<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Bachir, Lamouri</style></author><author><style face="normal" font="default" size="100%">Bousahaba, A.</style></author><author><style face="normal" font="default" size="100%">Halima, BELALITE</style></author><author><style face="normal" font="default" size="100%">Rachid, Touansa</style></author><author><style face="normal" font="default" size="100%">Soumia, Khanfer</style></author><author><style face="normal" font="default" size="100%">Manal, Marred</style></author><author><style face="normal" font="default" size="100%">Imen, Chairat</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et apport de la géophysique pour la mobilisation des ressources hydriques dans le bassin de Gadaine (Ain Yagout, Algérie NE)</style></title><secondary-title><style face="normal" font="default" size="100%">Le 1er Séminaire National en Géosciences et Environnement 23– 24 Octobre (SGSE-2019)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2019</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">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</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Tamanrasset, Algeria</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Hocine, Nadji</style></author><author><style face="normal" font="default" size="100%">Hmmimed, M.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et apport de la géophysique pour la mobilisation des ressources hydriques dans le bassin d&amp;rsquo;El Mather.</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2019</style></date></pub-dates></dates><pub-location><style face="normal" font="default" size="100%">Alger, Algérie</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Soumia, Khanfer</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude du basin Néogène Batna-ain Touta, limite aurès-Monts de Belezma</style></title><secondary-title><style face="normal" font="default" size="100%"> 1st National Seminar on GeoSciences and Environment SGSE 19 October 23-24, </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2019</style></date></pub-dates></dates><pub-location><style face="normal" font="default" size="100%">Tamanrasset, Algeria</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Marred, M.</style></author><author><style face="normal" font="default" size="100%">Kherchouche, A.</style></author><author><style face="normal" font="default" size="100%">Sana, Benmansour</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude du crétacé supérieur-Tertiaire: Cas de Djebel Arhane, bassin de Ghassira (Aurès Central, NE Algérien.</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2019</style></date></pub-dates></dates><pub-location><style face="normal" font="default" size="100%">Alger, Algérie</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Manal, Marred</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Abdellah, Boushaba</style></author><author><style face="normal" font="default" size="100%">Bachir, Lamouri</style></author><author><style face="normal" font="default" size="100%">Adila, Kherchouche</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Essai de caracterisation lithostratigraphiques et paléoenvironnementdes formations Eocène du bassin de Ghassira : Coupe du Kef El-Arous (Aurès Central, NE Algérien)</style></title><secondary-title><style face="normal" font="default" size="100%">1st National Seminar on GeoSciences and Environment SGSE 19 October 23-24, </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2019</style></date></pub-dates></dates><pub-location><style face="normal" font="default" size="100%">Tamanrasset, Algeria</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Khanfer, S.</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Bachir, Lamouri</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Evolution tectono-sédimentaire du bassin néogène de Batna-Ain Touta, limite Aurès-Monts de Belezma</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2019</style></date></pub-dates></dates><pub-location><style face="normal" font="default" size="100%">Alger, Algérie</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Redha, MENNANI Mohamed</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrochemical Characteristics under current condition exploitation usingstatistics methods : case of the Zana- Roknia plain, North east of Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">23 ème Colloque des Bassins Sédimentaires. 21 – 23 novembre </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2019</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://23cibs2019.sciencesconf.org/data/pages/Recueil_des_resumes_23cibs_2020.pdf</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Fès, Maroc</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	: 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-PlioQuaternary. 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 --, Clis 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.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Touansa, R.