By M. Koïta, H. Jourde (auth.), Nicolaos Lambrakis, George Stournaras, Konstantina Katsanou (eds.)

The booklet makes a speciality of the administration of the aquatic surroundings. it truly is aimed toward scientists, scholars, governmental officers and experts facing groundwater and surroundings. Its major aim is to notify the reader of rules, wisdom and adventure by way of a sustainable aquatic setting. the most issues are as follows: Water our bodies and Ecosystems; weather switch and Water our bodies; Water caliber and agriculture; interplay of floor and flooring waters; Karst Hydrogeology; non-stop Media Hydrogeology; Fissured Rocks Hydrogeology; Hydrochemistry; Geothermics and thermal waters; The position of water in development initiatives; Hydrology

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Owing to the collision of tectonic plates (Mouthereau and Lacombe 2006) a series of westward fold-and-thrust belts can be observed. The geological formation in this study area can be roughly separated from East to West into four regions by the orientation of faults. Region I at the most eastern side ranges in age from Eocene to Miocene, where the predominant lithology is massive slate rock accompanied with metasandstones and metasiltstones. Region II extends from Eocene to early Oligocene, the upper part is dominated by hard shale stone and the lower part is coarse quartz sandstone hosted.

Simple Skolithos burrows are often associated with larger burrows attributed to “Bergaueria” sp. The 24 H. Al Ajmi et al. almost “reef-like” horizons of Skolithos and/or Bergaueria are up to 13 meters thick. Most of the internal sedimentary structures have been destroyed by burrowing; however, the primary cross-bedding is often faintly visible. The presence of a variety of burrowing organisms and Cruziana sp. in both units testifies to deposition of the entire Dibsiyah in a marine environment. In their majority, the low-angle, 2D through cross-bedded horizons represent tidal channels.

Table 1. Litholog from existing borehole. 2 - 36m It should be noted that VES method is suitable only in case of 1-D structure. 1D inversion is often used to define aquifer geometry that is intrinsically multifaceted. This interpretational practice is erroneous due to unacknowledged multidimensional property. F. Oyedele, S. Oladele a.

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