@proceedings {63446,
	title = {Caract{\'e}risation g{\'e}ologique et apport de la g{\'e}ophysique pour la mobilisation des ressources hydriques dans le bassin de Gadaine (Ain Yagout, Alg{\'e}rie NE)},
	journal = {Le 1er S{\'e}minaire National en G{\'e}osciences et Environnement 23{\textendash} 24 Octobre (SGSE-2019)},
	year = {2019},
	month = {2019},
	address = {Tamanrasset, Algeria},
	url = {https://www.researchgate.net/profile/Athamena-Ali/publication/337603986_CARACTERISATION_GEOLOGIQUE_ET_APPORT_DE_LA_GEOPHYSIQUE_POUR_LA_MOBILISATION_DES_RESSOURCES_HYDRIQUES_DANS_LE_BASSIN_DE_GADAINE_AIN_YAGOUT_ALGERIE_NE/links/5e865d7ba6fdcca789ec8f40/CAR},
	author = {Fouad, DJAIZ and Ali, ATHAMENA and Bachir, Lamouri and Bousahaba, A. and Halima, BELALITE and Rachid, Touansa and Soumia, Khanfer and Manal, Marred and Imen, Chairat}
}
@proceedings {63395,
	title = {Caract{\'e}risation g{\'e}ologique et apport de la g{\'e}ophysique pour la mobilisation des ressources hydriques dans le bassin d\&rsquo;El Mather.},
	journal = {Premier Colloque sur la g{\'e}ologie des Bassins S{\'e}dimentaires Maghr{\'e}bins FSTGAT-USTHB 01 au 03-10-},
	year = {2019},
	month = {2019},
	address = {Alger, Alg{\'e}rie},
	author = {Fouad, DJAIZ and Hocine, Nadji and Hmmimed, M.}
}
@proceedings {63220,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude du basin N{\'e}og{\`e}ne Batna-ain Touta, limite aur{\`e}s-Monts de Belezma},
	journal = { 1st National Seminar on GeoSciences and Environment SGSE 19 October 23-24, },
	year = {2019},
	month = {2019},
	address = {Tamanrasset, Algeria},
	author = {Soumia, Khanfer and Fouad, DJAIZ}
}
@proceedings {63338,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude du cr{\'e}tac{\'e} sup{\'e}rieur-Tertiaire: Cas de Djebel Arhane, bassin de Ghassira (Aur{\`e}s Central, NE Alg{\'e}rien.},
	journal = {Premier Colloque sur la g{\'e}ologie des Bassins S{\'e}dimentaires Maghr{\'e}bins FSTGAT-USTHB 01 au 03-10},
	year = {2019},
	month = {2019},
	address = {Alger, Alg{\'e}rie},
	author = {Marred, M. and Kherchouche, A. and Sana, Benmansour and Fouad, DJAIZ}
}
@proceedings {63343,
	title = {Essai de caracterisation lithostratigraphiques et pal{\'e}oenvironnementdes formations Eoc{\`e}ne du bassin de Ghassira : Coupe du Kef El-Arous (Aur{\`e}s Central, NE Alg{\'e}rien)},
	journal = {1st National Seminar on GeoSciences and Environment SGSE 19 October 23-24, },
	year = {2019},
	month = {2019},
	address = {Tamanrasset, Algeria},
	author = {Manal, Marred and Fouad, DJAIZ and Abdellah, Boushaba and Bachir, Lamouri and Adila, Kherchouche}
}
@proceedings {63374,
	title = {Evolution tectono-s{\'e}dimentaire du bassin n{\'e}og{\`e}ne de Batna-Ain Touta, limite Aur{\`e}s-Monts de Belezma},
	journal = {Premier Colloque sur la g{\'e}ologie des Bassins S{\'e}dimentaires Maghr{\'e}bins FSTGAT-USTHB 01 au 03-10-},
	year = {2019},
	month = {2019},
	address = {Alger, Alg{\'e}rie},
	author = {Khanfer, S. and Fouad, DJAIZ and Bachir, Lamouri}
}
@proceedings {63576,
	title = {Hydrochemical Characteristics under current condition exploitation usingstatistics methods : case of the Zana- Roknia plain, North east of Algeria},
	journal = {23 {\`e}me Colloque des Bassins S{\'e}dimentaires. 21 {\textendash} 23 novembre },
	year = {2019},
	month = {2019},
	address = {F{\`e}s, Maroc},
	abstract = {
	: This paper is a contribution to evaluate the physicochemical characteristics of the groundwater of Merdja Zana-Chott Saboun. The study of geology with the geophysics highlights the existence of two formations aquifers. The first surface formation, formed by levels of sand, gravel, limestone and clay intercalations, dating to the age of the Mio-PlioQuaternary. The second formation is carbonated and formed primarily by limestones of the lower Cretaceous and superior Jurassic. The covering of surface reaches, in certain places, 150m of thickness in particular near the Chott and a low thickness in the vicinity of the mountains. T: This Thist t t he multivariate statistical techniques, were used to identify the hydrochemical processes and their relation with groundwater quality and to get an insight into the hydrochemical Chott Saboun aquifer groundwater chemistry evaluation. Twenty five samples are analyzed. The Piper diagram showed that water facies are magnesium bicarbonate on the sides of the western reliefs and magnesium chloride-sulphated at the north and the center of the plain. The PCA carried out on three factors revealed that on the factorial design F1-F3, nitrates negatively determine factor 3, indicating the presence of an agriculture pollution. On the factorial design F1-F2, HCO3 - negatively determine the factor 2, indicating the carbonated origin. However, the CA, based on variables, showed that the waters in the region can be classified into three groups according to flow direction while, the CA, based on major ion contents, defined three groups, reflecting the same hydrochemical facies. The first group characterized by Mg2+ and Cl- , HCO3 - . Samples of this group are mostly located in the north and northeastern part of the region. The second group characterized by Mg2+ and SO4 --, Clis located near the Northwestern and western outcrops. The third group coincides with the central part, the lowest of the plain, characterized by Mg2+ and SO4 --. The hydrochemical study made it possible to allot the evaporitic origin to the elements Na+, Mg2+ , K + , Cl- , SO4 - , while for element HCO3 - it results from the carbonated formations. These results showed that the presence of nitrates in the studied area is closely linked to the agricultural activity.

