(Selido ΤΟϜϟϣ 5

Total Page:16

File Type:pdf, Size:1020Kb

(Selido Œ§Œüœúœüœ£ 5 ΔΕΛΤΙΟ ΤΗΣ ΕΛΛΗΝΙΚΗΣ ΓΕΩΛΟΓΙΚΗΣ ΕΤΑΙΡΙΑΣ Τόμος XLIII, Νο 5 BULLETIN OF THE GEOLOGICAL SOCIETY OF GREECE Volume XLIII, Νο 5 1 (5) ΕΙΚΟΝΑ ΕΞΩΦΥΛΛΟΥ - COVER PAGE Γενική άποψη της γέφυρας Ρίου-Αντιρρίου. Οι πυλώνες της γέφυρας διασκοπήθηκαν γεωφυ- σικά με χρήση ηχοβολιστή πλευρικής σάρωσης (EG&G 4100P και EG&G 272TD) με σκοπό την αποτύπωση του πυθμένα στην περιοχή του έργου, όσο και των βάθρων των πυλώνων. (Εργα- στήριο Θαλάσσιας Γεωλογίας & Φυσικής Ωκεανογραφίας, Πανεπιστήμιο Πατρών. Συλλογή και επεξεργασία: Δ.Χριστοδούλου, Η. Φακίρης). General view of the Rion-Antirion bridge, from a marine geophysical survey conducted by side scan sonar (EG&G 4100P and EG&G 272TD) in order to map the seafloor at the site of the construction (py- lons and piers) (Gallery of the Laboratory of Marine Geology and Physical Oceanography, University of Patras. Data acquisition and Processing: D. Christodoulou, E. Fakiris). ΔΕΛΤΙΟ ΤΗΣ ΕΛΛΗΝΙΚΗΣ ΓΕΩΛΟΓΙΚΗΣ ΕΤΑΙΡΙΑΣ Τόμος XLIII, Νο 5 BULLETIN OF THE GEOLOGICAL SOCIETY OF GREECE Volume XLIII, Νο 5 12o ΔΙΕΘΝΕΣ ΣΥΝΕΔΡΙΟ ΤΗΣ ΕΛΛΗΝΙΚΗΣ ΓΕΩΛΟΓΙΚΗΣ ΕΤΑΙΡΙΑΣ ΠΛΑΝHΤΗΣ ΓH: Γεωλογικές Διεργασίες και Βιώσιμη Ανάπτυξη 12th INTERNATIONAL CONGRESS OF THE GEOLOGICAL SOCIETY OF GREECE PLANET EARTH: Geological Processes and Sustainable Development ΠΑΤΡΑ / PATRAS 2010 ISSN 0438-9557 Copyright © από την Ελληνική Γεωλογική Εταιρία Copyright © by the Geological Society of Greece 12o ΔΙΕΘΝΕΣ ΣΥΝΕΔΡΙΟ ΤΗΣ ΕΛΛΗΝΙΚΗΣ ΓΕΩΛΟΓΙΚΗΣ ΕΤΑΙΡΙΑΣ ΠΛΑΝΗΤΗΣ ΓΗ: Γεωλογικές Διεργασίες και Βιώσιμη Ανάπτυξη Υπό την Αιγίδα του Υπουργείου Περιβάλλοντος, Ενέργειας και Κλιματικής Αλλαγής 12th INTERNATIONAL CONGRESS OF THE GEOLOGICAL SOCIETY OF GREECE PLANET EARTH: Geological Processes and Sustainable Development Under the Aegis of the Ministry of Environment, Energy and Climate Change ΠΡΑΚΤΙΚΑ / PROCEEDINGS ΕΠΙΜΕΛΕΙΑ ΕΚΔΟΣΗΣ EDITORS Γ. ΚΟΥΚΗΣ G. KOUKIS Πανεπιστήμιο Πατρών University of Patras Α. ΖΕΛΗΛΙΔΗΣ A. ZELILIDIS Πανεπιστήμιο Πατρών University of Patras Ι. ΚΟΥΚΟΥΒΕΛΑΣ I. KOUKOUVELAS Πανεπιστήμιο Πατρών University of Patras Γ. ΠΑΠΑΘΕΟΔΩΡΟΥ G. PAPATHEODOROU Πανεπιστήμιο Πατρών University of Patras Μ. ΓΕΡΑΓΑ M. GERAGA Πανεπιστήμιο Πατρών University of Patras Β. ΖΥΓΟΥΡΗ V. ZYGOURI Πανεπιστήμιο Πατρών University of Patras PATRAS, May 2010 ΕΛΛΗΝΙΚΗ ΓΕΩΛΟΓΙΚΗ ΕΤΑΙΡΕΙΑ = ΔΙΟΙΚΗΤΙΚΟ ΣΥΜΒΟΥΛΙΟ (που εξελέγη στη Γενική Συνέλευση των μελών της Εταιρίας το Μάρτιο του 2010) ΠΡΟΕΔΡΟΣ Απόστολος ΑΛΕΞΟΠΟΥΛΟΣ ΑΝΤΙΠΡΟΕΔΡΟΣ Αλεξάνδρα ΖΑΜΠΕΤΑΚΗ-ΛΕΚΚΑ ΓΕΝ. ΓΡΑΜΜΑΤΕΑΣ Ευγενία ΜΩΡΑΪΤΗ ΕΙΔ. ΓΡΑΜΜΑΤΕΑΣ Δημήτριος ΓΑΛΑΝΑΚΗΣ ΤΑΜΙΑΣ Ασημίνα ΑΝΤΩΝΑΡΑΚΟΥ ΕΦΟΡΟΣ Χαράλαμπος ΚΡΑΝΗΣ ΜΕΛΗ Κωνσταντίνος ΒΟΥΔΟΥΡΗΣ Χρυσάνθη ΙΩΑΚΕΙΜ Αθανάσιος ΓΚΑΝΑΣ vi GEOLOGICAL SOCIETY OF GREECE = BOARD OF DIRECTORS (elected at the General Assembly of the members of the Society on March 2010) PRESIDENT Apostolos ALEXOPOULOS VICE-PRESIDENT Alexandra ZAMBETAKIS-LEKKAS GENERAL SECRETARY Evgenia MORAITI EXECUTIVE SECRETARY Dimitrios GALANAKIS TREASURER Asimina ANTONARAKOU TRUSTEE Charalambos ΚRANIS MEMBERS Konstantinos VOUDOURIS Chyssanthi IOAKIM Athanasios GANAS vii ΟΡΓΑΝΩΤΙΚΗ ΕΠΙΤΡΟΠΗ 12ου ΔΙΕΘΝΟΥΣ ΣΥΝΕΔΡΙΟΥ = ΠΡΟΕΔΡΟΣ Γεώργιος ΚΟΥΚΗΣ, Καθηγητής Πανεπιστημίου Πατρών ΑΝΤΙΠΡΟΕΔΡΟΣ Αβραάμ ΖΕΛΗΛΙΔΗΣ, Καθηγητής Πανεπιστημίου Πατρών ΓΕΝΙΚΟΣ ΓΡΑΜΜΑΤΕΑΣ Ιωάννης ΚΟΥΚΟΥΒΕΛΑΣ, Αν. Καθηγητής Πανεπιστημίου Πατρών ΕΙΔΙΚΟΣ ΓΡΑΜΜΑΤΕΑΣ Γεώργιος ΠΑΠΑΘΕΟΔΩΡΟΥ, Αν. Καθηγητής Πανεπιστημίου Πατρών ΤΑΜΙΑΣ Μαρία ΓΕΡΑΓΑ, Λέκτορας Πανεπιστημίου Πατρών ΜΕΛΗ Νικόλαος ΚΟΝΤΟΠΟΥΛΟΣ, Καθηγητής Πανεπιστημίου Πατρών Νικόλαος ΛΑΜΠΡΑΚΗΣ, Καθηγητής Πανεπιστημίου Πατρών Νικόλαος ΣΑΜΠΑΤΑΚΑΚΗΣ, Αν. Καθηγητής Πανεπιστημίου Πατρών Ευθύμιος ΣΩΚΟΣ, Επ. Καθηγητής Πανεπιστημίου Πατρών Δημήτριος ΠΑΠΟΥΛΗΣ, Λέκτορας Πανεπιστημίου Πατρών Μιχαήλ ΣΤΑΜΑΤΑΚΗΣ, Καθηγητής Εθνικού και Καποδιστριακού Πανεπιστημίου Αθηνών Απόστολος ΑΛΕΞΟΠΟΥΛΟΣ, Καθηγητής Εθνικού και Καποδιστριακού Πανεπι- στημίου Αθηνών, Πρόεδρος Ε.Γ.Ε. Κωνσταντίνος ΠΑΠΑΒΑΣΙΛΕΙΟΥ, Αν. Καθηγητής Εθνικού και Καποδιστριακού Πανεπιστημίου Αθηνών, Γενικός Δ/ντής Ι.Γ.Μ.Ε. Κωνσταντίνος ΜΑΚΡΟΠΟΥΛΟΣ, Καθηγητής Εθνικού και Καποδιστριακού Πανεπιστημίου Αθηνών, Δ/ντής Γεωδυναμικού Ινστιτούτου Ε.Α.Α. Εμμανουήλ ΜΑΝΟΥΤΣΟΓΛΟΥ, Αν. Καθηγητής Πολυτεχνείου Κρήτης Σπυρίδων ΠΑΥΛΙΔΗΣ, Καθηγητής Αριστοτελείου Πανεπιστημίου Θεσσαλονίκης Κωνσταντίνος ΠΑΠΑΚΩΝΣΤΑΝΤΙΝΟΥ, Πρόεδρος ΕΛ.ΚΕ.Θ.Ε. Γραμματεία Συνεδρίου Συνέδρα Ηρ. Πολυτεχνείου 92, 26442 Πάτρα • Τηλ.: 2610 432.200 • Fax: 2610 430.884 URL: www.synedra.gr • E-mail: [email protected] viii ORGANIZING COMMITTEE OF THE 12th INTERNATIONAL CONGRESS = PRESIDENT George KOUKIS, Professor, University of Patras VICE-PRESIDENT Abraham ZELILIDIS, Professor, University of Patras GENERAL SECRETARY Ioannis KOUKOUVELAS, Assoc. Professor, University of Patras EXECUTIVE SECRETARY George PAPATHEODOROU, Assoc. Professor, University of Patras TREASURER Maria GERAGA, Lecturer, University of Patras MEMBERS Nikolaos KONTOPOULOS, Professor, University of Patras Nikolaos LAMBRAKIS, Professor, University of Patras Nikolaos SABATAKAKIS, Assoc. Professor, University of Patras Eythimios SOKOS, Assist. Professor, University of Patras Dimitrios PAPOULIS, Lecturer, University of Patras Michael STAMATAKIS, Professor, National and Kapodistrian University of Athens Apostolos ALEXOPOULOS, Professor, National and Kapodistrian University of Athens. President of G.S.G. Constantinos PAPAVASSILEIOU, Assoc. Professor, National and Kapodistrian University of Athens, Gen. Director of I.G.M.E. Konstantinos MAKROPOULOS, Professor, National and Kapodistrian University of Athens, Director of Institute of Geodynamics, N.O.A. Emmanouil MANOUTSOGLOU, Assoc. Professor, Technical University of Crete Spyridon PAVLIDES, Professor, Aristotle University of Thessaloniki Konstantinos PAPACONSTANTINOU, President of H.C.M.R. Congress Secretariat Synedra Iroon Polytechneiou 92, GR 26442 Patras • Ph.: +302610 432.200 • Fax: +302610 430.884 URL: www.synedra.gr • E-mail: [email protected] ix ΧΟΡΗΓΟΙ ΤΟΥ 12ου ΔΙΕΘΝΟΥΣ ΣΥΝΕΔΡΙΟΥ ΤΗΣ ΕΛΛΗΝΙΚΗΣ ΓΕΩΛΟΓΙΚΗΣ ΕΤΑΙΡΕΙΑΣ = Υπό την Αιγίδα του ΥΠΟΥΡΓΕΙΟΥ ΠΕΡΙΒΑΛΛΟΝΤΟΣ, ΕΝΕΡΓΕΙΑΣ & ΚΛΙΜΑΤΙΚΗΣ ΑΛΛΑΓΗΣ και τη Συμβολή των ΤΜΗΜΑ ΓΕΩΛΟΓΙΑΣ ΠΑΝΕΠΙΣΤΗΜΙΟΥ ΠΑΤΡΩΝ ΙΝΣΤΙΤΟΥΤΟ ΓΕΩΛΟΓΙΚΩΝ ΚΑΙ ΜΕΤΑΛΛΕΥΤΙΚΩΝ ΕΡΕΥΝΩΝ ΓΕΩΤΕΧΝΙΚΟ ΕΠΙΜΕΛΗΤΗΡΙΟ ΕΛΛΑΔΑΣ ΚΟΙΝΩΦΕΛΕΣ ΙΔΡΥΜΑ ΑΚΤΩΡ Α.Τ.Ε. ΙΩΑΝΝΗ Σ. ΛΑΤΣΗ ΕΜΒΕΛΕΙΑ Α.Ε. ΠΑΝΕΠΙΣΤΗΜΙΟ ΠΑΤΡΩΝ ΕΛΛΗΝΙΚΑ ΛΑΤΟΜΕΙΑ Α.Ε. ΟΡΓΑΝΙΣΜΟΣ ΑΝΤΙΣΕΙΣΜΙΚΟΥ ΟΜΙΛΟΣ ΤΕΧΝΙΚΩΝ ΜΕΛΕΤΩΝ ΣΧΕΔΙΑΣΜΟΥ ΚΑΙ ΠΡΟΣΤΑΣΙΑΣ (ΟΤΜ) Α.Τ.Ε. ΓΕΦΥΡΑ Α.Ε. ΓΕΝΙΚΗ ΜΕΛΕΤΩΝ Ε.Π.Ε. «ΙΣΤΡΙΑ» ΣΥΝΔΕΣΜΟΣ ΜΕΤΑΛΛΕΥΤΙΚΩΝ ΕΠΙΧΕΙΡΗΣΕΩΝ ΔΕΛΦΟΙ-ΔΙΣΤΟΜΟΝ Α.Μ.Ε. ΓΕΩΜΗΧΑΝΙΚΗ Α.Τ.Ε. Α.Ε. ΤΣΙΜΕΝΤΩΝ ΤΙΤΑΝ ΕΔΑΦΟΣ ΣΥΜΒΟΥΛΟΙ ΜΗΧΑΝΙΚΟΙ Α.