</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Mabrouk, Boughdiri</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">La lithostratigraphie de l&amp;rsquo;Ammonitico Rosso de Djebel Kasserou (Monts de Batna)</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2019</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/342734904_La_Lithostratigraphie_de_L%27Ammonitico_Rosso_du_DjKasserou_Monts_de_Batna</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Alger, Algérie</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	La région de Kasserou est située dans la partie Nord-est des Monts de Batna-Belezma. Le Jurassique dans ces massifs constitue une série complète qui s'étale du Lias au Tithonique. Cette série est représentée à la fois par des formations carbonatées et calcaro-dolomitique dans sa partie sud, et marno-calcaire dans sa partie nord dont le précieux repère de l’Ammotitico rosso.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Nabil, Defaflia</style></author><author><style face="normal" font="default" size="100%">Benkhedda, A.</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Cerif, A.</style></author><author><style face="normal" font="default" size="100%">Djerab-Ruault, M.</style></author><author><style face="normal" font="default" size="100%">Gouadia, L.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les dépots Miocène de la région de Tébessa (Nord-est Algérien) : Analyses sédimentologiques, Micropaléontologiques et Paléoenvironnement</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2019</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Bachir, Lamouri</style></author><author><style face="normal" font="default" size="100%">Mabrouk, Boughdiri</style></author><author><style face="normal" font="default" size="100%">Rachid, Touansa</style></author><author><style face="normal" font="default" size="100%">Abdellah, Boushaba</style></author><author><style face="normal" font="default" size="100%">Manel, Mrred</style></author><author><style face="normal" font="default" size="100%">Soumia, Khaner</style></author><author><style face="normal" font="default" size="100%">Imen, Chairat</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les terrasses fluviatiles quaternaires de Oued El Gourzi et oued El Hay (Batna, NE Algérie) : Sédimentologie Caractéristiques de l&amp;rsquo;Environnement</style></title><secondary-title><style face="normal" font="default" size="100%"> Le 1er Séminaire National en Géosciences et Environnement SGSE</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2019</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">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'ENVIRONNEMENT_SEDIMENTAIRE_Materiels_et_Methodes</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Les sites d’études d’Oued El Hay et Oued El Gourzi sont situés à la limite des Monts de Batna-Belezma et les Aurès au nord-est de l’Algérie. Ils font partie du grand bassin hydrographique de chott-Melghir, ils sont limité au Nord par le bassin versant des Hautes Plateaux Constantinois, à l’Est par le bassin versant d’Oued L’Abiod et à l’Ouest par le bassin versant d’Chott- El Hodna. A notre connaissance, aucune analyse sédimentologique n'a été réalisée sur les terraces fluviatiles de ces cours d'eau. Les caractères hydrodynamiques de l'agent de transport et leur environnement de dépôt sont encore mal connus. Ce travail tente une première analyse pétro-physique du contenu du sédiment et de la granulométrie des niveaux identifiés.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Imen, Chairat</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Mabrouk, Boughdiri</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Reconsideration of the Cenomanian-Turonian stratigraphics units in the Tebessa region (Algero-TunisienConfines): Petroleum implications</style></title><secondary-title><style face="normal" font="default" size="100%">The 1st National Seminar in Geosciences and Environment (SGSE 2019)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2019</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/337011266_Reconsideration_of_the_Cenomanian-Turonian_stratigraphic_units_in_the_Tebessa_region_Algero-Tunisian_Confines_Petroleum_implications</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Tamanrasset, Algeria</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	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.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Nabil, Defaflia</style></author><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Bachir, Lamouri</style></author><author><style face="normal" font="default" size="100%">Mabrouk, Boughdiri</style></author><author><style face="normal" font="default" size="100%">Halima, BELALITE</style></author><author><style face="normal" font="default" size="100%">Abdellah, Boushaba</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geological Characterization and contibution of Geophysics to the mobilization of water resources in the ain djasser basin (South-Sétifien, Algeria NE)</style></title><secondary-title><style face="normal" font="default" size="100%">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</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2018</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Redha, MENANI Mohamed</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Halima, BELALITE</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The Impact of the Mobilization of Water Resources in Semi-Arid Areas on Sustainable Development: The Case of Timgad Basin, Northeastern of Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Conference of the Arabian Journal of Geosciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2018</style></date></pub-dates></dates><publisher><style face="normal" font="default" size="100%">Springer</style></publisher><pages><style face="normal" font="default" size="100%">355-357</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Sami, Kemoukh</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Qualité des eaux de surface d&amp;#39;Oued Saf-Saf (Nord Est Algerien)</style></title><secondary-title><style face="normal" font="default" size="100%">4eme Colloque International, les Géosciences au service du Développement durable, université Larbi Tebessi, 22 novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2018</style></date></pub-dates></dates><pub-location><style face="normal" font="default" size="100%">Tebessa, Algeria</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Halima, Bilalite</style></author><author><style face="normal" font="default" size="100%">Z, Ghenima</style></author><author><style face="normal" font="default" size="100%">S, Teffaha</style></author><author><style face="normal" font="default" size="100%">K, Kihel</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Impacts des plans d&amp;#39;Eau sur les régimes hydro-climatiques a l&amp;#39;échelle d&amp;#39;un bassin verssant, cas du barrage de Beni Haroun, Milan Est Algerien</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque international Eau–Société–Climat’2017 (ESC-2017),  le 2, 3 et 4 Octobre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2017</style></date></pub-dates></dates><pub-location><style face="normal" font="default" size="100%">Hammamet, Tunis</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">N, Defaflia</style></author><author><style face="normal" font="default" size="100%">Nafaa, Brinis</style></author><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">R, Marmi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geological, Hydrological and Hydrogeological Characterization of the Timgad&amp;rsquo;s Basin (Aures, Algeriane) for the Mobilization of Water Resources</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Environment and Water ISSN 2052-3408International Journal of Environment and Water ISSN 2052-3408</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2016</style></date></pub-dates></dates><number><style face="normal" font="default" size="100%">Issue 3</style></number><volume><style face="normal" font="default" size="100%">Vol 5</style></volume><pages><style face="normal" font="default" size="100%">pp 143</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">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 Chélia. 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. Caractérisation géologique, hydrologique et hydrogéologique du bassin de Timgad (Aurès, Algérie NE), pour la mobilisation des ressources hydriques Résumé : Le bassin de Timgad est située dans les Aurès. Il est caractérisé par une moyenne annuelle des précipitations de l’ordre de 800 mm. L’hydrologie tributaire du relief est la conséquence directe des eaux de surface et de la fonte des neiges provenant des hauteurs du massif de Chélia. L’alimentation de l’eau souterraine des différentes nappes phréatiques profondes à semi-profonde provient essentiellement de l’infiltration des eaux de pluies dans les couches géologiques. Ce cortège de roche forme une nappe libre qui est recoupée par des forages sur une profondeur de 137-400 m fournissant un débit de 6 l/s. et des grés blancs grossiers fracturés formant une nappe captive à 190 m avec un débit de 28 l/s. L’examen des coupes géoélectriques du bassin montrent que les formations du miocène et du crétacé sont dont l’ensemble, épais, hétérogène et susceptible de contenir de grandes potentialités d’aquifères à des niveaux différents. L’influence de failles normales verticales rend possible une éventuelle alimentation des aquifères entres eux. L’importance de l’implantation d’ouvrage de retenue dans le bassin est de minimiser le phénomène d’envasement, de réguler le débit d’écoulement et de contribuer à l’irrigation de la plaine ainsi que l’alimentation des briqueteries. L’objectif de cette approche, est la mobilisation des ressources en eaux superficielles décidée par l’état en vue d’une utilisation rationnelle et planifiée de ce facteur vital qui et l’eau.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mahtali, Sbih</style></author><author><style face="normal" font="default" size="100%">Zoubeir, Bensid</style></author><author><style face="normal" font="default" size="100%">Zohra, Bounouara</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Youcef, Ferrag</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Establishment theoretical of recommendation fertilization guide of vegetable crops in Algeria: concept and validation, ISSN 2349-0837</style></title><secondary-title><style face="normal" font="default" size="100%">JOURNAL OF ADVANCES IN AGRICULTUREJOURNAL OF ADVANCES IN AGRICULTURE</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2015</style></date></pub-dates></dates><number><style face="normal" font="default" size="100%">Numéro 1</style></number><volume><style face="normal" font="default" size="100%">Volume 5</style></volume><pages><style face="normal" font="default" size="100%">pp 606-620</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">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/kgâ€¦).