Changes

}}

}}

==Method==

==Method==

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file:sedimentary-basin-analysis_fig4-53.png|{{figure number|1}}32-layer, 1-D mathematical model constructed for the East Breaks 160-161 minibasin. After Dow et al.<ref name=ch04r29 /> &copy; Gulf Coast SEPM.

file:sedimentary-basin-analysis_fig4-53.png|{{figure number|1}}32-layer, 1-D mathematical model constructed for the East Breaks 160-161 minibasin. After Dow et al.<ref name=ch04r29 /> &copy; Gulf Coast SEPM.

sedimentary-basin-analysis_fig4-42.png|{{figure number|2}}Structural elements that define East Breaks 160-161 minibasin. From Armentrout et al.<ref name=Armentroutetal_1991>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.

sedimentary-basin-analysis_fig4-42.png|{{figure number|2}}Structural elements that define East Breaks 160-161 minibasin. From Armentrout et al.<ref name=Armentroutetal_1991>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.