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these basins formed. 2) During the Middle Pleistocene a rifting episode took place in the Campania margin that formed NE trending half grabens while the extension stopped in the Gaeta Basin. 3) Over the last 400 ky the Eastern Tyrrhenian margin the extension in the Campania Margin is associated to an intense volcanism and a dextral shear zone characterize the boundary between the deep Tyrrhenian basin and the Eastern Tyrrhenian continental Margin (Milia et al., 2009; Milia et al., 2010). The results of this geologic processes is the individuation of a breakway zone located in the Campania Margin that bound a microplate migrating toward the SE. Fig. 1. Seafloor morphology of the Tyrrhenian Sea (Marani et al., 2004) and location of the study area. References Iannace P., Massa B., Milia A., Torrente M.M. (2010) 3-D modeling of the structural features of Gaeta Bay (Eastern Tyrrhenian Sea margin). Rendiconti online Soc. Geol. It., Vol. 10, 73-75. Kastens, K.A., Mascle, J. and Others, O.D.P. (1988) Leg 107 in the Tyrrhenian Sea: insights into passive margin and backarc basin evolution. Geol. Soc. Amer. Bull. 100, 1140-1156. Marani M.P., Gamberi F., Bortoluzzi G., Carrarra G., Ligi M., Penintenti D. (2004) Seafloor morphology of the Tyrrhenian Sea, Scale 1:1,000,000. Included to Mem. Descr. Carta Geol. Italia, 44. Milia, A. 1999. Aggrading and prograding infill of a pery-tyrrhenian basin (Naples Bay, Italy). Geo-Mar. Lett., 19, 237-244. Milia A. and Torrente M.M. (1999) Tectonics and stratigraphic architecture of a pery-Tyrrhenian half-graben (Bay of Naples, Italy). Tectonop., 315, 297-314. Milia A. and Torrente M.M. (2007) The influence of paleogeographic setting and crustal subsidence on the architecture of ignimbrites in the Bay of Naples (Italy). Earth Planet. Scie. Lett., 263, 192-206. 102
Milia A., Turco E., Pierantoni P.P. and Schettino A. (2009) Four-dimensional tectono-stratigraphic evolution of the Southeastern peri-Tyrrhenian Basins (Margin of Calabria, Italy). Tectonoph., 476, 41-76. Milia A., Morabito S., Passero S., Ruggieri S., Turco E. (2010) Tectonics and Geomorpholgical processes between Sirene and Sartori Lineaments (Eastern Tyrrhenian Sea). Rendiconti online Soc. Geol. It., 10, 83. Sartori, R., 1990. The main results of ODP Leg 107 in the frame of Neogene to Recent geology of perityrrhenian areas. In: Kastens,K.A., Mascle, J., et al. (Eds.), Proceedings of the Ocean Drilling Program. Scientific Results 107, pp. 715– 730. Torrente M.M., Milia A., Bellucci F., Rolandi G. (2010) Extensional tectonics in the Campania Volcanic Zone (eastern Tyrrhenian Sea, Italy): new insights into the relationship between faulting and ignimbrite eruptions. Ital. J. Geosci. (Boll. Soc. Geol. It.), 129, 1-19. 103
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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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Page 65 and 66: ILP TASK FORCE on SEDIMENTARY BASIN
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 and 98: documented six terrace levels in th
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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,
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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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Page 152 and 153: Ionian zones. The thrust belt is ch
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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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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
show all

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