Ε. ΓΕΩΣΚΟΠΙΟ Α.Τ.Ε. Η Οργανωτική Επιτροπή του 12ου Διεθνούς Συνεδρίου της Ελληνικής Γεωλογικής Εταιρίας ευχαριστεί θερμά τα ανωτέρω Ιδρύματα, Ινστιτούτα Ερευνών, Οργανισμούς, Τεχνικές και Με- λετητικές Εταιρίες για την οικονομική υποστήριξη και συμβολή τους στην οργάνωση και υλο- ποίηση του Συνεδρίου. x SPONSORS OF THE 12th INTERNATIONAL CONGRESS OF THE GEOLOGICAL SOCIETY OF GREECE = Under the Aegis of the MINISTRY OF ENVIRONMENT, ENERGY AND CLIMATE CHANGE and the Contribution of the DEPARTMENT OF GEOLOGY, UNIVERSITY OF PATRAS INSTITUTE OF GEOLOGY AND MINERAL EXPLORATION GEOTECHNICAL CHAMBER OF GREECE JOHN S. LATSIS, PUBLIC BENEFIT AKTOR S.A. FOUNDATION EMBELIA S.A. UNIVERSITY OF PATRAS HELLENIC QUARRIES S.A.. EARTHQUAKE PLANNING AND CONSULTING ENGINEERING PROTECTION ORGANIZATION COMPANY (OTM) S.A. GEFYRA S.A. GENERAL CONSULTING LTD “ISTRIA” GREEK MINING ENTERPRISES ASSOCIATION DELFI-DISTOMON BAUXITE S.A. GEOMECHANIKI S.A. TITAN CEMENT COMPANY S.A. EDAFOS ENGINEERING CONSULTANTS S.A. GEOSCOPIO S.A. The Organizing Committee of the 12th International Congress of the Geological Society of Greece expresses its grateful thanks to the above Foundations, Institutes, Organizations, Construction and Consulting Companies for their substantial support. xi ΕΠΙΣΤΗΜΟΝΙΚΗ ΕΠΙΤΡΟΠΗ – SCIENTIFIC COMMITTEE = Η Οργανωτική Επιτροπή ευχαριστεί θερμά τους κριτές για τη συμβολή τους στην κρίση όλων των εργασιών. Κάθε εργασία κρίθηκε από δύο κριτές για την από- κτηση Πρακτικών υψηλού επιστημονικού επιπέδου. Η Οργανωτική Επιτροπή δεν έχει ευθύνη για το περιεχόμενο και τις απόψεις που εκφράζονται στις εργασίες από τους συγγραφείς. The Organizing Committee expresses sincere thanks to the reviewers for their contribu- tion in evaluating and approving of the submitted papers. Each paper has passed through two reviewers, producing Proceedings of high scientific level. The Organizing Commit- tee is not responsible for the content and the views expressed by the authors in the papers. Alexopoulos A., Alexopoulos I., Alexouli A., Anagnostou C., Antonarakou A., Argyraki A., Avramidis P., Bersezio R., Bogdanov K., Caputo R., Christanis K., Christaras B., Christidis G., Depountis N., Drakatos G., Dresnier Th. Drinia H., Economou G., Fassoulas C., Fer- entinos G., Fermeli G., Filippidis A., Fountoulis I. Frey M.L., Gaki – Papanastassiou K., Ganas A., Georgakopoulos A., Geraga M., Godelitsas A., Hatzipanagiotou K., Iliopoulos I., Ioakim C., Kalavrouziotis I., Kaleris V., Kallergis G., Kamberis E., Karakaisis G.F., Karakitsios V., Karastathis V., Karipi S., Katagas C., Kati M., Katsonopoulou D., Kilias A., Kiratzi A., Kitsou D., Kokkalas S., Kollaman H., Kondopoulou D., Konispoliatis N., Kon- stantinou C., Kontopoulos N., Koroneos A., Koukis G., Koukouvelas I., Lambrakis N., Laskou M., Lekkas E., Loupasakis C., Lykousis V., Magganas A., Manoutsoglou E., Mari- nos P.V., Markopoulos Th., Migiros G., Mladenova Th., Mountrakis D., Mposkos E., My- lonakis G., Nakov R., Nikolaou N., Oprsal I., Papadimitriou E., Papadimitriou P., Papadopoulos
Recommended publications
  • Bulletin of the Geological Society of Greece
