Changes

</gallery>

</gallery>

[[:file:sedimentary-basin-analysis_fig4-37.png|Figure 4]] is a map of the [http://wiki.seg.org/wiki/Dictionary:Seismic_facies seismic facies] of the ''Glob alt'' Sea_level_cycle_phase_and_systems_tracts#Lowstand_systems_tracts|lowstand]] interval ([[:file:sedimentary-basin-analysis_fig4-29.png|Figures 3]] and [[:file:sedimentary-basin-analysis_fig4-28.png|6]]). The mapped facies are observed in the interval immediately above the [[Definitions_of_depositional_system_elements#Sequence_boundaries|sequence boundary]] at the base of the ''Glob alt'' sequence in [[:file:sedimentary-basin-analysis_fig4-36.png|Figure 1]]. In the basin setting, the sequence boundary is, at seismic scale, essentially coincident with the underlying condensed section. The mapped facies are within the lowstand systems tract. Each observed facies is plotted along the transect of the seismic reflection profile, profile by profile. The area of [http://education.nationalgeographic.com/education/encyclopedia/continental-shelf/?ar_a=1 shelf]/[http://www.thefreedictionary.com/continental+slope slope] inflection is plotted, based on the location of the inflection point between [http://geography_glossary.enacademic.com/578/foreset_beds foreset] and [http://www.merriam-webster.com/dictionary/topset%20beds topset] elements of the clinoform. [[Fossil assemblage|Biofacies]] information ([[:file:sedimentary-basin-analysis_fig4-29.png|Figure 3]]) and sediment type ([[:file:sedimentary-basin-analysis_fig4-38.png|Figure 5]]) can then be overlain on the seismic facies map to provide an integrated data base for interpreting depositional environments ([[:file:sedimentary-basin-analysis_fig4-39.png|Figure 7]]).

[[:file:sedimentary-basin-analysis_fig4-37.png|Figure 4]] is a map of the [http://wiki.seg.org/wiki/Dictionary:Seismic_facies seismic facies] of the ''Glob alt'' [[Sea_level_cycle_phase_and_systems_tracts#Lowstand_systems_tracts|lowstand]] interval ([[:file:sedimentary-basin-analysis_fig4-29.png|Figures 3]] and [[:file:sedimentary-basin-analysis_fig4-28.png|6]]). The mapped facies are observed in the interval immediately above the [[Definitions_of_depositional_system_elements#Sequence_boundaries|sequence boundary]] at the base of the ''Glob alt'' sequence in [[:file:sedimentary-basin-analysis_fig4-36.png|Figure 1]]. In the basin setting, the sequence boundary is, at seismic scale, essentially coincident with the underlying condensed section. The mapped facies are within the lowstand systems tract. Each observed facies is plotted along the transect of the seismic reflection profile, profile by profile. The area of [http://education.nationalgeographic.com/education/encyclopedia/continental-shelf/?ar_a=1 shelf]/[http://www.thefreedictionary.com/continental+slope slope] inflection is plotted, based on the location of the inflection point between [http://geography_glossary.enacademic.com/578/foreset_beds foreset] and [http://www.merriam-webster.com/dictionary/topset%20beds topset] elements of the clinoform. [[Fossil assemblage|Biofacies]] information ([[:file:sedimentary-basin-analysis_fig4-29.png|Figure 3]]) and sediment type ([[:file:sedimentary-basin-analysis_fig4-38.png|Figure 5]]) can then be overlain on the seismic facies map to provide an integrated data base for interpreting depositional environments ([[:file:sedimentary-basin-analysis_fig4-39.png|Figure 7]]).

==Net sand map==

==Net sand map==