DOCSLIB.ORG

04; DIA- Sion of Previous Assumptions on the Geometry, Kinemat- Ics and the Tectonic Evolution of This Part of Northern MANTOPOULOS, 2004; OCAKOGLOU Et Al., 2005)

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
04; DIA- Sion of Previous Assumptions on the Geometry, Kinemat- Ics and the Tectonic Evolution of This Part of Northern MANTOPOULOS, 2004; OCAKOGLOU Et Al., 2005) Geologia Croatica 59/1 85–96 8 Figs. ZAGREB 2006 Plio–Quaternary Geometry and Kinematics of Ptolemais Basin (Northern Greece): Implications for the Intra-Plate Tectonics in Western Macedonia Anastasios DIAMANTOPOULOS Key words: Progressive shear strain, Intra-plate tec- Western Macedonia in Northern Greece. New structural tonics, Ptolemais Basin, Western Macedonia, North- data, observed in the Ptolemais basin are presented in ern Greece. order to elucidate the principal deformation styles and mechanisms in this area (Fig. 1). Distribution of defor- mational structures, the geometry and kinematics of Abstract deformation, and a new kinematic model for the Ptol- An integrated structural study of the Ptolemais basin of Northern Greece allows assessment of deformation processes and their impli- emais basin are also addressed. Finally, an integrated cation in the Pliocene–Quaternary structural evolution of this part of evaluation of new data and their implications allows a Western Macedonia. Normal and reverse faults within Plio–Quater- new improved comprehension of intra-plate tectonics of nary sediments, NE–SW striking anticlines in both Plio–Quaternary Western Macedonia. sediments and pre-Tertiary basement-units, torsions and deforma- tion partitioning, highlight the particular characteristics of intra-plate deformation. Field investigations and drilling data infer the conclusion 1.1. Previous studies and that intra-plate processes were governed by progressive shear strain target of this work during the Plio–Quaternary. A new kinematic model for the develop- ment of the Ptolemais basin is proposed, showing the importance of Previous studies of the Ptolemais basin by PAVLIDES progressive shear strain. (1985), DOUTSOS & KOUKOUVELAS (1998), MOUNTRAKIS et al. (1999), and GOLDSWORTHY & JACKSON (2000) provided an insight into the impor- tance of active faults and their role in the geomorphol- ogy and seismology of this basin. Structural data pre- sented in these papers were mainly concerned with the 1. INTRODUCTION geometry and kinematic characteristics of the observed fault sets. According to PAVLIDES (1985) and MOUN- Geological evidence in the Hellenic orogenic belt of TRAKIS et al. (1999), multiple tectonic phases during eastern Mediterranean confirms complex Neogene– Miocene–Quaternary times were recognized, each char- Quaternary tectonic processes, both in the orogenic acterized by compressional or extensional structures. front of the Central and South Aegean, and in the back- arc domain of the North Aegean and Western Mace- New structural analysis of the Ptolemais basin in donia (STEWART & HANCOCK, 1991; PIPER & Western Macedonia presented in this paper, allows revi- PERISSORATIS, 2003; KREEMER et al., 2004; DIA- sion of previous assumptions on the geometry, kinemat- ics and the tectonic evolution of this part of Northern MANTOPOULOS, 2004; OCAKOGLOU et al., 2005). Greece (Fig. 1). This structural synthesis is based on These observations make evident the importance of het- data obtained by field analysis, drilling and geophysical erogenous strain, including co-existence of strike-slip, investigations, which document the main structural pat- rotational and ductile structures. Since deformation and tern within Plio–Quaternary sediments, the sub-surface strain outline three-dimensional quantities, structural geometry of the Ptolemais basin fill and also the re-acti- heterogeneity from the lithospheric-scale to the grain- vation of the pre-Miocene structures by Plio–Quaterna- scale of observation mark an essential