The Igneous Rocks of Greece the Anatomy of an Orogen
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Genetics of the Peloponnesean Populations and the Theory of Extinction of the Medieval Peloponnesean Greeks
European Journal of Human Genetics (2017) 25, 637–645 Official journal of The European Society of Human Genetics www.nature.com/ejhg ARTICLE Genetics of the peloponnesean populations and the theory of extinction of the medieval peloponnesean Greeks George Stamatoyannopoulos*,1, Aritra Bose2, Athanasios Teodosiadis3, Fotis Tsetsos2, Anna Plantinga4, Nikoletta Psatha5, Nikos Zogas6, Evangelia Yannaki6, Pierre Zalloua7, Kenneth K Kidd8, Brian L Browning4,9, John Stamatoyannopoulos3,10, Peristera Paschou11 and Petros Drineas2 Peloponnese has been one of the cradles of the Classical European civilization and an important contributor to the ancient European history. It has also been the subject of a controversy about the ancestry of its population. In a theory hotly debated by scholars for over 170 years, the German historian Jacob Philipp Fallmerayer proposed that the medieval Peloponneseans were totally extinguished by Slavic and Avar invaders and replaced by Slavic settlers during the 6th century CE. Here we use 2.5 million single-nucleotide polymorphisms to investigate the genetic structure of Peloponnesean populations in a sample of 241 individuals originating from all districts of the peninsula and to examine predictions of the theory of replacement of the medieval Peloponneseans by Slavs. We find considerable heterogeneity of Peloponnesean populations exemplified by genetically distinct subpopulations and by gene flow gradients within Peloponnese. By principal component analysis (PCA) and ADMIXTURE analysis the Peloponneseans are clearly distinguishable from the populations of the Slavic homeland and are very similar to Sicilians and Italians. Using a novel method of quantitative analysis of ADMIXTURE output we find that the Slavic ancestry of Peloponnesean subpopulations ranges from 0.2 to 14.4%. -
Greece) Michael Foumelis1,*, Ioannis Fountoulis2, Ioannis D
ANNALS OF GEOPHYSICS, 56, 6, 2013, S0674; doi:10.4401/ag-6238 Special Issue: Earthquake geology Geodetic evidence for passive control of a major Miocene tectonic boundary on the contemporary deformation field of Athens (Greece) Michael Foumelis1,*, Ioannis Fountoulis2, Ioannis D. Papanikolaou3, Dimitrios Papanikolaou2 1 European Space Agency (ESA-ESRIN), Frascati (Rome), Italy 2 National and Kapodistrian University of Athens, Department of Dynamics Tectonics and Applied Geology, Athens, Greece 3 Agricultural University of Athens, Department of Geological Sciences and Atmospheric Environment, Laboratory of Mineralogy and Geology, Athens, Greece Article history Received October 19, 2012; accepted May 20, 2013. Subject classification: Satellite geodesy, Crustal deformations, Geodynamics, Tectonics, Measurements and monitoring. ABSTRACT while there are sufficient data for the period after 1810 A GPS-derived velocity field is presented from a dense geodetic network [Ambraseys and Jackson 1990]. Reports on damage and (~5km distance between stations) established in the broader area of displacement of ancient monuments [Papanastassiou Athens. It shows significant local variations of strain rates across a major et al. 2000, Ambraseys and Psycharis 2012] suggest in inactive tectonic boundary separating metamorphic and non-metamor- turns that Attica region has experienced several strong phic geotectonic units. The southeastern part of Athens plain displays earthquakes in the past. It is interesting that despite the negligible deformation rates, whereas towards the northwestern part unexpected catastrophic seismic event of September 7, higher strain rates are observed, indicating the control of the inactive tec- 1999, Mw=6.0 [Papadimitriou et al. 2002], no further tonic boundary on the contemporary deformation field of the region. monitoring of the region was held. -
Constraining the Tectonic Evolution of Extensional Fault Systems in the Cyclades (Greece) Using Low-Temperature Thermochronology Stephanie Brichau
Constraining the tectonic evolution of extensional fault systems in the Cyclades (Greece) using low-temperature thermochronology Stephanie Brichau To cite this version: Stephanie Brichau. Constraining the tectonic evolution of extensional fault systems in the Cyclades (Greece) using low-temperature thermochronology. Applied geology. Université Montpellier II - Sciences et Techniques du Languedoc; Johannes Gutenberg Universität Mainz, 2004. English. tel- 00006814 HAL Id: tel-00006814 https://tel.archives-ouvertes.fr/tel-00006814 Submitted on 3 Sep 2004 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Universität Mainz “Johannes Gutenberg” and Université de Montpellier II “Sciences et techniques du Languedoc” Dissertation zur Erlangung des Grades “DOKTOR DER NATURWISSENSCHAFTEN” am Fachbereich Geowissenschaften der Johannes Gutenberg-Universität Mainz THESE Pour obtenir le grade de “DOCTEUR DE L’UNIVERSITÉ MONTPELLIER II” Discipline: Terre solide, géodynamique Formation Doctorale: Structure et Evolution de la Lithosphère Ecole Doctorale: Science de la Terre et de l’Eau Presented and publicly defended at Mainz by Stéphanie Brichau June 29th, 2004 Title: Constraining the tectonic evolution of extensional fault systems in the Cyclades (Greece) using low-temperature thermochronology JURY M. Stephen Foley GP, Mainz President M. Michel Faure IST, Orléans Reviewer M. -