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by National Documentation Centre - EKT journals Bulletin of the Geological Society of Greece Vol. 43, 2010 GEOMORPHIC EVOLUTION OF WESTERN (PALIKI) KEPHALONIA ISLAND (GREECE) DURING THE QUATERNARY Gaki - Papanastassiou K. University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and Climatology Karymbalis E. Harokopio University, Department of Geography Maroukian H. University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and Tsanakas K. University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and http://dx.doi.org/10.12681/bgsg.11193 Copyright © 2017 K. Gaki - Papanastassiou, E. Karymbalis, H. Maroukian, K. Tsanakas To cite this article: Gaki - Papanastassiou, K., Karymbalis, E., Maroukian, H., & Tsanakas, K. (2010). GEOMORPHIC EVOLUTION OF WESTERN (PALIKI) KEPHALONIA ISLAND (GREECE) DURING THE QUATERNARY. Bulletin of the Geological Society of Greece, 43(1), 418-427. doi:http://dx.doi.org/10.12681/bgsg.11193 http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 10/01/2020 22:39:34 | Δελτίο της Ελληνικής Γεωλογικής Εταιρίας, 2010 Bulletin of the Geological Society of Greece, 2010 Πρακτικά 12ου Διεθνούς Συνεδρίου Proceedings of the 12th International Congress Πάτρα, Μάιος 2010 Patras, May, 2010 GEOMORPHIC EVOLUTION OF WESTERN (PALIKI) KEPHALONIA ISLAND (GREECE) DURING THE QUATERNARY Gaki - Papanastassiou K.1, Karymbalis E.2, Maroukian H.1 and Tsanakas K.1 1 University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and Climatologyy, 15771 Athens, Greece Emails: [email protected], [email protected], [email protected] 2 Harokopio University, Department of Geography, 70 El.
    [Show full text]
  • Mineralogical and Chemical Properties of FGD Gypsum from Florina, Greece
    Journal of Chemical Technology and Biotechnology J Chem Technol Biotechnol 83:20–26 (2008) Mineralogical and chemical properties of FGD gypsum from Florina, Greece Nikolaos Koukouzas1∗ and Charalampos Vasilatos2 1Centre for Research and Technology Hellas/Institute for Solid Fuels Technology and Applications, Attica Technology Park, P.O. Box 60228, 153 10 Ag. Paraskevi, Athens, Greece 2University of Athens, Department of Geology & Geoenvironment, Section of Economic Geology & Geochemistry, 15724, Panepistimiopolis, Athens, Greece Abstract BACKGROUND: The aim of this work is to define the chemical and mineralogical composition of the fuel gas desulphurization (FGD) gypsum produced from the Meliti thermal power plant in the region of Florina in North West Greece, in order to investigate potential uses in the cement industry. Mineralogical and microprobe analyses were carried out on FGD gypsum samples collected from the Meliti 330 MW lignite-fired power plant. RESULTS: Results show that the main component of the FGD gypsum is pure mineral gypsum (CaSO4·2H2O). The particle size of the gypsum ranges from 5 to 50 µm and the crystals are mainly of rhomboid shape. Microprobe analysis shows that the concentration of CaO and SO3, which are the main components, range from 31.9%–32.5% and from 45.90–46.40%, respectively. CONCLUSION: This FGD gypsum can easily substitute the natural gypsum used in the production of cement. 2007 Society of Chemical Industry Keywords: petrography; SEM; FGD gypsum; X-ray diffraction INTRODUCTION fly ash, for mine reclamation, to fill in openings that In 2001 the European Commission introduced the are left following the completion of mining activities.