},
	url = {https://23cibs2019.sciencesconf.org/data/pages/Recueil_des_resumes_23cibs_2020.pdf},
	author = {Ali, ATHAMENA and Redha, MENNANI Mohamed and Fouad, DJAIZ}
}
@proceedings {63200,
	title = {La lithostratigraphie de l\&rsquo;Ammonitico Rosso de Djebel Kasserou (Monts de Batna)},
	journal = {Premier Colloque sur la g{\'e}ologie des Bassins S{\'e}dimentaires Maghr{\'e}bins },
	year = {2019},
	month = {2019},
	address = {Alger, Alg{\'e}rie},
	abstract = {
	La r{\'e}gion de Kasserou est situ{\'e}e dans la partie Nord-est des Monts de Batna-Belezma. Le Jurassique dans ces massifs constitue une s{\'e}rie compl{\`e}te qui s{\textquoteright}{\'e}tale du Lias au Tithonique. Cette s{\'e}rie est repr{\'e}sent{\'e}e {\`a} la fois par des formations carbonat{\'e}es et calcaro-dolomitique dans sa partie sud, et marno-calcaire dans sa partie nord dont le pr{\'e}cieux rep{\`e}re de l{\textquoteright}Ammotitico rosso.

},
	url = {https://www.researchgate.net/publication/342734904_La_Lithostratigraphie_de_L\%27Ammonitico_Rosso_du_DjKasserou_Monts_de_Batna},
	author = {Touansa, R. and Fouad, DJAIZ and Mabrouk, Boughdiri}
}
@proceedings {63310,
	title = {Les d{\'e}pots Mioc{\`e}ne de la r{\'e}gion de T{\'e}bessa (Nord-est Alg{\'e}rien) : Analyses s{\'e}dimentologiques, Micropal{\'e}ontologiques et Pal{\'e}oenvironnement},
	journal = {Premier Colloque sur la g{\'e}ologie des Bassins S{\'e}dimentaires Maghr{\'e}bins},
	year = {2019},
	month = {2019},
	author = {Nabil, Defaflia and Benkhedda, A. and Fouad, DJAIZ and Cerif, A. and Djerab-Ruault, M. and Gouadia, L.}
}
@proceedings {63445,
	title = {Les terrasses fluviatiles quaternaires de Oued El Gourzi et oued El Hay (Batna, NE Alg{\'e}rie) : S{\'e}dimentologie Caract{\'e}ristiques de l\&rsquo;Environnement},
	journal = { Le 1er S{\'e}minaire National en G{\'e}osciences et Environnement SGSE},
	year = {2019},
	month = {2019},
	abstract = {
	Les sites d{\textquoteright}{\'e}tudes d{\textquoteright}Oued El Hay et Oued El Gourzi sont situ{\'e}s {\`a} la limite des Monts de Batna-Belezma et les Aur{\`e}s au nord-est de l{\textquoteright}Alg{\'e}rie. Ils font partie du grand bassin hydrographique de chott-Melghir, ils sont limit{\'e} au Nord par le bassin versant des Hautes Plateaux Constantinois, {\`a} l{\textquoteright}Est par le bassin versant d{\textquoteright}Oued L{\textquoteright}Abiod et {\`a} l{\textquoteright}Ouest par le bassin versant d{\textquoteright}Chott- El Hodna. A notre connaissance, aucune analyse s{\'e}dimentologique n{\textquoteright}a {\'e}t{\'e} r{\'e}alis{\'e}e sur les terraces fluviatiles de ces cours d{\textquoteright}eau. Les caract{\`e}res hydrodynamiques de l{\textquoteright}agent de transport et leur environnement de d{\'e}p{\^o}t sont encore mal connus. Ce travail tente une premi{\`e}re analyse p{\'e}tro-physique du contenu du s{\'e}diment et de la granulom{\'e}trie des niveaux identifi{\'e}s.

},
	url = {https://www.researchgate.net/publication/337604159_LES_TERRASSES_FLUVIATILES_QUATERNAIRES_DE_OUED_EL_GOURZI_ET_OUED_EL_HAY_BATNA_NE_ALGERIE_SEDIMENTOLOGIE_ET_CARACTERISTIQUES_DE_L{\textquoteright}ENVIRONNEMENT_SEDIMENTAIRE_Materiels_et_Methodes},
	author = {Fouad, DJAIZ and Bachir, Lamouri and Mabrouk, Boughdiri and Rachid, Touansa and Abdellah, Boushaba and Manel, Mrred and Soumia, Khaner and Imen, Chairat}
}
@proceedings {63390,
	title = {Reconsideration of the Cenomanian-Turonian stratigraphics units in the Tebessa region (Algero-TunisienConfines): Petroleum implications},
	journal = {The 1st National Seminar in Geosciences and Environment (SGSE 2019)},
	year = {2019},
	month = {2019},
	address = {Tamanrasset, Algeria},
	abstract = {
	The Algero-Tunisian confines (Tebessa region) is partially composed of Cenomano- Turonian carbonate outcrops; therefore, it presents a good example to highlight the black shale levels reported over a short period, around the Cenomanian-Turonian boundary. The lithostratigraphic study made it possible to specify the paleoenvironment during the Cenomano-Turonian in the Tebessa region. At that time, the depositional environment emphasized a relatively deep, calm and often confined ocean environment that was significantly shalloweron the north part of the study area. The lithology and the distribution of the facies in the Constantine domain allow us to underline the pelagic influences during the Upper Cretaceous and neritic during the lower Cretaceous period. We note a maximum thickness of the Cenomano- Turonian in the southern zones and a minimum (100m) appears further north. This Palaeogeographic organization continue laterally in Tunisia on the extension of the Constantine mole.

