DYNAMICS and ACTIVE PROCESSES - International Lithosphere ...

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Ustaszewski, K., Schmid, S.M., Fügenschuh, B., Tischler, M., Kissling, E. & Spakman, W. 2008: A map-view restoration of the Alpine-Carpathian-Dinaridic system for the Early Miocene. In: Orogenic processes in the Alpine collision zone (N. Froitzheim & S.M. Schmid, editors), Swiss Journal of Geosciences 101/Supplement 1: S273–S294. van Hinsbergen, D.J.J., Hafkenscheid, E., Spakman, W., Meulenkamp, J.E. & Wortel, R. (2005). Nappe stacking resulting from continental lithosphere below subduction of oceanic <strong>and</strong> Greece. Geology 33:325–328. 170
Figure 1: Major tectonic units of the Alps, Carpathians <strong>and</strong> Dinarides (from Schmid et al. 2008). 171
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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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112
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The first project of "Science for P
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116
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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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Page 152 and 153: Ionian zones. The thrust belt is ch
Page 154 and 155: 1. In the west: Amonice-Gernec-Gors
Page 156 and 157: 4. A family of four, including all
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Page 160 and 161: The primary purpose of this study i
Page 162 and 163: Non Clay Minerals present in Brari
Page 164 and 165: The deformation can be divided in t
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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
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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.
Page 214: (iii) to obtain a continuous record
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