Changes

==Effect on reservoir deposition==

==Effect on reservoir deposition==

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sedimentary-basin-analysis_fig4-29.png|{{figure number|3}}

sedimentary-basin-analysis_fig4-29.png|{{figure number|3}}Biofacies maps of the study area in the Gulf of Mexico. After Armentrout (1991, 1996); 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}}

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 (1993); courtesy Gulf Coast SEPM.

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