Changes

==Shelf-edge and ramp-type margin traps==

==Shelf-edge and ramp-type margin traps==

[[file:exploring-for-stratigraphic-traps_fig21-15.png|thumb|{{figure number|2}}After .<ref name=ch21r47>Van Wagoner, J., C., Mitchum, R., M., Campion, K., M., Rahmanian, V., D., 1990, Siliciclastic [[Sequence stratigraphy]] in Well Logs, Cores and Outcrops: Concepts for High-Resolution Correlation of Time and Facies: AAPG Methods in Exploration Series No. 7, 55 p.</ref>]]

[[file:exploring-for-stratigraphic-traps_fig21-15.png|thumb|{{figure number|2}}After .<ref name=ch21r47>Van Wagoner, J., C., Mitchum, R., M., Campion, K., M., Rahmanian, V., D., 1990, Siliciclastic Sequence stratigraphy in Well Logs, Cores and Outcrops: Concepts for High-Resolution Correlation of Time and Facies: [http://store.aapg.org/detail.aspx?id=1196 AAPG Methods in Exploration Series No. 7], 55 p.</ref>]]

[[:file:exploring-for-stratigraphic-traps_fig21-15.png|Figure 2]] shows two schematic cross sections showing potential stratigraphic and combination stratigraphic-structural plays associated with sequences and parasequences on shelf-edge and ramp margins. Shelf-edge margins are found in continental margin basins. Ramp margins are found in cratonic, continental margin, or lacustrine basins. The numbers in the cross sections correspond to the numbers in the table.

[[:file:exploring-for-stratigraphic-traps_fig21-15.png|Figure 2]] shows two schematic cross sections showing potential stratigraphic and combination stratigraphic-structural plays associated with sequences and parasequences on shelf-edge and ramp margins. Shelf-edge margins are found in continental margin basins. Ramp margins are found in cratonic, continental margin, or lacustrine basins. The numbers in the cross sections correspond to the numbers in the table.