Changes

[[file:exploring-for-stratigraphic-traps_fig21-21.png|300px|thumb|{{figure number|3}}Cross section from the Late Cenozoic of the Gulf of Mexico. From Mitchum et al.;<ref>Mitchum, R. M., P. R. Vail, and J. B. Sangree, 1977, [http://archives.datapages.com/data/specpubs/seismic1/data/a165/a165/0001/0100/0117.htm Seismic stratigraphy and global changes in sea level, part 6: stratigraphic interpretations of seismic reflection patterns in depositional sequences], in C. E. Payton, ed., Seismic Stratigraphy and Applications to Hydrocarbon Exploration: [http://store.aapg.org/detail.aspx?id=1157 AAPG Memoir 26], p. 117–133.</ref> courtesy AAPG.]]

[[file:exploring-for-stratigraphic-traps_fig21-21.png|300px|thumb|{{figure number|3}}Cross section from the Late Cenozoic of the Gulf of Mexico. From Mitchum et al.;<ref>Mitchum, R. M., P. R. Vail, and J. B. Sangree, 1977, [http://archives.datapages.com/data/specpubs/seismic1/data/a165/a165/0001/0100/0117.htm Seismic stratigraphy and global changes in sea level, part 6: stratigraphic interpretations of seismic reflection patterns in depositional sequences], in C. E. Payton, ed., Seismic Stratigraphy and Applications to Hydrocarbon Exploration: [http://store.aapg.org/detail.aspx?id=1157 AAPG Memoir 26], p. 117–133.</ref> courtesy AAPG.]]

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 [[turbidite]]s. 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.

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 [[turbidite]]s. 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==