constituent of ry tectonics. The study area is an open-pit lignite mine strain (JONES et al., 2005; DE PAOLA et al., 2005). exploited by the Public Power Corporation of Greece This work analyzes the Plio–Quaternary structures (PPC). and the deformation style in the Ptolemais basin of 2. GEOLOGY OF WESTERN MACEDONIA National Technical University of Athens, Department of Mining, Metallurgical & Engineering Geology, Section of Geosciences, 9 Herron Polytechniou Street, GR-15780, Zografou, Athens, Geological data, geophysical studies and GPS measure- Greece; e-mail: [email protected] ments in Western Macedonia denote on-going tectonic 86 Geologia Croatica 59/1 Fig. 1 Tectonic map of Western Macedonia. Three distinctive domains (dotted black boxes) with compressional field structures are illus- trated, see MOUNTRAKIS (1983), FOTIS (2004) and DIAMANTOPOULOS (2004). Inset map: The Hellenic orogenic arc in the Eastern Mediterranean, based on MARIOLAKOS et al. (2004) and DIAMANTOPOULOS (2004). Legend for inset map: AEP – Aegean plate; AFP – African plate; APMC – Apulia micro-continent; CFZ – Cephalonia Fault Zone; NAF – North Anatolia Fault; AFZ – Axios Fault Zone; STRMZ – Strymon Fault Zone; MNR – Morpho–Neotectonic Region; SA – Study area. activity (MOUNTRAKIS et al., 1999; FOUNTOULIS 3. GEOLOGY OF THE PTOLEMAIS BASIN et al., 2002; DRAKATOS et al., 2005; BURCHFIEL et al., 2005). Here, several tectonic basins of continental Sedimentary fill of the Ptolemais basin includes terres- origin developed during Miocene–Quaternary times trial and lacustrine sediments of Miocene up to Pleisto- (the Florina, Ptolemais, Kozani–Servia, Almopia basins cene age, abundant in lignite reserves (KOUKOUZAS – Fig. 1). The presence of Plio–Quaternary volcanism in et al., 2000; KVACEK et al., 2002). STEENBRINK the Almopia basin (VOUGIOUKALAKIS et al., 2004 (1998) studied distinctive sedimentary facies and con- cluded that the basin formation started during the Torto- and reference there in), also indicates re-arrangement of nian. DIAMANTOPOULOS & DIMITRAKOPOULOS the lithospheric material. The physiography of North- (2004a) by synthesis of tectono–sedimentary data, rec- western Greece is characterized by the two elevated ognized three distinctive lignite members of Miocene, domains of Pelagonian and Pindic Cordillera as well as Pliocene and Pleistocene age, intercalated with clas- by the two subsided domains of the Mesohellenic and tic sediments. The same authors also recognized two Axios basins (Fig. 1). The latter are interpreted as Ter- major unconformities within the sedimentary basin tiary (AUBOUIN, 1965) piggy-back basins with thick succession, i.e. the first one at the base of the Miocene, sedimentary accumulations. (between the first terrestrial sediments and the pre-Ter- Diamantopoulos: Plio–Quaternary Geometry and Kinematics of Ptolemais Basin... 87 A B Fig. 2 (A) Digital elevation model of Western Macedonia. Photos of Figs. 4 and 5 are depicted. (B) Simplified tectonic map of the southern part of the Ptolemais basin. Inset map shows the spatial distribution of the analyzed drillings in three domains I, II and III of Fig. 3. The location of the geological sections A–B–C of Fig. 7 is also illustrated. tiary basement units), and the second one between the Pre-Tertiary basement rocks of the Ptolemais basin Pleistocene strata and the Pliocene sediments. Arrange- can be subdivided into four distinctive tectonic units, ment and geometry of lignite layers of the Ptolemais (Fig. 2b). From the lowermost to the highest unit, they basin indicate a westward migration from the eastern are: (I) pre-Alpine Pelagonian Basement, separated into marginal domain (Vermion mountain) toward the west- Schist sub-unit, the Gneiss sub-unit, the granitoid mylo- ern marginal domain (Askion and Vernon mountains), nites and the granites (BRUNN, 1956; MOUNTRAKIS (DIAMANTOPOULOS & DIMITRAKOPOULOS, 1983; DIAMANTOPOULOS, 2005), (II) Almopia 