},
	url = {https://www.researchgate.net/publication/337011266_Reconsideration_of_the_Cenomanian-Turonian_stratigraphic_units_in_the_Tebessa_region_Algero-Tunisian_Confines_Petroleum_implications},
	author = {Imen, Chairat and Fouad, DJAIZ and Mabrouk, Boughdiri}
}
@article {64953,
	title = {Geological Characterization and contibution of Geophysics to the mobilization of water resources in the ain djasser basin (South-S{\'e}tifien, Algeria NE)},
	journal = {The Euro-arab Organization for Environment,Water and Desert Researches, (2018) Antalya, TurquieThe Euro-arab Organization for Environment,Water and Desert Researches, (2018) Antalya, Turquie},
	year = {2018},
	month = {2018},
	author = {Fouad, DJAIZ and Nabil, Defaflia and Ali, ATHAMENA and Bachir, Lamouri and Mabrouk, Boughdiri and Halima, BELALITE and Abdellah, Boushaba}
}
@proceedings {65170,
	title = {The Impact of the Mobilization of Water Resources in Semi-Arid Areas on Sustainable Development: The Case of Timgad Basin, Northeastern of Algeria},
	journal = {Conference of the Arabian Journal of Geosciences},
	year = {2018},
	month = {2018},
	pages = {355-357},
	publisher = {Springer},
	author = {Ali, ATHAMENA and Redha, MENANI Mohamed and Fouad, DJAIZ and Halima, BELALITE}
}
@proceedings {64721,
	title = {Qualit{\'e} des eaux de surface d\&$\#$39;Oued Saf-Saf (Nord Est Algerien)},
	journal = {4eme Colloque International, les G{\'e}osciences au service du D{\'e}veloppement durable, universit{\'e} Larbi Tebessi, 22 novembre},
	year = {2018},
	month = {2018},
	address = {Tebessa, Algeria},
	author = {Sami, Kemoukh and Fouad, DJAIZ and Ali, ATHAMENA}
}
@proceedings {64564,
	title = {Impacts des plans d\&$\#$39;Eau sur les r{\'e}gimes hydro-climatiques a l\&$\#$39;{\'e}chelle d\&$\#$39;un bassin verssant, cas du barrage de Beni Haroun, Milan Est Algerien},
	journal = {Colloque international Eau{\textendash}Soci{\'e}t{\'e}{\textendash}Climat{\textquoteright}2017 (ESC-2017),  le 2, 3 et 4 Octobre},
	year = {2017},
	month = {2017},
	address = {Hammamet, Tunis},
	author = {Ali, ATHAMENA and Fouad, DJAIZ and Halima, Bilalite and Z, Ghenima and S, Teffaha and K, Kihel}
}
@article {65470,
	title = {Geological, Hydrological and Hydrogeological Characterization of the Timgad\&rsquo;s Basin (Aures, Algeriane) for the Mobilization of Water Resources},
	journal = {International Journal of Environment and Water ISSN 2052-3408International Journal of Environment and Water ISSN 2052-3408},
	volume = {Vol 5},
	year = {2016},
	month = {2016},
	pages = {pp 143},
	abstract = {The basin of Timgad is located in the Aures. It is characterized by an average annual precipitation which reaches 800 mm. Hydrology tributary of the relief is the direct result of surface water and snowmelt from the heights of the Massif of Ch{\'e}lia. The origin of groundwater: semi-deep to deep aquifer is mainly from the infiltration of precipitation in the geological layers. This rock forms a water table that is intersected by drilling to a depth of 137-400 m giving a flow rate of 6 l / s. and white fractured sandstone forming a confined aquifer 190 m with a flow rate of 28 l / s. The check of geo-electric results of the basin show that the Miocene and Cretaceous layers have important thickness, they are heterogeneous and may contain large aquifer at different levels. The influence of vertical normal faults makes possible an exchange of waters between theses aquifers. The implementation of dam project in the basin will minimize the silting, regulate the flow rate, and contribute to the irrigation of the plain, it can be used for industry too. The objective of this approach is the mobilization of surface water resources decided by the government for a rational and planned of this vital factor which is water. Caract{\'e}risation g{\'e}ologique, hydrologique et hydrog{\'e}ologique du bassin de Timgad (Aur{\`e}s, Alg{\'e}rie NE), pour la mobilisation des ressources hydriques R{\'e}sum{\'e} : Le bassin de Timgad est situ{\'e}e dans les Aur{\`e}s. Il est caract{\'e}ris{\'e} par une moyenne annuelle des pr{\'e}cipitations de l{\textquoteright}ordre de 800 mm. L{\textquoteright}hydrologie tributaire du relief est la cons{\'e}quence directe des eaux de surface et de la fonte des neiges provenant des hauteurs du massif de Ch{\'e}lia. L{\textquoteright}alimentation de l{\textquoteright}eau souterraine des diff{\'e}rentes nappes phr{\'e}atiques profondes {\`a} semi-profonde provient essentiellement de l{\textquoteright}infiltration des eaux de pluies dans les couches g{\'e}ologiques. Ce cort{\`e}ge de roche forme une nappe libre qui est recoup{\'e}e par des forages sur une profondeur de 137-400 m fournissant un d{\'e}bit de 6 l/s. et des gr{\'e}s blancs grossiers fractur{\'e}s formant une nappe captive {\`a} 190 m avec un d{\'e}bit de 28 l/s. L{\textquoteright}examen des coupes g{\'e}o{\'e}lectriques du bassin montrent que les formations du mioc{\`e}ne et du cr{\'e}tac{\'e} sont dont l{\textquoteright}ensemble, {\'e}pais, h{\'e}t{\'e}rog{\`e}ne et susceptible de contenir de grandes potentialit{\'e}s d{\textquoteright}aquif{\`e}res {\`a} des niveaux diff{\'e}rents. L{\textquoteright}influence de failles normales verticales rend possible une {\'e}ventuelle alimentation des aquif{\`e}res entres eux. L{\textquoteright}importance de l{\textquoteright}implantation d{\textquoteright}ouvrage de retenue dans le bassin est de minimiser le ph{\'e}nom{\`e}ne d{\textquoteright}envasement, de r{\'e}guler le d{\'e}bit d{\textquoteright}{\'e}coulement et de contribuer {\`a} l{\textquoteright}irrigation de la plaine ainsi que l{\textquoteright}alimentation des briqueteries. L{\textquoteright}objectif de cette approche, est la mobilisation des ressources en eaux superficielles d{\'e}cid{\'e}e par l{\textquoteright}{\'e}tat en vue d{\textquoteright}une utilisation rationnelle et planifi{\'e}e de ce facteur vital qui et l{\textquoteright}eau.},
