DYNAMICS and ACTIVE PROCESSES - International Lithosphere ...

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References � ermák, V., 1993. Lithospheric thermal regimes in Europe. Phys. Earth Planet. Int., 79, 179-193. Ritsema, J., van Heijst, H., 2004.Global transition zone tomography. J. Geophys. Res, 109, B02302, doi:10.1029/2003JB002610. Mooney, W.D., 2009. in: Treatise on Geophysics, B. Romanowicz, A. Dziewonski, G. Schubert, Eds. (Elsevier, Amsterdam, NL), Vol. 1, Chap. 11, pp.361-417. Mooney, W., Kaban, K., 2010. The North American Upper Mantle: Density, Composition, and Evolution,J. Geophys. Res. (in print). Tesauro, M., Kaban, M.K, .Cloetingh, S.A.P.L., 2008. EuCRUST-07: A new reference model for the European crust. Geophys. Res. Lett. 35, LXXXXX doi:10.1029/2007GL032244. Tesauro, M., Kaban, M.K., Cloetingh, S.A.P.L., 2009. A new thermal and rheological model of the European lithosphere. Tectonophysics, 476, 478-495. 194
Fig. 1 (a) Moho depth, (b) Temperature (C˚) at 100 km depth, (c), Global Rheology Map of the Upper and Lower crust. Numbers stand as follows: 1, Granite-Mafic garnet granulite, 2, Granite- Diabase, 3, Quarzite-Diabase, 4, Quarzite-Diorite, 5, Diabase. 195
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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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Page 160 and 161: The primary purpose of this study i
Page 162 and 163: 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
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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 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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