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Results suggest that: a) The incision rate reaches the greatest values in the Osum area; b) The incision is more strongly controlled by the normal faults than the thrust faults; c) The normal faulting linked to the East Albanian graben systems seems more active than the normal faulting that affects the North West part of Greece. Table 1. Kinematic of active structures active analyzed from the incision of the terraces levels of the Vjosa, Osum, Devoll and Shkumbin rivers. Name Structure River Vertical slip movement (m/ka) Coastal pop - up PaleoSeman ~ 0.1 ( Fouache et al, 2010) Shkumbin Anticline Shkumbin ~ 0.2 Elbasan Graben Shkumbin > 1 Lushnje - Tepelenë Thrust Shkumbin ~ 0.9 Lushnje - Tepelenë Thrust Vjosa ~ 0.2 Tomorrica Thrust Devoll ~ 0.4 Burcal Normal Fault Devoll ~ 0.3 Nerotrivi Normal Fault Vjosa > 0.4 Konitsa Normal Fault Systems Vjosa > 0.4 Papingo West Normal Fault Vjosa ~1.8 between 25 and 17 Ka (Carcaillet, et al, 2009) West Graben Normal Fault Systems Devoll > 0.8 West Ersekë Normal Fault Systems Osum 1.7 – 2.1 References Aliaj, Sh., Melo, V., Hyseni, A., Skrami, J., Mëhillka, Ll. Muço, B., Sulstarova, E., Prifti, K., Pashko, P., Prillo, S., 1996. Neo-tectonic map of Albania, scale 1: 200000. Archive of seismology Institute, Tirana, Albania. Aliaj, S.H., 1997. Alpine geological evolution of Albania. Albanian Journal of Natural and Technology Sciences 3, 69-81. Aubouin, J, Ndojaj, I., 1964. Regard sur la géologie de l’Albanie et sa place dans la géologie des Dinarides. Bulletin de la Société Géologique de France 6, 539-625. Baker, C., Hatzfeld, D., Lyon-Caen, H., Papadimitriou, E., Rigo, A., 1997. Earthquake mechanisms of the Adriatic Sea and Western Greece: implications for the oceanic subduction-continental collision transition. Geophysical Journal International 131, 559-594. Carcaillet, J., Mugnier, J.L., Koçi, R., Jouanne, F., 2009. Uplift and active tectonics of southern Albania inferred from incision of alluvial terraces. Quaternary Research 71, 465-476. Fouache E., Vella C., Dimo, L., Gruda, G., Mugnier, J-L., Denèfle, M., Monnier, O., Hotyat, M., Huth. E., 2010. Shoreline reconstruction since the Middle Holocene in the vicinity of the ancient city of Apollonia (Albania, Seman and Vjosa deltas). Quaternary International 216, 118–128 Goldsworthy, M., Jackson, J., Haines, J., 2002. The continuity of active fault systems in Greece. Geophysical Journal International 148(3), 596-618. Hamlin, R.,Woodward, J., Black, S., Macklin, M.G., 2000. Sediment fingerprinting as 580 a tool for interpreting long- term river activity: the Voidomatis basin, NWGreece. In: 581 Foster, I.D.L. (Ed.), Tracers in Geomorphology. Wiley, Chichester, 473–501. Jouanne, F., Bushati, S., Mugnier, J.L., Shinko, I., Pasha, M., Koci, R. GPS constrains on current tectonics of Albania. Geophysical Research Letters, Submitted. Koçi, R., Bushati, S., Mugnier, J-L., Perenjesi, E., 2009. The river tarraces-indicators of the neotectonic movements in Albania. 5 th Congress of Balkan Geophysical Society. Belgrade, Serbia. Lewin, J., Macklin, M.G., Woodward, J.C., 1991. Late Quaternary fluvial sedimentation in the Voidomatis basin, Epirus, Northwest Greece. Quaternary Research 35, 103-115. Macklin, M.G., 2000. Sediment fingerprinting as a tool for interpreting long-term river activity: the Voidomatis basin, NW Greece. In: Foster I.D.L. (Ed.), Tracers in geomorphology. Wiley, Chichester, pp. 473-501. Roure, F., Nazaj, S., Mushka, K., Fili, I., Cadet, J.P., Bonneau, M., 2004. Kinematic evolution and petroleum systems - An appraisal of the Outer Albanides. In: Mc Clay K.R. (Ed.), Thrust tectonics and hydrocarbon systems. AAPG memoir 82, pp. 474-493. Woodward, J.C. Hamlin, R.B.H., Macklin, M.G., Karkanas, P., Kotjabopoulou E., 2001. Quantitative sourcing of slackwater deposits at Boila rockshelter: A record of late-glacial flooding and palaeolithic settlement in the Pindus Mountains, Northern Greece. Geoarchaeology 16(5), 501-536. 66
