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Auteur M.S. Benzagouta |
Documents disponibles écrits par cet auteur (5)
Affiner la recherche Interroger des sources externesCaractérisation minéralogique,physiqie et cartographie des sols gonflants dans le bassin de Tébessa, Impact sur le plan d'aménagement. / Mounira Aoun
Titre : Caractérisation minéralogique,physiqie et cartographie des sols gonflants dans le bassin de Tébessa, Impact sur le plan d'aménagement. Type de document : texte imprimé Auteurs : Mounira Aoun, Auteur ; M.S. Benzagouta, Directeur de thèse Editeur : جامعة الإخوة منتوري قسنطينة Année de publication : 2016 Importance : 209 f. Format : 30 cm. Note générale : 2 copies imprimées disponibles
Langues : Français (fre) Catégories : Français - Anglais
Sciences de la terreTags : Sols gonflants retrait gonflement caractenstiques de gonflement prevision de gonflement gypse sulfate swelling soil shrinkage swelling swelling prarameters assessement of swelling gypsum التربة المنتفخة الانكماش والانتفاخ خواص الانتفاخ الجبس السولفات Index. décimale : 550 Sciences de la terre Résumé : Prediction of soil swelling characteristics and accurate quality estimation can be of
great consideration and contribution regarding site stability. Any concerned investigation is correspondingly an advanced priority for project realization. Related inquiries allow potential reduction concerning financial and technical charges damage prior to any urban development. The determination of soil characteristics lead for a best recognition, and allow for the best choice of foundation type adopted for each site. Thus, in any urban case study, much gain can be made by team work recording and surveying the related data. In the considered city of El Kouif, located at Tebessa in Algeria, several buildings have been built mainly on expansive soils. Observations indicate different severe damages which were caused mostly in the nearby structures. These damages are characterized by deflection and failure of walls. Lateral and vertical displacements evidences support the presence of shear movements and subsidence. The scale up of these movements occurrence can reach millimetric shifting dimension.
Laboratory analysis was executed on soil study, results and discussion of those
analysis show that the soil study are characterized by a large range of geotechnical
parameters. Geotechnical classification shows that the soils are classified in the high to very high domain of swelling.
Ground and subsurface risk activity affecting El Kouif city site are also related to the presence of destructive chemical components such as sulfates. The chemical by
fluorescence, and mineralogical analysis (XRD), emphasizing, at the same time, the high percentage of sulfate with the clay minerals (smectite). The sulfate occurrence is illustrated through generally gypsum minerals concentration present in the concerned soil.
Source for these chemical products expansion might be associated to historical event: the city of El Kouif was the field of phosphates mining area in addition to established phosphate extraction plant. Thus, determination of soil characteristics and involvement of chemical components turn out to be the main objectives in this investigation.
Diplôme : Doctorat en sciences En ligne : ../theses/sc-terre/AOU6994.pdf Format de la ressource électronique : Permalink : index.php?lvl=notice_display&id=10400 Caractérisation minéralogique,physiqie et cartographie des sols gonflants dans le bassin de Tébessa, Impact sur le plan d'aménagement. [texte imprimé] / Mounira Aoun, Auteur ; M.S. Benzagouta, Directeur de thèse . - جامعة الإخوة منتوري قسنطينة, 2016 . - 209 f. ; 30 cm.
2 copies imprimées disponibles
Langues : Français (fre)
Catégories : Français - Anglais
Sciences de la terreTags : Sols gonflants retrait gonflement caractenstiques de gonflement prevision de gonflement gypse sulfate swelling soil shrinkage swelling swelling prarameters assessement of swelling gypsum التربة المنتفخة الانكماش والانتفاخ خواص الانتفاخ الجبس السولفات Index. décimale : 550 Sciences de la terre Résumé : Prediction of soil swelling characteristics and accurate quality estimation can be of
great consideration and contribution regarding site stability. Any concerned investigation is correspondingly an advanced priority for project realization. Related inquiries allow potential reduction concerning financial and technical charges damage prior to any urban development. The determination of soil characteristics lead for a best recognition, and allow for the best choice of foundation type adopted for each site. Thus, in any urban case study, much gain can be made by team work recording and surveying the related data. In the considered city of El Kouif, located at Tebessa in Algeria, several buildings have been built mainly on expansive soils. Observations indicate different severe damages which were caused mostly in the nearby structures. These damages are characterized by deflection and failure of walls. Lateral and vertical displacements evidences support the presence of shear movements and subsidence. The scale up of these movements occurrence can reach millimetric shifting dimension.
