DOCSLIB.ORG

Regional Geology Reviews

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

Regional Geology Reviews Series Editors Roland Oberh€ansli Maarten de Wit Francois M. Roure For further volumes: http://www.springer.com/series/8643 . Ja´nos Haas Editor Ja´nos Haas • Ge´za Ha´mor{ •A´ ron Ja´mbor • Sa´ndor Kova´cs{ • Andra´s Nagymarosy • Tibor Szederke´nyi Geology of Hungary Editor Ja´nos Haas Eotv€ os€ Lora´nd University Geological, Geophysical and Space Science Research Group Budapest Hungary ISBN 978-3-642-21909-2 ISBN 978-3-642-21910-8 (eBook) DOI 10.1007/978-3-642-21910-8 Springer Heidelberg New York Dordrecht London Library of Congress Control Number: 2012936971 # Springer-Verlag Berlin Heidelberg 2012 This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed. Exempted from this legal reservation are brief excerpts in connection with reviews or scholarly analysis or material supplied specifically for the purpose of being entered and executed on a computer system, for exclusive use by the purchaser of the work. Duplication of this publication or parts thereof is permitted only under the provisions of the Copyright Law of the Publisher’s location, in its current version, and permission for use must always be obtained from Springer. Permissions for use may be obtained through RightsLink at the Copyright Clearance Center. Violations are liable to prosecution under the respective Copyright Law. The use of general descriptive names, registered names, trademarks, service marks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use. While the advice and information in this book are believed to be true and accurate at the date of publication, neither the authors nor the editors nor the publisher can accept any legal responsibility for any errors or omissions that may be made. The publisher makes no warranty, express or implied, with respect to the material contained herein. Printed on acid-free paper Springer is part of Springer Science+Business Media (www.springer.com) Contents Introduction ......................................... ix Ja´nos Haas History of Geologic Research ............................ xi Ja´nos Haas Geography and Outline of Geologic Framework .............. xvii Ja´nos Haas Structural Units and Main Stages of the Structural Evolution . xxi Ja´nos Haas 1 Geology and History of Evolution of the ALCAPA Mega-Unit 1 1.1 Austroalpine Units . ........................... 1 Tibor Szederke´nyi 1.1.1 Lower Austroalpine Nappe System ............. 1 1.1.2 Upper Austroalpine Nappe System . 6 1.1.3 Penninic Unit . 6 1.2 Central and Internal Western Carpathian Units . 9 Sa´ndor Kova´cs and Ja´nos Haas 1.2.1 Veporic Unit . ........................... 9 1.2.2 Zemple´nic Unit . 10 1.2.3 Internal Western Carpathian Nappe-Stack ........ 11 1.2.3.1 Bo´dvaNappe...................... 12 1.2.3.2 Torna Nappe ...................... 14 1.2.3.3 Telekesoldal Nappe ................. 15 1.2.3.4 Szo˝lo˝sardo´ Unit . ................. 16 1.2.3.5 Silica–Aggtelek Nappe . .............. 17 1.3 Pelso Composite Unit . ......................... 21 Ja´nos Haas and Sa´ndor Kova´cs 1.3.1 Transdanubian Range Unit ................... 21 1.3.1.1 Variscan Evolutionary Cycle ........... 22 1.3.1.2 Alpine Evolutionary Cycle . .......... 25 1.3.2 Mid-Transdanubian Unit . 56 1.3.2.1 South Karavank Unit . ............... 56 1.3.2.2 Julian–Savinja Unit . ................ 57 1.3.2.3 South Zala and Kalnik Units ........... 57 v vi Contents 1.3.3 Bukk€ Composite Unit . .................... 58 1.3.3.1 BukkUnitss......................€ 59 1.3.3.2 Szendro˝ Unit . 73 1.3.3.3 Uppony Unit ...................... 76 1.4 Accretion of the ALCAPA Mega-Unit . 81 Andra´s Nagymarosy 1.4.1 Paratethys Evolution and Its Consequences for the Palaeogene–Neogene Chronostratigraphic Framework .............................. 81 1.4.2 Hungarian Palaeogene Basin .................. 83 1.4.2.1 General Trends of Evolution and Palaeogeography ................... 84 1.4.2.2 Eocene . ........................ 84 1.4.2.3 Oligocene ......................... 91 1.4.2.4 Late Egerian-Eggenburgian-Earliest Ottnangian . 95 1.4.2.5 Igneous Activity During the Paleogene- Eggenburgian . ................... 99 2 Geology and History of Evolution of the Tisza Mega-Unit .... 103 2.1 Pre-Variscan to Variscan Evolution . 103 Tibor Szederke´nyi 2.1.1 Crystalline Complexes . 104 2.1.2 Lithostratigraphy of the Tectono-stratigraphic Units and Tectono-metamorphic Evolution ............ 105 2.1.2.1 Slavonia–Drava Unit ................. 105 2.1.2.2 Kunsa´g Unit . ................. 106 2.1.2.3 Be´ke´s Unit ........................ 