Changes

==Seismic expression==

==Seismic expression==

The following figure is a north-south seismic section through the East Breaks 160-161 intraslope minibasin, showing the location of the East Breaks 160-161 field. Production is from the ''Trim A'' and ''Glob alt'' reservoirs within the rollover anticline downthrown to the north bounding fault A′. Fault A′ splays southwest off regional fault A (Figure 4-42) (see also .<ref name=ch04r86>Schanck, J., W., Cobb, C., C., Ivey, M., L. Jr., 1988, East Breaks 160 field on the offshore Texas shelf edge: a model for deepwater exploration and development: Proceedings, 20th Annual Offshore Technology conference, p. 157–162.</ref><ref name=ch04r7>Armentrout, J., M., 1991, Paleontological constraints on depositional [[modeling]]: examples of integration of biostratigraphy and seismic stratigraphy, Pliocene–Pleistocene, Gulf of Mexico, in Weimer, P., Link, M., H., eds., Seismic Facies and Sedimentary Processes of Submarine Fans and Turbidite Systems: New York, Springer-Verlag, p. 137–170.</ref>

The following figure is a north-south seismic section through the East Breaks 160-161 intraslope minibasin, showing the location of the East Breaks 160-161 field. Production is from the ''Trim A'' and ''Glob alt'' reservoirs within the rollover anticline downthrown to the north bounding fault A′. Fault A′ splays southwest off regional fault A (Figure 4-42) (see also .<ref name=ch04r86>Schanck, J., W., Cobb, C., C., Ivey, M., L. Jr., 1988, East Breaks 160 field on the offshore Texas shelf edge: a model for deepwater exploration and development: Proceedings, 20th Annual Offshore Technology conference, p. 157–162.</ref><ref name=ch04r7>Armentrout, J., M., 1991, Paleontological constraints on depositional [[modeling]]: examples of integration of biostratigraphy and seismic stratigraphy, Pliocene–Pleistocene, Gulf of Mexico, in Weimer, P., Link, M., H., eds., Seismic Facies and Sedimentary Processes of Submarine Fans and Turbidite Systems: New York, Springer-Verlag, p. 137–170.</ref>