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Groundwater flow in sedimentary basins

The main large-scale groundwater flow systems that may develop during the different stages of evolution of a sedimentary basin are described in Sections 2.1 to 2.3. These sections also present some examples of the relation between a basin type and type of groundwater flow system. Section 2.4 gives an overview of local groundwater flow systems of interest in petroleum-related studies. [Pg.24]

When the characteristics of a groundwater flow system are adjusted to the prevailing boundary conditions and remain constant in a sedimentary basin during a certain period, the groundwater flow system is said to be in steady state. Different groundwater flow systems may coexist and interact in the same [Pg.24]

System UOnstmegnphy HydmstrsSgrBphy Main hydmgeoiogical units [Pg.25]

IViassic Huvial deltaic and iacustrine elastics and limestones Oockum aquifer  [Pg.25]

Permian Salt, anhydrite, red beds and peritldal doiomite Evaporite aquifer Evaporite aquitard [Pg.25]

See other pages where Groundwater flow in sedimentary basins is mentioned: [Pg.18]    [Pg.23]    [Pg.25]    [Pg.27]    [Pg.29]    [Pg.31]    [Pg.33]    [Pg.35]    [Pg.37]    [Pg.39]    [Pg.41]    [Pg.43]    [Pg.45]    [Pg.47]    [Pg.49]    [Pg.51]    [Pg.52]    [Pg.53]    [Pg.55]    [Pg.57]    [Pg.59]    [Pg.61]    [Pg.63]    [Pg.65]    [Pg.67]    [Pg.69]    [Pg.71]    [Pg.73]    [Pg.75]    [Pg.77]    [Pg.78]    [Pg.79]    [Pg.255]    [Pg.20]   


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Basin, sedimentary groundwater

Groundwater flow

In groundwater

In groundwater flow

Sedimentary basins

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