108 2.1.2.4 Outliers . ...................... 109 2.1.3 Protoliths and Polymetamorphic Deformations . 111 2.1.4 Tectono-metamorphic Events . 112 2.2 Post-Variscan Evolution . ....................... 113 Tibor Szederke´nyi 2.2.1 Late Carboniferous–Permian Continental Formations ............................... 113 2.2.2 Late Carboniferous–Permian Cover of the Slavonia–Drava Unit . 113 2.2.3 Permian Cover of the Kunsa´g Unit . 117 2.2.4 Permian Cover of the Be´ke´s–Codru Unit . ....... 118 2.3 Alpine Evolution . ............................. 118 Ja´nos Haas 2.3.1 Fluvial Sedimentation in the Early Triassic . 119 2.3.2 Transgression in the Anisian – Siliciclastic Ramp Sedimentation . 120 Contents vii 2.3.3 Shallow Carbonate Ramp Evolution in the Middle Triassic . 122 2.3.4 Differentiation of the Facies Zones of the Tisza Mega-Unit . .............................. 124 2.3.5 Mecsek Facies Unit ........................ 124 2.3.5.1 Intensification of Continental Input in the Late Triassic . ................... 124 2.3.5.2 Coastal Swamp and Shallow Marine Siliciclastic Ramp in the Early Liassic . 125 2.3.5.3 Pelagic Marl Facies in the Middle Liassic to Early Dogger Interval . ........... 127 2.3.5.4 Siliceous and Carbonate Deep-Sea Facies in the Late Dogger to Malm Interval ..... 128 2.3.5.5 Basaltic Magmatism in the Early Cretaceous . 129 2.3.5.6 Tectogenic Episodes and Flexural Basins in the Late Cretaceous . 130 2.3.5.7 Palaeogene Flysch Deposition in the “Szolnok Flysch Trough” . 131 Andra´s Nagymarosy 2.3.5.8 Continental Palaeogene Basin in the Mecsek . 137 Andra´s Nagymarosy 2.3.6 Villa´ny–Bihor Facies Unit . 137 2.3.6.1 Coastal–Terrestrial Sedimentation in the Late Triassic . ............... 137 2.3.6.2 Discontinuous Shallow Marine Deposition in the Jurassic . 138 2.3.6.3 Carbonate Platform Development in the Early–Middle Cretaceous ........ 138 2.3.6.4 Pelagic Basin Formation at the End of the Mid-Cretaceous . 140 2.3.6.5 Senonian Basin Evolution . ........... 141 2.3.7 Be´ke´s–Codru Facies Unit ................... 142 2.4 Regional Geological Cross-sections .................. 142 Ja´nos Haas and Ge´za Ha´mor 3 Genesis and Evolution of the Pannonian Basin ............ 149 Andra´s Nagymarosy and Ge´za Ha´mor 3.1 Concept of the Pannonian Basin . .................... 149 3.1.1 Subsidence History and Tectonics of the Pannonian Basin . 151 3.1.2 Stratigraphic Considerations . 155 3.2 Early Miocene . 156 3.2.1 Post-Eggenburgian Early Miocene Formations in the ALCAPA Mega-Unit . ................ 156 3.2.2 Ottnangian Formations . ................ 159 3.2.2.1 Continental Formations, North Hungary . 159 viii Contents 3.2.2.2 Brackish to Marine Formations, North Hungary . 159 3.2.2.3 Marine Formations, Va´rpalota Basin . 160 3.2.3 Karpatian Formations . ..................... 161 3.2.3.1 Northwest Hungary .................. 161 3.2.3.2 Northeast Hungary .................. 162 3.2.4 Early Miocene Formations in the Tisza Mega-Unit . 163 3.2.5 Igneous Formations in the Early Miocene ........ 166 3.3 Middle Miocene . ............................... 168 3.3.1 Formations of Large Lateral Extension . ..... 170 3.3.1.1 Badenian Formations ................ 171 3.3.1.2 Sarmatian Formations . ............ 172 3.3.2 Regional Units . ........................... 173 3.3.2.1 Sopron Mountains . ................ 173 3.3.2.2 Little Hungarian Plain . ........... 174 3.3.2.3 Transdanubian Range . ............ 174 3.3.2.4 Northern Hungary (North Hungarian Range) . 176 3.3.2.5 Mecsek Mountains and Southeast Hungary . 177 3.3.2.6 Zala and Drava Basins . .............. 180 3.3.2.7 Basins in the Great Hungarian Plain ..... 181 3.3.3 Igneous Activity in the Middle Miocene . ..... 182 3.4 Late Miocene and Pliocene ........................ 186 3.4.1 Late Miocene or Pannonian . ................ 186 3.4.1.1 Marginal Sequences . 191 3.4.1.2 Sequences of the Deep Basins . 194 3.4.2 Pliocene . ................................ 197 3.4.3 Volcanic Activity in the Late Miocene-Pliocene .... 198 4 Quaternary Evolution ............................... 201 A´ ron Ja´mbor 4.1 Significance of the Quaternary Formations . 201 4.2 History of Quaternary Research in Hungary ............ 202 4.3 Major Characteristics of the Quaternary Depositional Areas .............................. 204 4.4 Volcanism . .................................. 211 4.5 Tectonics . 211 4.6 Present-Day Soils ............................... 211 4.7 History of Evolution ............................. 212 References ..........................................
Recommended publications
  • Analysis of Sub-Daily Precipitation for the Pannex Region