    [Show full text]
  • Bulletin of the Geological Society of Greece
    Bulletin of the Geological Society of Greece Vol. 43, 2010 GEOTECHNICAL INVESTIGATION OF THE ROCK SLOPE STABILITY PROBLEMS OCCURRED AT THE FOUNDATIONS OF THE COASTAL BYZANTINE WALL OF KAVALA CITY, GREECE Loupasakis C. Institute of Geology and Mineral Exploration, Engineering Geology Department Spanou N. Institute of Geology and Mineral Exploration, Engineering Geology Department Kanaris D. Institute of Geology and Mineral Exploration, Engineering Geology Department Exioglou D. Institute of Geology and Mineral Exploration, East Macedonia-Thrace Regional Branch Georgakopoulos A. Aristotle University of Thessaloniki, School of Geology, Department of Min eralogyPetrology-Economic Geology, Laboratory of Economic Geology https://doi.org/10.12681/bgsg.11299 Copyright © 2017 C. Loupasakis, N. Spanou, D. Kanaris, D. Exioglou, A. Georgakopoulos To cite this article: Loupasakis, C., Spanou, N., Kanaris, D., Exioglou, D., & Georgakopoulos, A. (2010). GEOTECHNICAL INVESTIGATION OF THE ROCK SLOPE STABILITY PROBLEMS OCCURRED AT THE FOUNDATIONS OF THE COASTAL BYZANTINE WALL OF KAVALA CITY, GREECE. Bulletin of the Geological Society of Greece, 43(3), 1230-1237. doi:https://doi.org/10.12681/bgsg.11299 http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 18/02/2021 15:49:19 | http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 18/02/2021 15:49:19 | Δελτίο της Ελληνικής Γεωλογικής Εταιρίας, 2010 Bulletin of the Geological Society of Greece, 2010 Πρακτικά 12ου Διεθνούς Συνεδρίου Proceedings of the 12th International Congress Πάτρα, Μάιος 2010 Patras, May, 2010 GEOTECHNICAL INVESTIGATION OF THE ROCK SLOPE STABILITY PROBLEMS OCCURRED AT THE FOUNDATIONS OF THE COASTAL BYZANTINE WALL OF KAVALA CITY, GREECE Loupasakis C.1, Spanou N.2, Kanaris D.3, Exioglou D.
    [Show full text]
  • Êåíôñï Ðåñéâáëëïíôéêçó Åêðáéäåõóçó Åëáóóïíáó
    ÊÅÍÔÑÏÊÅÍÔÑÏ ÐÅÑÉÂÁËËÏÍÔÉÊÇÓÐÅÑÉÂÁËËÏÍÔÉÊÇÓ ÅÊÐÁÉÄÅÕÓÇÓÅÊÐÁÉÄÅÕÓÇÓ ÅËÁÓÓÏÍÁÓÅËÁÓÓÏÍÁÓ ISBN: 978-960-99999-0-8 © Copyright 2011 ÊÝíôñï ÐåñéâáëëïíôéêÞò Åêðáßäåõóçò (Ê.Ð.Å.) Åëáóóüíáò Âëá÷ïäÞìïõ 1, 40200 Åëáóóüíá E-mail: [email protected] | [email protected] Éóôïóåëßäá: http://thess.pde.sch.gr/kpe Ôçë.: 24930 29571 FAX: 24930 29570 ÅÐÉÌÅËÅÉÁ ÅÊÄÏÓÇÓ ÁíáãíùóôÜêçò Óðõñßäùí Õðåýèõíïò ÊÐÅ ÃêáíÜôóéïò ÁíäñÝáò ÁíáðëçñùôÞò Õðåýèõíïò ÊÐÅ Óðáíüò Êùíóôáíôßíïò ÌÝëïò ÐáéäáãùãéêÞò ÏìÜäáò ÊÐÅ ÓÕÃÃÑÁÖÉÊÇ ÏÌÁÄÁ ÁíáãíùóôÜêçò Óðõñßäùí, Ãêáßôëé÷ Ìáñôßíïò, ÃêáíÜôóéïò ÁíäñÝáò ÆÜãêáò Èåüäùñïò , ÌçíÜò Èåüäùñïò, Ìðßóìðáò Êùíóôáíôßíïò ÑÜðôçò ÄçìÞôñéïò, ÑÜðôïõ Åõáããåëßá, ÓáìáñÜ ÖáíÞ Óá÷éíßäçò Êùíóôáíôßíïò, Óðáíüò Êùíóôáíôßíïò, ÓõíåöÜêçò Ãéþñãïò Öùôïãñáößåò © Copyright 2011 ÊÐÅ Åëáóóüíáò Áðáãïñåýåôáé ç áðïèÞêåõóç Þ áíáðáñáãùãÞ Þ áíáôýðùóçò ìÝñïõò Þ ôïõ óõíüëïõ ôùí öùôïãñáöéþí êáé ôùí êåéìÝíùí óå ïðïéáäÞðïôå ìïñöÞ êáé ìå ïðïéïäÞðïôå ìÝóï, ÷ùñßò Ýããñáöç Üäåéá ôïõ ÊÝíôñïõ ÐåñéâáëëïíôéêÞò Åêðáßäåõóçò Åëáóóüíáò. Ôï ðáñüí âéâëßï äå äéáôßèåôáé ðñïò ðþëçóç. Ôï ðáñüí åêðïíÞèçêå óôï ðëáßóéï ôçò ÐñÜîçò «ÊÝíôñá Åêðáßäåõóçò ãéá ôï ÐåñéâÜëëïí êáé ôçí Áåéöïñßá - ÄñÜóåéò ãéá ôïõò ìáèçôÝò» ôïõ Åðé÷åéñçóéáêïý ÐñïãñÜììáôïò «Åêðáßäåõóç êáé Äéá Âßïõ ÌÜèçóç», ìå ôç óõã÷ñçìáôïäüôçóç ôçò ÅõñùðáúêÞò ¸íùóçò (Åõñùðáúêü Êïéíùíéêü Ôáìåßï) êáé Åèíéêþí Ðüñùí». ÊÅÍÔÑÏ ÐÅÑÉÂÁËËÏÍÔÉÊÇÓ ÅÊÐÁÉÄÅÕÓÇÓ ÅËÁÓÓÏÍÁÓ ÐÑÁÊÔÉÊÁ ÓÅÌÉÍÁÑÉÙÍ ÖÅÂÑÏÕÁÑÉÏÓ 2011 - ÌÁÚÏÓ 2011 ÅËÁÓÓÏÍÁ ÉÏÕËÉÏÓ 2011 Ðåñéå÷üìåíá ×áéñåôéóìüò ÄçìÜñ÷ïõ Åëáóóüíáò........................................................................................9
    [Show full text]
  • Onshore Drilling Outcomes in Kefalonia Issued 16 September 2015
