Geochemistry of Gas Manifestations in Greece

Total Page:16

File Type:pdf, Size:1020Kb

Geochemistry of Gas Manifestations in Greece Università degli Studi di Palermo (Palermo, Italy) Dipartimento di Scienze della Terra e del Mare (DISTEM) National and Kapodistrian University of Athens (Athens, Greece) Department of Geology and Geoenvironment Istituto Nazionale di Geofisica e Vulcanologia (sez. Palermo, Italy) Co-supervision PhD in Geochemistry DOTTORATO DI RICERCA IN SCIENZE DELLA TERRA – GEOCHIMICA XXX° CICLO (GEO/08) DOCTORATE OF PHILOSOPHY IN APPLIED AND ENVIRONMENTAL GEOLOGY Geochemistry of Gas Manifestations in Greece PhD thesis by: Kyriaki Daskalopoulou IL COORDINATORE Aiuppa Alessandro SUPERVISORS Parello Francesco Kyriakopoulos Konstantinos CO-SUPERVISORS D’Alessandro Walter CICLO XXX January 2015 – December 2017 Università degli Studi di Palermo (Palermo, Italy) Dipartimento di Scienze della Terra e del Mare (DISTEM) National and Kapodistrian University of Athens (Athens, Greece) Department of Geology and Geoenvironment Istituto Nazionale di Geofisica e Vulcanologia (sez. Palermo, Italy) Co-supervision PhD in Geochemistry DOTTORATO DI RICERCA IN SCIENZE DELLA TERRA – GEOCHIMICA XXX° CICLO (GEO/08) DOCTORATE OF PHILOSOPHY IN APPLIED AND ENVIRONMENTAL GEOLOGY Geochemistry of Gas Manifestations in Greece PhD thesis by: Kyriaki Daskalopoulou IL COORDINATORE Aiuppa Alessandro SUPERVISORS Parello Francesco Kyriakopoulos Konstantinos CO-SUPERVISORS D’Alessandro Walter CICLO XXX January 2015 – December 2017 Στους γονείς μου Κώστα και Έφη, που με δίδαξαν να μάχομαι και να μην τα παρατάω… Στον Νίκο, τον «μικρό πρίγκηπα» που με έμαθε να ονειρεύομαι και να πετάω…. Acknowledgments During the three years of my thesis, many people contributed to this achievement, each one with his way. There is no doubt that my supervisors, Prof. Francesco Parello and Prof. Konstantinos Kyriakopoulos, stood by me all along this research. Always available for any discussion, scientific or not, each of their advice was always illuminating. It is impossible to count the hours we worked together. For these reasons I would like to greatly thank them. Nevertheless, I was lucky enough to have Dr. Walter D’Alessandro as a co-supervisor. Our collaboration counts more than four years, since the time when I was a master student in the Department of Geology and Geoenvironment at the National and Kapodistrian University of Athens. For all these years Dr. Walter D’Alessandro has been a mentor and a friend and I am really grateful to him for his continuous presence and support. Since the beginning of my PhD course, I had the pleasure to collaborate with Dr. Sergio Calabrese, a brilliant researcher of Università degli Studi di Palermo, who provided me with the opportunity to join a multidisciplinary team, and made me “discover” and “travel” in the magic world of Geochemistry and Volcanology. Also, I would like to thank Prof. Franco Tassi for the fruitful discussions regarding the evolution of this project and his helpful advices during these years. My collegue, Manfredi Longo, who helped me with the expansion of the database. Furthermore, I kindly acknowledge Francesco Capecchiacci (GC laboratory, UniFi), Mauro Martelli and Francesco Salerno (GC laboratory INGV-Pa), Ygor Oliveri and Aldo Sollami (MS laboratory INGV-Pa), Andrea Rizzo and Mariano Tantillo (Noble Gas laboratory INGV-Pa) for their kind and valuable support in the analyses. Among them, I am indebted with Dr. Markos Xenakis and Dr. Konstantinos Athanasoulis of the IGME for their precious information about the location of many interesting sites all around the Hellenic territory. I am also grateful for the insightful comments of Andri Stefansson and an anonymous referee and of the editor Hailiang Dong that helped me significantly improve the part of hydrocarbons. I am also indebted to David Hilton, who managed as editor the first round of review of the same manuscript. I was deeply touched by the notice of his death. Also, I kindly acknowledge Prof. Orlando Vaselli and Prof. Carlo Cardellini for their suggestions in the final revision of my thesis. Nevertheless, none of these would have happened without the moral and psychological support of my parents Kostas and Efi Daskalopoulos, who were always there to help me stand on my feet and go forward. Although he is not longer with us, I would like to thank my brother Nikos iv Daskalopoulos, who taught me how to fly and I am sure that he would have been very proud for his little sister. Also, I am grateful to my friends Despoina Zoura, Silvia Milazzo, Luciana Randazzo and Stefano Dell’Aria who showed great patience and gave priceless moral and psychological support during these three years despite my paranoias and stress. Last but not least, the Ministero dell'Istruzione, dell'Università e della Ricerca (MIUR) of Italy is greatly acknowledged for providing me the economic support through the 3-year scholarship, which was essential for accomplishing this task, and of course the Università degli Studi di Palermo and the Istituto Nazionale di Geofisica e Vulcanologia- Palermo are especially thanked for giving me the opportunity to carry out this thesis. v INDEX Acknowledgments ................................................................................................................................... iv ABSTRACT ............................................................................................................................................ 