Laboratory analysis was executed on soil study, results and discussion of those
analysis show that the soil study are characterized by a large range of geotechnical
parameters. Geotechnical classification shows that the soils are classified in the high to very high domain of swelling.
Ground and subsurface risk activity affecting El Kouif city site are also related to the presence of destructive chemical components such as sulfates. The chemical by
fluorescence, and mineralogical analysis (XRD), emphasizing, at the same time, the high percentage of sulfate with the clay minerals (smectite). The sulfate occurrence is illustrated through generally gypsum minerals concentration present in the concerned soil.
Source for these chemical products expansion might be associated to historical event: the city of El Kouif was the field of phosphates mining area in addition to established phosphate extraction plant. Thus, determination of soil characteristics and involvement of chemical components turn out to be the main objectives in this investigation.
Diplôme : Doctorat en sciences En ligne : ../theses/sc-terre/AOU6994.pdf Format de la ressource électronique : Permalink : index.php?lvl=notice_display&id=10400 Exemplaires (1)
Code-barres Cote Support Localisation Section Disponibilité AOU/6994 AOU/6994 Thèse Bibliothèque principale Thèses Disponible
Titre : Caractérisation d'un réservoir gréseux par simulation de carottes artificielles Type de document : texte imprimé Auteurs : Nada Achi, Auteur ; M.S. Benzagouta, Directeur de thèse Editeur : جامعة الإخوة منتوري قسنطينة Année de publication : 2015 Importance : 89 f. Format : 30 cm. Note générale : 2 copies imprimées disponibles
Langues : Français (fre) Catégories : Français - Anglais
Sciences de la terreTags : réservoir perméabilité porosité mouillabilité drainage imbibition hydrophile hydrophobe reservoir permeability porosity wettability hydrophilic hydrophobic"
المكمن النفاذية المسامية التبلل التجفيف التشريب محبة للماء كارهة للماءIndex. décimale : 550 Sciences de la terre Résumé : Reservoirs rocks and porous medium can be of high economical interest. The porous
mediums are allocated to fluid storage and circulation. They can be under the control of diverse parameters when they are found at reservoir conditions. Involvement of clay fraction and type, filling pores, is of high contribution towards the reduction of pore volumes. It is responsible for the creation of microbarriers and occlusion for fluid accumulation and mobility. In the case study, investigation based on laboratory experiments has revealed, in that regards, that reservoir is mainly controlled by compaction in addition to the type and fraction of simulated cement. It has been found that impact on petrophysical characteristics was own to the type of clay, beyond pressure and grain texture type. Kaolinite clay mineral type was the less harmful with regard to the permeability and porosity in comparison to illite and mainly bentonite. However, in the presence of aqueous solution, swelling intensity was higher with bentonite mineral in comparison to kaolinite and illite.
During drainage and essentially the imbibation, impact from the wettability (soaking....) system was defined.
Results were in harmony with the imbibation rather than drainage at atmospheric conditions.
Within the diphasiques phases, imbibition supports the hydrophilic character of the bentoniteillite clay minerals, whereas the kaolinite was as hydrophobic. Thus, and regarding the reservoir, sandstone reservoirs with the presence of kaolinite are better reservoir
characteristics but hydrphobe. Reservoirs with bentonite clay fraction are less petrophysical characteristics development; even so, it is important to mention that bentonite is hydrophilic type.
The overall results reveal that sandstone with illite clay fraction is the better concerned with permeability and porosity development or preservation leading to efficient fluid circulation and recovery.
Diplôme : Magistère En ligne : ../theses/sc-terre/ACH6800.pdf Format de la ressource électronique : Permalink : index.php?lvl=notice_display&id=10049 Caractérisation d'un réservoir gréseux par simulation de carottes artificielles [texte imprimé] / Nada Achi, Auteur ; M.S. Benzagouta, Directeur de thèse . - جامعة الإخوة منتوري قسنطينة, 2015 . - 89 f. ; 30 cm.