    Onshore Drilling Outcomes in Kefalonia Issued 16 September 2015 Summary The results of the geoscientific campaign unveiled a complex geo-tectonic and geological landscape beneath the Thinia valley, the isthmus separating the western peninsula of Paliki from the rest of Kefalonia. It has superseded the simple side-wall collapse and in-fill hypothesis and has raised another possibility, that of a massive rotational slump, leading to a toe-thrust and the elevation of an ancient marine channel. The critical question then becomes one of timing: could this rotational slump have occurred recently (in the last ~3,200 years) and therefore be responsible for in-filling and displacement of a Mycenaean age marine channel? Other promising findings include the discovery of ancient beach deposits buried under land-slip infill at the northern end of the Thinia valley and evidence of an ancient marine harbour that reached the foot of Kastelli Hill and that contained radiocarbon-datable samples attributable to the Bronze Age. An anomalous late-period lakebed, now dried out, is another intriguing finding. It is also worth reiterating that Mycenaean-era sites have been previously identified on both the western peninsula (called Paliki) and the remaining part of the island of Kefalonia, confirming that this land is of considerable historical and archaeological interest dating to the period in question. The geological research sponsored by Fugro and directed by Professor John Underhill has been completed safely, successfully and with no harm to the environment. Thinia valley panorama looking east from Paliki Project Background The objective of this phase of geoscientific research has been to test the proposition that the island of Ithaca may have been accurately described in Homer’s Odyssey as the furthest west of a group of four islands off the western coast of Greece, facing dusk, the open sea and being of low elevation.
    [Show full text]
  • Applicant UNESCO Global Geopark
    Applicant UNESCO Global Geopark Kefalonia-Ithaca, Greece Geographical and geological summary 1. Physical and human geography The Kefalonia – Ithaca applicant UNESCO Global Geopark is located in Western Greece (SE Europe). It is an island complex (Kefalonia-Ithaca-Atokos-Arkoudi) belonging to the Heptanese (Ionian Sea). It is located 340,3 km from Athens, the capital of Greece and 165.37 and 258 km from Albania and Italy respectively. Its surface area reaches 3.006 km2 and includes 913,075 km2 of land and 2.092,9 km2 of marine area. The geopark ‘s area belongs administratively to the Ionian Islands Perfecture. Kefalonia (38°12′44′′ N 20°32′00′′ E) occupies an area of 773 km2. Its capital city is Argostoli. According to the last census, 35.801 inhabitants were recorded living mainly in coastal settlements. Ithaca (38°23′59.28′′ N 20°41′21.11′′E) follows in size with 117 km2 surface area. Vathi is the capital city. In winter 3.084 residents are living on the island but in the summer the population is more than double. The local residents in the geopark ‘s area are mostly occupied with agriculture, fishery and tourism. Especially tourism plays an important role in the economic development of the area. Atokos (4,4 km2) and Arkoudi (4,275 km2) are small desolated islands north of Ithaca. Kefalonia includes four main peninsulas (Paliki, Erisos, Livatho and Atro). The mean altitude of the island is 358,5m. Approximately 37.5% is occupied by mountains, 42,5% is semi-mountainous and 20% is occupied by lowland areas.
