作者: Faten Houatmia , Sami Khomsi , Mourad Bédir
DOI: 10.1016/J.JAFREARSCI.2015.08.019
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摘要: Abstract The Sisseb El Alem-Enfidha basin is located in the northeastern Tunisia, It borded by Nadhour – Saouaf syncline to north, Kairouan plain south, Mediterranean Sea east and Tunisian Atlassic “dorsale” west. Oligocene Miocene deltaic deposits present main potential deep aquifers this with high porosity (25%–30%). interpretation of twenty seismic reflection profiles, calibrated wire line logging data twelve oil wells, hydraulic wells geologic field sections highlighted impact tectonics on structuring geometry Oligo-Miocene sandstones reservoirs their distribution raised structures subsurface depressions. seismostratigraphy analysis from Ain Ghrab Formation (Langhian) Segui (Quaternary) showed five third-order sequence nine extended lenticular sandy bodies limited toplap downlap surfaces unconformities, presented also third- order sequences reservoirs. Depth thickness maps these reservoir packages exhibited sub-basins characterized important lateral vertical geometric thichness variations. Petroleum correlation clay volume calculation an heterogeneous multilayer formed arrangement fourteen sandstone being able be good reservoirs, separated impermeable affected faults. Reservoirs levels correspond mainly lower system tract (LST) sequences. Intensive fracturing seated faults bounding different play a great role for water surface recharge inter-layer circulations between total pore study area, estimated about 4 × 10 12 m 3 equivalent 9 reserves.