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(iii) to obtain a continuous record containing information on volcanic activities and climate changes in the central northern Mediterranean region, and (iv) to better understand the impact of major geological/environmental events on general evolutionary patterns and shaping an extraordinary degree of endemic biodiversity as a matter of global significance. For this purpose, five primary drill sites were selected based on the results obtained from sedimentological studies, tectonic mapping in the catchment and detailed seismic surveys conducted between 2004 and 2008. For the recovery of up to ca. 680 m long sediment sequences at water depths of more than 260 m a newly developed platform operated by DOSECC shall be used. The drilling operation is planned to take place in 2011. 200
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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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This common or different characteri
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The gross lithologies observed are
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Flame structure:. Flame shaped stru
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Fig. 5: Power Velocity and Cumulati
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Mary FORD ILP TASK FORCE on SEDIMEN
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41.5° 41° 40.5° 40° 0 50 km 42
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Results suggest that: a) The incisi
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Uplift of the Gargano Promontory as
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features with a NE-SW shortening di
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interglacial epochs, on which the r
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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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ock in extension at the relatively
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Fig. 3. In-situ stress measurements
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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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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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Page 170 and 171: and Italy in the centre, and the Io
Page 172 and 173: Figure 1 - Geological context (from
Page 174 and 175: display rapid lateral variations in
Page 176 and 177: Figure 1 - Geological context of th
Page 178 and 179: Figure 2 - Example of porosity meas
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Page 182 and 183: as the Dinarides or Hellenides by a
Page 184 and 185: Ustaszewski, K., Schmid, S.M., Füg
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Page 188 and 189: In new geological map of Albania (i
Page 190 and 191: 1991), Preapulian and Ionian zones
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Page 194 and 195: Attention has been paid in drawing
Page 196 and 197: Hilterman, F.J., 1983. Seismic lith
Page 198 and 199: Figure 4. Heavy mineral strata in t
Page 200 and 201: References Breesch, L., Swennen, R.
Page 202 and 203: The Pb isotope ratios of all rocks
Page 204 and 205: Figure 3: Th/Yb versus Ta/Yb plot.
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Page 208 and 209: References � ermák, V., 1993. Li
Page 210 and 211: Fig. 2 Integrated Strength of the l
Page 212 and 213: during the flexure of the foreland.
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