Changes

file:sedimentary-basin-analysis_fig4-11.png|{{figure number|1}}Schematic diagram showing a series of cross sections representing the four phases of Late Triassic to Early Cretaceous evolution of the GOM basin. Modified from Buffler.<ref name=Buffler_1991>Buffler, R. T., 1991, Early evolution of the Gulf of Mexico basin, ''in'' D. Goldthwaite, ed., An introduction to Central Gulf Coast geology: New Orleans Geological Society, p. 1-16.</ref> Courtesy New Orleans Geological Society.

file:sedimentary-basin-analysis_fig4-11.png|{{figure number|1}}Schematic diagram showing a series of cross sections representing the four phases of Late Triassic to Early Cretaceous evolution of the GOM basin. Modified from Buffler.<ref name=Buffler_1991>Buffler, R. T., 1991, Early evolution of the Gulf of Mexico basin, ''in'' D. Goldthwaite, ed., An introduction to Central Gulf Coast geology: New Orleans Geological Society, p. 1-16.</ref> Courtesy New Orleans Geological Society.

file:sedimentary-basin-analysis_fig4-6.png|{{figure number|2}}Location of Figure 1. Modified from Buffler.<ref name=Buffler_1991 /> Courtesy New Orleans Geological Society.

file:sedimentary-basin-analysis_fig4-6.png|{{figure number|2}}Location of Figure 1. Modified from Buffler.<ref name=Buffler_1991 /> Courtesy New Orleans Geological Society.

file:sedimentary-basin-analysis_fig4-9.png|{{figure number|3}}Phase E began during the mid-Cenomanian with a rapid fall and rise of sea level superimposed on a long-term rise that terminally drowned the outer margins of the carbonate platforms, causing the margins to retreat landward.

file:sedimentary-basin-analysis_fig4-9.png|{{figure number|3}}Phase E began during the mid-Cenomanian with a rapid fall and rise of sea level superimposed on a long-term rise that terminally drowned the outer margins of the carbonate platforms, causing the margins to retreat landward. From Hall et al. (1993); courtesy Gulf Coast SEPM.

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