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etc, are found in concentrations higher then the limits of drinking water. In the diagram (not shown) of Total Mineralization (TM) versus well depth (H) was found that groundwater can maintain TM values less that 1.0 mg/l up to a depth that ranges from 400 to 500m according to the well position with respect to recharge and discharge zone. The basin of Kavaja forms a syncline (Hyseni, 1995), whose axial part consists of water-bearing Astian conglomerates and sandstone covered by Quaternary alluvial sediments, whereas the Piacensian clay formations construct the western and eastern flanks of the syncline (Fig. 1). � Fig. 1: Geological map of the Kavaja basin The groundwater of the Kavaja basin belongs mostly to Ca-Mg_HCO3 hydrochemical type (Fig.2,3). The groundwater evolves gradually from HCO3 type to Cl type, from southeastern (Shkumbini river) towards northwestern (Adriatc sea) (Beqiraj et.al., 2007), that is from the recharge to discharge zone (Fig.4). On the other hand, the vertical evaluation of the groundwater geochemical composition towards the depth is expressed by means of the increase of the General Mineralization. Another trend of the geochemical groundwater composition, shown by gradual increase of the General Mineralization and Hardness (Fig. 5.a,b), is from both western and eastern flanks of the Kavaja depression towards its central part. The horizontal evaluation of the 22
hydrochemical parameters of the Kavaja groundwater fits very well with the variation of the hydraulic conductivity values of the Kavaja aquifer. Thus, the highest values of the General Mineralization and Hardness correspond to the lowest values of the hydraulic conductivity. 23
Page 1: 6 th WORKSHOP of the ILP TASK FORCE
Page 5 and 6: Nr. Prénom NOM Afilation 1 Myqerem
Page 7 and 8: 6th workshop of the ILP Task Force
Page 9 and 10: 11h10-11h30: Vilson Silo, Salvatore
Page 11 and 12: 14h40-15h: Ariana Bejleri, Mensi Pr
Page 13 and 14: ABAZI Sheribane 71 ADDOUM Belkacem
Page 15 and 16: ILP TASK FORCE on SEDIMENTARY BASIN
Page 17: Topography, sediment and basement O
Page 20 and 21: REFERENCES Argnani A., Favali P., F
Page 23: ILP TASK FORCE on SEDIMENTARY BASIN
Page 29: Fig. 3: Source rocks distribution w
Page 38 and 39: � Fig.�3.�Map�of�the�gr
Page 43: Legend Well Fig. 1: A) Hydrographic
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Page 56 and 57: This common or different characteri
Page 58 and 59: The gross lithologies observed are
Page 60 and 61: Flame structure:. Flame shaped stru
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Page 67: Fig. 5: Power Velocity and Cumulati
Page 71: Mary FORD ILP TASK FORCE on SEDIMEN
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Page 80 and 81: Results suggest that: a) The incisi
Page 82 and 83: Uplift of the Gargano Promontory as
Page 84 and 85: features with a NE-SW shortening di
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interglacial epochs, on which the r
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ILP TASK FORCE on SEDIMENTARY BASIN
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agreement with the ~E-W extension p
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documented six terrace levels in th
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Koçi R., S Bushati, J.L. Mugnier,
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D e p t h (m) D e p t h (m) NW Shku
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Abstract ILP TASK FORCE on SEDIMENT
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mineralization increase, a reductio
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Besides the hydro-dynamic factors,
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these basins formed. 2) During the
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Adriatic coastline. The alluvial de
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The first project of "Science for P
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Upper Jurassic of the Ionian Zone c
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120
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ock in extension at the relatively
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Fig. 3. In-situ stress measurements
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126
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gneissic) rocks occurred on the nor
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132
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136
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Ionian zones. The thrust belt is ch
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1. In the west: Amonice-Gernec-Gors
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4. A family of four, including all
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144
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The primary purpose of this study i
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Non Clay Minerals present in Brari
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The deformation can be divided in t
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152
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154
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and Italy in the centre, and the Io
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Figure 1 - Geological context (from
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display rapid lateral variations in
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Figure 1 - Geological context of th
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Figure 2 - Example of porosity meas
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166
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as the Dinarides or Hellenides by a
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Ustaszewski, K., Schmid, S.M., Füg
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172
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In new geological map of Albania (i
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1991), Preapulian and Ionian zones
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Attention has been paid in drawing
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Hilterman, F.J., 1983. Seismic lith
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Figure 4. Heavy mineral strata in t
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References Breesch, L., Swennen, R.
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The Pb isotope ratios of all rocks
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Figure 3: Th/Yb versus Ta/Yb plot.
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192
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References � ermák, V., 1993. Li
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Fig. 2 Integrated Strength of the l
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during the flexure of the foreland.
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(iii) to obtain a continuous record
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