Changes

}}

}}

==Description==

==Description==

 

[[file:sedimentary-basin-analysis_fig4-48.png|thumb|{{figure number|1}}Well log cross-section of the ''Glob alt'' reservoir interval.]]

file:sedimentary-basin-analysis_fig4-48.png|thumb|{{figure number|1}}Well log cross-section of the ''Glob alt'' reservoir interval.

 

file:sedimentary-basin-analysis_fig4-47.png|thumb|{{figure number|2}}Seismic reflection profile showing the ''Glob alt'' reservoir interval.

[[file:sedimentary-basin-analysis_fig4-47.png|thumb|{{figure number|2}}Seismic reflection profile showing the ''Glob alt'' reservoir interval.]]

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.

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.