Changes

The scale should generally be [[distance::100 mi]] or more, and a grid of [[strike]] and [[dip]] sections should be made. Use all data that would aid in correlations, and show stratigraphic patterns including well data (logs, cuttings, and cores), seismic sections, and outcrop data.

The scale should generally be [[distance::100 mi]] or more, and a grid of [[strike]] and [[dip]] sections should be made. Use all data that would aid in correlations, and show stratigraphic patterns including well data (logs, cuttings, and cores), seismic sections, and outcrop data.

Use the diagram below to help identify large-scale carbonate platform stratal patterns in log cross sections or seismic sections.

Use [[:file:predicting-reservoir-system-quality-and-performance_fig9-84.png|Figure 1]] to help identify large-scale carbonate platform stratal patterns in log cross sections or seismic sections.

[[file:predicting-reservoir-system-quality-and-performance_fig9-84.png|thumb|{{figure number|9-84}}.]]

[[file:predicting-reservoir-system-quality-and-performance_fig9-84.png|thumb|{{figure number|1}}From Handford and Loucks.<ref name=Handfordandloucks_1995>Handford, C. R., and R. G. Loucks, 1995, [http://archives.datapages.com/data/specpubs/seismic2/data/a168/a168/0001/0000/0003.htm Carbonate depositional sequences and systems tracts]-responses of carbonate platforms to relative sea-level changes, ''in'' R. G. Loucks and J. F. Sarg, eds., Carbonate sequence stratigraphy: Recent developments and applications: AAPG Memoir 57, p. 3-42.</ref>]]

==See also==

==See also==