Changes

Sedimentary-basin-analysis_fig4-31.png|{{figure number|1}}Composite chronostratigraphic chart that serves as an age model for the GOM basin Pliocene and Pleistocene, summarizing nine studies published between 1982 and 1993. From Armentrout<ref name=ch04r9 />; courtesy The Geological Society, London.

Sedimentary-basin-analysis_fig4-31.png|{{figure number|1}}Composite chronostratigraphic chart that serves as an age model for the GOM basin Pliocene and Pleistocene, summarizing nine studies published between 1982 and 1993. From Armentrout<ref name=ch04r9 />; courtesy The Geological Society, London.

Sedimentary-basin-analysis_fig4-25.png|{{figure number|2}}Correlation of the third-order eustatic curve of Haq et al.<ref>Haq, B., J. Hardenbol, and P. R. Vail, 1988, Mesozoic and Cenozoic chronostratigraphy and cycles of sea-level change: SEPM Special Publication 42, p. 71–108.</ref> and the oxygen isotope curve of Williams and Trainor<ref>Williams, D. F., and D. M. Trainor, 1987, Integrated chemical stratigraphy of deep- water frontier areas of the northern Gulf of Mexico: Proceedings, Gulf Coast Section SEPM 8th Annual Research Conference, p. 151–158.</ref> with seven prograding clinoform intervals from the High Island South Addition in the GOM basin. From Armentrout;<ref>Armentrout, J. M., 1993, Relative seal-level variations and fault-salt response: offshore Texas examples: Proceedings, Gulf Coast Section SEPM 14th Annual Research Confer- ence, p. 1–7.</ref> courtesy Gulf Coast SEPM.

Sedimentary-basin-analysis_fig4-25.png|{{figure number|2}}Correlation of the third-order eustatic curve of Haq et al.<ref>Haq, B., J. Hardenbol, and P. R. Vail, 1988, Mesozoic and Cenozoic chronostratigraphy and cycles of sea-level change: SEPM Special Publication 42, p. 71–108.</ref> and the oxygen isotope curve of Williams and Trainor<ref>Williams, D. F., and D. M. Trainor, 1987, Integrated chemical stratigraphy of deep- water frontier areas of the northern Gulf of Mexico: Proceedings, Gulf Coast Section SEPM 8th Annual Research Conference, p. 151–158.</ref> with seven prograding clinoform intervals from the High Island South Addition in the GOM basin. From Armentrout;<ref>Armentrout, J. M., 1993, Relative seal-level variations and fault-salt response: offshore Texas examples: Proceedings, Gulf Coast Section SEPM 14th Annual Research Confer- ence, p. 1–7.</ref> courtesy Gulf Coast SEPM.

Sedimentary-basin-analysis_fig4-32.png|{{figure number|3}}Rock thickness vs. time plot for nine key wells south of east- ern Louisiana within the area of the 6–4 Ma depocenter. After Piggott and Pulham;<ref name=ch04r75 /> courtesy Gulf Coast SEPM.

Sedimentary-basin-analysis_fig4-32.png|{{figure number|3}}Rock thickness vs. time plot for nine key wells south of east- ern Louisiana within the area of the 6–4 Ma [[depocenter]]. After Piggott and Pulham;<ref name=ch04r75 /> courtesy Gulf Coast SEPM.

Sedimentary-basin-analysis_fig4-13.png|{{figure number|4}}Paleogeography of the Mississippi River depositional system from approximately 6 Ma to 4 Ma. After Piggott and Pulham;<ref name=ch04r75 /> courtesy Gulf Coast Section SEPM.

Sedimentary-basin-analysis_fig4-13.png|{{figure number|4}}Paleogeography of the Mississippi River depositional system from approximately 6 Ma to 4 Ma. After Piggott and Pulham;<ref name=ch04r75 /> courtesy Gulf Coast Section SEPM.

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