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Lineament (VDL) contribute in post-orogeny shaping and could also help migration of HC generated from nearby intra-platform basins. Despite the fact that the regional platform architecture setting is less studied and understood than the fertile Ionian basin in the south and because of discouraging results over the years, the future petroleum exploration efforts in this region should be diverted more and more towards the platform sub-thrust plays. Fig. 1: General view of the NW Albania – Montenegro region. Despite abundant oil shows in the region no discovery has been achieved so far till now. Fig. 2: Simplified geo-tectonic map showing the morphology between South Adriatic Basin and the Kruja-Dalmatian platform zones (After OMV, 2000). 14
Fig. 3: Source rocks distribution within the Mesozoic sequence (Modified after Zappatera, 1994). Analogue source rocks of Cretaceous age proved in Southern Appenines are expected in the Study Area. Fig. 4: Simplified regional geological section from Southern Appenines (Italy) to Krasta Zone (Albania) showing that deep seated autochthonous platform carbonates in onshore western Albania region resemble the Southern Apennines plays in Italy (Modified after Picha, 1995). 15
Page 1: 6 th WORKSHOP of the ILP TASK FORCE
Page 5 and 6: Nr. Prénom NOM Afilation 1 Myqerem
Page 7 and 8: 6th workshop of the ILP Task Force
Page 9 and 10: 11h10-11h30: Vilson Silo, Salvatore
Page 11 and 12: 14h40-15h: Ariana Bejleri, Mensi Pr
Page 13 and 14: ABAZI Sheribane 71 ADDOUM Belkacem
Page 15 and 16: ILP TASK FORCE on SEDIMENTARY BASIN
Page 17: Topography, sediment and basement O
Page 20 and 21: REFERENCES Argnani A., Favali P., F
Page 23: ILP TASK FORCE on SEDIMENTARY BASIN
Page 36 and 37: etc, are found in concentrations hi
Page 38 and 39: � Fig.�3.�Map�of�the�gr
Page 43: Legend Well Fig. 1: A) Hydrographic
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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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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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ILP TASK FORCE on SEDIMENTARY BASIN
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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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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
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