Abstract:The present study aims to charcaterize, by geophysical methods (electrical sounding and seismic refraction), the downstream part of the Oued Nador alluvial layer or deposits (Tipaza, Algeria) and the morphology of its bedrock to better locate the freshwater-saltwater limit. This will allow to better understand the marine intrusion.Indeed, the aquifer is defined by a clay and marl substratum of middle to lower Pliocene Piacenzian age rich in recent Neogene and Quaternary filling (Quaternary alluvium composed of… Show more
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