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| ==LST example== | | ==LST example== |
− | The cross section below is from the Late Cenozoic of the Gulf of Mexico. It shows the well log responses of a lowstand systems tract (labeled as PGC, or prograding complex, on the cross section). Log A is completely basinal with a slope fan overlain by shingled turbidites. Logs B and C have deltaic and delta front sands, and midslope turbidite sands. Log D has a “classic” coarsening-upward pattern. Log E has incised valley sands.
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− | [[file:exploring-for-stratigraphic-traps_fig21-21.png|thumb|{{figure number|21-21}}.]] | + | [[file:exploring-for-stratigraphic-traps_fig21-21.png|thumb|{{figure number|3}}.]] |
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| + | The cross section in [[:file:exploring-for-stratigraphic-traps_fig21-21.png|Figure 3]] is from the Late Cenozoic of the Gulf of Mexico. It shows the well log responses of a lowstand systems tract (labeled as PGC, or prograding complex, on the cross section). Log A is completely basinal with a slope fan overlain by shingled turbidites. Logs B and C have deltaic and delta front sands, and midslope turbidite sands. Log D has a “classic” coarsening-upward pattern. Log E has incised valley sands. |
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| ==See also== | | ==See also== |