    Analysis of Sub-Daily Precipitation for the Pannex Region

    atmosphere Article Analysis of Sub-Daily Precipitation for the PannEx Region Monika Lakatos 1,*, Olivér Szentes 1, Ksenija Cindri´cKalin 2, Irena Nimac 2, Katja Kozjek 3, Sorin Cheval 4 , 4 4 5,6 5 7 7 Alexandru Dumitrescu , Adrian Iras, oc , Petr Stepanek , Aleš Farda , Peter Kajaba , Katarína Mikulová , Dragan Mihic 8, Predrag Petrovic 8, Barbara Chimani 9 and David Pritchard 10 1 Hungarian Meteorological Service, 1024 Budapest, Hungary; [email protected] 2 Croatian Meteorological and Hydrological Service, 10000 Zagreb, Croatia; [email protected] (K.C.K.); [email protected] (I.N.) 3 Slovenian Environment Agency, 1000 Ljubljana, Slovenia; [email protected] 4 National Meteorological Administration, 013686 Bucharest, Romania; [email protected] (S.C.); [email protected] (A.D.); [email protected] (A.I.) 5 Global Change Research Institute, Czech Academy of Sciences, 603 00 Brno, Czech Republic; [email protected] (P.S.); [email protected] (A.F.) 6 Czech Hydrometeorological Institute, 616 67 Brno, Czech Republic 7 Slovak Hydrometeorological Institute, 833 15 Bratislava, Slovakia; [email protected] (P.K.); [email protected] (K.M.) 8 Republic Hydrometeorological Service of Serbia, 11030 Beograd, Serbia; [email protected] (D.M.); [email protected] (P.P.) 9 Zentralanstalt für Meteorologie und Geodynamik, 1190 Wien, Austria; [email protected] 10 School of Engineering, Newcastle University, Newcastle upon Tyne NE1 7RU, UK; [email protected] * Correspondence: [email protected]; Tel.: +36-1-346-4725 Citation: Lakatos, M.; Szentes, O.; Abstract: The PannEx is a GEWEX-initiated, community driven research network in the Pannonian Cindri´cKalin, K.; Nimac, I.; Kozjek, Basin.
  • Natural Radioactive Element Content of the Old Crystalline Rocks in Southern Transdanubia (Sw Hungary)