1 RIASSUNTO .......................................................................................................................................... 3 ΠΕΡΙΛΗΨΗ ............................................................................................................................................ 5 Introduction ............................................................................................................................................. 7 1. Study Area ..................................................................................................................................... 10 1.1. Geodynamic and Geotectonic setting ...................................................................................... 10 1.2. Geological regime .................................................................................................................. 12 1.3. Geothermal fields ................................................................................................................... 14 1.4. Heat flow and Crustal Thickness using the new Moho model, an overview ............................. 18 2. Materials and Methods ................................................................................................................... 19 2.1. Sampling methods .................................................................................................................. 19 2.1.1. Free gases………………………………………………………………………………….19 2.1.2. Dissolved gasses…………………………………………………………………………..20 2.2. Analytic methods in the laboratory ......................................................................................... 21 3. Results ........................................................................................................................................... 24 3.1. Chemical composition of the gases ......................................................................................... 24 3.2. Isotope composition of the gases ............................................................................................ 28 4. Discussion ..................................................................................................................................... 30 4.1. Gas Components .................................................................................................................... 30 4.2. Origin and sources of He and CO2 in the gas manifestations of Greece ................................... 32 4.3. Helium isotope values and CO2 concentrations related to Geodynamics and Volcanism .......... 49 4.4. Light Hydrocarbons ............................................................................................................... 56 4.4.1. An overview in the classification of hydrocarbons………………………………………..56 4.4.2. Origin of hydrocarbon compounds in Greece……………………………………………..59 4.4.3. Secondary post-genetic processes………………………………………………………...64 4.5. Environmental Hazards .......................................................................................................... 67 Conclusions ........................................................................................................................................... 70 References............................................................................................................................................. 75 Appendix .............................................................................................................................................. 98 vi FIGURE INDEX Figure 1: Map of the major tectonic structures and the current horizontal stress field main axes. Fault lines derive from the CSSs upper edge of GreDaSS (2014). .............................................. 11 Figure 2: Structural zones of the Hellenides after Mountrakis (1986)......................................... 13 Figure 3: Map of geotectonic zones and thermal springs (Athanasoulis et al., 2009) .................. 15 Figure 4: a) Heat flow map of Greece by Fytikas and Kolios (1979). The heat flow values are presented in mWm-2; b) The new Moho depth model (km) from deep seismic imaging data as proposed by Grigoriadis et al., 2016. ........................................................................................
