl.doe.gov/dataset/laboratory-constraints-and-models-of-pressure-hydrate-and-stability-in-shallow-mississippi-canyon

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Last Updated	September 29, 2016, 15:05 (LMT)
Created	September 29, 2016, 15:05 (LMT)
Citation	Dugan, Brandon1, Jack Germaine2, William Winters1, Peter Flemings3 ---- Roy Long, Laboratory Constraints and Models of Pressure, Hydrate, and Stability in Shallow Mississippi Canyon Sediments (MC 855), Deepwater Gulf of Mexico, 2016-09-29, https://edx.netl.doe.gov/dataset/laboratory-constraints-and-models-of-pressure-hydrate-and-stability-in-shallow-mississippi-canyon
Netl Product	yes
Poc Email	Roy.long@netl.doe.gov
Point Of Contact	Roy Long
Program Or Project	KMD
Publication Date	2004-4-21

Laboratory Constraints and Models of Pressure, Hydrate, and Stability in Shallow Mississippi Canyon Sediments (MC 855), Deepwater Gulf of Mexico

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