Research Article

Simulating the Evolution of Fluid Underpressures in the Great Plains, by Incorporation of Tectonic Uplift and Tilting, with a Groundwater Flow Model

Table 2

Stratigraphic column.

AgeGeohydrologic unit nameLithologic descriptionGeohydrologic unit typeModel layerRange of thickness (feet)

NeogeneOgallala FormationTerrestrial gravel, sand, and clayAquifer10–300

Neogene-PaleogeneLaramide Basin FillTerrestrial gravel, sand, and clayAquifer20–2,300

Late CretaceousPierre & Niobrara FormationsMarine shales and carbonates, some sand layersAquitard30–6,800

Early CretaceousDakota FormationSandstoneAquifer40–500

Jurassic-Triassic-late PermianMorrison-Leonardian FormationsTerrestrial sand, silt, and clay with upper Permian shale and evaporitesAquitard50–1,200

Early PermianWolfcampian FormationClastic marine sediments with carbonate bedsAquifer60–1,100

PennsylvanianVirgilian-Missourian FormationClastic marine sediments with carbonate bedsAquifer7400–1,600

PennsylvanianDesmoinesian FormationMarine carbonates in the east, terrestrial sediments in the westAquitard in west, aquifer in east8100–700

Early PennsylvanianBasal Pennsylvanian UnitMarine shales with some carbonatesAquitard9100

Early PaleozoicMississippian-Silurian-Ordovician-Cambrian UnitsLimestones and dolomites with karst weathering, & lesser interbedded shalesAquifer100–1,100

PrecambrianPrecambrian BasementGranite and gneissNo-flow boundaryModel lower boundaryNA