Recommended publications
  • Du 18E CONGRÈS De L’ASSOCIATION INTERNATIONALE Pour L’HISTOIRE Du VERRE C Y M B C Y M B
    ANNALES Thessaloniki 2009 du 18e CONGRÈS de l’ASSOCIATION INTERNATIONALE pour l’HISTOIRE du VERRE C Y M B C Y M B C Y M B ANNALES du 18e CONGRÈS de l’ASSOCIATION INTERNATIONALE pour l’HISTOIRE du VERRE Editors Despina Ignatiadou, Anastassios Antonaras Editing Committee Nadia Coutsinas Ian C. Freestone Sylvia Fünfschilling Caroline Jackson Janet Duncan Jones Marie-Dominique Nenna Lisa Pilosi Maria Plastira-Valkanou Jennifer Price Jane Shadel Spillman Marco Verità David Whitehouse B M Y C Thessaloniki 2009 C Y M B i C Y M B C Y M B C Y M B B M Y C Couverture / Cover illustration The haematinon bowl from Pydna. Height 5.5 cm. © 27th Ephorate of Prehistoric and Classical Antiquities, Greece. The bowl (skyphos) is discussed in the paper by Despina Ignatiadou ‘A haematinon bowl from Pydna’, p. 69. © 2012 Thessaloniki AIHV and authors ISBN: 978-90-72290-00-7 Editors: Despina Ignatiadou, Anastassios Antonaras AIHV Association Internationale pour l’Histoire du Verre International Association for the History of Glass http: www.aihv.org Secretariat: The Corning Museum of Glass One Museum Way B M Corning NY, 14830 USA Y C Printed by: ZITI Publishing, Thessaloniki, Greece http: www.ziti.gr C Y M B ii C Y M B C Y M B C Y M B C Y M B CONTENTS PRÉFACE – MARIE-DOMINIQUE NENNA . xiii PREFACE – MARIE-DOMINIQUE NENNA . xv GREEK LITERARY SOURCES STERN MARIANNE EVA Ancient Greek technical terms related to glass production . 1 2nd MILLENNIUM BC / BRONZE AGE GLASS NIGHTINGALE GEORG Glass and faience and Mycenaean society .
    [Show full text]
  • Contextualizing the Archaeometric Analysis of Roman Glass
    Contextualizing the Archaeometric Analysis of Roman Glass A thesis submitted to the Graduate School of the University of Cincinnati Department of Classics McMicken College of Arts and Sciences in partial fulfillment of the requirements of the degree of Master of Arts August 2015 by Christopher J. Hayward BA, BSc University of Auckland 2012 Committee: Dr. Barbara Burrell (Chair) Dr. Kathleen Lynch 1 Abstract This thesis is a review of recent archaeometric studies on glass of the Roman Empire, intended for an audience of classical archaeologists. It discusses the physical and chemical properties of glass, and the way these define both its use in ancient times and the analytical options available to us today. It also discusses Roman glass as a class of artifacts, the product of technological developments in glassmaking with their ultimate roots in the Bronze Age, and of the particular socioeconomic conditions created by Roman political dominance in the classical Mediterranean. The principal aim of this thesis is to contextualize archaeometric analyses of Roman glass in a way that will make plain, to an archaeologically trained audience that does not necessarily have a history of close involvement with archaeometric work, the importance of recent results for our understanding of the Roman world, and the potential of future studies to add to this. 2 3 Acknowledgements This thesis, like any, has been something of an ordeal. For my continued life and sanity throughout the writing process, I am eternally grateful to my family, and to friends both near and far. Particular thanks are owed to my supervisors, Barbara Burrell and Kathleen Lynch, for their unending patience, insightful comments, and keen-eyed proofreading; to my parents, Julie and Greg Hayward, for their absolute faith in my abilities; to my colleagues, Kyle Helms and Carol Hershenson, for their constant support and encouragement; and to my best friend, James Crooks, for his willingness to endure the brunt of my every breakdown, great or small.