	author = {Fouad, DJAIZ and N, Defaflia and Nafaa, Brinis and Ali, ATHAMENA and R, Marmi}
}
@article {65826,
	title = {Establishment theoretical of recommendation fertilization guide of vegetable crops in Algeria: concept and validation, ISSN 2349-0837},
	journal = {JOURNAL OF ADVANCES IN AGRICULTUREJOURNAL OF ADVANCES IN AGRICULTURE},
	volume = {Volume 5},
	year = {2015},
	month = {2015},
	pages = {pp 606-620},
	abstract = {The goal of fertilization is to meet the nutritional needs of plants by completing the supply of soil nutrients in an economically profitable and environmentally friendly. Achieving on-farm optimum economic crop yields of marketable quality with minimum adverse environmental impact requires close attention to fertilization guide. The recommendations seek to do this by ensuring that the available supply of plant nutrients in soil is judiciously supplemented by additions of nutrients in fertilizers. The objective is that crops must have an adequate supply of nutrients, and many crops show large and very profitable increases in yield from the correct use of fertilizers to supply nutrients. The main objective of this work is to establishing a reference guide of fertilization of vegetable crops and cereal in Algeria. To meet this objective, we have processes in two steps: 1) Establishment of theoretical fertilizer recommendation from international guide of crop fertilization; 2) Validation of these developed theoretical fertilizer recommendation by trials in the fields. Sixteen fertilization guides of vegetable crops from the Canadian provinces (5 guides), USA (10 guides) and countries of northern Europe England (1 guide). Generally, the rating of these recommendation is ranging from poor soil to soil exceedingly rich; however, the numbers of fertility classes are very different. Indeed, Quebec Ontario, Minnesota, Wisconsin New England, Maryland and Kentucky and Florida guides are subdivided into 5 fertility classes, ranging from poor soil to soil exceedingly rich. The recommendation of New Brunswick and Manitoba contain six classes. The recommendation of Michigan, Nova Scotia and England contain 10 and 7 fertility classes respectively. The recommendation fertilizer of New York and New Jersey have 3classes. Unlike the systems of fertilization recommendation mentioned above, the recommendation fertilizer of Pennsylvania is based on continuous models of P, K and contains 34 classes for P and 22 classes K. Then we standardized the P soil analysis with conversion equations (Olsen method) and units of measurement (kg/ha, mg/kg{\^a}{\texteuro}{\textbrokenbar}).Following this procedure we transformed discontinued systems of fertility classes in to continuous models to facilitate comparison between the different fertilization recommendation models in one hand, in other hand to obtain critical value (CV).Finally, we used statistics of the conditional expectation in order to generate the theoretical recommendation fertilization guide of fertilization with 7 fertility classes (VL, L, M, MH, OP, H and VH). The next step was calibrating soil tests against yield responses to applied nutrient in field experiments. A database (not published data) from agriculture and agri-food Canada, were used. Production of pumpkin responded positively and significantly to P or K soil fertility levels, increases being observed with P more often than with K. According to the Cate-Nelson methods, the critical value of Olsen-P in the top 20 cm of soil was about 25 mg/kg: at values of greater than or equal to 25 mg/kg, crops achieved about 80\% of their maximal yield in the absence of fertilizer application. The CV of K in soil for this crop was about 140 mg/kg. The CV found was very close to this generated by the theoretical method for recommendation of fertilization guide. Finally, we used the procedure of Cope and Rouse in both sides of the CV in order to make subdivisions of different groups of soil fertility. One calibrates the soil-test value against yield response to tile nutrient to predict fertilizer requirement.},
	author = {Mahtali, Sbih and Zoubeir, Bensid and Zohra, Bounouara and Fouad, DJAIZ and Youcef, Ferrag}
}
@article {66063,
	title = {Impact de la mobilisation des ressources hydriques dans les zones semi arides sur le d{\'e}veloppement durable, Cas du bassin de Timgad, Alg{\'e}rie, ISSN 2052-3408},
	journal = {International Journal of Environment \& WaterInternational Journal of Environment \& Water},
	volume = {Volume 4},
	year = {2015},
	month = {2015},
	pages = {pp 118-123},
	abstract = {La retenue collinaire est un ouvrage destin{\'e} g{\'e}n{\'e}ralement {\`a} am{\'e}liorer une agricultureexistante par l{\textquoteright}irrigation de petits p{\'e}rim{\`e}tres et par cons{\'e}quent am{\'e}liorer les terres irrigu{\'e}es,elle peut avoir d{\textquoteright}autres objectifs.L{\textquoteright}{\'e}tude de faisabilit{\'e} de tout terrain (r{\'e}gion) restefondamentale avant d{\textquoteright}entreprendre tout projet de recherche appliqu{\'e}e. Notre travailpropos{\'e} rev{\^e}t une importance socio-{\'e}conomique pour la r{\'e}gion de Timgad. Les r{\'e}sultats de ce travail constituent un apport scientifique utilisable aussi bien par les op{\'e}rateurs socio-{\'e}conomiques que les d{\'e}cideurs pour tout plan d{\textquoteright}am{\'e}nagement. Dans la r{\'e}gion {\'e}tudi{\'e}e, Les ressources hydriques sont en {\'e}troite relation avec les formations g{\'e}ologiques de la r{\'e}gion, donc l{\textquoteright}analyse de ces derniers est primordial. L{\textquoteright}objectif principal de l{\textquoteright}implantation de la retenue de Foum Toub est de contribuer {\`a} l{\textquoteright}irrigation de la plaine de Foum Toub, de r{\'e}gulariser le d{\'e}bit de l{\textquoteright}Oued Foum Toub et de minimiser le ph{\'e}nom{\`e}ne d{\textquoteright}envasement du barrage de Koudiet Lemdaour. Pour cela, les sites retenus pour la construction de cet ouvrage sont repr{\'e}sent{\'e}s par un substratum imperm{\'e}able. Les mat{\'e}riaux meubles, favorable pour servir de zones d{\textquoteright}emprunt sont localis{\'e}s dans les d{\'e}pressions avoisinantes ainsi que les gr{\`e}s qui peuvent {\^e}tre utilis{\'e}s comme mat{\'e}riaux de construction de la digue.},
