Changes

==Description==

==Description==

The deepwater sands of the ''Glob alt'' reservoir are encased in hemipelagic mudstones and have a top seal associated with the condensed section of the ''Glob alt'' depositional cycle.<ref name=ch04r7>Armentrout, J., M., 1991, Paleontological constraints on depositional [[modeling]]: examples of integration of biostratigraphy and seismic stratigraphy, Pliocene–Pleistocene, Gulf of Mexico, in Weimer, P., Link, M., H., eds., Seismic Facies and Sedimentary Processes of Submarine Fans and Turbidite Systems: New York, Springer-Verlag, p. 137–170.</ref> The well-log cross section in Figure 4-48 shows the correlation of the ''Glob alt'' sandstones. The top seal, which occurs above the log cross section, is a major mudstone condensed interval coincident with the ''Glob alt'' datum labeled on Figure 4-47. Precondensed section mudstones encasing the ''Glob alt'' sandstones provide local top seal and lateral seal.

 

 

The deepwater sands of the ''Glob alt'' reservoir are encased in hemipelagic mudstones and have a top seal associated with the condensed section of the ''Glob alt'' depositional cycle.<ref name=ch04r7>Armentrout, J., M., 1991, Paleontological constraints on depositional [[modeling]]: examples of integration of biostratigraphy and seismic stratigraphy, Pliocene–Pleistocene, Gulf of Mexico, in Weimer, P., Link, M., H., eds., Seismic Facies and Sedimentary Processes of Submarine Fans and Turbidite Systems: New York, Springer-Verlag, p. 137–170.</ref> The well-log cross section in [[:file:sedimentary-basin-analysis_fig4-48.png|Figure 1]] shows the correlation of the ''Glob alt'' sandstones. The top seal, which occurs above the log cross section, is a major mudstone condensed interval coincident with the ''Glob alt'' datum labeled on [[:file:sedimentary-basin-analysis_fig4-47.png|Figure 2]]. Precondensed section mudstones encasing the ''Glob alt'' sandstones provide local top seal and lateral seal.

==Effectiveness==

==Effectiveness==