    [Show full text]
  • Geochemical Status and Interactions Between Soil and Groundwater Systems in the Area of Akrefnio, Central Greece
    DOI: 10.2478/v10025-012-0012-1 JOURNAL OF WATER AND LAND DEVELOPMENT J. Water Land Dev. No. 15, 2011: 127–144 Geochemical status and interactions between soil and groundwater systems in the area of Akrefnio, Central Greece. Risk assessment, under the scope of mankind and natural environment Evangelos TZIRITIS, Akindinos KELEPERTSIS, Gina FAKINOU University of Athens, Section of Economic Geology and Geochemistry, Faculty of Geology, Panepis- timioupolis, Ano Ilisia, 15784, Greece; [email protected] Abstract: Totally 50 samples of groundwater and soil were collected from the area of Akrefnio (cen- tral Greece), in order to assess the geochemical status and the risk for humans and natural environ- ment. The analytical results and processing of the initial data revealed that the main factors control- ling hydrogeochemistry are the natural enrichment from calcareous substrate and the manmade pollu- tion through extensive use of N-fertilizers. Soil geochemistry was mainly influenced by the occur- rence of lateritic horizons, which gave raise to elevated concentrations of Ni and Cr in the majority of soil samples. Although most of the geochemical enrichment processes between soil and groundwater are common, the above geochemical systems don’t seem to interact, and act most of the times inde- pendently. Risk assessment of natural and mankind environment revealed that groundwater is suitable for drinking but not for irrigation, due to high salinity. Finally, soils are highly polluted by Ni and Cr, and thus are inappropriate for the existing agricultural land uses. Key words: Akrefnio, central Greece, geochemistry, groundwater, risk assessment, soil INTRODUCTION The study area is located in the vicinity of Akrefnio city, which lies about 100 km northern of Athens, central Greece.
    [Show full text]
  • Isolation and Preliminary Characterization of Cyanobacteria Strains from Freshwaters of Greece
    Open Life Sci. 2015; 10: 52–60 Research Article Open Access Spyros Gkelis*, Pablo Fernández Tussy, Nikos Zaoutsos Isolation and preliminary characterization of cyanobacteria strains from freshwaters of Greece Abstract: Cyanobacterial harmful algal blooms (or 1 Introduction CyanoHABs) represent one of the most conspicuous waterborne microbial hazards. The characterization of Cyanobacteria are photosynthetic, prokaryotic organisms the bloom communities remains problematic because which occur primarily in freshwater and saline the cyanobacterial taxonomy of certain genera has not environments, but also in terrestrial ecosystems. Their yet been resolved. In this study, 29 planktic and benthic presence in lakes with high nutrient levels can lead to a cyanobacterial strains were isolated from freshwaters mass increase in cyanobacterial cell numbers, with the located in Greece. The strains were assigned to the genera formation of blooms, which results in a depreciation of Chroococcus, Microcystis, Synechococcus, Jaaginema, water quality [1]. Cyanobacterial harmful algal blooms Limnothrix, Pseudanabaena, Anabaena, and Calothrix (or CyanoHABs) represent one of the most conspicuous and screened for the production of the cyanotoxins waterborne microbial hazards to human and agricultural microcystins (MCs), cylindrospermopsins (CYNs), and water supplies, fishery production, and freshwater and saxitoxins (STXs) using molecular (PCR amplification of marine ecosystems [2]. This hazard results from the seven genes implicated in cyanotoxin biosynthesis)