    [Show full text]
  • Accelerated Lignite Exit in Bulgaria, Romania and Greece
    Accelerated lignite exit in Bulgaria, Romania and Greece May 2020 Report: Accelerated lignite exit in Bulgaria, Romania and Greece Authors: REKK: Dr. László Szabó, Dr. András Mezősi, Enikő Kácsor (chapters 1, 2, 3, 4 and 5) TU Wien: Dr. Gustav Resch, Lukas Liebmann (chapters 2, 3, 4 and 5) CSD: Martin Vladimirov, Dr. Todor Galev, Dr. Radostina Primova (chapter 3) EPG: Dr. Radu Dudău, Mihnea Cătuți, Andrei Covatariu, Dr. Mihai Bălan (chapter 5) FACETS: Dr. Dimitri Lalas, Nikos Gakis (chapter 4) External Experts: Csaba Vaszkó, Alexandru Mustață (chapters 2.4, 3.2, 4.2 and 5.2) 2 The Regional Centre for Energy Policy Research (REKK) is a Budapest based think tank. The aim of REKK is to provide professional analysis and advice on networked energy markets that are both commercially and environmentally sustainable. REKK has performed comprehensive research, consulting and teaching activities in the fields of electricity, gas and carbon-dioxide markets since 2004, with analyses ranging from the impact assessments of regulatory measures to the preparation of individual companies' investment decisions. The Energy Economics Group (EEG), part of the Institute of Energy Systems and Electrical Drives at the Technische Universität Wien (TU Wien), conducts research in the core areas of renewable energy, energy modelling, sustainable energy systems, and energy markets. EEG has managed and carried out many international as well as national research projects funded by the European Commission, national governments, public and private clients in several fields of research, especially focusing on renewable- and new energy systems. EEG is based in Vienna and was originally founded as research institute at TU Wien.
    [Show full text]
  • A New Hydrobiid Species (Caenogastropoda, Truncatelloidea) from Insular Greece
    Zoosyst. Evol. 97 (1) 2021, 111–119 | DOI 10.3897/zse.97.60254 A new hydrobiid species (Caenogastropoda, Truncatelloidea) from insular Greece Canella Radea1, Paraskevi Niki Lampri1,3, Konstantinos Bakolitsas2, Aristeidis Parmakelis1 1 Section of Ecology and Systematics, Department of Biology, National and Kapodistrian University of Athens, 15784 Panepistimiopolis, Greece 2 High School, Agrinion, 3rd Parodos Kolokotroni 11, 30133 Agrinion, Greece 3 Institute of Marine Biological Resources and Inland Waters, Hellenic Centre for Marine Research, 46.7 km of Athens – Sounio ave., 19013 Anavissos Attica, Greece http://zoobank.org/FE7CB458-9459-409C-B254-DA0A1BA65B86 Corresponding author: Canella Radea ([email protected]) Academic editor: T. von Rintelen ♦ Received 1 November 2020 ♦ Accepted 18 January 2021 ♦ Published 5 February 2021 Abstract Daphniola dione sp. nov., a valvatiform hydrobiid gastropod from Western Greece, is described based on conchological, anatomical and molecular data. D. dione is distinguished from the other species of the Greek endemic genus Daphniola by a unique combination of shell and soft body character states and by a 7–13% COI sequence divergence when compared to congeneric species. The only population of D. dione inhabits a cave spring on Lefkada Island, Ionian Sea. Key Words Freshwater diversity, Lefkada Island, taxonomy, valvatiform Hydrobiidae Introduction been described so far. More than 60% of these genera inhabit the freshwater systems of the Balkan Peninsula The Mediterranean Basin numbers among the first 25 (Radea 2018; Boeters et al. 2019; Delicado et al. 2019). Global Biodiversity Hotspots due to its biological and The Mediterranean Basin, the Balkan, the Iberian and ecological biodiversity and the plethora of threatened bi- the Italian Peninsulas seem to be evolutionary centers of ota (Myers et al.
    [Show full text]
  • The Physical and Mechanical Properties of Composite Cements Manufactured with Calcareous and Clayey Greek Diatomite Mixtures
    Cement & Concrete Composites 27 (2005) 205–209 www.elsevier.com/locate/cemconcomp The physical and mechanical properties of composite cements manufactured with calcareous and clayey Greek diatomite mixtures D. Fragoulis a,*, M.G. Stamatakis b, D. Papageorgiou a, E. Chaniotakis a a TITAN Cement Company S.A. Kamari Plant, P.O. Box 18, Elefsina 19 200, Attica, Greece b Department of Geology, National University of Athens, Panepistimiopolis, Ano Ilissia, 157 84 Athens, Greece Abstract The aim of the present study is to test diatomite rocks as alternative pozzolanic materials that could be used for the manu- facturing of pozzolanic cements in Greece. The diatomite rocks used occur in Samos Island and in the Elassona, Greece. The Samos diatomites were mainly consisted of calcite and opal-A, whereas the Elassona diatomite consisted of opal-A, clay minerals, feldspars and quartz. As a result, the Samos samples were rich in CaO and SiO2, while the Elassona ones were rich in SiO2,Al2O3 and Fe2O3. The specific surface of the laboratory-produced cements was high, with the grindability of the Elassona diatomites being lower than that of Samos. The water demand of all blended cements was higher than that of the laboratory produced OPC. The late com- pressive strength of most diatomite cements studied was improved with respect to the lab OPC. Ó 2004 Elsevier Ltd. All rights reserved. Keywords: Diatomite; Diatom frustules; Pozzolana; Cement; Amorphous silica 1. Introduction Central Greece for the production of laboratory cements (LPC). These cements were evaluated by determination Amorphous silica is found in nature in the form of of their specific surface (Blaine), water demand, initial siliceous microfossils such as diatoms, radiolarians, sili- and final setting time and compressive strength.