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.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Redha, MENANI Mohamed</style></author><author><style face="normal" font="default" size="100%">Malika, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Impact de la mobilisation des ressources hydriques dans les zones semi arides sur le développement durable, Cas du bassin de Timgad, Algérie, ISSN 2052-3408</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Environment &amp; WaterInternational Journal of Environment &amp; Water</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2015</style></date></pub-dates></dates><number><style face="normal" font="default" size="100%">Numéro 2</style></number><volume><style face="normal" font="default" size="100%">Volume 4</style></volume><pages><style face="normal" font="default" size="100%">pp 118-123</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">La retenue collinaire est un ouvrage destiné généralement à améliorer une agricultureexistante par l’irrigation de petits périmètres et par conséquent améliorer les terres irriguées,elle peut avoir d’autres objectifs.L’étude de faisabilité de tout terrain (région) restefondamentale avant d’entreprendre tout projet de recherche appliquée. Notre travailproposé revêt une importance socio-économique pour la région de Timgad. Les résultats de ce travail constituent un apport scientifique utilisable aussi bien par les opérateurs socio-économiques que les décideurs pour tout plan d’aménagement. Dans la région étudiée, Les ressources hydriques sont en étroite relation avec les formations géologiques de la région, donc l’analyse de ces derniers est primordial. L’objectif principal de l’implantation de la retenue de Foum Toub est de contribuer à l’irrigation de la plaine de Foum Toub, de régulariser le débit de l’Oued Foum Toub et de minimiser le phénomène d’envasement du barrage de Koudiet Lemdaour. Pour cela, les sites retenus pour la construction de cet ouvrage sont représentés par un substratum imperméable. Les matériaux meubles, favorable pour servir de zones d’emprunt sont localisés dans les dépressions avoisinantes ainsi que les grès qui peuvent être utilisés comme matériaux de construction de la digue.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Redha, MENANI Mohamed</style></author><author><style face="normal" font="default" size="100%">Malika, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Impact de la mobilisation des ressources hydriques dans les zones semi- arides sur le développement durable, Cas du bassin de Timgad, Algérie nord oriental</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Environment and WaterInternational Journal of Environment and Water</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2015</style></date></pub-dates></dates><number><style face="normal" font="default" size="100%">Issue 4</style></number><volume><style face="normal" font="default" size="100%">Vol.2</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">La retenue collinaire est un ouvrage destiné généralement à améliorer une agriculture existante par l’irrigation de petits périmètres et par conséquent améliorer les terres irriguées, elle peut avoir d’autres objectifs. L’étude de faisabilité de tout terrain (région) reste fondamentale avant d’entreprendre tout projet de recherche appliquée. Notre travail proposé revêt une importance socio-économique pour la région de Timgad. Les résultats de ce travail constituent un apport scientifique utilisable aussi bien par les opérateurs socio-économiques que les décideurs pour tout plan d’aménagement. Dans la région étudiée, Les ressources hydriques sont en étroite relation avec les formations géologiques de la région, donc l’analyse de ces derniers est primordial. L’objectif principal de l’implantation de la retenue de Foum Toub est de contribuer à l’irrigation de la plaine de Foum Toub, de régulariser le débit de l’Oued Foum Toub et de minimiser le phénomène d’envasement du barrage de Koudiet Lemdaour. Pour cela, les sites retenus pour la construction de cet ouvrage sont représentés par un substratum imperméable. Les matériaux meubles, favorable pour servir de zones d’emprunt sont localisés dans les dépressions avoisinantes ainsi que les grès qui peuvent être utilisés comme matériaux de construction de la digue.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Ramdane, Marmi</style></author><author><style face="normal" font="default" size="100%">Ali, Ayhamena</style></author><author><style face="normal" font="default" size="100%">Nafaa, Brinis</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">La mobilisation des ressources hydriques dans le bassin de Timgad (Aurès, Algérie NE)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2015</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Ramdane, Marmi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Le bassin néogène de Timgad : Paléocourants et sédimentation (Algérie Nord-Orientale)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2015</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Malika, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Ramdane, Marmi</style></author><author><style