Changes

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.

Associated [[Foraminifera|foraminiferal]] [[Fossil assemblage|biofacies]] shown in [[:file:sedimentary-basin-analysis_fig4-27.png|Figure 2]] and [[:file:sedimentary-basin-analysis_fig4-29.png|Figure 3]] support this analysis. The ''Glob alt'' sequence is the fourth clinoform from the right, the fourth-most basinward of five oblique clinoforms that [http://homepage.ufp.pt/biblioteca/Seismic/Pages/Page22.htm toplap] along a common horizon. Superjacent clinoforms show progressively more [http://www.merriam-webster.com/dictionary/topset%20beds topset] deposition forming sigmoidal clinoforms, suggesting relative rise of sea level (with consistent widespread increase in accommodation space). Observations of [http://wiki.seg.org/wiki/Dictionary:Seismic_facies seismic facies] from a single phase of deposition, such as lowstand or highstand, are recorded on a map and contoured to convey the distribution of each seismic facies ([[:file:sedimentary-basin-analysis_fig4-37.png|Figures 4]] and [[:file:sedimentary-basin-analysis_fig4-38.png|5]]).

Associated [[Foraminifera|foraminiferal]] [[Fossil assemblage|biofacies]] shown in [[:file:sedimentary-basin-analysis_fig4-27.png|Figure 2]] and [[:file:sedimentary-basin-analysis_fig4-29.png|Figure 3]] support this analysis. The ''Glob alt'' sequence is the fourth clinoform from the right, the fourth-most basinward of five oblique clinoforms that [http://homepage.ufp.pt/biblioteca/Seismic/Pages/Page22.htm toplap] along a common horizon. Superjacent clinoforms show progressively more [http://www.merriam-webster.com/dictionary/topset%20beds topset] deposition forming sigmoidal clinoforms, suggesting relative rise of sea level (with consistent widespread increase in accommodation space). Observations of [http://wiki.seg.org/wiki/Dictionary:Seismic_facies seismic facies] from a single phase of deposition, such as [[Sea_level_cycle_phase_and_systems_tracts#Lowstand_systems_tracts|lowstand]] or [[Sea_level_cycle_phase_and_systems_tracts#Highstand_systems_tracts|highstand]], are recorded on a map and contoured to convey the distribution of each seismic facies ([[:file:sedimentary-basin-analysis_fig4-37.png|Figures 4]] and [[:file:sedimentary-basin-analysis_fig4-38.png|5]]).

==Seismic facies map==

==Seismic facies map==