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Incision (m) versus ages of terrace units (ka) Breks on slope are materialized by the vertical dashed grey lines (J. Carcaillet et al, 2009). Based on age determinations for each level and their height from the river bed we found that the average lifting have been from 0.5 mm to 10 mm per year. Comparing the available data for the terrace deposits of the river valleys in Albania with those of Mediterranean area, it is concluded that it is a good respective correlation between the terrace units and their ages (Table 1, after M.G. Macklin, 2001). The data show that neotectonic movements, which affected our country territory during Pliocene and Quaternary period, have been of the same time with those of Mediterranean area. References Table 1: Age data from some rivers of Mediterranean are (after M.G. Macklin et al, 2001).� Aliaj, Sh., Melo, V., Hyseni, A., Skrami, J., Mëhillka, Ll. Muço, B., Sulstarova, E., Prifti, K., Pashko, P., Prillo, S., 1996. Neo-tectonic map of Albania, scale 1: 200000. Archive of seismology Institute, Tirana, Albania. Carcaillet J., J.L. Mugnier, R. Koçi, F. Jouanne, 2009. Uplift and active tectonics of Albania from incision of alluvial tarraces. Quaternary Research 71 (2009) 465-476. Koçi, R., 2005. Neo-tectonic of Tirana-Durres area and its role on the terraces formation of Erzeni river.Archive of seismology Institute, Tirana, Albania. Koçi, R., 2008. Doctorate thesis: Expression of the neo-tectonic movements in terraces of some rivers of Albania. Archive of seismology Institute, Tirana, Albania. 84
Koçi R., S Bushati, J.L. Mugnier, E. Perenjesi, 2009. The river tarraces-indicators of the neotectonic movements in Albania. 5th Congress of Balkan Geophysical Society. Belgrade, Serbia. Lewin, J, Macklin, G. M., Woodward, D. J., 1989. Late Quaternary fluvial sedimentation in Voidomatis Basin Epiris, northwest Greece. The Godwin Laboratory, Sub department of Quaternary Research, University of Cambridge CB2 3RS, UK. Macklin M.G., I.C. Fuller, J. Lewin, D.G. Passmore, J. Rose, J.C. Woodward, S. Black, R.H.B. Hamlin, J.S. Rowan, 2001. Correlation of fluvial sequences in the Mediterranean basin over the last 200 ka and their relationship to climate change. Quaternary Science Reviews 2, 1633-1641. Prifti, K, Meçaj. N., 1990. Geomorphologic development of river valleys in Albania and their practice importance. Geographic Studies, Nr. 4, Tirana, Albania. 85
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6 th WORKSHOP of the ILP TASK FORCE
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Nr. Prénom NOM Afilation 1 Myqerem
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6th workshop of the ILP Task Force
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11h10-11h30: Vilson Silo, Salvatore
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14h40-15h: Ariana Bejleri, Mensi Pr
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ABAZI Sheribane 71 ADDOUM Belkacem
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ILP TASK FORCE on SEDIMENTARY BASIN
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Topography, sediment and basement O
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REFERENCES Argnani A., Favali P., F
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Fig. 3: Source rocks distribution w
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etc, are found in concentrations hi
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� Fig.�3.�Map�of�the�gr
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Legend Well Fig. 1: A) Hydrographic
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___________________________________
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Page 51 and 52: ILP TASK FORCE on SEDIMENTARY BASIN
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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
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Page 78 and 79: 41.5° 41° 40.5° 40° 0 50 km 42
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
Page 86 and 87: interglacial epochs, on which the r
Page 92 and 93: agreement with the ~E-W extension p
Page 97: documented six terrace levels in th
Page 105 and 106: D e p t h (m) D e p t h (m) NW Shku
Page 107 and 108: Abstract ILP TASK FORCE on SEDIMENT
Page 112 and 113: mineralization increase, a reductio
Page 114 and 115: Besides the hydro-dynamic factors,
Page 116 and 117: these basins formed. 2) During the
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Page 124 and 125: Adriatic coastline. The alluvial de
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Page 128 and 129: The first project of "Science for P
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Page 132 and 133: Upper Jurassic of the Ionian Zone c
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Page 136 and 137: ock in extension at the relatively
Page 138 and 139: Fig. 3. In-situ stress measurements
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Page 144 and 145: gneissic) rocks occurred on the nor
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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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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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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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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
show all

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