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). -
Pospiviroidae Viroids in Naturally Infected Stone and Pome Fruits In
21st International Conference on Virus and other Graft Transmissible Diseases of Fruit Crops Pospiviroidae viroids in naturally infected stone and pome fruits in Greece Kaponi, M.S.1, Luigi, M.2, Barba, M.2, Kyriakopoulou, P.E.I I Agricultural University of Athens, Iera Odos 75, 11855 Athens, Greece 2 CRA-PAV, Centro di Ricerca per la Patologia Vegeta le, 00156 Rome, Italy Abstract Viroid research on pome and stone fruit trees in Greece is important, as it seems that such viroids are widespread in the country and may cause serious diseases. Our research dealt with three Pospiviroidae species infecting pome and stone fruit trees, namely Apple scar skin viroid (ASSVd), Pear blister canker viroid (PBCVd) and Hop stunt viroid (HSVd). Tissue-print hybridization, reverse transcription-polymerase chain reaction (RT-PCR), cloning and sequencing techniques were successfully used for the detection and identification of these viroids in a large number of pome and stone fruit tree samples from various areas of Greece (Peloponnesus, Macedonia, Thessaly, Attica and Crete). The 58 complete viroid sequences obtained (30 ASSVd, 16 PBCVd and 12 HSVd) were submitted to the Gen Bank. Our results showed the presence of ASSVd in apple, pear, wild apple (Malus sylvestris), wild pear (Pyrus amygdaliformis) and sweet cherry; HSVd in apricot, peach, plum, sweet cherry, bullace plum (Prunus insititia), apple and wild apple; and PBCVd in pear, wild pear, quince, apple and wild apple. This research confirmed previous findings of infection of Hellenic apple, pear and wild pear with ASSVd, pear, wild pear and quince with PBCVd and apricot with HSVd. -
The Cognitive Benefits of Learning Native Language
Short Communication Open Access J Neurol Neurosurg Volume 10 Issue 3 - March 2019 DOI: 10.19080/OAJNN.2019.10.555788 Copyright © All rights are reserved by Genc Struga The Cognitive Benefits of Learning Native Language Genc Struga1* and Thomas Bak2 1Department of Neuroscience, University Hospital Mother Teresa, Albania 2Department of Psychology, Psychology and Language Sciences University of Edinburgh, UK Submission: February 05, 2019; Published: March 26, 2019 *Corresponding author: Genc Struga, Department of Neuroscience, University Hospital Mother Teresa, Albania Abstract Background The cognitive benefits of learning native language and bilingualism project focuses on Arvanites, a bilingual population in Greece that speak theAvantika, ability a for dialect further of learningAlbanian and language acquisition still spokenof other in languages. vast areas of Greece. It is classified as a minority and an endagered language and is considered in risk of extinction. The project aims to examine possible cognitive benefits of bilingualism in native speakers of Avantika, including Method We aim to achieve statistically important number of Arvanites equal Bilingual and monolingual to be interview using a up to date questionnaire and TEA or TEA like cognitive screening. This is a cross-sectional population study including bilingual and monolingual speakers orwithout 15% ofexclusion population. criteria and with respects to gender equality, stratified random sampling responders in the areas where Arvanite population traditionally lived achieving -
Successive Steps Towards the Creation of a Marina at Loutraki
Transactions on the Built Environment vol 40 © 1999 WIT Press, www.witpress.com, ISSN 1743-3509 Successive steps towards the creation of a Marina at Loutraki - West end of Korinth Canal - Greece AJ. Rogan, SJ. Rogan, G. Papageorgiou, C. Solomonidis Rogan Associates, Consulting Engineers - Architects Email: [email protected] Abstract The scope of this paper is the presentation of all the necessary stages for the creation of a marina in a maritime European country, such as Greece, from the starting point of its scheduling as a node in the National network of leisure harbours, to it's final design phase. The whole procedure is demonstrated with the example of a new 700 berthing places Marina at Loutraki, a well-known resort at the northwestern end of the Gulf of Korinthos. A number of parameters are examined, such as the