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==Sandbody geometries==
 
==Sandbody geometries==
 
<gallery>
 
<gallery>
file:sedimentary-basin-analysis_fig4-40.png|{{figure number|1}}See text for explanation.
+
file:sedimentary-basin-analysis_fig4-40.png|{{figure number|2}}See text for explanation.
file:sedimentary-basin-analysis_fig4-49.png|{{figure number|2}}See text for explanation.
+
file:sedimentary-basin-analysis_fig4-49.png|{{figure number|3}}See text for explanation.
file:sedimentary-basin-analysis_fig4-57.png|{{figure number|3}}See text for explanation.
+
file:sedimentary-basin-analysis_fig4-57.png|{{figure number|4}}See text for explanation.
 
</gallery>
 
</gallery>
   −
The gravity-flow sandstone reservoirs within the field were transported from the north, southward into the East Breaks 160-161 mini basin ([[:file:sedimentary-basin-analysis_fig4-40.png|Figure 1]]), where the mapped pattern of the ''Glob alt'' sandstones show elongate and lobate north-to-south geometries ([[:file:sedimentary-basin-analysis_fig4-49.png|Figure 2]]). These north-to-south depositional geometries are draped over the east–west down-to-the-north rollover anticline, resulting in a seismic reflection amplitude pattern that shows north-to-south flank structural downdip termination ([[:file:sedimentary-basin-analysis_fig4-57.png|Figure 3C]]). East-to-west reflection amplitude termination is stratigraphically controlled by sand distribution. This petroleum-associated reflection amplitude pattern is in contrast to that for sheet sands that would drape over the entire structure and show four-way downdip structural termination of seismic reflection ([[:file:sedimentary-basin-analysis_fig4-57.png|Figure 3D]]).
+
The gravity-flow sandstone reservoirs within the field were transported from the north, southward into the East Breaks 160-161 mini basin ([[:file:sedimentary-basin-analysis_fig4-40.png|Figure 2]]), where the mapped pattern of the ''Glob alt'' sandstones show elongate and lobate north-to-south geometries ([[:file:sedimentary-basin-analysis_fig4-49.png|Figure 3]]). These north-to-south depositional geometries are draped over the east–west down-to-the-north rollover anticline, resulting in a seismic reflection amplitude pattern that shows north-to-south flank structural downdip termination ([[:file:sedimentary-basin-analysis_fig4-57.png|Figure 4C]]). East-to-west reflection amplitude termination is stratigraphically controlled by sand distribution. This petroleum-associated reflection amplitude pattern is in contrast to that for sheet sands that would drape over the entire structure and show four-way downdip structural termination of seismic reflection ([[:file:sedimentary-basin-analysis_fig4-57.png|Figure 4D]]).
    
==Tying seismic to well data==
 
==Tying seismic to well data==

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