	author = {Ali, ATHAMENA and Redha, MENANI Mohamed and Malika, ATHAMENA and Fouad, DJAIZ}
}
@article {66062,
	title = {Impact de la mobilisation des ressources hydriques dans les zones semi- arides sur le d{\'e}veloppement durable, Cas du bassin de Timgad, Alg{\'e}rie nord oriental},
	journal = {International Journal of Environment and WaterInternational Journal of Environment and Water},
	volume = {Vol.2},
	year = {2015},
	month = {2015},
	abstract = {La retenue collinaire est un ouvrage destin{\'e} g{\'e}n{\'e}ralement {\`a} am{\'e}liorer une agriculture existante par l{\textquoteright}irrigation de petits p{\'e}rim{\`e}tres et par cons{\'e}quent am{\'e}liorer les terres irrigu{\'e}es, elle peut avoir d{\textquoteright}autres objectifs. L{\textquoteright}{\'e}tude de faisabilit{\'e} de tout terrain (r{\'e}gion) reste fondamentale avant d{\textquoteright}entreprendre tout projet de recherche appliqu{\'e}e. Notre travail propos{\'e} rev{\^e}t une importance socio-{\'e}conomique pour la r{\'e}gion de Timgad. Les r{\'e}sultats de ce travail constituent un apport scientifique utilisable aussi bien par les op{\'e}rateurs socio-{\'e}conomiques que les d{\'e}cideurs pour tout plan d{\textquoteright}am{\'e}nagement. Dans la r{\'e}gion {\'e}tudi{\'e}e, Les ressources hydriques sont en {\'e}troite relation avec les formations g{\'e}ologiques de la r{\'e}gion, donc l{\textquoteright}analyse de ces derniers est primordial. L{\textquoteright}objectif principal de l{\textquoteright}implantation de la retenue de Foum Toub est de contribuer {\`a} l{\textquoteright}irrigation de la plaine de Foum Toub, de r{\'e}gulariser le d{\'e}bit de l{\textquoteright}Oued Foum Toub et de minimiser le ph{\'e}nom{\`e}ne d{\textquoteright}envasement du barrage de Koudiet Lemdaour. Pour cela, les sites retenus pour la construction de cet ouvrage sont repr{\'e}sent{\'e}s par un substratum imperm{\'e}able. Les mat{\'e}riaux meubles, favorable pour servir de zones d{\textquoteright}emprunt sont localis{\'e}s dans les d{\'e}pressions avoisinantes ainsi que les gr{\`e}s qui peuvent {\^e}tre utilis{\'e}s comme mat{\'e}riaux de construction de la digue.},
	author = {Ali, ATHAMENA and Redha, MENANI Mohamed and Malika, ATHAMENA and Fouad, DJAIZ}
}
@book {65920,
	title = {La mobilisation des ressources hydriques dans le bassin de Timgad (Aur{\`e}s, Alg{\'e}rie NE)},
	year = {2015},
	month = {2015},
	author = {Fouad, DJAIZ and Ramdane, Marmi and Ali, Ayhamena and Nafaa, Brinis}
}
@book {65921,
	title = {Le bassin n{\'e}og{\`e}ne de Timgad : Pal{\'e}ocourants et s{\'e}dimentation (Alg{\'e}rie Nord-Orientale)},
	year = {2015},
	month = {2015},
	author = {Fouad, DJAIZ and Ramdane, Marmi}
}
@book {66312,
	title = {caract{\'e}risation g{\'e}ologique, hydrologique et hydrog{\'e}ologique du bassin de timgad (Aur{\`e}s, Alg{\'e}rie NE), pour la mobilisation des ressources hydrique},
	volume = {Vol. 5},
	year = {2014},
	month = {2014},
	address = {Hammamet (Tunisie)},
	author = {Fouad, DJAIZ and Ali, ATHAMENA and Malika, ATHAMENA and Ramdane, Marmi and Nafaa, Brinis and Redha, MENANI Mohamed}
}
@book {66206,
	title = {Etude de la salinit{\'e} des eaux souterraines dans les zones arides Cas de l\&rsquo;aquif{\`e}re d\&rsquo;El-Outaya R{\'e}gion Nord ouest de Biskra \&ndash; Algerie.},
	year = {2014},
	month = {2014},
	address = {Amman Jordan},
	author = {Nafaa, Brinis and Abderahmane, Boudoukha and Fouad, DJAIZ}
}
@article {66205,
	title = {Etude de la salinit{\'e} des eaux souterraines dans les zones arides Cas de l\&rsquo;aquif{\`e}re d\&rsquo;El-Outaya R{\'e}gion Nord ouest de Biskra \&ndash; ALGERIE; ISSN 2052-3408,},
	journal = {International Journal of Environment \& WaterInternational Journal of Environment \& Water},
	volume = {Vol 3},
	year = {2014},
	month = {2014},
	abstract = {Le bassin d{\textquoteright}El-Outaya se trouve dans la wilaya de BISKRA, une zone aride au sud alg{\'e}rien {\`a} environ 500 Km au sud de la capital Alger. Il constitue une ressource importante pour l{\textquoteright}eau d{\textquoteright}irrigation en plus d{\textquoteright}un barrage {\`a} l{\textquoteright}amont. La population de la plaine d{\'e}passe 11 000 habitants, leur activit{\'e} principale est l{\textquoteright}agriculture.La plaine {\'e}tudi{\'e}e correspond {\`a} un bassin subsident orient{\'e} sensiblement E.NE {\textendash} W.SW et situ{\'e} entre deux anticlinaux. Il se trouve au nord de l{\textquoteright}anticlinal du Dj.Bou Rhezel (Biskra) et au sud du d{\^o}me de Dj. El Melah. Il a fonctionn{\'e} comme un bassin de s{\'e}dimentation pendant tout le N{\'e}og{\`e}ne. Il est constitu{\'e} {\`a} la base par un mioc{\`e}ne laguno-marin, recouvert par du messinien (pontien) gr{\'e}seux fluviatile, puis par des poudingues plioc{\`e}nes. Les termes sup{\'e}rieurs, plus particuli{\`e}rement plioc{\`e}nes, sont fortement inclin{\'e}s vers le centre du bassin o{\`u} ils disparaissent sous une {\'e}paisseur consid{\'e}rable du Quaternaire.Le d{\'e}pouillement des analyses chimiques a aboutit {\`a} trois faci{\`e}s chimiques: Le faci{\`e}s chlorur{\'e} sodique, le faci{\`e}s sulfat{\'e} magn{\'e}sien et le faci{\`e}s sulfat{\'e} sodique.Le suivi des variables chimiques dominant selon les axes des {\'e}coulements souterrains permet de suivre l{\textquoteright}{\'e}volution des faci{\`e}s dans aquif{\`e}re ainsi que l{\textquoteright}origine de chaque faci{\`e}s.},
	author = {Nafaa, Brinis and Abderahmane, Boudoukha and Fouad, DJAIZ}
}
@article {66204,
	title = {Etude de la salinit{\'e} des eaux souterraines dans les zones arides Cas de l\&rsquo;aquif{\`e}re d\&rsquo;El-Outaya R{\'e}gion Nord ouest de Biskra \&ndash; ALGERIE, 2014. ISSN 2052-3408.},