2004a). Unit, with Triassic–Lower Jurassic marbles and meta- 88 Geologia Croatica 59/1 A B Fig. 3 (A) Quantitative thickness variation of the Pliocene lignite sequences; (B) Quantitative thickness variation of the Plio–Quaternary sedi- ments (overburden cover of Pliocene lignites). The spatial distribution of the domains I, II and III is depicted in the inset map of Fig. 2. sediments of Late Jurassic age (DIAMANTOPOULOS, also show a great difference in lithostratigraphic devel- 2005), (III) Ultramafic–Mafic Unit of Mesozoic age, opment and sedimentary evolution, which makes strati- and (IV) Cretaceous Unit, with platform limestones graphic correlation of Plio–Quaternary strata between and Maastrichtian flysch (MERCIER, 1968). Steep and these sub-basins difficult (DIAMANTOPOLOUS & low-angle shear zones, formed in brittle–ductile condi- DIMITRAKOLOPOUS, 2004a). tions, separate distinctive tectonic units. Recent struc- tural studies show that during the Oligo–Miocene, a 3.2. Quantitative and qualitative analysis strong orogen-perpendicular stretching re-arranged the of borehole data geometry of the pre-Tertiary sequences (MOUNTRA- KIS, 2004; DIAMANTOPOULOS, 2005). The NW–SE Borehole data, which include 720 boreholes that pen- strike of the Ptolemais basin is controlled by pre-exist- etrated the Plio–Quaternary basin fill and 50 boreholes ing shear zones in pre-Tertiary basement units, which that reached the pre-Tertiary basement have been taken accommodated Oligocene stretching of the Internal Hel- into account, and are distributed in 3 domains (Fig. 2b). lenides (DIAMANTOPOULOS, 2005). These inherited The thickness of the Pliocene lignite sequence and also structures correspond to several shear zones between the thickness of the Plio–Quaternary sediments (the pre-Tertiary basement sequences. overburden of the Pliocene lignite sequence) have been quantitatively analyzed. Diagrams A and B of Fig. 3 3.1. Morphotectonic units of shows the following thickness-variation pattern: the Ptolemais Basin a) Thicknesses of the lignite
Load more

Recommended publications
  • A New Consideration About the Almopia-Paikon Boundary Based on the Geological Mapping in the Area of Nerostoma-Lakka (Central Macedonia, Greece)
    Δελτίο της Ελληνικής Γεωλογικής Εταιρίας τομ. ΧΧΧΧ, Bulletin of the Geological Society of Greece vol. XXXX, 2007 2007 Proceedings of the 11th International Congress, Athens, May, Πρακτικά 11ou Διεθνούς Συνεδρίου, Αθήνα, Μάιος 2007 2007 A NEW CONSIDERATION ABOUT THE ALMOPIA-PAIKON BOUNDARY BASED ON THE GEOLOGICAL MAPPING IN THE AREA OF NEROSTOMA-LAKKA (CENTRAL MACEDONIA, GREECE) Tranos M. D. \ Plougarlis A. P.!, and Mountrakis D. Μ.l 1 Aristotle University of Thessaloniki, School of Geology, Department of Geology, GR-54124 Thessaloniki, Greece, [email protected], [email protected], [email protected] Abstract Geological mapping along the boundary of Almopia and Paikon zone in the 'Nerostoma' region, NNW of Lakka village defines mafic volcanogenic rocL·, meta-pelites and radiolarites, thick-bedded to massive micritic limestones and flysch meta-sediments that dip mainly towards SW. Middle-Late Cretaceous fossiliferous limestones overlie unconformably the flysch meta-sediments and are characterised only by a primary foliation SO that dips at shallow angles to the NNW-N. Secondary foliations SI (sub-parallel to SO) and S2 are observed in the meta-clastic rocks. A Dl event caused Fl and progressively F2 folds to which S2 is the axial plane schistosity dipping to SW. This event which has not affected the fossiliferous limestones is related to an oblique convergence or inclined transpression during the Late Jurassic-Early Cretaceous. A D2 event dated in Early Tertiary caused an intense NE-thrusting and S-C cataclastic fabric defining top-to-the NE sense-of-shear. At many parts, the unconformity contact between the fossiliferous limestones and the underlying flysch is obliterated by this thrusting event.
