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D e p t h (m) D e p t h (m) 100 50 0 45 4 45 -50 0 W D-11 VES-1 VES-2 65 7 32 110 D-11 VES-1 VES-2 100 50 0 0-10 ohmm - Sand VES-3 VES-4 D-3-A 80 19 36 70 30 50 80 10-20 ohmm - Clay - alevrolite 20-30 ohmm - Breccia, gravel VES-5 30 Shkumbin's River 52 VES-6 VES-7 100 32 70 14 28 500 1000 1500 2000 2500 3000 3500 D i s t a n c e (m) D-3-A VES-3 VES-4 VES-5 30 VES-6 L e g e n d 15 52 VES-7 VES-8 20 30 200 190 -50 0 500 1000 1500 2000 2500 3000 3500 D i s t a n c e (m) 30-50 ohmm - Clay - alevrolite - sand 50-100 ohmm - Gravel VES-8 100-200 ohmm - Carsted limstone E VES-9 VES-10 VES-9 23 70 VES-10 D-11 VES-1 Tectonic Applied drilling Applied VES Fig. 4: Geological - geophysical cross-section after VES carried out in the Profile 3-3 Krastë - Shushicë. Conclusions 1. Drillings Kozani-8, Papri-1, Maraku-1 have proved neotectonic regime of geological setting of Elbasn’s water basin, interpreted after seismic profile. 2. Gravel horizon interpreted after VES in cross-section profile of Vidhas - Gjergjan results fragmented with normal faults and thickness of depositions that vary from 7 until 200 m. 3. Geoelectrical environments with variation of apparent electraical resistivity values after cross-section profile of Krastë - Shushicë represents neotectonic planes of overthrusting faults of Mirdita’s zone on sub-zone Krasta and Krasta’s zone on Kruja’s zone. References Melo V., 1961. Review of neotectonic movement in building of Shkumbini’s terraces in Elbasan -Paper sector. Geological Sciences Bulletin No. 1, Tirana. Naço P., Kodra A., Çina A., Bedini E., 2005. Active tectonics evaporites and permanent seismicity of Elbasani area. Albania 14 th Meeting of the Association of European Geological Society. Torino, Italy, September, 2005. Naço P., Bedini E., Leka P., 2006. The Aquifer Basin of Elbasani, tectonic-forming conditions and the problems of its management. Geological Sciences Bulletin Nr. 1, 47-57, Tirana. Naço P., Bedini E., Leka P., 2006. Searching for hydrocarbons under large tectonic overthrusts of Albanides. Geological Sciences Bulletin No. 2, 33-42, Tirana. Leka P., Naço P., Vinçani F., Bedini E., 2007. Qualificative evaluation of Elbasani’s aquifer basin through Schlumberger electrical Soundings. Geological Sciences Bulletin Nr. 2, 47-56, Tirana. 92
Abstract ILP TASK FORCE on SEDIMENTARY BASINS 2010 International Workshop November 7-12, 2010, Tirana (Albania) Environment impact of closed copper mine in Rehova Skender Lipo Faculty of Geology and Mining, Tirana Albania Edmond Hoxha Faculty of Geology and Mining, Tirana, Albania In our country there are more than 30 closed mines that cause environmental pollution constantly beside them. One of them is the Rehova copper mine, closed 15 years ago, which continues to be a source of pollution and risks to the environment and population of this area. Waters going out from mine workings and the dump of the mineral processing plant are mixed with water flowing in Lubonja stream bringing its ongoing pollution, especially in the periods of intensive rainfall. The opencast mine stairs collapse leads to the expansion of their borders, destroying forests and pasture lands near the opencast area. The collapse of underground mining works not only damages constantly the surface of the new agricultural land, but is also a danger to people and livestock moving in this area. Large areas occupied from the opencast works are surfaces that need to be regenerated and turn back on forest and pasture. The wastes resulting from the enrichment of copper ore, has occupied a considerable area of land, and they pollute the waters passing through the waste mass. From the other side the breaks of the damp slopes risks to cause the slide of this waste mass over the road and agricultural lands nearby. The subject of this article is the assessment of the mentioned above phenomena and bringing of some thoughts on minimizing the damage to the environment. Reference � B. Shushku, E. Goskolli, 2009, Emergence risk situation and risk reduction at four Albanian tailing dams. 3 rd Balkan Mining Congress. Izmir, Turkey. � Lipo S., Kuka R., and al. 2007. Assessment of surface subsidence impacted from mining activity in coal mine Mezes. Geology and Mining Faculty, Tirana, Albania. � E. Hoxha, S. Lipo. 2005, Damage of infrastructure objects and agriculture production from mining activity at Rehova copper Mine. Faculty of Geology and Mining, Tirana, Albania. 93
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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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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 65 and 66: ILP TASK FORCE on SEDIMENTARY BASIN
Page 67: Fig. 5: Power Velocity and Cumulati
Page 71: Mary FORD ILP TASK FORCE on SEDIMEN
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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
Page 99: Koçi R., S Bushati, J.L. Mugnier,
Page 105: D e p t h (m) D e p t h (m) NW Shku
Page 112 and 113: mineralization increase, a reductio
Page 114 and 115: Besides the hydro-dynamic factors,
Page 116 and 117: these basins formed. 2) During the
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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
Page 154 and 155: 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
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