ILP TASK FORCE on SEDIMENTARY BASINS 2010 International Workshop November 7-12, 2010, Tirana (Albania) CONTRACTION and VERTICAL MOVEMENTS in the GARGANO PROMONTORY and ADJACENT OFFSHORE: IMPLICATION for the TECTONICS of the SOUTH ADRIATIC DOMAIN Nicolaas J. HARDEBOL and Giovanni BERTOTTI Delft Univ. of Techn., Stevinweg 1, 2628 CN Delft, the Netherlands; VU University, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands; T +31 15 27 81352; E N.J.Hardebol@tudelft.nl Introduction The Adriatic plate has been described as a double-verging plate that is bordered to the west by the Apenninic and to the east by the Dinaric-Helvetic fold-and-thrust belts (Figure 1a). The interior of the plate supposedly hosts a north-south trending flexural bulge from Istria to the Gargano promontory (and the Apulian Ridge), which divides the Adriatic basins in respect to their relative foreland position to either the Apenninic or Dinaride orogenic systems. The Neogene deformation history and vertical motions in the interior of the Adriatic plate is subject to flexural forcing or compressional effects transmitted from the plate margins. This study present new field and offshore seismic data from the Gargano Promontory and adjacent Southern Adriatic Basin to examine their deformation history. The Southern Adriatic Basin (SAB) stretches southeast-ward offshore of the Gargano and Puglia coastlines (Figure 1a) and is underlain by a basement of Triassic-Lias salts to platform carbonates and a Lias-Cretaceous succession of mostly pelagic carbonates and marls that show an eastward, Dinaric-Hellenic facing dip. The SAB contains an Oligocene to Quaternary succession of mainly siliciclastics and calcarenites and subject to tilting and faulting of strata that are commonly regarded as transtensional and transpressional expressions linked to basement lineaments. The Gargano Promontory (GP) to the north forms up to 1000m relief and comprises mostly Jurassic-Cretaceous carbonates. The GP exhibits a peculiar morphological shape with four prominent peneplains that are divided by high and steep slopes (Figure 1d). Miocene shallowwater limestones cover the eroded substratum unconformably and are found over most of the Gargano Promotory. Post-Lower Messinian deposits however are scarce and especially developed onto the two lowermost peneplains at 80m and 200m along the southern border of the GP (Figure 1b). These Mio-Pliocene deposits cover erosional surfaces and contain diagnostic coastal cliff facies linked to abrasive marine terrace that help deciphering the Tertiary deformation and relief development (Casolari et al., 2000; Bertotti et al., 2001). This study presents new data from the GP and from offshore seismic profiles of the SAB. We examine their contrasting physiographic expression in effect to a Miocene-Pliocene contractional and uplift-subsidence history. We especially focus on the marine terrace sediments in association to their tilted substratum for the GP and on the coeval depositional and deformation history in the adjacent SAB. The onshore field data and offshore seismic interpretations are combined aiming at a more univocal picture of the kinematics and vertical motions for Tertiary times. 67
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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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Page 43: Legend Well Fig. 1: A) Hydrographic
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Page 56 and 57: This common or different characteri
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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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Page 107 and 108: Abstract ILP TASK FORCE on SEDIMENT
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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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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
show all

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