    [Show full text]
  • For Municipal Solid Waste Management in Greece
    Journal of Open Innovation: Technology, Market, and Complexity Article Description and Economic Evaluation of a “Zero-Waste Mortar-Producing Process” for Municipal Solid Waste Management in Greece Alexandros Sikalidis 1,2 and Christina Emmanouil 3,* 1 Amsterdam Business School, Accounting Section, University of Amsterdam, 1012 WX Amsterdam, The Netherlands 2 Faculty of Economics, Business and Legal Studies, International Hellenic University, 57001 Thessaloniki, Greece 3 School of Spatial Planning and Development, Aristotle University of Thessaloniki, 54124 Thessaloniki, Greece * Correspondence: [email protected]; Tel.: +30-2310-995638 Received: 2 July 2019; Accepted: 19 July 2019; Published: 23 July 2019 Abstract: The constant increase of municipal solid wastes (MSW) as well as their daily management pose a major challenge to European countries. A significant percentage of MSW originates from household activities. In this study we calculate the costs of setting up and running a zero-waste mortar-producing (ZWMP) process utilizing MSW in Northern Greece. The process is based on a thermal co-processing of properly dried and processed MSW with raw materials (limestone, clay materials, silicates and iron oxides) needed for the production of clinker and consequently of mortar in accordance with the Greek Patent 1003333, which has been proven to be an environmentally friendly process. According to our estimations, the amount of MSW generated in Central Macedonia, Western Macedonia and Eastern Macedonia and Thrace regions, which is conservatively estimated at 1,270,000 t/y for the year 2020 if recycling schemes in Greece are not greatly ameliorated, may sustain six ZWMP plants while offering considerable environmental benefits. This work can be applied to many cities and areas, especially when their population generates MSW at the level of 200,000 t/y, hence requiring one ZWMP plant for processing.
    [Show full text]
  • Travertine Caves in Almopia, Greece
    See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/320310627 Travertine caves in Almopia, Greece Article in Cave and Karst Science · October 2017 CITATIONS READS 0 169 3 authors, including: Georgios Lazaridis Konstantinos Trimmis Aristotle University of Thessaloniki Cardiff University 29 PUBLICATIONS 47 CITATIONS 14 PUBLICATIONS 1 CITATION SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Using LEGO to explore Archaeology and acquire Modern Greek Vocabulary View project Exploring Archaeology in Museums through the 3E method View project All content following this page was uploaded by Konstantinos Trimmis on 10 October 2017. The user has requested enhancement of the downloaded file. Cave and Karst Science, Vol.44, No.2, (2017) 58–63 © British Cave Research Association 2017 Transactions of the British Cave Research Association ISSN 1356-191X Travertine caves in Almopia, Greece Georgios LAZARIDIS 1, Konstantinos P TRIMMIS 2 and Spyridoula PAPPA 3 1 Department of Geology, Laboratory of Geology and Palaeontology, Aristotle University of Thessaloniki, 54124, Thessaloniki, Greece. E-mail: [email protected] 2 Department of Archaeology and Conservation, Cardiff University, Cardiff, Wales, UK. E-mail: [email protected] 3 Department of Earth Sciences, The Natural History Museum, Cromwell Road, London, SW7 5BD, UK. E-mail: [email protected] Abstract: Seven caves have been explored and surveyed within two travertine terraces (Aspri Petra and Baina) in the Almopia region, Greece. The Aspri Petra terrace is less faulted than the Baina and the caves of each terrace demonstrate differences that could be related to the degree of faulting.