    Natural Radioactive Element Content of the Old Crystalline Rocks in Southern Transdanubia (Sw Hungary)

    Acta Mineralogica-Petrographica, Szeged, XL, 121-138, 1999 NATURAL RADIOACTIVE ELEMENT CONTENT OF THE OLD CRYSTALLINE ROCKS IN SOUTHERN TRANSDANUBIA (SW HUNGARY) E. PÁL MOLNÁR*, I. VADOS**, I. GERZSON**, B. KÓBOR* •Department of Mineralogy, Geochemistry and Pétrology, Attila József University "Mecsekérc Environment Protection Co. ABSTRACT On the basis of systématisation of several thousand radioactive element content analyses made in laboratories since the 50's, U and Th content of old granitoid rocks of Southern Transdanubia proved to be much higher than the average U and Th content of granitoids in the world. This value of rocks from areas west of Mecsek Mountains as well as near Szalatnak village and Pecs city is twice higher than the world average. Areas west of the Mecsek Mountains show higher U and lower Th contents than areas east of these mountains. Uranium accumulation is higher in aplites and hydrothermal formations than in granites. The western and eastern granites are less and highly sensitive to leaching, respectively. The intensive U migration resulted in significant U accumulation in young sediments in some places. INTRODUCTION Study of natural radioactive element (U /Ra1, Th, K) content of the rocks in Hungary was performed by the Mecseki Ércbányászati Vállalat (Mecsek Ore Mining Company) until 1990, when uranium exploration was stopped in Hungary. Aim of the analyses was to research U sources, therefore, rocks supposed to contain perspective U accumulation were mainly studied. The aim of this paper is to elaborate many thousands radiological data of granitoid rocks, gneisses and amphibolite-like metamorphic rocks coming from Southern Transdanubia (south of the Szekszárd-Kaposvár-Kutas line to the state boundary, and east of the Kutas-Csokonyavisonta-Barcs line to the Danube).
  • S. Transdanubia Action Plan, by Pécs-Baranya, HU

    S. Transdanubia Action Plan, by Pécs-Baranya, HU

    Cultural and Creative Industries (CCIs) contribution to Cultural and Creative Tourism (CCT) in Europe Action Plan for South Transdanubia, Hungary ChamMap of partnerber of are Commercea / Partner info and Industry of Pécs- Baranya May 2021 Cultural and Creative Industries contribution to Cultural and Creative Tourism in Europe _________________________ © Cult-CreaTE Project Partnership and Chamber of Commerce and Industry of Pécs-Baranya, Hungary This publication may be reproduced in whole or in part and in any form for educational or non-profit purposes without special permission from the copyright holder, provided acknowledgement of the source is made. No use of this publication may be made for resale or for any other commercial purpose whatsoever without prior permission in writing from the Cult-CreaTE Project Management and Coordination Unit and the respective partner: Chamber of Commerce and Industry of Pécs-Baranya Citation: Interreg Europe Project Cult-CreaTE Action Plan Chamber of Commerce and Industry of Pécs- Baranya, Hungary The Cult-CreaTE Project Communications unit would appreciate receiving a copy of any publication that uses this action plan as a source, sent to e-mail: [email protected] Disclaimer This document has been prepared with the financial support of Interreg Europe 2014-2020 interregional cooperation programme. The content of the document is the sole responsibility of Chamber of Commerce and Industry of Pécs-Baranya and in no way reflect the views of the Cult-CreaTE partnership, the European Union institutions, nor the Managing Authority of the Programme. Any reliance or action taken based on the information, materials and techniques described within this document are the responsibility of the user.
  • House in Carpathians1