	journal = {International Journal of Environment \& WaterInternational Journal of Environment \& Water},
	volume = {Vol 3},
	year = {2014},
	month = {2014},
	author = {Nafaa, Brinis and Abderahmane, Boudoukha and Fouad, DJAIZ}
}
@article {66313,
	title = {Importance des ressources hydriques et leurs impacts sur le d{\'e}veloppement durable dans le bassin de Timgad (Alg{\'e}rie nord orientale), ISSN 2170-1318,D{\'e}cembre 2014},
	journal = {Journal of Arid And Environment (AJAE)Journal of Arid And Environment (AJAE)},
	volume = {vol. 4},
	year = {2014},
	month = {2014},
	pages = {pp 78-87},
	abstract = {Located in the Aures mountains Foum Toub is characterized by an annual average rainfall of\&nbsp; 800mm. The hydrology subordinate to the terrain is the direct consequence of surface waters and of snow melting from the heights of Chelia Mountain. The aim of the implantation of the Foum Toub backwater is to minimize the siltation phenomenon at the upstream of the Koudiate El Mdaour dam, to regularize the Rebaa creek flow which runs from south to north and to contribute to the irrigation of the Foum Toub plain. This study puts the emphasis on the mobilization of surface water resources, a policy of the Ministry of Agriculture and Rural Development with a view to rationalize the use and planning of this vital factor, i.e. water. The site selected for the construction of this structure is characterized by a waterproof marly substratum, favourable for implanting the dike and the basin. The clay-silty-gravelly material furniture localized in the depressions as well as sandstones are used as areas for the construction materials of this structure. Stability is one of the most important parameters to take into account for the choice of the site, so as to avoid any problem linked to the withdrawal-swelling phenomena on the banks of creek. However, the sliding possibility, however weak it is, can be generated on the left bank of the creek within deposit and recent silt. The choice of the site for the implantation of this hydraulic structure remains subject to laboratory tests.},
	author = {Fouad, DJAIZ and Ali, ATHAMENA and Malika, ATHAMENA}
}
@book {66453,
	title = {Risque de pollution des eaux souterraines de la plaine de Zana, Est Alg{\'e}rien},
	year = {2014},
	month = {2014},
	address = {Hammamet (Tunisie)},
	author = {Ali, ATHAMENA and Malika, ATHAMENA and Fouad, DJAIZ}
}
@book {66784,
	title = {Accident probablement responsable de la pr{\'e}sence des sources thermales, Cas de la source thermale de Guergima, Batna Est Alg{\'e}rien},
	year = {2013},
	month = {2013},
	author = {Ali, ATHAMENA and Malika, ATHAMENA and Fouad, DJAIZ}
}
@book {66582,
	title = {Etude des faci{\`e}s chimiques des eaux souterraines de la plaine d\&rsquo;El-Outaya au sud alg{\'e}rien. Types et {\'e}volution dans l\&rsquo;espace aquif{\`e}re},
	year = {2013},
	month = {2013},
	author = {Nafaa, Brinis and Abderahmane, Boudoukha and Fouad, DJAIZ}
}
@book {66782,
	title = {G{\'e}othermie des eaux souterraines cas de la source thermale de Guergima, Batna est-alg{\'e}rien},
	year = {2013},
	month = {2013},
	author = {Ali, ATHAMENA and Malika, ATHAMENA and Fouad, DJAIZ}
}
@book {66683,
	title = {Importance de la mobilisation des ressources hydriques et l\&rsquo;impact sur le d{\'e}veloppement durable dans le bassin de Timgad Alg{\'e}rie nord orientale},
	year = {2013},
	month = {2013},
	author = {Fouad, DJAIZ and Malika, ATHAMENA and Ali, ATHAMENA}
}
@book {66783,
	title = {La contribution de la g{\'e}ophysique dans les {\'e}tudes thermales, cas des sources des monts des Aures},
	year = {2013},
	month = {2013},
	author = {Ali, ATHAMENA and Malika, ATHAMENA and Fouad, DJAIZ}
}
@book {66678,
	title = {Le Bassin n{\'e}og{\`e}ne de Timgad et son aspect structural (atlas saharien alg{\'e}rien oriental)},
	year = {2013},
	month = {2013},
	address = {TEBESSA {\textendash}ALGERIE},
	author = {Fouad, DJAIZ and Ramdane, Marmi}
}
@article {66680,
	title = {Le remplissage s{\'e}dimentaire du bassin de Timgad et aquif{\`e}res potentiels (Atlas saharien Alg{\'e}rien oriental)\&raquo;.1 septembre 2013, ISSN 1813-548X.},
	journal = {Afrique ScienceAfrique SCIENCE},
	volume = {Vol.09},
	year = {2013},
	month = {2013},
	abstract = {Le bassin de Timgad, orient{\'e} suivant une direction sub-latitudinale, appartient {\`a} l{\textquoteright}Atlas Saharien nord-oriental. Il est bord{\'e} au nord par Dj. Bou Arif-Dj. Fedjoudj-Dj. Tarf et au sud par les Monts des Aur{\`e}s. Il comprend un substratum m{\'e}sozo{\"\i}que correspondant {\`a} une s{\'e}rie marine gr{\'e}so-carbonat{\'e}e, surmont{\'e} en discordance par des formations du N{\'e}og{\`e}ne. Ces derniers sont repr{\'e}sent{\'e}s \&nbsp;essentiellement par des s{\'e}diments d{\'e}tritiques o{\`u} dominent les d{\'e}p{\^o}ts silicoclastiques. La puissance de toute la s{\'e}rie d{\'e}passe les 1000 m{\`e}tres. Le contact, entre les deux s{\'e}ries \&nbsp;lithostratigraphiques, m{\'e}sozo{\"\i}que et n{\'e}og{\`e}nes, est soulign{\'e} par une discordance majeure marqu{\'e}e tant{\^o}t par des conglom{\'e}rats polyg{\'e}niques, tant{\^o}t par des niveaux calcaires souvent gr{\'e}seux. Le Plio-Quaternaire, repr{\'e}sent{\'e} surtout par des s{\'e}diments d{\'e}tritiques grossiers, surmonte en discordance les s{\'e}ries ant{\'e}rieures. Du point de vue structurale, le bassin est affect{\'e} par une tectonique polyphas{\'e}e qui l{\textquoteright}a compartiment{\'e} en blocs dont les accidents transverses NW-SE et NE-SW sont nettement exprim{\'e}s. La phase compressive, situ{\'e}e {\`a} la limite plioc{\`e}ne-quaternaire, serait {\`a} l{\textquoteright}origine du model{\'e} du relief actuel. L{\textquoteright}{\'e}tude g{\'e}ophysique, consistant en l{\textquoteright}exploitation \&nbsp;des profils sismiques et des coupes g{\'e}o {\'e}lectriques, a permis de mettre en {\'e}vidence d{\textquoteright}une part la g{\'e}om{\'e}trie profonde des diff{\'e}rents accidents dans le bassin et les aquif{\`e}res potentiels d{\textquoteright}autre part. Une formation relativement r{\'e}sistante, correspond {\`a} un intervalle gr{\'e}seux du Mioc{\`e}ne, rev{\^e}t un int{\'e}r{\^e}t particulier sur le plan hydrog{\'e}ologique.},