    [Show full text]
  • UCLA Electronic Theses and Dissertations
    UCLA UCLA Electronic Theses and Dissertations Title Cremation, Society, and Landscape in the North Aegean, 6000-700 BCE Permalink https://escholarship.org/uc/item/8588693d Author Kontonicolas, MaryAnn Emilia Publication Date 2018 Peer reviewed|Thesis/dissertation eScholarship.org Powered by the California Digital Library University of California UNIVERSITY OF CALIFORNIA Los Angeles Cremation, Society, and Landscape in the North Aegean, 6000 – 700 BCE A dissertation submitted in partial satisfaction of the requirements for the degree Doctor of Philosophy in Archaeology by MaryAnn Kontonicolas 2018 © Copyright by MaryAnn Kontonicolas 2018 ABSTRACT OF THE DISSERTATION Cremation, Society, and Landscape in the North Aegean, 6000 – 700 BCE by MaryAnn Kontonicolas Doctor of Philosophy in Archaeology University of California, Los Angeles, 2018 Professor John K. Papadopoulos, Chair This research project examines the appearance and proliferation of some of the earliest cremation burials in Europe in the context of the prehistoric north Aegean. Using archaeological and osteological evidence from the region between the Pindos mountains and Evros river in northern Greece, this study examines the formation of death rituals, the role of landscape in the emergence of cemeteries, and expressions of social identities against the backdrop of diachronic change and synchronic variation. I draw on a rich and diverse record of mortuary practices to examine the co-existence of cremation and inhumation rites from the beginnings of farming in the Neolithic period
    [Show full text]
  • The GEOLOGY of ALMOPIA SPELEOPARK
    Scientific Annals, School of Geology Special volume 98 27-31 Thessaloniki, 2006 Aristotle University of Thessaloniki (AUTH) THE GEOLOGY OF ALMOPIA SPELEOPARK George ElEftHEriadis1 Abstract: The Almopia Speleopark is located on the boundary of two geological zones: the Almopia (Axios) zone eastwards and the Pelagonian zone westwards. The Almopia zone in the area of study is comprised of metamorphic rocks (schists, marbles and cipolines), ophiolites, limestones and clastic formations whereas the Pelagonian zone consist of carbonate rocks of Triassic-Jurassic age, sediments of Upper Cretaceous age and flysch of Upper Maastrictian-Lower Paleocene. In the area there are also travertine deposits of signifi- cant quantity and excellent quality. The seismicity in the area can be considered as not significant. Key words: Almopia, Speleopark, geology, volcanology, seismicity. INTRODUCTION The Almopia area geotectonicaly belongs to the Almopia zone, which together with the Peonia and Paikon zones constitute the old Axios (Vardar) zone (Μercier, 1968). The Axios zone Kossmat,( 1924) is situated between the Pelagonian massif to the west and the Serbo-Macedonian massif to the east. The Almopia and Peonia zones, con- stituting the westernmost and easternmost parts of the Axios zone, respectively, were deep-water oceans sepa- rated by the shallow ocean of the Paikon zone, consisting of thick carbonate rocks of mainly Triassic to Cretaceous age.The Almopia zone is characterized by huge masses of ophiolites (Bebien et al., 1994). The Almopia zone was deformed during two oro- genic periods: the Upper Jurassic-Lower Cretaceous and the Upper Cretaceous-Middle Eocene. During the first period the Almopia ocean closed, the Almopia zone emerged temporary until the Middle-Upper Cretaceous transgression and the ophiolitic rocks overthrusted on the Pelagonian platform westwards (Μercier, 1968).
    [Show full text]
  • The Shaping of the New Macedonia (1798-1870)
    VIII. The shaping of the new Macedonia (1798-1870) by Ioannis Koliopoulos 1. Introduction Macedonia, both the ancient historical Greek land and the modern geographical region known by that name, has been perhaps one of the most heavily discussed countries in the world. In the more than two centuries since the representatives of revolutionary France introduced into western insular and continental Greece the ideas and slogans that fostered nationalism, the ancient Greek country has been the subject of inquiry, and the object of myth-making, on the part of archaeologists, historians, ethnologists, political scientists, social anthropologists, geographers and anthropogeographers, journalists and politicians. The changing face of the ancient country and its modern sequel, as recorded in the testimonies and studies of those who have applied themselves to the subject, is the focus of this present work. Since the time, two centuries ago, when the world’s attention was first directed to it, the issue of the future of this ancient Greek land – the “Macedonian Question” as it was called – stirred the interest or attracted the involvement of scientists, journalists, diplomats and politicians, who moulded and remoulded its features. The periodical cri- ses in the Macedonian Question brought to the fore important researchers and generated weighty studies, which, however, with few exceptions, put forward aspects and charac- teristics of Macedonia that did not always correspond to the reality and that served a variety of expediencies. This militancy on the part of many of those who concerned themselves with the ancient country and its modern sequel was, of course, inevitable, given that all or part of that land was claimed by other peoples of south-eastern Europe as well as the Greeks.