    [Show full text]
  • New VERYMACEDONIA Pdf Guide
    CENTRAL CENTRAL ΜΑCEDONIA the trip of your life ΜΑCEDONIA the trip of your life CAΝ YOU MISS CAΝ THIS? YOU MISS THIS? #can_you_miss_this REGION OF CENTRAL MACEDONIA ISBN: 978-618-84070-0-8 ΤΗΕSSALΟΝΙΚΙ • SERRES • ΙΜΑΤΗΙΑ • PELLA • PIERIA • HALKIDIKI • KILKIS ΕΣ. ΑΥΤΙ ΕΞΩΦΥΛΛΟ ΟΠΙΣΘΟΦΥΛΛΟ ΕΣ. ΑΥΤΙ ΜΕ ΚΟΛΛΗΜΑ ΘΕΣΗ ΓΙΑ ΧΑΡΤΗ European emergency MUSEUMS PELLA KTEL Bus Station of Litochoro KTEL Bus Station Thermal Baths of Sidirokastro number: 112 Archaeological Museum HOSPITALS - HEALTH CENTERS 23520 81271 of Thessaloniki 23230 22422 of Polygyros General Hospital of Edessa Urban KTEL of Katerini 2310 595432 Thermal Baths of Agkistro 23710 22148 23813 50100 23510 37600, 23510 46800 KTEL Bus Station of Veria 23230 41296, 23230 41420 HALKIDIKI Folkloric Museum of Arnea General Hospital of Giannitsa Taxi Station of Katerini 23310 22342 Ski Center Lailia HOSPITALS - HEALTH CENTERS 6944 321933 23823 50200 23510 21222, 23510 31222 KTEL Bus Station of Naoussa 23210 58783, 6941 598880 General Hospital of Polygyros Folkloric Museum of Afytos Health Center of Krya Vrissi Port Authority/ C’ Section 23320 22223 Serres Motorway Station 23413 51400 23740 91239 23823 51100 of Skala, Katerini KTEL Bus Station of Alexandria 23210 52592 Health Center of N. Moudania USEFUL Folkloric Museum of Nikiti Health Center of Aridea 23510 61209 23330 23312 Mountain Shelter EOS Nigrita 23733 50000 23750 81410 23843 50000 Port Authority/ D’ Section Taxi Station of Veria 23210 62400 Health Center of Kassandria PHONE Anthropological Museum Health Center of Arnissa of Platamonas 23310 62555 EOS of Serres 23743 50000 of Petralona 23813 51000 23520 41366 Taxi Station of Naoussa 23210 53790 Health Center of N.
    [Show full text]
  • HYDROGEOCHEMICAL CONDITION of the PIKROLIMNI LAKE (KILKIS GREECE) Dotsika E.1, Maniatis Y.1 , Tzavidopoulos E.1, Poutoukis D.2 and Albanakis K.3
    ∆ελτίο της Ελληνικής Γεωλογικής Εταιρίας τοµ. XXXVI, 2004 Bulletin of the Geological Society of Greece vol. XXXVI, 2004 Πρακτικά 10ου ∆ιεθνούς Συνεδρίου, Θεσ/νίκη Απρίλιος 2004 Proceedings of the 10th International Congress, Thessaloniki, April 2004 HYDROGEOCHEMICAL CONDITION OF THE PIKROLIMNI LAKE (KILKIS GREECE) Dotsika E.1, Maniatis Y.1 , Tzavidopoulos E.1, Poutoukis D.2 and Albanakis K.3. 1 Inst.of Material science, N.C.S.R. «Demokritos», Aghia Paraskevi, Attiki 2 General secretary Research and Technology, Mesogion 12-14, Athens 3 School of Geology, Aristotle University of Thessaloniki ABSTRACT In order to understand the hydrogeochemical conditions of the basin of Pikrolimni we collected water samples from the borehole in the thermal spa of Pikrolimni and samples of brine and sediments from the lake. We also sampled fresh water of the region. The depth of the borehole in the thermal spa is approximately 250 meters. This water is naturally sparkling, with a metallic aftertaste and a slight organic smell. The samples were taken twice during the year: in summer (8/2002) and in winter (2003). The analytical scheme includes field measurements of temperature, conductivity and pH. + + 2+ 2+ - - 2- 2- - - - - Major ions (Na , K , Ca , Mg , Cl , Br , SO4 , CO3 , HCO3 , NO3 ), F and Br were determined, in laboratory, according to standard analytical methods. Samples were also subjected to isotopic analysis of δ18O and δ2H. The results from the chemical analyses of the samples, show that the waters taken from the borehole, are of the type Mg- (Na-Ca)-HCO3 and the salts of the lake are of the type Na-Cl- (CO3- SO4).
