File:Sedimentary-basin-analysis fig4-43.png|{{figure number|5}}North-South seismic section through the East Breaks 160-161 field.
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[[:file:sedimentary-basin-analysis_fig4-47.png|Figure 3]] is a seismic reflection profile showing the ''Glob alt'' reservoir interval. Section A is uninterpreted; section B is interpreted. The reservoir thins southward between the top seal at the ''Glob alt'' condensed section datum and the underlying, unlabeled datum (thick black lines). The reservoir is penetrated by the 160-1 well in the faulted anticlinal trap formed by the rollover into the growth-fault complex bounding the north side of the minibasin (Figures 4-42 through 4-44). The 160-1 electric log pattern is spontaneous potential.
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[[:file:sedimentary-basin-analysis_fig4-47.png|Figure 3]] is a seismic reflection profile showing the ''Glob alt'' reservoir interval. Section A is uninterpreted; section B is interpreted. The reservoir thins southward between the top seal at the ''Glob alt'' condensed section datum and the underlying, unlabeled datum (thick black lines). The reservoir is penetrated by the 160-1 well in the faulted anticlinal trap formed by the rollover into the growth-fault complex bounding the north side of the mini basin ([[:file:sedimentary-basin-analysis_fig4-42.png|Figures 4]], [[:file:sedimentary-basin-analysis_fig4-43.png|5]], and [[:file:sedimentary-basin-analysis_fig4-44.png|2]]). The 160-1 electric log pattern is spontaneous potential.