    [Show full text]
  • Visa & Residence Permit Guide for Students
    Ministry of Interior & Administrative Reconstruction Ministry of Foreign Affairs Directorate General for Citizenship & C GEN. DIRECTORATE FOR EUROPEAN AFFAIRS Immigration Policy C4 Directorate Justice, Home Affairs & Directorate for Immigration Policy Schengen Email: [email protected] Email: [email protected] www.ypes.gr www.mfa.gr Visa & Residence Permit guide for students 1 Index 1. EU/EEA Nationals 2. Non EU/EEA Nationals 2.a Mobility of Non EU/EEA Students - Moving between EU countries during my short-term visit – less than three months - Moving between EU countries during my long-term stay – more than three months 2.b Short courses in Greek Universities, not exceeding three months. 2.c Admission for studies in Greek Universities or for participation in exchange programs, under bilateral agreements or in projects funded by the European Union i.e “ERASMUS + (placement)” program for long-term stay (more than three months). - Studies in Greek universities (undergraduate, master and doctoral level - Participation in exchange programs, under interstate agreements, in cooperation projects funded by the European Union including «ERASMUS+ placement program» 3. Refusal of a National Visa (type D)/Rights of the applicant. 4. Right to appeal against the decision of the Consular Authority 5. Annex I - Application form for National Visa (sample) Annex II - Application form for Residence Permit Annex III - Refusal Form Annex IV - Photo specifications for a national visa application Annex V - Aliens and Immigration Departments Contacts 2 1. Students EU/EEA Nationals You will not require a visa for studies to enter Greece if you possess a valid passport from an EU Member State, Iceland, Liechtenstein, Norway or Switzerland.
    [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]
  • Visa & Residence Permit Guide for Students
    Ministry of Interior & Administrative Reconstruction Ministry of Foreign Affairs Directorate General for Citizenship & C GEN. DIRECTORATE FOR EUROPEAN AFFAIRS Immigration Policy C4 Directorate Justice, Home Affairs & Directorate for Immigration Policy Schengen Email: [email protected] Email: [email protected] www.ypes.gr www.mfa.gr Visa & Residence Permit guide for students 1 Index 1. EU/EEA Nationals 2. Non EU/EEA Nationals 2.a Mobility of Non EU/EEA Students - Moving between EU countries during my short-term visit – less than three months - Moving between EU countries during my long-term stay – more than three months 2.b Short courses in Greek Universities, not exceeding three months. 2.c Admission for studies in Greek Universities or for participation in exchange programs, under bilateral agreements or in projects funded by the European Union i.e “ERASMUS + (placement)” program for long-term stay (more than three months). - Studies in Greek universities (undergraduate, master and doctoral level - Participation in exchange programs, under interstate agreements, in cooperation projects funded by the European Union including «ERASMUS+ placement program» 3. Refusal of a National Visa (type D)/Rights of the applicant. 4. Right to appeal against the decision of the Consular Authority 5. Annex I - Application form for National Visa (sample) Annex II - Application form for Residence Permit Annex III - Refusal Form Annex IV - Photo specifications for a national visa application Annex V - Aliens and Immigration Departments Contacts 2 1. Students EU/EEA Nationals You will not require a visa for studies to enter Greece if you possess a valid passport from an EU Member State, Iceland, Liechtenstein, Norway or Switzerland.
    [Show full text]
  • The History and Antiquities of the Doric Race, Vol. 1 of 2 by Karl Otfried Müller
    The Project Gutenberg EBook of The History and Antiquities of the Doric Race, Vol. 1 of 2 by Karl Otfried Müller This eBook is for the use of anyone anywhere at no cost and with almost no restrictions whatsoever. You may copy it, give it away or re-use it under the terms of the Project Gutenberg License included with this eBook or online at http://www.gutenberg.org/license Title: The History and Antiquities of the Doric Race, Vol. 1 of 2 Author: Karl Otfried Müller Release Date: September 17, 2010 [Ebook 33743] Language: English ***START OF THE PROJECT GUTENBERG EBOOK THE HISTORY AND ANTIQUITIES OF THE DORIC RACE, VOL. 1 OF 2*** The History and Antiquities Of The Doric Race by Karl Otfried Müller Professor in the University of Göttingen Translated From the German by Henry Tufnell, Esq. And George Cornewall Lewis, Esq., A.M. Student of Christ Church. Second Edition, Revised. Vol. I London: John Murray, Albemarle Street. 1839. Contents Extract From The Translators' Preface To The First Edition.2 Advertisement To The Second Edition. .5 Introduction. .6 Book I. History Of The Doric Race, From The Earliest Times To The End Of The Peloponnesian War. 22 Chapter I. 22 Chapter II. 39 Chapter III. 50 Chapter IV. 70 Chapter V. 83 Chapter VI. 105 Chapter VII. 132 Chapter VIII. 163 Chapter IX. 181 Book II. Religion And Mythology Of The Dorians. 202 Chapter I. 202 Chapter II. 216 Chapter III. 244 Chapter IV. 261 Chapter V. 270 Chapter VI. 278 Chapter VII. 292 Chapter VIII. 302 Chapter IX.
