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[[:file:sedimentary-basin-analysis_fig4-36.png|Figure 1]] is the interpreted [[Seismic facies mapping|seismic facies]] pattern for part of one [[Seismic interpretation|seismic reflection profile]] down the axis of the High Island-East Breaks [[depocenter]].<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> This is the same seismic profile shown in [[:file:sedimentary-basin-analysis_fig4-27.png|Figure 2]].

[[:file:sedimentary-basin-analysis_fig4-36.png|Figure 1]] is the interpreted [http://wiki.seg.org/wiki/Dictionary:Seismic_facies seismic facies] pattern for part of one [[Seismic interpretation|seismic reflection profile]] down the axis of the High Island-East Breaks [[depocenter]].<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> This is the same seismic profile shown in [[:file:sedimentary-basin-analysis_fig4-27.png|Figure 2]].

Each [[Well_log_sequence_analysis#Parasequence_stacking_patterns|prograding]] [http://unterm.un.org/DGAACS/unterm.nsf/8fa942046ff7601c85256983007ca4d8/6d701a3f58b3c00d852570d70052c711?OpenDocument clinoform] contains a rotated package of chaotic facies within the upper and steepest part of the clinoform facies and basinward of the tabular facies. The clinoform facies is [http://www.glossary.oilfield.slb.com/en/Terms.aspx?LookIn=term%20name&filter=onlap onlapped] by parallel, moderate-amplitude, onlapping reflections of the onlap-fill facies, which are subsequently [http://www.glossary.oilfield.slb.com/en/Terms/d/downlap.aspx downlapped] onto by the next overlying prograding clinoform. In a broader sense, the drape facies below these clinoforms and the ''Glob N'' datum represent basinal deposits; the clinoform and onlapping-fill facies represent [http://www.thefreedictionary.com/continental+slope slope] deposits; and the overlying tabular facies above the clinoforms and the ''Glob M'' datum represent [http://education.nationalgeographic.com/education/encyclopedia/continental-shelf/?ar_a=1 shelf] deposits—all part of a basin-filling succession.

Each [[Well_log_sequence_analysis#Parasequence_stacking_patterns|prograding]] [http://unterm.un.org/DGAACS/unterm.nsf/8fa942046ff7601c85256983007ca4d8/6d701a3f58b3c00d852570d70052c711?OpenDocument clinoform] contains a rotated package of chaotic facies within the upper and steepest part of the clinoform facies and basinward of the tabular facies. The clinoform facies is [http://www.glossary.oilfield.slb.com/en/Terms.aspx?LookIn=term%20name&filter=onlap onlapped] by parallel, moderate-amplitude, onlapping reflections of the onlap-fill facies, which are subsequently [http://www.glossary.oilfield.slb.com/en/Terms/d/downlap.aspx downlapped] onto by the next overlying prograding clinoform. In a broader sense, the drape facies below these clinoforms and the ''Glob N'' datum represent basinal deposits; the clinoform and onlapping-fill facies represent [http://www.thefreedictionary.com/continental+slope slope] deposits; and the overlying tabular facies above the clinoforms and the ''Glob M'' datum represent [http://education.nationalgeographic.com/education/encyclopedia/continental-shelf/?ar_a=1 shelf] deposits—all part of a basin-filling succession.