@article {6922,
	title = {Characterization of Cenomanian-Turonian oxic facies in Tunisia: sequence stratigraphy and correlation of recorded bioevents},
	journal = {Arabian Journal of Geosciences},
	volume = {14},
	year = {2021},
	abstract = {On the southwestern Tethyan Margin of Tunisia, the well-known anoxic black shale facies of the Cenomanian-Turonian transition contrasts with oxic fossiliferous carbonates, first characterized here as lateral equivalents. In terms of sequence stratigraphy, the analysis of four wisely sampled sections in Central and Southern Tunisia led to interpret these deposits as a transgressive interval (TST). This interval spans the\&nbsp;Whiteinella archaeocretacea\&nbsp;Zone of foraminifera and is capped with a glauconite-rich highly bioturbated maximum flooding surface (MFS). In the reference section of Oued Bahloul and the Kalaat Senan area of North-Central Tunisia, these deposits overlay a Shelf Margin Wedge made of conglomeratic and bioclastic limestones. In South-Central and Southern Tunisia, the TST is characterized by the onset of oxic facies relaying laminated carbonates with local emergence surfaces. The analysis of both oxic and anoxic facies from the Cenomanian-Turonian transition allows identifying five successive bioevent markers, known elsewhere within the Tethyan domain: the extinction of the foraminifera genus\&nbsp;Rotalipora\&nbsp;(or\&nbsp;Thomasinella), the\&nbsp;Heterohelix\&nbsp;shift, the\&nbsp;Whiteinella\&nbsp;proliferation, the filament event, and the appearance of\&nbsp;Helvetotruncana helvetica. Among these bioevents, the\&nbsp;Heterohelix\&nbsp;shift coincides with the transgressive surface, while the filament event announces the maximal flooding surface. These Cenomanian-Turonian transition bioevents are of a particular relevance for regional and long-distance high-resolution correlations.},
	author = {Hanini, Amine and Houla, Yassine and DJAIZ, Foued and Chairat, Imen and Boughdiri, Mabrouk and Maamri, Ridha and Zagrarni,Mohamed-Faouzi}
}
@article {63468,
	title = {Geological Characterization and contibution of Geophysics to the mobilization of water resources in the Ain Djasser basin (South-S{\'e}tifien, Algeria NE), ISSN 2052-3408},
	journal = {The Euro-arab Organization for Environment and Water and Desert Researches, International Journal of Environment and WaterThe Euro-arab Organization for Environment and Water and Desert Researches, International Journal of Environment and Water},
	volume = {Vol. 8},
	year = {2019},
	month = {2019},
	pages = {pp. 66-77},
	abstract = {Le bassin d{\textquoteright}Ain Djasser fait partie de l{\textquoteright}ensemble Sud-S{\'e}tifien. Ce dernier est repr{\'e}sent{\'e} par une plaine inter-montagneuse appartenant au bassin des hauts plateaux constantinois. Il est caract{\'e}ris{\'e} par un climat de type m{\'e}diterran{\'e}en. L{\textquoteright}hydrologie tributaire du relief est la cons{\'e}quence directe des eaux de surface et de la fonte des neiges. La synth{\`e}se g{\'e}ologique montre un domaine allochtone r{\'e}sultant d{\textquoteright}une histoire polyphas{\'e}e associant les tectoniques atlasique et alpine. Ce dernier est caract{\'e}ris{\'e} par des s{\'e}ries s{\'e}dimentaires carbonat{\'e}es colmat{\'e} par d{\textquoteright}abondantes formations terrig{\`e}nes. L{\textquoteright}alimentation de l{\textquoteright}eau souterraine des diff{\'e}rentes nappes profondes {\`a} semi-profondes provient essentiellement de l{\textquoteright}infiltration des eaux de pluies. Ce cort{\`e}ge de roche forme une nappe libre et captive, par endroit recoup{\'e}e par des forages {\`a} des profondeurs de 178 {\`a} 330 m, fournissant un d{\'e}bit moyen de 15 l/s. L{\textquoteright}interpr{\'e}tation des coupes g{\'e}o{\'e}lectriques du bassin montrent, (i) des formations alluvionnaires du mio-plio-quaternaire de quelques dizaines de m{\`e}tres qui forment un bon aquif{\`e}re superficiel, (ii) des calcaires fissur{\'e}s du jurassico-cr{\'e}tac{\'e} dont le toit est atteint {\`a} des profondeurs variables est un aquif{\`e}re captif. L{\textquoteright}influence d{\textquoteright}accidents entre les diff{\'e}rents blocs rend possible une {\'e}ventuelle alimentation des aquif{\`e}res entres eux. L{\textquoteright}analyse litho-stratigraphique montre que le substratum et la couverture s{\'e}dimentaire ne pr{\'e}sentent pas de grandes variations lat{\'e}rales. Par contre, nous observons au niveau des sondages une variation dans l{\textquoteright}{\'e}paisseur et la lithologie des couches, essentiellement au niveau de la formation du remplissage mio-plio-quaternaire. L{\textquoteright}objectif de cette {\'e}tude r{\'e}side pour l{\textquoteright}essentiel, dans la mobilisation des ressources en eaux superficielles et souterraine pour leurs exploitations dans les domaines agricoles et l{\textquoteright}{\'e}levage, en vue d{\textquoteright}une utilisation rationnelle et planifi{\'e}e de cet {\'e}l{\'e}ment vital qu{\textquoteright}est l{\textquoteright}eau},
	author = {Djaiz, Fouad and Nabil, Defaflia and Ali, ATHAMENA and Lamouri, Bachir and Boughdiri, Mabrouk and Belalite, Halima and Abdellah, Boushaba}
}