hinterland, which the marina will serve as well as the existing transport accesses. A thorough analysis of the existing and future demand for berthing places in leisure harbours, both for the whole of Greece, and more specifically for the Attica and Argolis areas is performed, setting as time horizon for the estimates the year 2014. The demand is compared to the existing capacity in berthing places, thus establishing the necessity of creating new marinas in the area. The required capacity of the marina is then calculated in terms of places in the sea and on dry, in relation to the local demand, but subject to geographical and other constraints. The main goals of the Master Plan of the marina are outlined and the design proposal is presented with emphasis given on the architectural concept which was followed. -
Civil Affairs Handbook on Greece
Preliminary Draft CIVIL AFFAIRS HANDBOOK on GREECE feQfiJtion Thirteen on fcSSLJC HJI4LTH 4ND S 4 N 1 T £ T I 0 N THE MILITARY GOVERNMENT DIVISION OFFICE OF THE PROVOST MARSHAL GENERAL Preliminary Draft INTRODUCTION Purposes of the Civil Affairs Handbook. International Law places upon an occupying power the obligation and responsibility for establishing government and maintaining civil order in the areas occupied. The basic purposes of civil affairs officers are thus (l) to as- sist the Commanding General of the combat units by quickly establishing those orderly conditions which will contribute most effectively to the conduct of military operations, (2) to reduce to a minimum the human suffering and the material damage resulting from disorder and (3) to create the conditions which will make it possible for civilian agencies to function effectively. The preparation of Civil Affairs Handbooks is a part of the effort of the War Department to carry out this obligation as efficiently and humanely as is possible. The Handbooks do not deal with planning or policy. They are rather ready reference source books of the basic factual information needed for planning and policy making. Public Health and Sanitation in Greece. As a result of the various occupations, Greece presents some extremely difficult problems in health and sanitation. The material in this section was largely prepared by the MILBANK MEMORIAL FUND and the MEDICAL INTELLI- GENCE BRANCH OF THE OFFICE OF THE SURGEON GENERAL. If additional data on current conditions can be obtained, it willJse incorporated in the final draft of the handbook for Greece as a whole. -
Pronunciation Booklet
PRONUNCIATION BOOKLET Word Phonetic pronunciation (mine) What Meaning (if known) Actual sacred space or enclosure attached to a temple of ab-are-ton Abaton Asclepius where those wanting to be cured slept Acayo a-key-owe Fictional character - a Spartan soldier Greek name meaning out of step/ill-timed Acropolis ac-rop-o-liss Actual fortified part of a city, normally built on a hill Actual ancient Greek King of Athens, father of the hero Aegeus ee-gee-us Greek name meaning protection Theseus Actual Ancient Greek name given to the public open space Agora ag-or-are Greek name meaning gathering place or assembly used for markets Agrias ag-ree-us Fictional character - Alexis' father, and King of Trachis Greek name of unknown meaning Aigai ay-gay Greek name meaning place of goats Actual ancient first capital of Macedonia, now called Vergina Fictional character - Princess of Thermopylae, daughter of Greek name meaning helper and defender (can be male Alexis al-ex-us Agrias & Melina or female name) Amazonomachiai am-a-zon-e-mack-ee Plural of the battle of the Amazonomachy Portrayal of a mythical battle between the Amazons and Amazonomachy am-a-zon-e-mack-ee Amazon battle Ancient Greeks Amphissa am-f-iss-are Actual ancient city in Phocis, now known as Amfissa Greek name meaning surround Actual Ancient Greek jar or jug with two handles and a Amphora am-for-a From Greek word amphoreus meaning to bear narrow neck (singular) Amphorae am-for-i Actual plural of the Ancient Greek jars or jugs called amphora Amyntas arm-in-t-us Actual King of Macedonia Amyntas -
Facies and Environments
The Geological Society of America Digital Map and Chart Series 17 2014 Notes on Maps of the Callovian and Tithonian Paleogeography of the Caribbean, Atlantic, and Tethyan Realms: Facies and Environments Caroline Wilhem* Institute of Earth Sciences, Faculty of Geosciences and Environments, University of Lausanne, Geopolis, 1015 Lausanne, Switzerland A. NOTE detailed in Hochard (2008). The Mesozoic reconstructions were partly presented and discussed in Flores (2009) for the Pacifi c The Callovian-Tithonian period of the Atlantic and its and Caribbean realms; in Stampfl i and Borel (2002, 2004) for connected oceans was tectonically intense. It was mainly the Atlantic realm; and in Stampfl i (2000, 2001), Stampfl i et al. marked by the opening of the Caribbean Seaway, the pursu- (2001a, 