    [Show full text]
  • Elephas Antiquus in Greece: New finds and a Reappraisal of Older Material (Mammalia, Proboscidea, Elephantidae)
    Quaternary International xxx (2010) 1e11 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Elephas antiquus in Greece: New finds and a reappraisal of older material (Mammalia, Proboscidea, Elephantidae) Evangelia Tsoukala a,*, Dick Mol b, Spyridoula Pappa a, Evangelos Vlachos a, Wilrie van Logchem c, Markos Vaxevanopoulos d, Jelle Reumer e a Aristotle University, School of Geology, University campus, 54 124 Thessaloniki, Macedonia, Greece b Natural History Museum Rotterdam and Mammuthus Club International, Gudumholm 41, 2133 HG Hoofddorp, The Netherlands c Mammuthus Club International, Bosuilstraat 12, 4105 WE Culemborg, The Netherlands d Ministry of Culture, Ephorate of Palaeoanthropology-Speleology of Northern Greece, Navarinou 28, 55131, Thessaloniki, Greece e Faculty of Geosciences, Utrecht University and Natural History Museum Rotterdam, PO Box 23452, 3001 KL Rotterdam, The Netherlands article info abstract Article history: This paper briefly describes some recently discovered remains of the straight-tusked elephant, Elephas Available online xxx antiquus, from Greece. Material of this extinct proboscidean was found in four localities in Northern Greece: Kaloneri and Sotiras in Western Macedonia, Xerias in Eastern Macedonia, and Larissa in Thessaly. In addition, published elephant remains from Ambelia, Petres and Perdikas, also from Northern Greece, are reinterpreted and also attributed to E. antiquus. Of all these, the Kaloneri elephant shows an inter- esting paleopathology: it was disabled by a broken right tusk. Ó 2010 Elsevier Ltd and INQUA. All rights reserved. 1. Introduction of E. namadicus comes from India. Maglio (1973) considered the Asiatic form E. namadicus to be a senior synonym of the European Fossil Proboscidea are known from Neogene and Quaternary form E.
    [Show full text]
  • Mineralogy and Geochemistry of Greek and Chinese Coal Fly
    Fuel 85 (2006) 2301–2309 www.fuelfirst.com Mineralogy and geochemistry of Greek and Chinese coal fly ash Nikolaos K. Koukouzas a,*, Rongshu Zeng b, Vassilis Perdikatsis c, Wendong Xu b, Emmanuel K. Kakaras a a Centre for Research and Technology Hellas, Institute for Solid Fuels Technology and Applications, Attica Technology Park, GR-15310, Agia Paraskevi, Athens, Greece b Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China c Technical University of Crete, Department of Mineral Resources Engineering, 73100 Chania, Crete, Greece Received 5 May 2005; received in revised form 6 February 2006; accepted 6 February 2006 Available online 15 June 2006 Abstract In this paper the mineralogy and geochemistry of Greek and Chinese coal fly ash are examined. Annual production of fly ash in China is around 160 Mt while in Greece lignite fly ash accounts around 10 Mt. Even though the mineralogical and chemical composition of the fly ashes coming from these two countries differs, there are common questions on the utilization of this material. The variation of the Greek fly ash’ chemical composition, from Ca-poor to Ca-rich fly ash, has resulted to applications such as dam construction, use in cement and possibly in concrete and road construction. The Chinese fly ash, which is rich in mullite, is broadly applied for brick making. Ó 2006 Elsevier Ltd. All rights reserved. Keywords: Fly ash; Mineralogy; Geochemistry 1. Introduction mary energy after the United States. According to the data published by State Bureau of Statistics, China’s GDP was Lignite plays an important role in Greece’s energy sector 15987.8 billion RMB (about 1998.4 billion USD) in 2004.
    [Show full text]
  • Wednesday 24 September 2014
    THE GEODYNAMIC AND SEISMOTECTONIC SETTING OF CEPHALONIA (IONIAN SEA, WESTERN GREECE) AS FACTOR CONTROLLING THE DISTRIBUTION OF EARTHQUAKE ENVIRONMENTAL EFFECTS AND STRUCTURAL DAMAGE INDUCED BY THE EARLY 2014 EARTHQUAKES (JANUARY 26th and FEBRUARY 3rd, Mw 6.0) by LEKKAS, E., MAVROULIS, S., ALEXOUDI, V. National and Kapodistrian University of Athens, School of Sciences, Faculty of Geology and Geoenvironment, Department of Dynamic Tectonic Applied Geology Cephalonia is the largest of the Ionian Islands in Western Greece and is located on the tectonic front of the Hellenic thrust and fold belt developed only a few km east of the Hellenic Trench representing an active plate boundary where the Eastern Mediterranean lithosphere is being subducted beneath the Aegean one. The subduction zone terminates against the Cephalonia Transform Fault Zone connecting the subduction boundary to the continental collision between the Apulian microplate and the Hellenic foreland and playing a significant role in the region's geodynamic complexity. Historical seismic data indicate that Cephalonia has been repeatedly struck by moderate and strong, shallow earthquakes producing large seismic intensities and causing a large number of human casualties and great economic losses. One more episode in the geodynamic evolution of the island is the early 2014 earthquake sequence comprising two main shocks with the same magnitude (Mw 6.0) occurring successively in short time (January 26th and February 3rd) and space (neotectonic macrostructure of Paliki peninsula in the western part of Cephalonia). According to geological data collected in the field during our reconnaissance immediately after both earthquakes, it is concluded that each earthquake was induced by the rupture of a different pre-existing active fault zone located in Paliki peninsula.
    [Show full text]