    House in Carpathians1

    Ethnologia Polona, 2014, 35, s. 25-77 Ethnologia Polona, vol. 35: 2014, 25 – 77 PL ISSN 0137 - 4079 HOUSE IN CARPATHIANS1 JIŘÍ LANGER AND HELENA BOČKOVÁ ROŽNOV POD RADHOŠTĚM and BRNO, CZECH REPUBLIC INTRODUCTION The problem of the folk culture has always been a great topic for the ethnographers. Since the last century an attention of many explorers from many countries has focused on it. A common interest in finding the answers to the questions of the causes of the specifications of their cultural manifestation in the Carpathians connected them. They seemed to be different from firmly rooted ideas about the typical features of individual nations. Anachronisms provoke everybody who was looking for the originalities of their own national or Slavonic culture. They served to the creating of romantic fanta- sies about the culture in the mountains surviving into the period in which European nations formed. From the point of view of a historian this culture is considered to be very young, having been created before our eyes. Our generation could still study it by the very watching. We know it from autopsy. It differed from neighbouring lower situated areas with the early evolution forms, transferring of their phenomena for long distances, strong penetration and co operation with neighbouring social environments and ethnic heterogeneity. This all enabled people in the mountains to survive even in the worst climatic and social conditions. The principles of the folk culture being thought to be specific for the whole Carpathians touching vast areas of Europe connected fairly different forms of the way of the life from the Balkan to White Russia and from the river Morava (CZ) as far as the coast of the Black Sea.
  • Arsenic- Water in Vojvodina 2010..Pdf

    Arsenic- Water in Vojvodina 2010..Pdf

    This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Environmental Research 111 (2011) 315–318 Contents lists available at ScienceDirect Environmental Research journal homepage: www.elsevier.com/locate/envres Reports from the Field Arsenic occurrence in drinking water supply systems in ten municipalities in Vojvodina Region, Serbia$ Dragana Jovanovic a,n, Branko Jakovljevic´ b, Zorica Rasicˇ ´-Milutinovic´ c, Katarina Paunovic´ b, Gordana Pekovic´ c, Tanja Knezevic´ a a Institute of Public Health of Serbia ‘‘Dr Milan Jovanovic Batut’’, Dr Subotica 5, Belgrade, Serbia b Institute of Hygiene and Medical Ecology, School of Medicine, Belgrade, Serbia c Department of Endocrinology, University Hospital Zemun, Belgrade, Serbia article info abstract Article history: Vojvodina, a northern region of Serbia, belongs to the Pannonian Basin, whose aquifers contain high Received 9 August 2010 concentrations of arsenic. This study represents arsenic levels in drinking water in ten municipalities in Received in revised form Serbia. Around 63% of all water samples exceeded Serbian and European standards for arsenic in drinking 15 November 2010 water.
  • Geological Analysis of the Kis-Alföld Based on Satellite-Photos L

    Geological Analysis of the Kis-Alföld Based on Satellite-Photos L

    GEOLOGICAL ANALYSIS OF THE KIS-ALFÖLD BASED ON SATELLITE-PHOTOS L. JAKUCS The research introduced only in its main results in this study is a part óf a five-year scientificic program which was carried out by the Institute of Physical Geography of Attila József University of Sciences within the frame of the theme "Satellite Research of Natural Resources of Hungary" at the commission of the Central Institute of Geology. The members of the team lead by dr. prof László Jakucs are as follows: reader dr. Mihály Andó, senior lecturer dr. József Fehér, Senior lecturer dr. Mrs Ferenc Kevei, lecturer candidate dr. Gábor Mezősi and senior lec- turer dr. Imre Tóth. The available LANDSAT longdistance survaillances show that defining the Kis-Alföld as a physical geographical region is a simple task only with a cursory examination because its margins protrude deeply into the wide valley-plains of the bordering Carpathian and Transdanubian rivers. On the satellitephotos of the LANDSAT-satellites (I; II; III.) these marginal regions, which are quastionable and subjectively treatable, too, stand out clearly and this fact helps making a more exact genetic limitation. Yet during our work of interpretation we overstepped the actual borders of the Kis-Alfpld for we saw comparation standing out at all points which says that the regionmargins drawn on geomorphological or soilgeographycal basis are not at the same time the margins of the natural factors determining the development of a region. For quality and quantityration óf past and recens hydro- logical, climatological, sedimentational and structural many times determinant) factors determining and directing the geographycal and sedimentological develop- ment of the Kis-Alföld are controlled far from the frontier, mainly from the direction of the Alps and the Carpathians.
  • Microtectonic Measurements and Interpretation of the Mesozoic Formations in the Villány Hills and Görcsöny–Máriakéménd Ridge, Hungary