2 copies imprimées disponibles
Langues : Français (fre)
Catégories : Français - Anglais
Sciences de la terreTags : réservoir perméabilité porosité mouillabilité drainage imbibition hydrophile hydrophobe reservoir permeability porosity wettability hydrophilic hydrophobic"
المكمن النفاذية المسامية التبلل التجفيف التشريب محبة للماء كارهة للماءIndex. décimale : 550 Sciences de la terre Résumé : Reservoirs rocks and porous medium can be of high economical interest. The porous
mediums are allocated to fluid storage and circulation. They can be under the control of diverse parameters when they are found at reservoir conditions. Involvement of clay fraction and type, filling pores, is of high contribution towards the reduction of pore volumes. It is responsible for the creation of microbarriers and occlusion for fluid accumulation and mobility. In the case study, investigation based on laboratory experiments has revealed, in that regards, that reservoir is mainly controlled by compaction in addition to the type and fraction of simulated cement. It has been found that impact on petrophysical characteristics was own to the type of clay, beyond pressure and grain texture type. Kaolinite clay mineral type was the less harmful with regard to the permeability and porosity in comparison to illite and mainly bentonite. However, in the presence of aqueous solution, swelling intensity was higher with bentonite mineral in comparison to kaolinite and illite.
During drainage and essentially the imbibation, impact from the wettability (soaking....) system was defined.
Results were in harmony with the imbibation rather than drainage at atmospheric conditions.
Within the diphasiques phases, imbibition supports the hydrophilic character of the bentoniteillite clay minerals, whereas the kaolinite was as hydrophobic. Thus, and regarding the reservoir, sandstone reservoirs with the presence of kaolinite are better reservoir
characteristics but hydrphobe. Reservoirs with bentonite clay fraction are less petrophysical characteristics development; even so, it is important to mention that bentonite is hydrophilic type.
The overall results reveal that sandstone with illite clay fraction is the better concerned with permeability and porosity development or preservation leading to efficient fluid circulation and recovery.
Diplôme : Magistère En ligne : ../theses/sc-terre/ACH6800.pdf Format de la ressource électronique : Permalink : index.php?lvl=notice_display&id=10049 Exemplaires (1)
Code-barres Cote Support Localisation Section Disponibilité ACH/6800 ACH/6800 Thèse Bibliothèque principale Thèses Disponible
Titre : Les Dolomies des Monts d’Aïn M’lila. Cas du Dj. Teioualt : Exploitation, Utilisation Industrielle et Impact sur l’Environnement Type de document : texte imprimé Auteurs : Billel Boulmaiz, Auteur ; M.S. Benzagouta, Directeur de thèse Editeur : constantine [Algérie] : Université Constantine 1 Année de publication : 2014 Importance : 189 f. Format : 30 cm. Note générale : 2 copies imprimées disponibles
Langues : Français (fre) Catégories : Français - Anglais
Sciences de la terreTags : Teioualt Dolomies Volanginien tectonique Dolomite Valonginian tectonic تايوالت دولوميت القالنجيني تكتونيك Index. décimale : 550 Sciences de la terre Résumé : The region of Ain M'lila, located in eastern Algeria, is part of the outer zones of the alpine chain of oriental Algeria.
It is an area characterized by large carbonate deposits (limestone and dolomite). These deposits, which are in majority Cretaceous, have been affected by diagenetic events such as dissolutions, replacements, compaction ... etc.
Structurally, the massifs of Ain M'lila are characterized by tectonic especially breakable with folded structures. These structures are also affected by many accidents. These brittle accidents include the recesses which are numerous and whose direction is generally NW-SE. Accidents NS direction are also present in the form of faults, especially normal.
Outcrops forming the Valanginian of the massifs of Ain M'lila are mainly formed of dolomite. On the industrial side, these dolomites form important deposits of exploitation.
Many careers, including that of the massif of Teioualt were implanted in this region. The main objective of these careers is the exploitation of these valanginian dolomite of which physical, chemical and mechanical properties that make them valuable to the exploitation and thus meet the requirements of several industries.
Knowledge more detailed of this type of rocks of sedimentary, petrographic and diagenetic point of view is of great importance for understanding the genesis of dolomite (dolomitization), its transformation (dédolomitisation) and its distribution in the space. The characterization physicochemical properties of these dolomites are also of considerable importance for the confirmation of the quality of the material.
