Changes

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}}Depositional strike seismic reflection profile across one of these valleys.

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}}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.;<ref name=ch04r7 /> 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.;<ref name=Armetal1991>Armentrout, J. M., S. J. Malacek, P. Braithwaite, and C. R. Beeman, 1991, Seismic facies of slope basin turbidite reservoirs, East Breaks 160-161 field: Pliocene–Pleistocene, northwestern Gulf of Mexico, in P. Weimer and M. J. Link, eds., Seismic Facies and Sedimentary Processes of Submarine Fans and Turbidite Systems: New York, Springer-Verlag, p. 223–239.</ref> courtesy Springer-Verlag.

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_fig4-43.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}}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.

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.