face="normal" font="default" size="100%">Nafaa, Brinis</style></author><author><style face="normal" font="default" size="100%">Redha, MENANI Mohamed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">caractérisation géologique, hydrologique et hydrogéologique du bassin de timgad (Aurès, Algérie NE), pour la mobilisation des ressources hydrique</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2014</style></date></pub-dates></dates><number><style face="normal" font="default" size="100%">No. 1</style></number><pub-location><style face="normal" font="default" size="100%">Hammamet (Tunisie)</style></pub-location><volume><style face="normal" font="default" size="100%">Vol. 5</style></volume><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Nafaa, Brinis</style></author><author><style face="normal" font="default" size="100%">Abderahmane, Boudoukha</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la salinité des eaux souterraines dans les zones arides Cas de l&amp;rsquo;aquifère d&amp;rsquo;El-Outaya Région Nord ouest de Biskra &amp;ndash; Algerie.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2014</style></date></pub-dates></dates><pub-location><style face="normal" font="default" size="100%">Amman Jordan</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Nafaa, Brinis</style></author><author><style face="normal" font="default" size="100%">Abderahmane, Boudoukha</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la salinité des eaux souterraines dans les zones arides Cas de l&amp;rsquo;aquifère d&amp;rsquo;El-Outaya Région Nord ouest de Biskra &amp;ndash; ALGERIE; ISSN 2052-3408,</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Environment &amp; WaterInternational Journal of Environment &amp; Water</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2014</style></date></pub-dates></dates><number><style face="normal" font="default" size="100%">Issue 1</style></number><volume><style face="normal" font="default" size="100%">Vol 3</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Le bassin d’El-Outaya se trouve dans la wilaya de BISKRA, une zone aride au sud algérien à environ 500 Km au sud de la capital Alger. Il constitue une ressource importante pour l’eau d’irrigation en plus d’un barrage à l’amont. La population de la plaine dépasse 11 000 habitants, leur activité principale est l’agriculture.La plaine étudiée correspond à un bassin subsident orienté sensiblement E.NE – W.SW et situé entre deux anticlinaux. Il se trouve au nord de l’anticlinal du Dj.Bou Rhezel (Biskra) et au sud du dôme de Dj. El Melah. Il a fonctionné comme un bassin de sédimentation pendant tout le Néogène. Il est constitué à la base par un miocène laguno-marin, recouvert par du messinien (pontien) gréseux fluviatile, puis par des poudingues pliocènes. Les termes supérieurs, plus particulièrement pliocènes, sont fortement inclinés vers le centre du bassin où ils disparaissent sous une épaisseur considérable du Quaternaire.Le dépouillement des analyses chimiques a aboutit à trois faciès chimiques: Le faciès chloruré sodique, le faciès sulfaté magnésien et le faciès sulfaté sodique.Le suivi des variables chimiques dominant selon les axes des écoulements souterrains permet de suivre l’évolution des faciès dans aquifère ainsi que l’origine de chaque faciès.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Nafaa, Brinis</style></author><author><style face="normal" font="default" size="100%">Abderahmane, Boudoukha</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la salinité des eaux souterraines dans les zones arides Cas de l&amp;rsquo;aquifère d&amp;rsquo;El-Outaya Région Nord ouest de Biskra &amp;ndash; ALGERIE, 2014. ISSN 2052-3408.</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Environment &amp; WaterInternational Journal of Environment &amp; Water</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2014</style></date></pub-dates></dates><number><style face="normal" font="default" size="100%">Issue 1</style></number><volume><style face="normal" font="default" size="100%">Vol 3</style></volume><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Malika, ATHAMENA</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Importance des ressources hydriques et leurs impacts sur le développement durable dans le bassin de Timgad (Algérie nord orientale), ISSN 2170-1318,Décembre 2014</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Arid And Environment (AJAE)Journal of Arid And Environment (AJAE)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2014</style></date></pub-dates></dates><number><style face="normal" font="default" size="100%">n° 2</style></number><volume><style face="normal" font="default" size="100%">vol. 4</style></volume><pages><style face="normal" font="default" size="100%">pp 78-87</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Located in the Aures mountains Foum Toub is characterized by an annual average rainfall of&amp;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.