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file:sedimentary-basin-analysis_fig4-40.png|{{figure number|1}}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.

file:sedimentary-basin-analysis_fig4-40.png|{{figure number|1}}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.

file:sedimentary-basin-analysis_fig4-41.png|{{figure number|2}}.

file:sedimentary-basin-analysis_fig4-41.png|{{figure number|2}}Depositional strike seismic reflection profile across one of these valleys.

file:sedimentary-basin-analysis_fig4-42.png|{{figure number|3}}. Copyright: Armentrout et al. (1991); courtesy Springer-Verlag.

file:sedimentary-basin-analysis_fig4-42.png|{{figure number|3}}Structural elements that define the East Breaks 160-161 minibasin, which is bound on the north by fault A, on the east by faults B and C, and on the south by a salt-cored high. Copyright: Armentrout et al. (1991); courtesy Springer-Verlag.

file:sedimentary-basin-analysis_fig4-43.png|{{figure number|4}}See text for explanation.

file:sedimentary-basin-analysis_fig4-43.png|{{figure number|4}}North–south seismic section through the East Breaks 160-161 intraslope minibasin, showing the location of the East Breaks 160-161 field.

file:sedimentary-basin-analysis_fig4-56.png|{{figure number|5}}. Copyright: Dow et al. (1990); courtesy Gulf Coast SEPM.

file:sedimentary-basin-analysis_fig4-56.png|{{figure number|5}}North–south seismic section showing the hypothetical model for migration pathways within the East Breaks 160-161 field. Copyright: Dow et al. (1990); courtesy Gulf Coast SEPM.

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