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Rhoujjati, A., Nourelbait, M., Benkaddour, A., Damnati, B., Baali, A., Taieb, M., Decobert, M., Farid Malek, F. and Cheddadi, R. (2012) Significations paléoen-vironnementales des dépôts du remplissage holocène du lac Iffer (Moyen Atlas, Maroc). Quaternaire, 23, 241-252. https://doi.org/10.4000/quaternaire.6300

has been cited by the following article:

• TITLE: Application of Electrical Tomography to Put in Evidence the Thickness and Structure of the Filling of Dayet Iffer (Middle Atlas, Morocco)

  AUTHORS: Bouchra Lemdeghri Alaoui, Abdennasser Baali, Mohamed Chibout, Anasse Benslimane, Fatima Zahra Faqihi

  KEYWORDS: Electrical Tomography, Resistivity, Lacustrine Sediments, Dayet, Quaternary, Middle Atlas

  JOURNAL NAME: International Journal of Geosciences, Vol.11 No.4, April 20, 2020

  ABSTRACT: The Dayet Iffer belongs to the Dayets of tectono-karst origin of the Northern Middle Atlas. After its watershed genesis of middle altitude during the Quaternary, two lacustrine formations were deposited on the surface while other thick formations exist in depth. The detailed sedimentological study of the soltanian and holocene lithological sections on the surface and the 14C datings helped recognize part of the history of the watershed. The geophysical study allowed to detect the thickness of the superficial geological formations as well as the various geological phenomena (tectonic and/or karst) that affected them from the genesis to the present. The current shape of the watershed where the Dayet Iffer exists is only the result of an evolution where sedimentary, tectonic and karst phenomena interfere. The tomography obtained with Res2DInv software, performed for the first time at the Dayet Iffer, reveals the presence of three ranges which can be interpreted as three resistive, intermediate and conductive zones with a large set of faults. These results helped determine the thickness (over 160 m) of the sedimentary filling. This shows that the hydrological behavior of the Dayet Iffer takes into account both horizontal flows at the stratification and/or karstic joints and the movement of sub-vertical fractures.