By projecting the case of the deposit of the massif of Teioualt on dolomitic formations of the other massifs of Ain M'lila, this valanginian dolomite may be a safe bet for future exploitations.Diplôme : Magistère En ligne : ../theses/sc-terre/BOU6643.pdf Format de la ressource électronique : Permalink : index.php?lvl=notice_display&id=9776 Les Dolomies des Monts d’Aïn M’lila. Cas du Dj. Teioualt : Exploitation, Utilisation Industrielle et Impact sur l’Environnement [texte imprimé] / Billel Boulmaiz, Auteur ; M.S. Benzagouta, Directeur de thèse . - constantine [Algérie] : Université Constantine 1, 2014 . - 189 f. ; 30 cm.
2 copies imprimées disponibles
Langues : Français (fre)
Catégories : Français - Anglais
Sciences de la terreTags : Teioualt Dolomies Volanginien tectonique Dolomite Valonginian tectonic تايوالت دولوميت القالنجيني تكتونيك Index. décimale : 550 Sciences de la terre Résumé : The region of Ain M'lila, located in eastern Algeria, is part of the outer zones of the alpine chain of oriental Algeria.
It is an area characterized by large carbonate deposits (limestone and dolomite). These deposits, which are in majority Cretaceous, have been affected by diagenetic events such as dissolutions, replacements, compaction ... etc.
Structurally, the massifs of Ain M'lila are characterized by tectonic especially breakable with folded structures. These structures are also affected by many accidents. These brittle accidents include the recesses which are numerous and whose direction is generally NW-SE. Accidents NS direction are also present in the form of faults, especially normal.
Outcrops forming the Valanginian of the massifs of Ain M'lila are mainly formed of dolomite. On the industrial side, these dolomites form important deposits of exploitation.
Many careers, including that of the massif of Teioualt were implanted in this region. The main objective of these careers is the exploitation of these valanginian dolomite of which physical, chemical and mechanical properties that make them valuable to the exploitation and thus meet the requirements of several industries.
Knowledge more detailed of this type of rocks of sedimentary, petrographic and diagenetic point of view is of great importance for understanding the genesis of dolomite (dolomitization), its transformation (dédolomitisation) and its distribution in the space. The characterization physicochemical properties of these dolomites are also of considerable importance for the confirmation of the quality of the material.
By projecting the case of the deposit of the massif of Teioualt on dolomitic formations of the other massifs of Ain M'lila, this valanginian dolomite may be a safe bet for future exploitations.Diplôme : Magistère En ligne : ../theses/sc-terre/BOU6643.pdf Format de la ressource électronique : Permalink : index.php?lvl=notice_display&id=9776 Exemplaires (1)
Code-barres Cote Support Localisation Section Disponibilité BOU/6643 BOU/6643 Thèse Bibliothèque principale Thèses Disponible
Titre : Etude des formations carbonatées du versant sud du massif de l'Oued Settas : Approche quantitative et qualitative Type de document : texte imprimé Auteurs : Wassila Nacer ; Univ. de Constantine, Éditeur scientifique ; M.S. Benzagouta, Directeur de thèse Année de publication : 2005 Importance : 161 f. Note générale : 01 Disponible à la salle de recherche 02 Disponibles au magazin de la bibliothèque centrale 01 CD Langues : Français (fre) Catégories : Français - Anglais
Sciences de la terreTags : Formations carbonatées Oued Settas Approche quantitative Approcha qualitative Index. décimale : 550 Sciences de la terre En ligne : ../theses/sc-terre/NAC4379.pdf Permalink : index.php?lvl=notice_display&id=4291 Etude des formations carbonatées du versant sud du massif de l'Oued Settas : Approche quantitative et qualitative [texte imprimé] / Wassila Nacer ; Univ. de Constantine, Éditeur scientifique ; M.S. Benzagouta, Directeur de thèse . - 2005 . - 161 f.
