Fractured rocks influence on hydrological flow in of the Agourai plateau, Middle Atlas, Morocco: Inferences from Isobase lineaments and field data

Authors

  • Soukaina Mouljebouj Geosciences laboratory, Department of Geology, Faculty of Sciences, Mohammed V University in Rabat, Morocco
  • Afaf Amine Geosciences laboratory, Department of Geology, Faculty of Sciences, Mohammed V University in Rabat, Morocco
  • Hmidou El Ouardi Equipe CartoTec, Department of Geology, Faculty of Sciences, Moulay Ismail university of Meknes, Morocco
  • Rida Haddane Geosciences laboratory, Department of Geology, Faculty of Sciences, Mohammed V University in Rabat, Morocco
  • Toufik Kouya Equipe CartoTec, Department of Geology, Faculty of Sciences, Moulay Ismail university of Meknes, Morocco
  • Ali Ouargaga Laboratory of Geology of the Environment and Natural Resources (GERN), Abdelmalek Essaâdi University, Faculty of Sciences of Tetouan, Morocco

DOI:

https://doi.org/10.55407/geogaceta104534

Keywords:

isobase lineaments, water circulation, Agourai plateau, tabular middle atlas, Morocco

Abstract

This study provides new data of hydrological flow direction in the Agourai plain, Tabular Middle Atlas, north central Morocco. Given its major economic interest in term of agricultural production, the analysis of fracture networks remain essential for a good management of water resources. Mapping fractures network, using isobase maps combined with field data reveal three groups of fractures oriented N-S, NE-SW and NW SE. the latter was poorly described and lies with the setting of three main springs in the area. Fractures analysis in the Bouchermou spring, confirm the predominance of NW direction, which control of the water flow in this area.

References

Amine, A., El Ouardi, H. (2017). Geogaceta, 61, 71-74

Bouya, N. (2014). Utilisation des données géophysiques aéroportées magnétiques et spectrométriques dans la cartographie géologique de la partie NE du massif central marocain et des causses moyenatlasiques. Thèse de Doctorat, Univ. Moulay Ismail, Meknès, Maroc, 179 p.

Bouya, N., and El Ouardi, H. (2014). Geological interpretation of aeromagnetic data from Bou Chber area, Central Moroccan Massif. Geogaceta, 56, 39-42. https://doi.org/10.1556/CEuGeol.56.2013.4.5

Charrière, A. (1990). Héritage hercynien et évolution géodynamique alpine d'une chaîne intracontinentale: le Moyen Atlas au SE de Fès (Maroc). Thèse de Doctorat d'Etat, Toulouse, 589 p.

El Fartati, M., Hinaje, S., Yaagoub, D., El Fellah Idrissi, D., Amrani, S., Gharmane, Y., Laiche, M., Drissi, Y., and Tagma, T. (2023). Journal of African Earth Sciences, 205, 104996. https://doi.org/10.1016/j.jafrearsci.2023.104996

El Ouardi, H., Boualoul, M., Ouhaddach, H., Habibi, M., Muzarafuti, A., Allaoui, A., and Amine, A. (2018). Geogaceta, 63, 119-122.

Filosofov, V.P. (1960). Brief guide to morphometric methods in search oftectonic structures. Saratov University Publishing House, Saratov (in Russian).

Grohmann, C. H., Riccomini, C., and Chamani, M. A. C. (2011). Hydrology and Earth System Sciences, 15 (5), 1493-1504. https://doi.org/10.5194/hess-15-1493-2011

Hinaje, S. (2004). Tectonique cassante et paléochamps de contraintes dans le Moyen Atlas et le Haut Atlas central (Midelt -Errachidia) depuis le Trias jusqu'à l'Actuel. Thèse Doctorat d'Etat, Université Mohamed V, Rabat, 363 p.

Downloads

Published

2024-12-02

How to Cite

Mouljebouj, S., Amine, A., El Ouardi, H., Haddane, R., Kouya, T., & Ouargaga, A. (2024). Fractured rocks influence on hydrological flow in of the Agourai plateau, Middle Atlas, Morocco: Inferences from Isobase lineaments and field data. GEOGACETA, 76, 35–38. https://doi.org/10.55407/geogaceta104534

Issue

Section

Artículos

Most read articles by the same author(s)