The synthetic data were calculated for the similar model expected in field data inversion and inversion result of these synthetic data used as a guide for the interpretation of the inverse data resistivity sections. The high resolution capabilities of the electrical tomography were used to define the geological draining features in the framework of water paths from the TMA to the karstic springs. Electrical resistivity tomography (ERT) survey was focused on the Bittit area that is one of the most important outlet discharges, and it is representative of the relations between the TMA and the Sa'is Basin.
The TMA is one of the most important aquifers in northern Morocco that supplies the deep aquifer of the Sa'is Basin. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.ĭirect current Resistivity (DCR) method was carried out to characterize the hydrogeological connection between the Tabular Middle Atlas (TMA) and the Sals Basin.
Rouai, 30 June 2011 Accepted 16 September 2011 Academic Editor: Pantelis SoupiosĬopyright © 2012 Kh.
Le Carlier de Veslud2ġĞarth Sciences Department, Faculty of Sciences, Moulay Ismail University, 11201 Zitoune, Meknes 50000, MoroccoĢ Geosciences Rennes, Rennes 1 University, UMR CNRS 6118, Avenue GL Leclerc, Campus Beaulieu, Bat 15 CS74205, 35042 Rennes Cedex, FranceģĜNRS-CEREGE, Aix-Marseille University, UMR 6635 Europole de l'Arbois, BP 80, 13545 Aix en Provence, Cedex 4, France Correspondence should be addressed to M. Geoelectrical Tomography Investigating and Modeling of Fractures Network around Bittit Spring (Middle Atlas, Morocco) Hindawi Publishing Corporation International Journal of Geophysics Volume 2012, Article ID 489634, 13 pages doi:10.1155/2012/489634
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