Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Faten Houatmia"'
Publikováno v:
Arabian Journal of Geosciences. 14
Eastern Tunisia is a semi-arid to arid area, located in the southern Mediterranean side, in North Africa. It is facing water scarcity, overexploitation, and decreasing water quality of the phreatic water table. Water supply and storage do not respond
Publikováno v:
Hydrological Sciences Journal. :1-13
The Sebkhet El Behira–Garaat El Majdoul multilayer aquifer system is composed of Mio-Plio-Quaternary and Oligocene groundwater exploited in Sidi Bouzid and Kairouan governorates. Annual withdrawal volumes from El Behira Oligocene groundwater were a
Autor:
Hajer Azaiez, Faten Houatmia, Sami Khomsi, Dalila Jallalia, Sourour Thebti, Hakim Gabtni, Techcnologies. Borj Cédria Technopark, Belgacem Redhaounia, Mourad Bédir
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Journal of African Earth Sciences. 111:434-450
The Sisseb El Alem-Enfidha basin is located in the northeastern Tunisia, It is borded by Nadhour – Saouaf syncline to the north, Kairouan plain to the south, the Mediterranean Sea to the east and Tunisian Atlassic “dorsale” to the west. Oligoce
Publikováno v:
Arabian Journal of Geosciences. 8:4221-4238
The Sidi Saad basin is located in the NS axis in central Tunisia. This zone was affected by several distension and compression phases inducing the structuring and the distribution of Neogene deposits. The study area is known by the presence of import
Publikováno v:
Arabian Journal of Geosciences. 9
Most of hydrocarbon accumulations within the Gulf of Hammamet foreland basins in eastern Tunisia are reservoired within the Upper Miocene Birsa and Saouaf sandstones. It is the case of Birsa, Tazarka, Oudna, Baraka, Maamoura, Cosmos and Yasmine field
Publikováno v:
Environmental Earth Sciences. 75
Oligocene and Mio-Plio-Quaternary siliciclastic deposits constitute the most important deep aquifers of the Kairouanai-Sahel region. Considering the over-exploitation and contamination of the surface groundwater, recourse to use deep groundwater was