	author = {Fouad, DJAIZ and Nafaa, Brinis and R, Marmi}
}
@article {66679,
	title = {Le remplissage s{\'e}dimentaire du bassin de Timgad et aquif{\`e}res potentiels (atlas saharien Alg{\'e}rien oriental). ISSN 1813-548X.},
	journal = {Afrique SCIENCEAfrique SCIENCE},
	volume = {Vol 09},
	year = {2013},
	month = {2013},
	pages = {pp 66{\textendash}76},
	abstract = {Le bassin de Timgad, orient{\'e} suivant une direction sub-latitudinale, appartient {\`a} l{\textquoteright}Atlas Saharien nord-oriental. Il est bord{\'e} au nord par Dj. Bou Arif-Dj. Fedjoudj-Dj. Tarf et au sud par les Monts des Aur{\`e}s. Il comprend un substratum m{\'e}sozo{\"\i}que correspondant {\`a} une s{\'e}rie marine gr{\'e}so-carbonat{\'e}e, surmont{\'e} en discordance par des formations du N{\'e}og{\`e}ne. Ces derniers sont repr{\'e}sent{\'e}s \&nbsp;essentiellement par des s{\'e}diments d{\'e}tritiques o{\`u} dominent les d{\'e}p{\^o}ts silicoclastiques. La puissance de toute la s{\'e}rie d{\'e}passe les 1000 m{\`e}tres. Le contact, entre les deux s{\'e}ries \&nbsp;lithostratigraphiques, m{\'e}sozo{\"\i}que et n{\'e}og{\`e}nes, est soulign{\'e} par une discordance majeure marqu{\'e}e tant{\^o}t par des conglom{\'e}rats polyg{\'e}niques, tant{\^o}t par des niveaux calcaires souvent gr{\'e}seux. Le Plio-Quaternaire, repr{\'e}sent{\'e} surtout par des s{\'e}diments d{\'e}tritiques grossiers, surmonte en discordance les s{\'e}ries ant{\'e}rieures. Du point de vue structurale, le bassin est affect{\'e} par une tectonique polyphas{\'e}e qui l{\textquoteright}a compartiment{\'e} en blocs dont les accidents transverses NW-SE et NE-SW sont nettement exprim{\'e}s. La phase compressive, situ{\'e}e {\`a} la limite plioc{\`e}ne-quaternaire, serait {\`a} l{\textquoteright}origine du model{\'e} du relief actuel. L{\textquoteright}{\'e}tude g{\'e}ophysique, consistant en l{\textquoteright}exploitation \&nbsp;des profils sismiques et des coupes g{\'e}o {\'e}lectriques, a permis de mettre en {\'e}vidence d{\textquoteright}une part la g{\'e}om{\'e}trie profonde des diff{\'e}rents accidents dans le bassin et les aquif{\`e}res potentiels d{\textquoteright}autre part. Une formation relativement r{\'e}sistante, correspond {\`a} un intervalle gr{\'e}seux du Mioc{\`e}ne, rev{\^e}t un int{\'e}r{\^e}t particulier sur le plan hydrog{\'e}ologique.},
	author = {Fouad, DJAIZ and Nafaa, Brinis and Ramdane, Marmi}
}
@book {66684,
	title = {Les mouvements des sols, G{\'e}orisques et Urbanisation. 2{\`e}me Colloque International sur La Gestion Int{\'e}gr{\'e}e des Ressources en Eau, 22-23 Octobre 2013},
	year = {2013},
	month = {2013},
	publisher = {GIRE, D{\'e}p. Sc. de la Terre et de l{\textquoteright}Univers / Facult{\'e} des Sciences - Universit{\'e} Hadj Lakhdar {\textendash} Batna.},
	organization = {GIRE, D{\'e}p. Sc. de la Terre et de l{\textquoteright}Univers / Facult{\'e} des Sciences - Universit{\'e} Hadj Lakhdar {\textendash} Batna.},
	author = {Fouad, DJAIZ and A, BOUMEZBEUR and Ramdane, Marmi and Ali, ATHAMENA and Redha, MENANI Mohamed}
}
@book {66685,
	title = {Les mouvements des sols,G{\'e}orisques et Urbanisation},
	year = {2013},
	month = {2013},
	author = {Fouad, DJAIZ and A, BOUMEZBEUR and Ramdane, Marmi and Ali, ATHAMENA and Redha, MENANI Mohamed}
}
@book {66681,
	title = {L\&rsquo;apport de la g{\'e}ophysique a la g{\'e}om{\'e}trie des couches profondes et les aquif{\`e}res potentiels du bassin de timgad (Atlas Saharien Alg{\'e}rien Oriental). 22-23 Octobre 2013},
	year = {2013},
	month = {2013},
	address = {Batna},
	author = {Fouad, DJAIZ and Nafaa, Brinis and Ahmed, Inal and Ramdane, Marmi and Redha, MENANI Mohamed}
}
@book {66682,
	title = {L\&rsquo;apport de la g{\'e}ophysique {\`a} la g{\'e}om{\'e}trie des couches profondes et les aquif{\`e}res potentiels du bassin de timgad (Atlas Saharien Alg{\'e}rien Oriental)},
	year = {2013},
	month = {2013},
	author = {Fouad, DJAIZ and Nafaa, Brinis and Ahmed, Inal and Ramdane, Marmi and Redha, MENANI Mohamed}
}
@book {66677,
	title = {Risque naturel li{\'e}e au mouvements des terrains affaissables dans une zone urbaine \&ndash;Batna},
	year = {2013},
	month = {2013},
	author = {Fouad, DJAIZ and Ramdane, Marmi and A, BOUMEZBEUR}
}
@book {66894,
	title = {analyse microfaciologique et d{\'e}coupage s{\'e}quentiel de la s{\'e}rie c{\'e}nomanienne de la coupe de Mennchar Ali Guera (nord-est Alg{\'e}rie)},
	year = {2012},
	month = {2012},
	author = {S, Benmansour and Fouad, DJAIZ and Ouahab, Yahaoui Abedel}
}
@book {67012,
	title = {Caract{\'e}risation g{\'e}ologique et hydrog{\'e}ologique du bassin de Timgad},
	year = {2012},
	month = {2012},
	author = {Fouad, DJAIZ and Ramdane, Marmi}
}
@book {67014,
	title = {Etude g{\'e}ologique du bassin de Timgad},
	year = {2012},
	month = {2012},
	author = {Fouad, DJAIZ and Nafaa, Brinis}
}
@book {67013,
	title = {Etude g{\'e}ologique du bassin de Timgad 2},
	year = {2012},
	month = {2012},
	address = {Ouargla,Alger},
	author = {Fouad, DJAIZ and Nafaa, Brinis and Ahmed, Inal}
}
@book {67285,
	title = {Impact, importance et mobilisation des ressources hydriques dans le bassin mioc{\`e}ne de Timgad},
	year = {2011},
	month = {2011},
	author = {Fouad, DJAIZ and Nafaa, Brinis and Ahmed, Inal and Ali, ATHAMENA and Malika, ATHAMENA}
}
@book {67442,
	title = {D{\'e}couverte de nouveaux gisements de Mammif{\`e}res dans le Constantinois (Alg{\'e}rie nord-orientale) : Int{\'e}r{\^e}t biostratigraphique},
	year = {2010},
	month = {2010},
	author = {Ramdane, Marmi and C, Benabbas and Fouad, DJAIZ}
}
@book {67515,
	title = {Importance des carri{\`e}res dans la vie socio-{\'e}conomique et leurs impact sur l\&$\#$39;environnement (Batna\&ndash;Ain Touta)},
	year = {2010},
	month = {2010},
	address = {Tlemcen, Alger},
