@article { author = {Belhassan, K.}, title = {Hydro-Geological Context of Mikkes Springs and Different Variations of their Flows (Morocco)}, journal = {Iranian Journal of Earth Sciences}, volume = {2}, number = {2}, pages = {143-149}, year = {2010}, publisher = {Islamic Azad University, Mashhad Branch}, issn = {2008-8779}, eissn = {2228-785X}, doi = {}, abstract = {The Mikkes basin is located at the north center of Morocco. It comprises three different zones which represent diversified geologies which shelter a phreatic and confined aquifer in the Sais basin and a shallow aquifer in the Tabular Middle Atlas. The springs in the Sais phreatic aquifer have suffered a maximum depletion. The springs with a deep or mixed origin are known as low flow variation springs. Actually, the variations of the fall of spring’s flows could be linked to a different hydro-geological context of these springs.}, keywords = {Morocco,Mikkes,Sais phreatic aquifer,Sais confined aquifer,Tabular aquifer,springs,Flow,hydro-geological context}, url = {http://ijes.mshdiau.ac.ir/article_522723.html}, eprint = {http://ijes.mshdiau.ac.ir/article_522723_2e4847701f2cc7daf688f9e71fa9686f.pdf} }