    [Show full text]
  • Hydrochemical.Pdf
    Bulletin of the Geological Society of Greece Vol. 36, 2004 HYDROGEOCHEMICAL CONDITION OF THE PIKROLIMNI LAKE (KILKIS GREECE) Dotsika E. Inst.of Material science, N.C.S.R. «Demokritos» Maniatis Y. Inst.of Material science, N.C.S.R. «Demokritos» Tzavidopoulos E. Inst.of Material science, N.C.S.R. «Demokritos» Poutoukis D. General secretary Research and Technology Albanakis K. School of Geology, Aristotle University of Thessaloniki https://doi.org/10.12681/bgsg.16618 Copyright © 2018 E. Dotsika, Y. Maniatis, E. Tzavidopoulos, D. Poutoukis, K. Albanakis To cite this article: Dotsika, E., Maniatis, Y., Tzavidopoulos, E., Poutoukis, D., & Albanakis, K. (2004). HYDROGEOCHEMICAL CONDITION OF THE PIKROLIMNI LAKE (KILKIS GREECE). Bulletin of the Geological Society of Greece, 36(1), 192-195. doi:https://doi.org/10.12681/bgsg.16618 http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 07/04/2020 09:53:29 | Δελτίο της Ελληνικής Γεωλογικής Εταιρίας τομ XXXVI, 2004 Bulletin of the Geological Society of Greece vol. XXXVI, 2004 Πρακτικά 10ou Διεθνούς Συνεδρίου, Θεσ/νίκη Απρίλιος 2004 Proceedings of the 10th International Congress, Thessaloniki, April 2004 HYDROGEOCHEMICAL CONDITION OF THE PIKROLIMNI LAKE (KILKIS GREECE) Dotsika E.1, Maniatis Y.1 , Tzavidopoulos E.1, Poutoukis D.2 and Albanakis K.3. 11nst.of Material science, N.C.S.R. «Demokritos», Aghia Paraskevi, Attiki 2 General secretary Research and Technology, Mesogion 12-14, Athens 3 School of Geology, Aristotle University of Thessaloniki ABSTRACT In order to understand the hydrogeochemical conditions of the basin of Pikrolimni we collected water samples from the borehole in the thermal spa of Pikrolimni and samples of brine and sediments from the lake.
    [Show full text]
  • Glass Making in the Greco-Roman World Studies in Archaeological Sciences 4
    Glass Making in the Greco-Roman World Studies in Archaeological Sciences 4 The series Studies in Archaeological Sciences presents state-of-the-art methodological, technical or material science contributions to Archaeological Sciences. The series aims to reconstruct the integrated story of human and material culture through time and testifies to the necessity of inter- and multidisciplinary research in cultural heritage studies. Editor-in-Chief Prof. Patrick Degryse, Centre for Archaeological Sciences, KU Leuven, Belgium Editorial Board Prof. Ian Freestone, Cardiff Department of Archaeology, Cardiff University, United Kingdom Prof. Carl Knappett, Department of Art, University of Toronto, Canada Prof. Andrew Shortland, Centre for Archaeological and Forensic Analysis, Cranfield University, United Kingdom Prof. Manuel Sintubin, Department of Earth & Environmental Sciences, KU Leuven, Belgium Prof. Marc Waelkens, Centre for Archaeological Sciences, KU Leuven, Belgium Glass Making in the Greco-Roman World Results of the ARCHGLASS Project Edited by Patrick Degryse Leuven University Press Published with support of © 2014 by Leuven University Press / Presses Universitaires de Louvain / Universitaire Pers Leuven. Minderbroedersstraat 4, B-3000 Leuven (Belgium). All rights reserved. Except in those cases expressly determined by law, no part of this publication may be multiplied, saved in an automated datafile or made public in any way whatsoever without the express prior written consent of the publishers. ISBN 978 94 6270 007 9 D / 2014 / 1869 / 86 NUR: 682/933 Lay-out: Friedemann Vervoort Cover: Jurgen Leemans 5 Preface The ARCHGLASS “Archaeometry and Archaeology of Ancient Glass Production as a Source for Ancient Technology and Trade of Raw Materials” project, is a Seventh Framework Programme “Ideas” project funded under the European Research Council Starting Grant scheme.
