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Line 85: − 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. − + + +
Well log sequence analysis (view source)
Revision as of 20:26, 24 February 2014
, 20:26, 24 February 2014→LST example
==LST example==
==LST example==
[[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}}.]]
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.
==See also==
==See also==