D.5.1.1. Identification, Ranking and Characterization of Potential Geothermal Reservoirs
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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. -
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. -
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. -
The Golden Valley – Heaven for Food and Wine Lovers with More Than 30 Wineries and Forts
TRIP IDEAS fact! Romans called this region Vallis Aurea (the Golden Valley) TZ PSZ The Golden Valley – heaven for food and wine lovers With more than 30 wineries and forts. There are numerous legends prov- three wine roads, Požega-Slavonia ing that this has been a region rich in County offers a unique wine and wine since the ancient times. There is a story that Veuve Clicquot, the widow food experience that conquered the 19th century world with her champagne, visited Pleter- nica on her way to Petrograd and was Fertile fields of Slavonia have al- so thrilled by the rolling hills she saw, ways fed the inhabitants of Požega- that upon her return to Champagne she Slavonia County, and as early as the sent vine roots to the people of Pleter- TZ PSZ Roman times it got the name of Val- nica. She was later honoured by having lis Aurea or the Golden Valley. This not only local wines named after her - a Aurelius’ wine, found in what used to be County is a must visit place for the lov- Riesling, which is a graševina coupage, Roman woods. ers of wine, especially graševina. More a white pinot, and local grappa, but also This region, however, is not famous only than 30 wineries and three wine roads a hill. They are called Klikun, the name for its wine – the food is exquisite as (Požega – Pleternica Vineyards, Kutje- similar to the way locals pronounced the well, and you will not stay hungry. Pre- vo Vineyards and Pakrac Vineyards) widow’s last name Clicquot. -
Evolution of the Pannonian Basin and Its Geothermal Resources
Geothermics 53 (2015) 328–352 Contents lists available at ScienceDirect Geothermics jo urnal homepage: www.elsevier.com/locate/geothermics Invited Review Evolution of the Pannonian basin and its geothermal resources a,b a,∗ b,f d e c a F. Horváth , B. Musitz , A. Balázs , A. Végh , A. Uhrin , A. Nádor , B. Koroknai , d a a N. Pap , T. Tóth , G. Wórum a Geomega Ltd., Mester u. 4, H-1095 Budapest, Hungary b Department of Geophysics and Space Sciences, Eötvös Loránd University, Pázmány Péter st. 1/c, H-1117 Budapest, Hungary c Geological and Geophysical Institute of Hungary, Stefánia út 14, H-1442 Budapest, Hungary d Department of Political Geography and Regional Development, University of Pécs, Vasvári Pál u. 4., H-7622 Pécs, Hungary e Eriksfiord AS, Prof. Olav Hanssens vei 7A, Ipark, N-4021 Stavanger, Norway f Utrecht University, Faculty of Geosciences, Utrecht, The Netherlands a r t i c l e i n f o a b s t r a c t Article history: The Pannonian basin is an integral part of the convergence zone between the Eurasian and Nubian plates Received 25 March 2013 characterized by active subductions of oceanic and continental plates, and formation of backarc basins. Accepted 18 July 2014 The first part of this paper presents an overview of the evolution of the Alpine-Mediterranean region in order to understand the large scale crustal and upper mantle processes in and around the Pannonian basin, Keywords: resulting a collage of terranes of Alpine and Adriatic origin. It will be followed by a summary of the history Pannonian basin of sedimentation, volcanism and tectonic activity. -
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
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. -
3. Osijek-Baranja County Basic Information
CONTENTS 1. FOREWORD .........................................................................................................................................................5 Published by 2. REPUBLIC OF CROATIA ........................................................................................................................................7 Osijek - Baranja County 2.1. Basic information..............................................................................................................................................7 For publisher 2.2. Administrative and political structure ........................................................................................................7 Krešimir Bubalo, County prefect 2.3. Geographical position ....................................................................................................................................8 2.4. Economy .............................................................................................................................................................8 Developed by Center for Entrepreneurship Osijek 3. OSIJEK-BARANJA COUNTY ..................................................................................................................................9 3.1. Basic information ............................................................................................................................................10 Project coordination 3.2. Geographical position ...................................................................................................................................10 -
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
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. -
Analysis of the Transdanubian Region of Hungary According to Plant Species Diversity and Floristic Geoelement Categories
FOLIA OECOLOGICA – vol. 44, no. 1 (2017), doi: 10.1515/foecol-2017-0001 Review article Analysis of the Transdanubian region of Hungary according to plant species diversity and floristic geoelement categories Dénes Bartha1*†, Viktor Tiborcz1* *Authors with equal contribution 1Department of Botany and Nature Conservation, Faculty of Forestry, University of West Hungary, H-9400 Sopron, Bajcsy-Zsilinszky 4, Hungary Abstract Bartha, D., Tiborcz, V., 2017. Analysis of the Transdanubian region of Hungary according to plant species diversity and floristic geoelement categories.Folia Oecologica, 44: 1–10. The aim of this study was to describe the proportion of floristic geoelements and plant biodiversity in the macroregions of Transdanubia. The core data source used for the analysis was the database of the Hungar- ian Flora Mapping Programme. The analysed data were summarized in tables and distribution maps. The percentage of continental elements was higher in dry areas, whereas the proportion of circumboreal elements was higher in humid and rainy parts of Transdanubia. According to the climatic zones, the highest value of continental geoelement group occurred in the forest-steppe zone. The plant species diversity and geoele- ments were analysed also on a lower scale, with Transdanubia specified into five macroregions. The highest diversity values were found in the Transdanubian Mountain and West-Transdanubian regions because of the climatic, topographic, and habitat diversity. Keywords Borhidi’s climatic zones, climatic variables, floristic geoelement categories, macroregion, species diversity, Transdanubia Introduction Hungary is influenced by many different environmental In some European countries, floristic assessments conditions which are also reflected in the floristic diver- have already been made based on published flora at- sity. -
Lithofacies Definition Based on Cut-Offs in Indicator Kriging Mapping, Case Study Lower Pontian Reservoir, Sava Depression K
Lithofacies definition based on cut-offs in Indicator Kriging mapping, case study Lower Pontian reservoir, Sava Depression K. Novak Zelenika ORIGINAL SCIENTIFIC PAPER Mapping of the lithofacies is very important for getting insight to sedimentary environments, shapes and boundaries of hydrocarbon reservoirs especially in reservoir characterization. Indicator Kriging technique is most often used for lithofacies mapping. It is based on indicator transformed input data, depending on presence or absence of the certain lithofacies. Indicator transformation of the input data is performed based on cut-offs into values 0 or 1. Turbidites were dominant clastic transport mechanism in the Croatian part of the Pannonian Basin System during the Early Pontian. Most of transported detritus had been eroded in the Eastern Alps and re-deposited several times before the suspended materials entered the Sava Depression. Due to long transport only medium and fine grained sands and silts (Tb - Td Bouma sequences) reached the Sava Depression. When turbiditic currents were not active, typical calm deep water sediment was deposited. It was presented how to use core and log data to define proper cut-offs for describing different lithofacies. Obtained results are probability maps and with a proper cut-offs definition some of them can show turbiditic channel and material transport direction. Key words: lithofacies, turbidites, Indicator Kriging, Upper Miocene, Sava Depression, Croatia 1. INTRODUCTION The Late Pannonian and Early Pontian periods belong to the 2nd transtensional phase.10, when thermal subsidence gen- erally re-opened many depressional areas along the entire Pannonian Basin Sys- tem, created depositional spaces for the accommodation of a huge volume of sandy ma- terial.