01 Disponible à la salle de recherche 02 Disponibles au magazin de la bibliothèque centrale 01 CD
Langues : Français (fre)
Catégories : Français - Anglais
Sciences de la terreTags : Formations carbonatées Oued Settas Approche quantitative Approcha qualitative Index. décimale : 550 Sciences de la terre En ligne : ../theses/sc-terre/NAC4379.pdf Permalink : index.php?lvl=notice_display&id=4291 Exemplaires (1)
Code-barres Cote Support Localisation Section Disponibilité NAC/4379 NAC/4379 Thèse Bibliothèque principale Thèses Disponible
Titre : Étude tectono-sédimentaire du coniaciensantonien dans le bassin du sud-est constantinois : Intêret pétrolier. Type de document : texte imprimé Auteurs : Manel Cheriet, Auteur ; M.S. Benzagouta, Directeur de thèse Editeur : جامعة الإخوة منتوري قسنطينة Année de publication : 2017 Importance : 204 f. Format : 30 cm. Note générale : 2 copies imprimées disponibles
Langues : Français (fre) Catégories : Français - Anglais
Sciences de la terreTags : Coniacien-Santonien Sud-Est Constantinois tectono-sédimentaire Caractéristiques pétrophysiques Diagénèse Corrélations Potentiel Pétrolier Roche mère réservoir Coniacien-Santonian South East Constantine tectonic-sedimentary petrophysical characteristics diagenesis correlations Oil Potential Source rock reservoir جنوب الشرق القسنطيني التكتوني الرسوبية الخصائص الصخرية التحولات
الخزان الارتباطات النفط المحتملة صخرة اللامIndex. décimale : 550 Sciences de la terre Résumé : The South East Constantine basin looks like a geologically complex area but seemed to important and promising oil potential for oil exploration. This basin was the subject of several studies and research related to several geological topical in the image of tectonics, sedimentology, stratigraphy and including oil interests. However, studies conducted previously also require more expertise can lead a better geological understanding of the above-cited basin.
In our case, study one of the missions to be considered regarding the tectonicsedimentary investigation in the SE Constantine basin with a focus on Coniacien levels Santonian (Upper Cretaceous) and their potential H-C.
The completion of this study required several investigations tools with subsurface data that have been an important contribution.
Several approaches especially sedimentological and tectonic stratigraphic oil interest were discussed. Additional support has been completed from surface investigation.
This investigation was based primarily on geological surveys conducted in the region.
Among the results characterizing the basin SE Constantine and stratigraphically, one could discern that the formations constituting the filling of this basin are training for carbonated dominance with marl alternations. These types of training including characterize Coniacien levels Santonian. This typical lithological dominance was seconded by the geological section of land made in the region (Tamarin - El Kantara) especially in formations of Santonian Coniacien South flank Dj Metlili.
Sedimentary perspective and according to the facies description, this study allowed begun to highlight several types of facies. These facies were determined on the petrographic map: ranging from mudstone to reach the grainstone with typical fauna revealing contents varying energy levels. The Synsedimentary analysis showed the
presence of major sequences optionally composed of Mésoséquence and together may constitute an opening megasequence.
The interpretation sedimentological and faunal content of these facies mainly foraminifera, echinoderms, inoceramids, ostracods and bivalves may be indicative platform sedimentation whose type is ramp.
The lithostratigraphic framework based on drilling wells correlations and data unveiled a relative homogeneity as to the lithological distribution of these constituent formations. According to these correlations, we could see a thickening trend of these levels to the South East Constantine basin center.
On the oil front and a potential evaluation of the rock and its contents, a geochemical database study was introduced. It has been found that in the SE Constantine basin, possibly among the levels of C-H generator, the Late Cretaceous remains promising.
Several rock levels are present with particular geochemical characteristics and also lithological variables. The data obtained was based TOC assessment, maturity, and quality of the rock, revealed a possible generation and accumulation of hydrocarbon potential (oil window) favorable. These H-C were characterized by a find of organic
matter with a type II C.O.T varying between 0.4% and 2.8% with a variable geothermal gradient. The conditions for generating the H-C were changing from one rock to another and from one area to another. These diversifications are related to the conditions of maturity that are particularly pressure and particularly temperaturerelated impacts phenomenal burial and uplift (tectonic-sedimentary effect) that affected the study area.
In the tank, essentially Coniacien level Santonian, its characterization in the South East Constantine basin was established primarily has based logging records drilling data and the description of cores from the study area. Among the findings was contracted as reservoir quality, these reservoirs levels (Coniacien Santonian) with
relatively low petrophysical characteristics: permeability not exceeding 50md and a porosity of up to a maximum of 10%. Similar features can classify ConiacienSantonian reservoir levels as a moderate of up to type (tight). Diagenetic sedimentary effect and also were important impacts in the evolution of these reservoir levels.
Diplôme : Doctorat en sciences En ligne : ../theses/sc-terre/CHE7264.pdf Format de la ressource électronique : Permalink : index.php?lvl=notice_display&id=10861 Étude tectono-sédimentaire du coniaciensantonien dans le bassin du sud-est constantinois : Intêret pétrolier. [texte imprimé] / Manel Cheriet, Auteur ; M.S. Benzagouta, Directeur de thèse . - جامعة الإخوة منتوري قسنطينة, 2017 . - 204 f. ; 30 cm.
