DYNAMICS and ACTIVE PROCESSES - International Lithosphere ...

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Organizing Committee Kristaq MUSKA (PUTirana, Albania) Shaqir NAZAJ (PUTirana, Albania) Liviu MATENCO (VU-Amsterdam, the Netherlands) François ROURE (IFP, France) Scientific Committee Giovanni BERTOTTI (VU-Amsterdam, the Netherlands) Salvator BUSHATI (Academy of Sciences, Tirana, Albania) Sierd CLOETINGH (VU-Amsterdam, the Netherlands) Carlo DOGLIONI (Univ. La Sapienza, Roma, Italy) Ilia FILI (Visoka Energy Co., Fieri, Albania) Perparim HOXHA (PUTirana, Albania) François JOUANNE (Grenoble Univ., France) Anastasia KIRATZI (Aristotle Univ., Thessaloniki, Greece) Ibrahim MILUSHI (Institute of Geosciences, Tirana, Albania) Giuseppe NARDI (Univ. Federico II, Naples, Italy) Adil NEZIRAJ (Geological Survey, Tirana, Albania) Luan NIKOLLA (National Agency of Natural Resources, Tirana, Albania) Frederik PREMTI (PUTirana, Albania) Magdalena SCHECK-WENDEROTH (GFZ, Germany) Rudy SWENNEN (KU-Leuven) Bruno TOMJELOVIC (Zagreb Univ., Croatia) Fied Trips committee Çerçir DURMISHI (PUTirana, Albania) Avni MESHI (PUTirana, Albania) Bardhyl MUCEKU (PUTirana) Kujtim ONUZI (Institute of Geosciences, Tirana, Albania)
Page 1: 6 th WORKSHOP of the ILP TASK FORCE
Page 6 and 7: 47 Vangjel MELO Faculty of Geology
Page 8 and 9: 14-14h30: Liviu Matenco and M. Duce
Page 10 and 11: 8h20-8h50: Anastasia Kiratzi (Arist
Page 12 and 13: Ylbert Muceku, Jani Skrami, Edmond
Page 14 and 15: MUCO Betim 113 MUGNIER Jean-Louis 6
Page 16 and 17: Figure 1: Map of the Arabian Penins
Page 19 and 20: ILP TASK FORCE on SEDIMENTARY BASIN
Page 21: Fig. 1: Isochron map (seconds, TWT)
Page 25: ILP TASK FORCE on SEDIMENTARY BASIN
Page 28 and 29: Lineament (VDL) contribute in post-
Page 37 and 38: hydrochemical parameters of the Kav
Page 39: � References� Appelo C.A.J. and
Page 42 and 43: The DRASTIC model has four assumpti
Page 47 and 48: ___________________________________
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TOPO-EUROPE addresses the 4-D topog
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ILP TASK FORCE on SEDIMENTARY BASIN
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The north-western flank and the cen
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Fig. 2: Epicentral map of September
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Alfred FRASHERI ILP TASK FORCE on S
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��
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Incision rate (m/ka) developed duri
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structure which is an active seismo
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Neo-tectonic role on formation of t
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Incision (m) versus ages of terrace
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� Aquifer basin of Mirdita’s zo
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D e p t h (m) D e p t h (m) 100 50
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� Serafimovski T., Alderton M., D
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� ILP TASK FORCE on SEDIMENTARY B
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from the Southern part to the direc
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Milia A., Turco E., Pierantoni P.P.
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ILP�TASK�FORCE�on�SEDIMENTA
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Fig. 2 PGA distribution for 90% of
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KEYWORDS: source rock levels, TOC,
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consequences for the geometry and k
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tracing the MTFC as curved system l
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gas with hydrogen sulfide concentra
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GROUPING of ALBANIAN OILS Oils from
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sandstones of Miocene deposits. Alb
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Minerals identification by XRD indi
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westward migration of the extension
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Figure 2 - Detailed localisation an
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macroporous sp., lepidorbitoides sp
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Lycian nappes possibly represent an
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Figure 1: Major tectonic units of t
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SEISMOGENIC DEEP FAULTS in IONIAN Z
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2. Bajo I., 1984. Evaporitet e zone
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Figure 2: Extended multi-element va
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REFERENCES 1. Lapierre H., Bosch D.
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Fig. 1 (a) Moho depth, (b) Temperat
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