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Malika, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Risque de pollution des eaux souterraines de la plaine de Zana, Est Algérien</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2014</style></date></pub-dates></dates><pub-location><style face="normal" font="default" size="100%">Hammamet (Tunisie)</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Malika, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Accident probablement responsable de la présence des sources thermales, Cas de la source thermale de Guergima, Batna Est Algérien</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2013</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Nafaa, Brinis</style></author><author><style face="normal" font="default" size="100%">Abderahmane, Boudoukha</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude des faciès chimiques des eaux souterraines de la plaine d&amp;rsquo;El-Outaya au sud algérien. Types et évolution dans l&amp;rsquo;espace aquifère</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2013</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Malika, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Géothermie des eaux souterraines cas de la source thermale de Guergima, Batna est-algérien</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2013</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Malika, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Importance de la mobilisation des ressources hydriques et l&amp;rsquo;impact sur le développement durable dans le bassin de Timgad Algérie nord orientale</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2013</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Malika, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">La contribution de la géophysique dans les études thermales, cas des sources des monts des Aures</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2013</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Ramdane, Marmi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Le Bassin néogène de Timgad et son aspect structural (atlas saharien algérien oriental)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2013</style></date></pub-dates></dates><pub-location><style face="normal" font="default" size="100%">TEBESSA –ALGERIE</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Nafaa, Brinis</style></author><author><style face="normal" font="default" size="100%">R, Marmi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Le remplissage sédimentaire du bassin de Timgad et aquifères potentiels (Atlas saharien Algérien oriental)&amp;raquo;.1 septembre 2013, ISSN 1813-548X.</style></title><secondary-title><style face="normal" font="default" size="100%">Afrique ScienceAfrique SCIENCE</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2013</style></date></pub-dates></dates><number><style face="normal" font="default" size="100%">N°03</style></number><volume><style face="normal" font="default" size="100%">Vol.09</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Le bassin de Timgad, orienté suivant une direction sub-latitudinale, appartient à l’Atlas Saharien nord-oriental. Il est bordé au nord par Dj. Bou Arif-Dj. Fedjoudj-Dj. Tarf et au sud par les Monts des Aurès. Il comprend un substratum mésozoïque correspondant à une série marine gréso-carbonatée, surmonté en discordance par des formations du Néogène. Ces derniers sont représentés &amp;nbsp;essentiellement par des sédiments détritiques où dominent les dépôts silicoclastiques. La puissance de toute la série dépasse les 1000 mètres. Le contact, entre les deux séries &amp;nbsp;lithostratigraphiques, mésozoïque et néogènes, est souligné par une discordance majeure marquée tantôt par des conglomérats polygéniques, tantôt par des niveaux calcaires souvent gréseux. Le Plio-Quaternaire, représenté surtout par des sédiments détritiques grossiers, surmonte en discordance les séries antérieures. Du point de vue structurale, le bassin est affecté par une tectonique polyphasée qui l’a compartimenté en blocs dont les accidents transverses NW-SE et NE-SW sont nettement exprimés. La phase compressive, située à la limite pliocène-quaternaire, serait à l’origine du modelé du relief actuel. L’étude géophysique, consistant en l’exploitation &amp;nbsp;des profils sismiques et des coupes géo électriques, a permis de mettre en évidence d’une part la géométrie profonde des différents accidents dans le bassin et les aquifères potentiels d’autre part. Une formation relativement résistante, correspond à un intervalle gréseux du Miocène, revêt un intérêt particulier sur le plan hydrogéologique.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Nafaa, Brinis</style></author><author><style face="normal" font="default" size="100%">Ramdane, Marmi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Le remplissage sédimentaire du bassin de Timgad et aquifères potentiels (atlas saharien Algérien oriental). ISSN 1813-548X.