	author = {Fouad, DJAIZ and Nafaa, Brinis and Ahmed, Inal and Manel, Cheriet}
}
@book {67516,
	title = {Importance des carri{\`e}res dans la vie socio-{\'e}conomique et leurs impacts sur l\&rsquo;environnement (Batna-Ain Touta)},
	year = {2010},
	month = {2010},
	author = {Fouad, DJAIZ and Nafaa, Brinis and Ahmed, Inal}
}
@book {67674,
	title = {Impact des ressources hydriques sur le d{\'e}veloppement durable dans le basin de Timgad-Alg{\'e}rie Nord Orientale},
	year = {2009},
	month = {2009},
	author = {Fouad, DJAIZ and Ali, ATHAMENA}
}
@article {62282,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude p{\'e}tro-structurale de la bordure Est et Sud Est du socle de la Petite Kabylie Nord-Est Alg{\'e}rie. Juin (2008)},
	journal = {Sciences \& TechnologieSciences \& Technologie},
	year = {2008},
	month = {2008},
	pages = {pp. 71-76},
	abstract = {The area of study belongs to the higher building of the base of Small Kabylie. It consists of several tectono-lithological units affected by a metamorphism {\'e}pizonale to m{\'e}sozonale of low pressure and high temperature. This last estimated at P=4-5 Kbar and T=650-700{\textdegree}C is underlined by the presence of the veins of leucozones and the myrm{\'e}kite thus near to the field of partial fusion. The structural draft shows the superposition of schisto-sandy units {\'e}pizonales on units of higher rank. This area is overcome in its Western and Eastern part by formations of Oligo-Mioc{\`e}ne-Kabyle. The study of the syn-schistous deformation highlights an extensive component at vergency is and of the lin{\'e}ations of stretching of direction E - W (D1) with a virgation towards the NNE. This deformation induces the shape in arc marked by plans of schistosity and foliation resulting from the deformation (D2) due to the accommodation of the total overlapping of the building of Beni-Fergu{\`e}ne towards the NW. Alpine and eo-alpine post-schistous deformations of lower (Pt), at vergency East and South, are highlighted.},
	author = {Fouad, DJAIZ}
}
@book {62283,
	title = {The impact of hydraulic resources on sustainable development of the Timgad basin north-east of Algerie},
	year = {2008},
	month = {2008},
	author = {Fouad, DJAIZ and Ali, ATHAMENA}
}
@book {62154,
	title = {Cons{\'e}quences de la phase tectonique alpine sur les d{\'e}formations syn-schisteuses tardi-hercyniennes du socle de la Petite Kabylie (Alg{\'e}rie Nord-orientale)},
	year = {2007},
	month = {2007},
	author = {Fouad, DJAIZ and Y, Mahdjoub}
}
@book {62153,
	title = {Etude stratigraphique et s{\'e}dimentologique de Manchar Ali Guera, versant Nord de Djebel Bou Arif (Aur{\`e}s, Nord est D\&rsquo;Alg{\'e}rie)},
	year = {2007},
	month = {2007},
	author = {Fouad, DJAIZ and S, Benmansour}
}
@book {62152,
	title = {L\&rsquo;hypoth{\`e}se de l\&rsquo;existence d\&rsquo;un d{\^o}me gneissique extensif dans le secteur de Bouchtata-Tamalous bordure orientale du socle de la Petite Kabylie (Alg{\'e}rie nord-orientale)},
	year = {2007},
	month = {2007},
	author = {Fouad, DJAIZ and Ramdane, Marmi}
}
@book {62037,
	title = {Caract{\'e}ristiques g{\'e}ologiques, g{\'e}otechniques et hydrologiques d\&rsquo;un site destin{\'e} {\`a} l\&rsquo;am{\'e}nagement d\&rsquo;un ouvrage hydraulique (Aur{\`e}s, Alg{\'e}rie Nord-Orientale)},
	year = {2006},
	month = {2006},
	author = {Fouad, DJAIZ and Ramdane, Marmi and Ali, ATHAMENA}
}
@book {62075,
	title = {Observations g{\'e}ologiques des glissements de terrain dans le Constantinois : cas du tron{\c c}on d\&rsquo;autoroute Massinissa, Didouche Mourad et Anouche Ali. (Alg{\'e}rie nord-orientale)},
	year = {2006},
	month = {2006},
	author = {Ramdane, Marmi and A, BOUMEZBEUR and Fouad, DJAIZ}
}
@book {61968,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude p{\'e}tro-structurale du secteur Bouchtata-Tamalous situ{\'e} dans la bordure orientale du socle de la Petite Kabylie},
	year = {2005},
	month = {2005},
	author = {Fouad, DJAIZ and Ramdane, Marmi}
}
@book {61967,
	title = {Faisabilit{\'e} de la retenue collinaire de Foum Toub : Etude g{\'e}ologique et g{\'e}otechnique (Aur{\`e}s, Batna)},
	year = {2005},
	month = {2005},
	author = {Fouad, DJAIZ and A, BOUMEZBEUR and Ramdane, Marmi and Nafaa, Brinis and Ali, ATHAMENA}
}
@book {61969,
	title = {Faisabilit{\'e} g{\'e}ologique de la retenue collinaire de Foum toub},
	year = {2005},
	month = {2005},
	author = {Fouad, DJAIZ and Ramdane, Marmi and A, BOUMEZBEUR and Nafaa, Brinis}
}
@book {61965,
	title = {L\&rsquo;apport g{\'e}otechnique {\`a} l\&rsquo;{\'e}tude du ph{\'e}nom{\`e}ne du mouvement du sol : retrait gonflement},
	year = {2005},
	month = {2005},
	author = {Fouad, DJAIZ and A, BOUMEZBEUR and Ramdane, Marmi}
}
@book {61966,
	title = {Risque naturels li{\'e}e au ph{\'e}nom{\`e}ne retrait-gonflement des sols \&laquo; Cas de Djerma-Batna \&raquo;},
	year = {2005},
	month = {2005},
	author = {Fouad, DJAIZ and A, BOUMEZBEUR and Ramdane, Marmi}
}
@book {61990,
	title = {Tectonique compressive polyphas{\'e}e dans la cha{\^\i}ne alpine en Alg{\'e}rie : l\&rsquo;exemple du M{\^o}le Constantinois et de son avant-pays},
	year = {2005},
	month = {2005},
	author = {Ramdane, Marmi and R, Guiraud and Fouad, DJAIZ}
}
@book {61913,
	title = {Etude des pal{\'e}o-courants dans les formations du barr{\'e}mien et du mioc{\`e}ne : Nouvelle hypoth{\`e}se sur les apports d{\'e}tritiques mioc{\`e}nes dans l\&rsquo;Aur{\`e}s Nord},
	year = {2004},
	month = {2004},
	author = {Ramdane, Marmi and Fouad, DJAIZ}
}
@book {61902,
	title = {Pal{\'e}o-environnement des calcaires {\`a} Rudistes d\&rsquo;{\^a}ge Coniacien inf{\'e}rieur (Berriche) des Monts de Belezma (Alg{\'e}rie orientale)},
	year = {2004},
	month = {2004},
	author = {K, Yahiaoui and Ahmed, Inal and Fouad, DJAIZ}
}
@book {61781,
	title = {Etude p{\'e}tro-structurale de la bordure sud est du socle de la Petite Kabylie \&ndash;r{\'e}gion de Sidi Mezghiche, Alg{\'e}rie},
	year = {2000},
	month = {2000},
	author = {Fouad, DJAIZ and Y, Mahdjoub}
}