    [Show full text]
  • Thessaloniki Perfecture
    SKOPIA - BEOGRAD SOFIA BU a MONI TIMIOU PRODROMOU YU Iriniko TO SOFIASOFIA BU Amoudia Kataskinossis Ag. Markos V Karperi Divouni Skotoussa Antigonia Melenikitsio Kato Metohi Hionohori Idomeni 3,5 Metamorfossi Ag. Kiriaki 5 Ano Hristos Milohori Anagenissi 3 8 3,5 5 Kalindria Fiska Kato Hristos3,5 3 Iliofoto 1,5 3,5 Ag. Andonios Nea Tiroloi Inoussa Pontoiraklia 6 5 4 3,5 Ag. Pnevma 3 Himaros V 1 3 Hamilo Evzoni 3,5 8 Lefkonas 5 Plagia 5 Gerakari Spourgitis 7 3 1 Meg. Sterna 3 2,5 2,5 1 Ag. Ioanis 2 0,5 1 Dogani 3,5 Himadio 1 Kala Dendra 3 2 Neo Souli Em. Papas Soultogianeika 3 3,5 4 7 Melissourgio 2 3 Plagia 4,5 Herso 3 Triada 2 Zevgolatio Vamvakia 1,5 4 5 5 4 Pondokerassia 4 3,5 Fanos 2,5 2 Kiladio Kokinia Parohthio 2 SERES 7 6 1,5 Kastro 7 2 2,5 Metala Anastassia Koromilia 4 5,5 3 0,5 Eleftherohori Efkarpia 1 2 4 Mikro Dassos 5 Mihalitsi Kalolivado Metaxohori 1 Mitroussi 4 Provatas 2 Monovrissi 1 4 Dafnoudi Platonia Iliolousto 3 3 Kato Mitroussi 5,5 6,5 Hrisso 2,5 5 5 3,5 Monoklissia 4,5 3 16 6 Ano Kamila Neohori 3 7 10 6,5 Strimoniko 3,5 Anavrito 7 Krinos Pentapoli Ag. Hristoforos N. Pefkodassos 5,5 Terpilos 5 2 12 Valtoudi Plagiohori 2 ZIHNI Stavrohori Xirovrissi 2 3 1 17,5 2,5 3 Latomio 4,5 3,5 2 Dipotamos 4,5 Livadohori N.
    [Show full text]
  • Geothermal Exploration and Development Activities in Greece During 1995-1999
    GEOTHERMAL EXPLORATION AND DEVELOPMENT ACTIVITIES IN GREECE DURING 1995-1999 Michael Fytikas1, Nikolaos Andritsos2, Grigorios Karydakis3, Nikolaos Kolios3, Dimitrios Mendrinos4 and Maria Papachristou1 1Aristotle University of Thessaloniki, Dept. of Geology, GR 54006, Thessaloniki, Greece 2CPERI & Dept. Chemical Engineering, AUTh, P.O Box 1517, GR 54006, Thessaloniki, Greece 3IGME, Dept. of Geothermal Energy, Mesogeion 70, GR 115 27, Athens, Greece 4Omega European Consulting, Navarinou 6, Pefki 15121, Athens, Greece Key Words: geothermal exploration, geothermal uses, country has markedly expanded through the continuation of research update, Greece. and productive activities. The bulk of exploration activities were carried out by the Institute of Geological and Mineral ABSTRACT Exploration (IGME). A map with the geothermal localities in Greece is shown in Figure 1. The paper reviews the research and development activities in geothermal energy in Greece during the period 1995-1999. The low enthalpy geothermal research has proceeded at a Information is also provided on the current status of relative high rate. A significant amount of data and information geothermal direct heat uses. Greece has a great geothermal has been gathered, revealing new geothermal fields (mainly potential. This potential has been confirmed and verified by the low enthalpy fields, most of which are located in Northern discovery and exploration of new geothermal fields during the Greece), or expanding the areas of known fields. Even in past five years (1995-1999). During this period the geothermal Western Greece, which is the least favorable territory in terms research and applications were mainly related to low enthalpy of geothermics, and particularly in the areas of Antirrio and fields.