    Microtectonic Measurements and Interpretation of the Mesozoic Formations in the Villány Hills and Görcsöny–Máriakéménd Ridge, Hungary

    Central European Geology, Vol. 53/1, pp. 21–42 (2010) DOI: 10.1556/CEuGeol.53.2010.1.2 Microtectonic measurements and interpretation of the Mesozoic formations in the Villány Hills and Görcsöny–Máriakéménd Ridge, Hungary Attila Petrik Department of Regional Geology Eötvös Lóránd University, Budapest Within the framework of a National Research Fund project, different types of scientific investigations were carried out with the aim of a comprehensive paleogeographic reconstruction of the Tisza structural unit. As part of this project microtectonic measurements in the area of the Villány Hills and Görcsöny–Máriakéménd Ridge were carried out. Several publications have already appeared concerning the structural development of the Mecsek–Villány area (Csontos and Bergerat 1988, 1993; Benkovics 1997; Csontos et al. 2002), but in these the Villány Hills and their surroundings played a secondary role compared to the Mecsek Mountains. The goal of the present study was to establish the limits of the structural phases and determine their relative and absolute ages. An important issue has been to clarify to what degree the suggested events of structural deformation could be integrated into regional geologic processes. The tectonic conditions of the area of interest were studied through description and analysis of structural elements of 12 investigated quarries within it. Calculated stress field data were also analyzed. Seven quarries in the Villány Hills, five in the Görcsöny–Máriakéménd area, the data of over 650 striae, 550 joints, various ductile deformation elements (folds, flexures) as well as stylolites, were recorded. Integrating these structural elements into the regional geologic processes was of significant importance. Introduction and geologic background The Tisza Unit (Fig.
  • Recent Aspects of the Development of the Hungarian Settlement Network Within the European Structure

    Recent Aspects of the Development of the Hungarian Settlement Network Within the European Structure

    RECENT ASPECTS OF THE DEVELOPMENT OF THE HUNGARIAN SETTLEMENT NETWORK WITHIN THE EUROPEAN STRUCTURE After Settlement History and Theory Investigations hy Dr. Jeno I1Iajor R. NYITR.4..Y Department of Town Planning, Technical University of Budapest, H-1521 Received: November 10. 1989 Presented by: Prof. Dr. Tam~ls }!egyesi Ahstract Due to investigations by Dr. J cno Major on settlement history and theory, main trends of Hungarian urbanization and settlement network development offer an insight into the de­ velopment of European settlement network. His partly archival - research results underly­ ing settlement science methodology are without precedence. It is attempted to fit development aspects of the Hungarian settlement network to the new regional structures of the to-be Unit­ ed States of Europe. A survey is given of the rapid urbanization process in Hungary after the Mongol invasion, of periods of mediaeval urbanization surges, as well as of the settlement net­ work of industrializing-capitalizing Hungary. Inter-war settlement development, and urbanization surge after World War II point to he intensity of relations between town aud country. Dr. Jeno Major has published his study on thc bcginnings of thc dcyelop­ mcnt of Hungarian towns and settlement net,\'ork* with the intcntion to soon report on his latest findings. His available manuscripts probabilize this intention. But his unforesecn decease interrupted the puhlication of his recognitions from the examination of 11th-12th-century markets and "mar­ ketplaces" . His theoretical statements on these factors to he determinant permit to disclose regions of settlement groups functionally coherent with the market­ places, as well as their structural features.
  • Preliminary Report on the Research of Early Holocene Period in the Nwpart of Great Hungarian Plain KERTÉSZ Róbert Damjanich János Múzeum, Szolnok

    Preliminary Report on the Research of Early Holocene Period in the Nwpart of Great Hungarian Plain KERTÉSZ Róbert Damjanich János Múzeum, Szolnok

