Changes

[[:file:sedimentary-basin-analysis_fig4-11.png|Figure 1D]] of Early Cretaceous age is characterized by broad carbonate platforms rimmed by reef buildups along the margins established at the boundary of differential subsidence between thin and thick crust. Fine-grained carbonates were deposited in the adjacent deep basin. Terrigenous clastics continued to be input at local points along the northern margin. Known and potential reservoirs occur within both carbonate and clastic depositional systems of these early Cretaceous rocks.

[[:file:sedimentary-basin-analysis_fig4-11.png|Figure 1D]] of Early Cretaceous age is characterized by broad carbonate platforms rimmed by reef buildups along the margins established at the boundary of differential subsidence between thin and thick crust. Fine-grained carbonates were deposited in the adjacent deep basin. Terrigenous clastics continued to be input at local points along the northern margin. Known and potential reservoirs occur within both carbonate and clastic depositional systems of these early Cretaceous rocks.

[[file:sedimentary-basin-analysis_fig4-9.png|thumb|{{figure number|3}}.]]

[[file:sedimentary-basin-analysis_fig4-9.png|thumb|{{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 .]]

===Phase E===

===Phase E===