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sedimentary-basin-analysis_fig4-29.png|{{figure number|3}}Biofacies maps of the study area in the Gulf of Mexico. After Armentrout;<ref name=ch04r7 /><ref>Armentrout, J. M., 1996, High-resolution sequence biostratigraphy: examples from the Gulf of Mexico Plio–Pleistocene, in J. Howell and J. Aiken, eds., High Resolution Sequence Stratigraphy: Innovations and Applications: The Geological Society of London Special Publication 104, p. 65–86.</ref> courtesy Springer-Verlag, Geological Society of London.

sedimentary-basin-analysis_fig4-29.png|{{figure number|3}}Biofacies maps of the study area in the Gulf of Mexico. After Armentrout;<ref name=ch04r7 /><ref>Armentrout, J. M., 1996, High-resolution sequence biostratigraphy: examples from the Gulf of Mexico Plio–Pleistocene, in J. Howell and J. Aiken, eds., High Resolution Sequence Stratigraphy: Innovations and Applications: The Geological Society of London Special Publication 104, p. 65–86.</ref> courtesy Springer-Verlag, Geological Society of London.

sedimentary-basin-analysis_fig4-40.png|{{figure number|4}}Relationship between 23 fields in the High Island–East Breaks depocenter that produce from the ''Glob alt'' sandstones and the ''Glob alt sandstone'' 200-ft (60-m) isopach.

sedimentary-basin-analysis_fig4-40.png|{{figure number|4}}Relationship between 23 fields in the High Island–East Breaks [[depocenter]] that produce from the ''Glob alt'' sandstones and the ''Glob alt sandstone'' 200-ft (60-m) isopach.

sedimentary-basin-analysis_fig4-33.png|{{figure number|5}}Rock accumulation rates for the Green Canyon 166 No. 1 well as a histogram (lower graph) and as a set of burial history curves (upper graph). After Piggott and Pulham;<ref>Piggott, N., and A. Pulham, 1993, Sedimentation rate as the control on hydrocarbon sourcing, generation, and migration in the deepwater Gulf of Mexico: Proceedings, Gulf Coast Section SEPM 14th Annual Research Conference, p. 179–191.</ref> courtesy Gulf Coast SEPM.

sedimentary-basin-analysis_fig4-33.png|{{figure number|5}}Rock accumulation rates for the Green Canyon 166 No. 1 well as a histogram (lower graph) and as a set of burial history curves (upper graph). After Piggott and Pulham;<ref>Piggott, N., and A. Pulham, 1993, Sedimentation rate as the control on hydrocarbon sourcing, generation, and migration in the deepwater Gulf of Mexico: Proceedings, Gulf Coast Section SEPM 14th Annual Research Conference, p. 179–191.</ref> courtesy Gulf Coast SEPM.

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