    Fol. Hist.-nat. Mus. Matr., 16: 29-44, 1991 Preliminary report on the research of Early Holocene period in the NWpart of Great Hungarian Plain KERTÉSZ Róbert Damjanich János Múzeum, Szolnok ABSTRACT? In this paper the author publishes a material collected from the surface during a field survey at Jászberény I, a recently discovered Mesolithic site in the Zagyva basin in the NW part of the Great Hungarian Plain. This microlithic industry belonging to the Late Mesolithic period may throw a new light upon the Early Holocene history of the above-mentioned region. On the basis of the assemblage of typical implements found at Jászberény I the theory of a hiatus between the Paleolithic and the Neolithic in Hungary can be rejected. This site makes us to suppose that even the Great Hungarian Plain participated with equal importance in those processes which took plane in the marginal areas of the Carpathian Basin at the end of the Boreal an at the beginning of the Atlantic period. PREFACE In spite of continuously made intensive topographic surveys in the country the Hungarian Mesolithic could be defined with great difficulties. The emergence of hypotheses often contradictory to each other, the pros and cons on the question of cultural continuity and general uncertainty itself in this matter are due first of all to the fact that this period is represented mostly by less charac­ teristic find assemblages originated usually from surface collection therefore lacking stratigraphie data. The dating of these finds is different also because at certain sites prehistoric pottery was found together with the chipped stone implements.
  • Magyarországi Nevek Magyar-Angol Névmutatója Névmutató Névváltozatok

    Magyarországi Nevek Magyar-Angol Névmutatója Névmutató Névváltozatok

    Bradlo, Szl., 543, C2 Déda, Rom., J4 Feketebalog, Szl., E2 Gutin-hágó, Rom., I3 Istállós-kő, Ma., 959, F2 Szerb., E5 Kurjantó-tó, Ma., E4 Máriafalva, Rom., L4 Nagy (Ferenc)-csatorna, Oláhlápos, Rom., I3 Podgorac, Horv., D5 Ruszkova, Rom., J3 Szászorbó, Rom., I5 Taktaköz, Ma., G2 Újbázos, Rom., G5 Vulkán-hg., Rom., H5-I5 Branyiszkó-hágó, Szl., F1 Dél-bácskai-teraszvidék, Fekete-Cseremos, Ukr., J2 Gutin Tomnatek, Ukr., 2016, Isten dombja, Ma., 338, B4 Kishartyán, Ma., E2 Kurói (Tilicsi)-hágó, Len./Szl., Máriafölde, Rom., F5 Szerb., E5 Oláhszentgyörgy, Rom., J3 Podolin, Szl., F1 Ruszt, Au., B3 Szászrégen, Rom., J4 Talabor, Ukr., I2 Újbezdán, Horv., D5 Vurpód, Rom., J5 Ez a névmutató csak azon Kőlyuk-galya = Kőlyuk-galya forest . 8. A személyneveket nem fordítjuk. geographical names in English- complete them by a generic term Névmutató Brassó, Rom., K5 Szerb., E5 Fekete-Dunajec, Len., E1 J2 Isten széke, Rom., 1380, J3 Kis-havas, Rom., H5 G1 Márianosztra, Ma., D3 Nagyfödémes, Szl., C2 Ólom-hegy, Ma., 174, E4 Podságai-szoros, Rom., I4 Rybotycze, Len., H1 Szászsebes, Rom., I5 Taliándörögd, Ma., C4 Újegyház, Rom., J5 Vysoká, Cs., 1024, D1 Magyarországi nevek magyar-angol névmutatója természetföldrajzi nevek angol Pl.: János-hegy = János Hill . language publications. The main written in lower case: Bükkalja = Oszágnév rövidítések: Len. Lengyelország Brassói-havasok, Rom., K5 Delelő-hegy, 1549, E1 Fekete-h., Ukr., 565, I2 Guvno, BH., 363, B5 Istenmezeje, Ma., F2 Kis-havas, Rom., 1802, H5 Kutina, Horv., B5 Máriapócs, Ma., G3-H3 Nagy-Galla, Ma., 479, D3 Olt, Rom., K4-J5 Podu Calului, Rom., 1439, L5 Rymanów-Zdrój, Len., G1 Szásztyukos, Rom., K5 Tállya, Ma., G2 Újfehértó, Ma., G3 Watkowa, Len., 846, G1 4.
  • Geology of Hungary

