Changes

file:sedimentary-basin-analysis_fig4-4.png|{{figure number|1}}Major sand influxes into the northern Gulf of Mexico from Late Cretaceous to recently. After Winker;<ref name=Winker1982>Winker, C. D., Cenozoic shelf margins, northwestern Gulf of Mexico: Gulf Coast Assoc. of Geological Societies Transactions, vol. 32, p. 427-448.</ref> courtesy Gulf Coast Association of Geological Societies.

file:sedimentary-basin-analysis_fig4-4.png|{{figure number|1}}Major sand influxes into the northern Gulf of Mexico from Late Cretaceous to recently. After Winker;<ref name=Winker1982>Winker, C. D., Cenozoic shelf margins, northwestern Gulf of Mexico: Gulf Coast Assoc. of Geological Societies Transactions, vol. 32, p. 427-448.</ref> courtesy Gulf Coast Association of Geological Societies.

file:sedimentary-basin-analysis_fig4-6.png|{{figure number|2}}Tectonic map of the GOM basin. Modified from Buffler;<ref name=Buffler1991>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 Gulf Coast Geological Society, p. 1-16.</ref> courtesy New Orleans Geological Society.

file:sedimentary-basin-analysis_fig4-6.png|{{figure number|2}}Tectonic map of the GOM basin. Modified from Buffler;<ref name=Buffler1991>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 Gulf Coast Geological Society, p. 1-16.</ref> courtesy New Orleans Geological Society.

file:sedimentary-basin-analysis_fig4-8.png|{{figure number|3}}Traditional regional cross section showing highly deformed salt rooted within the in-place Middle Jurassic mother salt. Modified after Antoine et al. (1974);<ref name=Antoine1974>Antoine, J. W., R. G. Ray, Jr., T. G. Pyle, and W. R. Bryant, 1974, Continental margins of the Gulf of Mexico, in C. A. Burk and C. L. Drake, eds., The geology of margins: New York, Springer-Verlag, p. 683-693</ref> courtesy Springer Verlag.

file:sedimentary-basin-analysis_fig4-8.png|{{figure number|3}}Traditional regional cross section showing highly deformed salt rooted within the in-place Middle Jurassic mother salt. Modified after Antoine et al.;<ref name=Antoine1974>Antoine, J. W., R. G. Ray, Jr., T. G. Pyle, and W. R. Bryant, 1974, Continental margins of the Gulf of Mexico, in C. A. Burk and C. L. Drake, eds., The geology of margins: New York, Springer-Verlag, p. 683-693</ref> courtesy Springer Verlag.

file:sedimentary-basin-analysis_fig4-9.png|{{figure number|4}}More recent model of salt deformation recognizing both the in-place Middle Jurassic mother salt and displaced sheets of Middle Jurassic salt that have become detached from the mother salt. From Hall et al (1993);{{citation needed}}; courtesy Gulf Coast SEPM.

file:sedimentary-basin-analysis_fig4-9.png|{{figure number|4}}More recent model of salt deformation recognizing both the in-place Middle Jurassic mother salt and displaced sheets of Middle Jurassic salt that have become detached from the mother salt. From Hall et al (1993);{{citation needed}}; courtesy Gulf Coast SEPM.

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