2 copies imprimées disponibles
Langues : Français (fre)
Catégories : Français - Anglais
Sciences de la terreTags : Coniacien-Santonien Sud-Est Constantinois tectono-sédimentaire Caractéristiques pétrophysiques Diagénèse Corrélations Potentiel Pétrolier Roche mère réservoir Coniacien-Santonian South East Constantine tectonic-sedimentary petrophysical characteristics diagenesis correlations Oil Potential Source rock reservoir جنوب الشرق القسنطيني التكتوني الرسوبية الخصائص الصخرية التحولات
الخزان الارتباطات النفط المحتملة صخرة اللامIndex. décimale : 550 Sciences de la terre Résumé : The South East Constantine basin looks like a geologically complex area but seemed to important and promising oil potential for oil exploration. This basin was the subject of several studies and research related to several geological topical in the image of tectonics, sedimentology, stratigraphy and including oil interests. However, studies conducted previously also require more expertise can lead a better geological understanding of the above-cited basin.
In our case, study one of the missions to be considered regarding the tectonicsedimentary investigation in the SE Constantine basin with a focus on Coniacien levels Santonian (Upper Cretaceous) and their potential H-C.
The completion of this study required several investigations tools with subsurface data that have been an important contribution.
Several approaches especially sedimentological and tectonic stratigraphic oil interest were discussed. Additional support has been completed from surface investigation.
This investigation was based primarily on geological surveys conducted in the region.
Among the results characterizing the basin SE Constantine and stratigraphically, one could discern that the formations constituting the filling of this basin are training for carbonated dominance with marl alternations. These types of training including characterize Coniacien levels Santonian. This typical lithological dominance was seconded by the geological section of land made in the region (Tamarin - El Kantara) especially in formations of Santonian Coniacien South flank Dj Metlili.
Sedimentary perspective and according to the facies description, this study allowed begun to highlight several types of facies. These facies were determined on the petrographic map: ranging from mudstone to reach the grainstone with typical fauna revealing contents varying energy levels. The Synsedimentary analysis showed the
presence of major sequences optionally composed of Mésoséquence and together may constitute an opening megasequence.
The interpretation sedimentological and faunal content of these facies mainly foraminifera, echinoderms, inoceramids, ostracods and bivalves may be indicative platform sedimentation whose type is ramp.
The lithostratigraphic framework based on drilling wells correlations and data unveiled a relative homogeneity as to the lithological distribution of these constituent formations. According to these correlations, we could see a thickening trend of these levels to the South East Constantine basin center.
On the oil front and a potential evaluation of the rock and its contents, a geochemical database study was introduced. It has been found that in the SE Constantine basin, possibly among the levels of C-H generator, the Late Cretaceous remains promising.
Several rock levels are present with particular geochemical characteristics and also lithological variables. The data obtained was based TOC assessment, maturity, and quality of the rock, revealed a possible generation and accumulation of hydrocarbon potential (oil window) favorable. These H-C were characterized by a find of organic
matter with a type II C.O.T varying between 0.4% and 2.8% with a variable geothermal gradient. The conditions for generating the H-C were changing from one rock to another and from one area to another. These diversifications are related to the conditions of maturity that are particularly pressure and particularly temperaturerelated impacts phenomenal burial and uplift (tectonic-sedimentary effect) that affected the study area.
In the tank, essentially Coniacien level Santonian, its characterization in the South East Constantine basin was established primarily has based logging records drilling data and the description of cores from the study area. Among the findings was contracted as reservoir quality, these reservoirs levels (Coniacien Santonian) with
relatively low petrophysical characteristics: permeability not exceeding 50md and a porosity of up to a maximum of 10%. Similar features can classify ConiacienSantonian reservoir levels as a moderate of up to type (tight). Diagenetic sedimentary effect and also were important impacts in the evolution of these reservoir levels.
Diplôme : Doctorat en sciences En ligne : ../theses/sc-terre/CHE7264.pdf Format de la ressource électronique : Permalink : index.php?lvl=notice_display&id=10861 Exemplaires (1)
Code-barres Cote Support Localisation Section Disponibilité CHE/7264 CHE/7264 Thèse Bibliothèque principale Thèses Disponible