    [Show full text]
  • 2020 Sustainable Development Report
    2019 - 2020 Sustainable Development Report Kilometer-based tolling for the first time in Greece Our aim is to connect places and people, by carrying goods, ideas, dreams, culture and opportunities Our ambition is that Olympia Odos lifts all kinds of exclusion CONTENTS 1. Message from the Management 4 2. Our Response to COVID-19 6 3. Milestones 2019-2020 8 4. The Project 10 5. Corporate Governance & Structure 16 6. Our Approach Towards Sustainable Development 28 7. Travel Experience & Service 40 8. Road Safety and Infrastructure 52 9. The Project’s Human Resources 66 10. Preserving the Environmental Wealth 78 11. Our Social Footprint 88 12 .Goals per Sustainable Development Strategy Pillar 108 13. Annex 112 14. About the Report 120 15. GRI Content Index 122 1. MESSAGE FROM THE MANAGEMENT “We are breaking ground having in mind our vision that is to ensure a future interwoven with innovative technologies, sustainable practices in the field of transports, but always focusing on the people. We develop innovative practices that help upgrade our infrastructure and services, improve the quality of life of the local communities in which we are active and of the society in general.” 4 | ΟLYMPIA ODOS The second Sustainable Development Report of Olympia The introduction of new technologies and innovation also Odos is issued in a critical period where the health crisis helps us achieve our strategic environmental goals and creates uncertainty and concerns about the future, while it commitments. Within this context, in 2019-2020 we invested clearly appears that this crisis will have long-term impacts in important actions aiming at reducing our carbon footprint.
    [Show full text]
  • Events Guide
    Oinoxeneia - Landscapes and tastes of Aigialeia 17-27 August 2017 “The colors of taste” Aigialeia is dressed up, wearing white, rosé and red colors! It pairs fine local wines with flavors and viands of the local cuisine, offering a joyful and delightful experience in its beautiful landscapes. «The colors of flavor» is the theme of «Oinoxeneia 2017». Our journey is full of beautiful surprises! Flavour balancing guided by wine| Artistic events | Events in wineries | Tours in vineyards | Wine tasting | Explorations | Exhibitions |Concerts This year’s Oinoxeneia will be an opportunity to explore the harmony of tastes in a land which uniquely combines nature with people, tradition with culture, long history with the present day and sea with fir! A land praised by Pausanias (Greek traveller and geographer of the 2nd century AD) for its vineyards and by Alexander Payne (Academy award winner director) “International ambassador of Aigialeia’s wines”, for its wines and hospitality. A land with flavor complexity and long aftertaste! Oinoxeneia is organized for the 5th year by DI.K.EP.A. - Municipal Welfare Business of Aigialeia and is one of the most important wine tourism festivities in the country. Protagonists and conjoiners of all the events are the fine local wines and wineries of the Oinoxeneia network. This year accessing Aigialeia will be quicker and safer via the new Olympia Odos highway. You are all invited to enjoy the journey through the Wine Roads of Aigialeia, living the Oinoxeneia experience! a multidimensional festival organized
    [Show full text]