| Titre : |
ontribution à L’élaboration de la carte Hydrogéologique au 1/50.000 de Constantine (feuille N°73)-Secteur Centre. |
| Type de document : |
texte imprimé |
| Auteurs : |
Sief eddine Belguet, Auteur ; Yasser Baka, Auteur ; Nabil Chabour, Directeur de thèse |
| Editeur : |
CONSTANTINE [ALGERIE] : Université Frères Mentouri Constantine |
| Année de publication : |
2018 |
| Importance : |
32 f. |
| Format : |
30 cm. |
| Note générale : |
Une copie elelctronique PDF disponible en Buc |
| Langues : |
Français (fre) |
| Catégories : |
Sciences de terre et de l'univers:Sciences Géologiques
|
| Tags : |
Karst aquifer thermal water geochemistry isotopic Constantine Algeria. |
| Index. décimale : |
207 Hydrogéologie |
| Résumé : |
The hydrothermal karstic of Constantine is the effect of an intense fracturation
in the limestone formation since the Mesozoïc. The great number of the thermal
springs, belonging Hamma Bouziane (Constantine), at times, with a very high
flow rate such as Ain Zouaoui (800 l/s in Hamma Bouziane), constitute the
outlet of the open complex aquifer karstic.
The fracturation (regenerated in the field of the active tectonic distortion in PlioQuaternary) of the made flushing carbonated Jurassic and cretaceous are in
appearance the only way to supply the aquifer (infiltration of rainwater and loss
of Rhumel and Bou Merzoug).
However the results of the chemical analysis, carried out on some samples of
water, have furnished signs (low correlation between Na and Cl species) which
nshowed circulation of waters inside a neogen formation of sedimentation
according the continental lagoon.
This situation means that neogen deposits would make up with carbonate, an
infiltration zone of the karstic system and also an aquifer system, which is
partially captive. The isotopic data obtained with carbon 13, oxygen 18 and
those furnished by calcocarbonic equilibriums, have revealed a mixture of
waters coming from infiltration and also from deep hydrothermal, before the
emergence. Thus, owing to elements supplied by hydro geochemistry, one has
set up a complement of information on the process of aquifer system. |
| Diplome : |
Master 2 |
| Permalink : |
https://bu.umc.edu.dz/master/index.php?lvl=notice_display&id=10781 |
ontribution à L’élaboration de la carte Hydrogéologique au 1/50.000 de Constantine (feuille N°73)-Secteur Centre. [texte imprimé] / Sief eddine Belguet, Auteur ; Yasser Baka, Auteur ; Nabil Chabour, Directeur de thèse . - CONSTANTINE [ALGERIE] : Université Frères Mentouri Constantine, 2018 . - 32 f. ; 30 cm. Une copie elelctronique PDF disponible en Buc Langues : Français ( fre)
| Catégories : |
Sciences de terre et de l'univers:Sciences Géologiques
|
| Tags : |
Karst aquifer thermal water geochemistry isotopic Constantine Algeria. |
| Index. décimale : |
207 Hydrogéologie |
| Résumé : |
The hydrothermal karstic of Constantine is the effect of an intense fracturation
in the limestone formation since the Mesozoïc. The great number of the thermal
springs, belonging Hamma Bouziane (Constantine), at times, with a very high
flow rate such as Ain Zouaoui (800 l/s in Hamma Bouziane), constitute the
outlet of the open complex aquifer karstic.
The fracturation (regenerated in the field of the active tectonic distortion in PlioQuaternary) of the made flushing carbonated Jurassic and cretaceous are in
appearance the only way to supply the aquifer (infiltration of rainwater and loss
of Rhumel and Bou Merzoug).
However the results of the chemical analysis, carried out on some samples of
water, have furnished signs (low correlation between Na and Cl species) which
nshowed circulation of waters inside a neogen formation of sedimentation
according the continental lagoon.
This situation means that neogen deposits would make up with carbonate, an
infiltration zone of the karstic system and also an aquifer system, which is
partially captive. The isotopic data obtained with carbon 13, oxygen 18 and
those furnished by calcocarbonic equilibriums, have revealed a mixture of
waters coming from infiltration and also from deep hydrothermal, before the
emergence. Thus, owing to elements supplied by hydro geochemistry, one has
set up a complement of information on the process of aquifer system. |
| Diplome : |
Master 2 |
| Permalink : |
https://bu.umc.edu.dz/master/index.php?lvl=notice_display&id=10781 |
|
ontribution à L’élaboration de la carte Hydrogéologique au 1/50.000 de Constantine (feuille N°73)-Secteur Centre.
