Résumé
► In this work a methodology for characterizing a complex aquifer was developed. ► Geometric model was done using seismic-reflection and wireline logging techniques. ► Hydrodynamic study was followed to determine the influence of tectonic structure. ► Hydrochemical study was used to introduce a distribution of water quality.
The Zéramdine and Mahdia–Jébéniana blocks are located in the Sahel region in east-central Tunisia. Active tectonics have divided the region into numerous sub-units, as result of multiple phases of distension and compression. The Miocene fluvio-deltaic sediment sandy layers have aquiferous capacities but their hydraulic properties are still unknown, due to the lack of investigation wells. This study proposes a new description of the regional hydrogeology of Miocene deposits. Seismic-reflection and wireline logging of petroleum and water wells were used to understand the structure and the geometry of the Miocene reservoirs. The groundwater flow and its relationship to the sedimentary and tectonic context were then identified by studying piezometry and hydrochemistry.
Two Miocene deep aquifer systems were identified: (1) Zéramdine–Béni Hassen to the north and (2) Jébéniana–Ksour Essef to the south. These aquifers are separated by the Mahdia graben. Other major tectonic structures, such as the Zéramdine fault corridor, the Moknine graben, and the El-Jem half-graben represent lateral boundaries for these aquifers. Other deeper sandy and clayey-sandy reservoirs were also identified in the area. Their repartition, thickness and depth vary from one block to other.
Hydrodynamics of the deep aquifers seems to be controlled by geological structures. Two independent compartments were identified: in the northern block groundwater flows from West to East and from Northwest to Southeast, while in the southern block it flows from Northwest to Southeast. Geochemical facies are of two types: Na–Ca–Cl–SO
4 for the Zéramdine–Béni Hassen deep aquifer and Na–Cl for the Jébéniana–Ksour Essef deep aquifer. The hydrodynamic and geochemical results confirm the sharing of the Miocene sediments into two aquifers.