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==Depositional model summary==
 
==Depositional model summary==
All the observations made from seismic profiles, isochron maps, seismic facies maps, well-log cross sections, cuttings, biofacies, and cores have been used to construct a depositional model for the ''Glob alt'' cycle of the High Island-East Breaks 160-161 minibasin. This model incorporates far-traveled gravity-flow sands that accumulated in a depositional thick, filling an upper-slope salt-withdrawal sea-floor low. Laterally shifting fan lobes resulted in a complex architectural framework ([[:file:sedimentary-basin-analysis_fig4-48.png|Figure 6]]). The profile pattern ([[:file:sedimentary-basin-analysis_fig4-47.png|Figure 3]]), combined with the mapped isochron and seismic facies pattern of [[:file:sedimentary-basin-analysis_fig4-46.png|Figure 1]] and the net sandstone patterns of [[:file:sedimentary-basin-analysis_fig4-49.png|Figure 7]], have been interpreted as minibasin basin-floor sheet sandstones, amalgamated-lobe sandstones, and leveed-channel sandstones by Armentrout et al.<ref name=ch04r7 />) (see [[:file:sedimentary-basin-analysis_fig4-48.png|Figure 6]]).
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All the observations made from seismic profiles, [[isochron]] maps, seismic facies maps, well-log cross sections, cuttings, biofacies, and cores have been used to construct a depositional model for the ''Glob alt'' cycle of the High Island-East Breaks 160-161 minibasin. This model incorporates far-traveled gravity-flow sands that accumulated in a depositional thick, filling an upper-slope salt-withdrawal sea-floor low. Laterally shifting fan lobes resulted in a complex architectural framework ([[:file:sedimentary-basin-analysis_fig4-48.png|Figure 6]]). The profile pattern ([[:file:sedimentary-basin-analysis_fig4-47.png|Figure 3]]), combined with the mapped isochron and seismic facies pattern of [[:file:sedimentary-basin-analysis_fig4-46.png|Figure 1]] and the net sandstone patterns of [[:file:sedimentary-basin-analysis_fig4-49.png|Figure 7]], have been interpreted as minibasin basin-floor sheet sandstones, amalgamated-lobe sandstones, and leveed-channel sandstones by Armentrout et al.<ref name=ch04r7 />) (see [[:file:sedimentary-basin-analysis_fig4-48.png|Figure 6]]).
    
==Depositional model diagram==
 
==Depositional model diagram==
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