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   Hydro-Geological Context of Mikkes Springs and Different Variations of their Flows (Morocco)  
   
نویسنده Belhassan K.
منبع iranian journal of earth sciences - 2010 - دوره : 2 - شماره : 2 - صفحه:143 -149
چکیده    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.
کلیدواژه Morocco ,Mikkes ,Sais phreatic aquifer ,Sais confined aquifer ,Tabular aquifer ,Springs ,Flow ,Hydro-geological context.
آدرس UFR: Geology Applied to Hydro-Geological Researches, Faculty of Sciences Dhar Mehraz, Morocco
پست الکترونیکی belhassankal@yahoo.fr
 
     
   
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