</style></title><secondary-title><style face="normal" font="default" size="100%">Afrique SCIENCEAfrique SCIENCE</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2013</style></date></pub-dates></dates><number><style face="normal" font="default" size="100%">Issue 3</style></number><volume><style face="normal" font="default" size="100%">Vol 09</style></volume><pages><style face="normal" font="default" size="100%">pp 66–76</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Le bassin de Timgad, orienté suivant une direction sub-latitudinale, appartient à l’Atlas Saharien nord-oriental. Il est bordé au nord par Dj. Bou Arif-Dj. Fedjoudj-Dj. Tarf et au sud par les Monts des Aurès. Il comprend un substratum mésozoïque correspondant à une série marine gréso-carbonatée, surmonté en discordance par des formations du Néogène. Ces derniers sont représentés &amp;nbsp;essentiellement par des sédiments détritiques où dominent les dépôts silicoclastiques. La puissance de toute la série dépasse les 1000 mètres. Le contact, entre les deux séries &amp;nbsp;lithostratigraphiques, mésozoïque et néogènes, est souligné par une discordance majeure marquée tantôt par des conglomérats polygéniques, tantôt par des niveaux calcaires souvent gréseux. Le Plio-Quaternaire, représenté surtout par des sédiments détritiques grossiers, surmonte en discordance les séries antérieures. Du point de vue structurale, le bassin est affecté par une tectonique polyphasée qui l’a compartimenté en blocs dont les accidents transverses NW-SE et NE-SW sont nettement exprimés. La phase compressive, située à la limite pliocène-quaternaire, serait à l’origine du modelé du relief actuel. L’étude géophysique, consistant en l’exploitation &amp;nbsp;des profils sismiques et des coupes géo électriques, a permis de mettre en évidence d’une part la géométrie profonde des différents accidents dans le bassin et les aquifères potentiels d’autre part. Une formation relativement résistante, correspond à un intervalle gréseux du Miocène, revêt un intérêt particulier sur le plan hydrogéologique.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">A, BOUMEZBEUR</style></author><author><style face="normal" font="default" size="100%">Ramdane, Marmi</style></author><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Redha, MENANI Mohamed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les mouvements des sols, Géorisques et Urbanisation. 2ème Colloque International sur La Gestion Intégrée des Ressources en Eau, 22-23 Octobre 2013</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2013</style></date></pub-dates></dates><publisher><style face="normal" font="default" size="100%">GIRE, Dép. Sc. de la Terre et de l’Univers / Faculté des Sciences - Université Hadj Lakhdar – Batna.</style></publisher><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">A, BOUMEZBEUR</style></author><author><style face="normal" font="default" size="100%">Ramdane, Marmi</style></author><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author><author><style face="normal" font="default" size="100%">Redha, MENANI Mohamed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les mouvements des sols,Géorisques et Urbanisation</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2013</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Nafaa, Brinis</style></author><author><style face="normal" font="default" size="100%">Ahmed, Inal</style></author><author><style face="normal" font="default" size="100%">Ramdane, Marmi</style></author><author><style face="normal" font="default" size="100%">Redha, MENANI Mohamed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">L&amp;rsquo;apport de la géophysique a la géométrie des couches profondes et les aquifères potentiels du bassin de timgad (Atlas Saharien Algérien Oriental). 22-23 Octobre 2013</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2013</style></date></pub-dates></dates><pub-location><style face="normal" font="default" size="100%">Batna</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Nafaa, Brinis</style></author><author><style face="normal" font="default" size="100%">Ahmed, Inal</style></author><author><style face="normal" font="default" size="100%">Ramdane, Marmi</style></author><author><style face="normal" font="default" size="100%">Redha, MENANI Mohamed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">L&amp;rsquo;apport de la géophysique à la géométrie des couches profondes et les aquifères potentiels du bassin de timgad (Atlas Saharien Algérien Oriental)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2013</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Ramdane, Marmi</style></author><author><style face="normal" font="default" size="100%">A, BOUMEZBEUR</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Risque naturel liée au mouvements des terrains affaissables dans une zone urbaine &amp;ndash;Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2013</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">S, Benmansour</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Ouahab, Yahaoui Abedel</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">analyse microfaciologique et découpage séquentiel de la série cénomanienne de la coupe de Mennchar Ali Guera (nord-est Algérie)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2012</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Ramdane, Marmi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et hydrogéologique du bassin de Timgad</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2012</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Nafaa, Brinis</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude géologique du bassin de Timgad</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2012</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Nafaa, Brinis</style></author><author><style face="normal" font="default" size="100%">Ahmed, Inal</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude géologique du bassin de Timgad 2</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2012</style></date></pub-dates></dates><pub-location><style face="normal" font="default" size="100%">Ouargla,Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" 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Brinis</style></author><author><style face="normal" font="default" size="100%">Ahmed, Inal</style></author><author><style face="normal" font="default" size="100%">Manel, Cheriet</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Importance des carrières dans la vie socio-économique et leurs impact sur l&amp;⋕39;environnement (Batna&amp;ndash;Ain Touta)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2010</style></date></pub-dates></dates><pub-location><style face="normal" font="default" size="100%">Tlemcen, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Nafaa, Brinis</style></author><author><style face="normal" font="default" size="100%">Ahmed, Inal</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Importance des carrières dans la vie socio-économique et leurs impacts sur l&amp;rsquo;environnement (Batna-Ain Touta)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2010</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Impact des ressources hydriques sur le développement durable dans le basin de Timgad-Algérie Nord Orientale</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2009</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude pétro-structurale de la bordure Est et Sud Est du socle de la Petite Kabylie Nord-Est Algérie. Juin (2008)</style></title><secondary-title><style face="normal" font="default" size="100%">Sciences &amp; TechnologieSciences &amp; Technologie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2008</style></date></pub-dates></dates><number><style face="normal" font="default" size="100%">N°27</style></number><pages><style face="normal" font="default" size="100%">pp. 71-76</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">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 épizonale to mésozonale of low pressure and high temperature. This last estimated at P=4-5 Kbar and T=650-700°C is underlined by the presence of the veins of leucozones and the myrmékite thus near to the field of partial fusion. The structural draft shows the superposition of schisto-sandy units épizonales on units of higher rank. This area is overcome in its Western and Eastern part by formations of Oligo-Miocène-Kabyle. The study of the syn-schistous deformation highlights an extensive component at vergency is and of the linéations 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-Ferguène towards the NW. Alpine and eo-alpine post-schistous deformations of lower (Pt), at vergency East and South, are highlighted.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The impact of hydraulic resources on sustainable development of the Timgad basin north-east of Algerie</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2008</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Y, Mahdjoub</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Conséquences de la phase tectonique alpine sur les déformations syn-schisteuses tardi-hercyniennes du socle de la Petite Kabylie (Algérie Nord-orientale)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2007</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2007</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">S, Benmansour</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude stratigraphique et sédimentologique de Manchar Ali Guera, versant Nord de Djebel Bou Arif (Aurès, Nord est D&amp;rsquo;Algérie)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2007</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2007</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Ramdane, Marmi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">L&amp;rsquo;hypothèse de l&amp;rsquo;existence d&amp;rsquo;un dôme gneissique extensif dans le secteur de Bouchtata-Tamalous bordure orientale du socle de la Petite Kabylie (Algérie nord-orientale)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2007</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2007</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author><author><style face="normal" font="default" size="100%">Ramdane, Marmi</style></author><author><style face="normal" font="default" size="100%">Ali, ATHAMENA</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractéristiques géologiques, géotechniques et hydrologiques d&amp;rsquo;un site destiné à l&amp;rsquo;aménagement d&amp;rsquo;un ouvrage hydraulique (Aurès, Algérie Nord-Orientale)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2006</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2006</style></date></pub-dates></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ramdane, Marmi</style></author><author><style face="normal" font="default" size="100%">A, BOUMEZBEUR</style></author><author><style face="normal" font="default" size="100%">Fouad, DJAIZ</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Observations géologiques des glissements de terrain dans le Constantinois : cas du tronçon d&amp;rsquo;autoroute Massinissa, Didouche Mourad et Anouche Ali. 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