2001b, 2002, 2003), Stampfl i and Borel (2004), Stamp- ance of the Atlantic and Tethyan spreading, as well as the fl i and Kozur (2006), Bagheri and Stampfl i (2008), Bonev and North Atlantic rifting. This period is characterized by a gen- Stampfl i (2008, 2011), Moix et al. (2008), and Stampfl i and eral deepening of the oceans. At the same time, the sedimen- Hochard (2009) for the Tethyan realm. tation passed from largely siliceous to carbonaceous deposits Key localities and linked references used for the elabora- within the Tethyan realm. tion of the Callovian and Tithonian maps are geographically Callovian and Tithonian facies and environments were com- presented in section B. The Dercourt et al. (1993, 2000) atlases piled and added to a plate tectonics model that constrains their were used as general references. The characteristics and devel- arrangements. -
Offshore Marine Actinopterygian Assemblages from the Maastrichtian–Paleogene of the Pindos Unit in Eurytania, Greece
Offshore marine actinopterygian assemblages from the Maastrichtian–Paleogene of the Pindos Unit in Eurytania, Greece Thodoris Argyriou1 and Donald Davesne2,3 1 UMR 7207 (MNHN—Sorbonne Université—CNRS) Centre de Recherche en Paléontologie, Museum National d’Histoire naturelle, Paris, France 2 Department of Earth Sciences, University of Oxford, Oxford, UK 3 UMR 7205 (MNHN—Sorbonne Université—CNRS—EPHE), Institut de Systématique, Évolution, Biodiversité, Museum National d’Histoire naturelle, Paris, France ABSTRACT The fossil record of marine ray-finned fishes (Actinopterygii) from the time interval surrounding the Cretaceous–Paleogene (K–Pg) extinction is scarce at a global scale, hampering our understanding of the impact, patterns and processes of extinction and recovery in the marine realm, and its role in the evolution of modern marine ichthyofaunas. Recent fieldwork in the K–Pg interval of the Pindos Unit in Eurytania, continental Greece, shed new light on forgotten fossil assemblages and allowed for the collection of a diverse, but fragmentary sample of actinopterygians from both late Maastrichtian and Paleocene rocks. Late Maastrichtian assemblages are dominated by Aulopiformes (†Ichthyotringidae, †Enchodontidae), while †Dercetidae (also Aulopiformes), elopomorphs and additional, unidentified teleosts form minor components. Paleocene fossils include a clupeid, a stomiiform and some unidentified teleost remains. This study expands the poor record of body fossils from this critical time interval, especially for smaller sized taxa, while providing a rare, paleogeographically constrained, qualitative glimpse of open-water Tethyan ecosystems from both before and after the extinction event. Faunal similarities Submitted 21 September 2020 Accepted 9 December 2020 between the Maastrichtian of Eurytania and older Late Cretaceous faunas reveal a Published 20 January 2021 higher taxonomic continuum in offshore actinopterygian faunas and ecosystems Corresponding author spanning the entire Late Cretaceous of the Tethys. -
Morphotectonic Analysis Along the Northern Margin of Samos Island, Related to the Seismic Activity of October 2020, Aegean Sea, Greece
geosciences Article Morphotectonic Analysis along the Northern Margin of Samos Island, Related to the Seismic Activity of October 2020, Aegean Sea, Greece Paraskevi Nomikou 1,* , Dimitris Evangelidis 2, Dimitrios Papanikolaou 1, Danai Lampridou 1, Dimitris Litsas 2, Yannis Tsaparas 2 and Ilias Koliopanos 2 1 Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupoli Zografou, 15784 Athens, Greece; [email protected] (D.P.); [email protected] (D.L.) 2 Hellenic Navy Hydrographic Service, Mesogeion 229, TGN 1040 Cholargos, Greece; [email protected] (D.E.); [email protected] (D.L.); [email protected] (Y.T.); [email protected] (I.K.) * Correspondence: [email protected] Abstract: On 30 October 2020, a strong earthquake of magnitude 7.0 occurred north of Samos Island at the Eastern Aegean Sea, whose earthquake mechanism corresponds to an E-W normal fault dipping to the north. During the aftershock period in December 2020, a hydrographic survey off the northern coastal margin of Samos Island was conducted onboard R/V NAFTILOS. The result was a detailed bathymetric map with 15 m grid interval and 50 m isobaths and a morphological slope map. The morphotectonic analysis showed the E-W fault zone running along the coastal zone with 30–50◦ of Citation: Nomikou, P.; Evangelidis, slope, forming a half-graben structure. Numerous landslides and canyons trending N-S, transversal D.; Papanikolaou, D.; Lampridou, D.; Litsas, D.; Tsaparas, Y.; Koliopanos, I. to the main direction of the Samos coastline, are observed between 600 and 100 m water depth. The Morphotectonic Analysis along the ENE-WSW oriented western Samos coastline forms the SE margin of the neighboring deeper Ikaria Northern Margin of Samos Island, Basin.