    [Show full text]
  • Almopia Speleopark, PELLA, MACEDONIA, GREECE)
    Scientific Annals, School of Geology Special volume 98 41-67 Thessaloniki, 2006 Aristotle University of Thessaloniki (AUTH) PALEONTOLOGICAL AND STRATIGRAPHICAL RESEARCH IN LOUTRA ARIDEAS BEAR CAVE (alMopia speleoparK, PELLA, MACEDONIA, GREECE) Evangelia TSOUKALA1, Katerina ChatZopoUloU1, Gernot RabeDer2, Spyridoula Pappa1, Doris nagel2 & Gerhard WithalM2 ABSTRACT: Excavation in Loutra Arideas Bear Cave has yielded thousand of fossilized specimens, thus it can be considered one of the richest in Late Pleistocene paleontological material of Greece. The abundance of the cave bear remains is remarkable. The large mammalian associated fauna comprises of Ursus ingres­ sus, Crocuta crocuta spelaea, Panthera leo spelaea, Panthera pardus, Vulpes vulpes, Canis lupus, Meles meles, mustelids, Bos primigenius, Capra ibex, Cervus elaphus and Dama dama, as well as of 25 species of micro- mammals, excluding bats. This excavation in the site during 1992-2006 involved in total: 90 participants (researchers, students and co-operators) in 12 systematic excavation seasons, 34 excavated squares with a total of 206 levels, resulting in 15 thousand specimens of large mammals and thousands of specimens of micromammals from the sieving procedure. The research on the cave bear continues with new techniques afforded by the use of the Scanning Electron Microscope (SEM) in milk carnassials, as well as in milk ca- nines. The bear teeth and the metapodials are also discussed as well as comparisons between Ursus ingressus from Loutra and from Gamssulzen Cave in Upper Austria, the cave that is usually used as the standard for comparisons within the cave bear group. Key words: Late Pleistocene Cave Fauna, Stratigraphy, Loutra Arideas, Macedonia, Greece. INTRODUCtion situated on the slopes of the Voras Mt.
    [Show full text]
  • Active Faults in North Greece
    The Greek Database of Seismogenic Sources (GreDaSS): state-of-the-art for northern Greece. Caputo R.*, Chatzipetros A.°, Pavlides S.° and Sboras S.* *) Department of Earth Sciences, University of Ferrara, Italy °) Department of Geology, Aristotle University of Thessaloniki, Greece Abstract The Greek Database of Seismogenic Sources (GreDaSS) is a repository of geological, tectonic and active fault data for the Greek territory and its surroundings. In this paper, we present the state-of- the-art of an on-going project devoted to the building of GreDaSS, which represents the results of decades of investigations by the authors and a myriad of other researchers working on the active tectonics of the broader Aegean Region. The principal aim of this international project is to create a homogenized framework of all data relevant to the seismotectonics, and especially the seismic hazard assessment, of Greece and its surroundings as well as a common research platform for performing seismic hazard analyses, modelling and scenarios from specific seismogenic structures. In particular, we introduce and synthetically describe the results obtained (and included in the database) up to date relative to the northern sector of continental Greece and Aegean Sea. As a first step we collected all available data (both published and unpublished) relative to the historical and instrumental seismicity determining the causative faults. Following the experience of recent 'surprising' earthquakes (e.g. 1995 Kozani and 1999 Athens), we realized the deficiency of such approach and decided to include in GreDaSS also active faults (i.e. seismogenic sources) recognized on the basis of geological, structural, morphotectonic, palaeoseismological and geophysical investigations.
    [Show full text]