    Geology of Hungary

    Regional Geology Reviews Geology of Hungary Alter und Altern: Wirklichkeiten und Deutungen Bearbeitet von Janós Haas 1. Auflage 2012. Buch. xxii, 246 S. Hardcover ISBN 978 3 642 21909 2 Format (B x L): 17,8 x 25,4 cm Weitere Fachgebiete > Geologie, Geographie, Klima, Umwelt > Geologie > Geologie: Allgemeines Zu Leseprobe schnell und portofrei erhältlich bei Die Online-Fachbuchhandlung beck-shop.de ist spezialisiert auf Fachbücher, insbesondere Recht, Steuern und Wirtschaft. Im Sortiment finden Sie alle Medien (Bücher, Zeitschriften, CDs, eBooks, etc.) aller Verlage. Ergänzt wird das Programm durch Services wie Neuerscheinungsdienst oder Zusammenstellungen von Büchern zu Sonderpreisen. Der Shop führt mehr als 8 Millionen Produkte. Contents Introduction ......................................... ix Ja´nos Haas History of Geologic Research ............................ xi Ja´nos Haas Geography and Outline of Geologic Framework .............. xvii Ja´nos Haas Structural Units and Main Stages of the Structural Evolution . xxi Ja´nos Haas 1 Geology and History of Evolution of the ALCAPA Mega-Unit 1 1.1 Austroalpine Units . ........................... 1 Tibor Szederke´nyi 1.1.1 Lower Austroalpine Nappe System ............. 1 1.1.2 Upper Austroalpine Nappe System . 6 1.1.3 Penninic Unit . 6 1.2 Central and Internal Western Carpathian Units . 9 Sa´ndor Kova´cs and Ja´nos Haas 1.2.1 Veporic Unit . ........................... 9 1.2.2 Zemple´nic Unit . 10 1.2.3 Internal Western Carpathian Nappe-Stack ........ 11 1.2.3.1 Bo´dvaNappe...................... 12 1.2.3.2 Torna Nappe ...................... 14 1.2.3.3 Telekesoldal Nappe ................. 15 1.2.3.4 Szo˝lo˝sardo´ Unit . ................. 16 1.2.3.5 Silica–Aggtelek Nappe .
  • EGU2012-403-4, 2012 EGU General Assembly 2012 © Author(S) 2012

    EGU2012-403-4, 2012 EGU General Assembly 2012 © Author(S) 2012

    Geophysical Research Abstracts Vol. 14, EGU2012-403-4, 2012 EGU General Assembly 2012 © Author(s) 2012 Pleistocene alterations of drainage network between the Alps and the Pannonian Basin G. Kovács (1,2) (1) Dept. of Geophysics and Space Sciences, Eötvös Loránd University, Budapest, Hungary ([email protected]), (2) Dept. of Physical Geography, Eötvös Loránd University, Budapest, Hungary The investigated study area is situated in the transition zone between the still uplifting Eastern Alps and the sub- siding Little Hungarian Plain (Joó 1992), bordered by Lafnitz (Lapincs), Répce (Rabnitz) and Rába (Raab) rivers. The contrasting forcing of the regions of differential uplift created a distinctive surface morphology of typically low relief that has a characteristic drainage network pattern as well. Our study is aimed at the reconstruction of the surface evolution by separation of individual geomorphic domains delineated by their geomorphometric characteristics. The hilly area is mostly covered by Miocene sediments. The mesoscale geomorphological units of the study area are influenced by the uplifting metamorphic core complex of Koszeg–Rechnitz Mountains (Tari – Horváth 1995), by the also metamorphic and relatively uplifting Vas Hill as well as by the subsiding grabens. There are two dominant flow directions alternating downstream. Valley segments are often bordered by steep scarps, which were identified by previous research as listric normal faults and grabens. Largely, the investigated area consists of tilted blocks bordered by 30-60 m high and steep, fault-related escarpments as it was demonstrated by the anal- ysis of lignite layers, topographic sections and topographic swath analyses (Kovács et al. 2010, Kovács et al.