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Line 22: − file:sedimentary-basin-analysis_fig4-13.png|{{figure number|3}}After Piggott and Pulham<ref name=ch04r75 />). Copyright: Gulf Coast Section SEPM. − file:sedimentary-basin-analysis_fig4-14.png|{{figure number|4}}After Piggott and Pulham<ref name=ch04r75 />). Copyright: Gulf Coast Section SEPM. − file:sedimentary-basin-analysis_fig4-15.png|{{figure number|5}}After Piggott and Pulham<ref name=ch04r75 />). Copyright: Gulf Coast Section SEPM. − file:sedimentary-basin-analysis_fig4-16.png|{{figure number|6}}After Piggott and Pulham<ref name=ch04r75 />). Line 45:
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Example: mapping depocenters through time (view source)
Revision as of 15:10, 28 March 2014
, 15:10, 28 March 2014→GOM basin depocenter time intervals
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);{{citation needed}} 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. (1974);{{citation needed}} 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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[[:file:sedimentary-basin-analysis_fig4-13.png|Figures 3]], [[:file:sedimentary-basin-analysis_fig4-14.png|4]], [[:file:sedimentary-basin-analysis_fig4-15.png|5]], and [[:file:sedimentary-basin-analysis_fig4-16.png|6]] are maps of depocenters and paleogeography for intervals A, B, D, and E. These were constructed by correlating wells using fossil extinction events and grids of interpreted seismic reflection profiles. The High Island–East Breaks study area is shown on each map.
<gallery>
file:sedimentary-basin-analysis_fig4-13.png|{{figure number|5}}Paleogeography of the Mississippi River depositional system from approximately 6 Ma to 4 Ma (interval A). After Piggott and Pulham<ref name=ch04r75 />). Copyright: Gulf Coast Section SEPM.
file:sedimentary-basin-analysis_fig4-14.png|{{figure number|6}}Paleogeography from approximately 4 Ma to 3 Ma (interval B). After Piggott and Pulham<ref name=ch04r75 />). Copyright: Gulf Coast Section SEPM.
file:sedimentary-basin-analysis_fig4-15.png|{{figure number|7}}Paleogeography from approximately 2.5 Ma to 2vMa (interval D). After Piggott and Pulham<ref name=ch04r75 />). Copyright: Gulf Coast Section SEPM.
file:sedimentary-basin-analysis_fig4-16.png|{{figure number|8}Paleogeography from approximately 1 Ma to the present (interval E). After Piggott and Pulham<ref name=ch04r75 />). Courtesy Gulf Coast Section SEPM. Also after Weimer (1990){{citation needed}}; courtesy AAPG.
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[[:file:sedimentary-basin-analysis_fig4-13.png|Figures 5]], [[:file:sedimentary-basin-analysis_fig4-14.png|6]], [[:file:sedimentary-basin-analysis_fig4-15.png|7]], and [[:file:sedimentary-basin-analysis_fig4-16.png|8]] are maps of depocenters and paleogeography for intervals A, B, D, and E. These were constructed by correlating wells using fossil extinction events and grids of interpreted seismic reflection profiles. The High Island–East Breaks study area is shown on each map.
==Formation of high island-east breaks depocenter==
==Formation of high island-east breaks depocenter==