@article {63109,
	title = {Swelling properties and lime stabilization of N{\textquoteright}Gaous expansive marls, NE Algeria},
	journal = {Journal of African Earth SciencesJournal of African Earth Sciences},
	volume = {170},
	year = {2020},
	month = {2020},
	pages = {103895},
	isbn = {1464-343X},
	author = {Benyahia, Sabah and Boumezbeur, Abderrahmane and Lamouri, Bachir and Fagel, Nathalie}
}
@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}
}
@article {64995,
	title = {Quaternary fluviatile terraces of the Oued El Gourzi (Batna, NE Algeria): sedimentology and characteristics of the depositional},
	journal = {Advances in Science, Technology \& InnovationAdvances in Science, Technology \& Innovation},
	year = {2018},
	month = {2018},
	pages = {pp 331-334},
	abstract = {Field observations and sedimentological analyses of alluvial terraces of the O. Gourzi (Batna, NE Algeria) lead us to consider sediments as dominated by clayey and silty-sandy fractions overlain by gravel and calcareous coarser fractions. Moderate CaO3 contents would have resulted from the dissolution of the nearby carbonate relieves. They are mainly composed of Maastrichtian limestones. The distribution of the mineral fraction led us to identify 07 levels including horizons of coarse fractions alternating with layers rich in sand and silt with a roughly constant clay fraction through the stratigraphic column. Kurtosis values, frequency histograms of a prokurtic type, rarily mesokurtic, mark a constant power mode for the transport agent. Classification indices indicate poorly- to moderately sorted material, indicating a turbiditic depositional environment. Quartz grain nature and morphoscopy refer to Miocene sandstones as a potential origin. The ferruginous coating is due to the initiating pedogenesis.},
	author = {Djaiz, Fouad and Nabil, Defaflia and Lamouri, Bachir and Abdellah, Boushaba}
}
@conference {64952,
	title = {Quaternary fluviatile terraces of the Oued El Gourzi (Batna, NE Algeria): sedimentology and characteristics of the depositional environment},
	booktitle = {CAJG 2018: Paleobiodiversity and Tectono-Sedimentary Records in the Mediterranean Tethys and Related Eastern Areas },
	year = {2018},
	month = {2018},
	pages = {331{\textendash}334},
	abstract = {
	Field observations and sedimentological analyses of alluvial terraces of the O. Gourzi (Batna, NE Algeria) lead us to consider sediments as dominated by clayey and silty-sandy fractions overlain by gravel and calcareous coarser fractions. Moderate CaO3\&nbsp;contents would have resulted from the dissolution of the nearby carbonate relieves. They are mainly composed of Maastrichtian limestones. The distribution of the mineral fraction led us to identify 07 levels including horizons of coarse fractions alternating with layers rich in sand and silt with a roughly constant clay fraction through the stratigraphic column. Kurtosis values, frequency histograms of a prokurtic type, rarily mesokurtic, mark a constant power mode for the transport agent. Classification indices indicate poorly- to moderately sorted material, indicating a turbiditic depositional environment. Quartz grain nature and morphoscopy refer to Miocene sandstones as a potential origin. The ferruginous coating is due to the initiating pedogenesis.

},
	url = {https://link.springer.com/chapter/10.1007/978-3-030-01452-0_79},
	author = {Djaiz, Fouad and Defaflia, Nabil and Lamouri, Bachir and Boushaba, Abdellah and I, Chairat}
}
@proceedings {64996,
	title = {Quaternary Fluviatile Terraces of the Oued El Gourzi (Batna, NE Algeria): Sedimentology and Characteristics of the Depositional Environment},
	journal = {Conference of the Arabian Journal of Geosciences},
	year = {2018},
	month = {2018},
	pages = {331-334},
	publisher = {Springer},
	author = {Djaiz, Fouad and Defaflia, Nabil and Lamouri, Bachir and Boushaba, Abdallah and Chairat, Imen}
}
@proceedings {64994,
	title = {TERRASSES FLUVIATILES QUATERNAIRES DE L\&$\#$39;OUED EL HAY (BATNA, NE ALG{\'E}RIE): S{\'E}DIMENTOLOGIE ET CARACT{\'E}RISTIQUES DE L\&$\#$39;ENVIRONNEMENT S{\'E}DIMENTAIRE.},
	year = {2018},
	month = {2018},
	abstract = {Une {\'e}tude stratigraphique et s{\'e}dimentologique a {\'e}t{\'e} r{\'e}alis{\'e}e sur une terrasse alluviale de la r{\'e}gion d{\textquoteright}Oued El Hay, au sud de Batna (NE Alg{\'e}rie). Les structures s{\'e}dimentaires observ{\'e}es sont principalement des zones d{\textquoteright}{\'e}rosion, des zones inondables, des figures en biseau et des variations d{\textquoteright}{\'e}paisseur associ{\'e}es {\`a} des joints de stratification. Du point de vue s{\'e}dimentologique, les s{\'e}diments sont domin{\'e}s par des fractions argilo-limono-sableuses, suivies par des fractions de gravier et de cailloux. Les teneurs mod{\'e}r{\'e}es en CaCO3 r{\'e}sultent de la dissolution des reliefs calcaires {\`a} proximit{\'e} (calcaire cr{\'e}tac{\'e}) associ{\'e}e {\`a} l{\textquoteright}augmentation de la temp{\'e}rature et l{\textquoteright}humidit{\'e} du milieu. L{\textquoteright}observation morphoscopique de grains de quartz avec une loupe binoculaire permet d{\textquoteright}offrir une {\'e}volution plus ou moins importante, car ils sont souvent {\'e}mouss{\'e}s ou sous-arrondis. L{\textquoteright}{\'e}tude s{\'e}dimentologique a {\'e}t{\'e} r{\'e}alis{\'e}e sur 16 {\'e}chantillons pr{\'e}lev{\'e}s syst{\'e}matiquement du haut vers le bas de la coupe stratigraphique. L{\textquoteright}examen de la taille brute de la fraction inf{\'e}rieure {\`a} 2 mm a permis d{\textquoteright}individualiser 03 niveaux dans des couches s{\'e}dimentaires, certaines fractions grossi{\`e}res riches (gravier, cailloux et blocs) alternant avec des couches riches en sable et en limon. Le pourcentage de fraction d{\textquoteright}argile est dominant et reste pratiquement constant presque tout au long de la section stratigraphique.},
	author = {Djaiz, Fouad and Nabil, Defaflia and Lamouri, Bachir and Ali, ATHAMENA and Abdellah, Boushaba}
}
