DOCSLIB.ORG

Pannonian Basin – Depression Filled by up to 4,500 M Thick Tertiary and Quaternary Formations

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Pannonian Basin – Depression Filled by up to 4,500 M Thick Tertiary and Quaternary Formations NATURAL ANALOGUES IN SERBIA Snežana KomatinaKomatina--PetroviPetrović October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 1. GeologyGeologyofof Serbia Complex geological structure. Satellite assemblage of Balkan and Apennines (Landsat(Landsat--33 images). October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 1. GeologyGeologyofof Serbia Regional geological map of Balkan and Apennines. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 1. GeologyGeologyofof Serbia Geological map of Serbia. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 1. GeologyGeologyofof Serbia Geotectonic/geomorphological/ hydrogeological units: • Dinarides (SW Serbia) and Carphatobalkanides (E. Serbia) - extremely karstified limestones; • Šumadija-Kosovo belt (W.Serbia) – different lithological structure; • Serbian crystalline basement – crystalline schists basement, covered by Tertiary formations; • Pannonian basin – depression filled by up to 4,500 m thick Tertiary and Quaternary formations. GW in Serbian part of the Danube river basin. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 1. GeologyGeologyofof Serbia Types of aquifers: • intensively karstified Mesozoic limestones, characterized by karst springs; • fractured aquifers of Šumadija- Kosovo belt; • aquifers with intergranular porosity in Pannonian basin and other depressions; • alluvial aquifers. Hydrogeological map. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 1. GeologyGeologyofof Serbia Numerous gw springs and different chemical content are result of presence of various deep aquifers. GeoteGeotecctontonicic units of Serbia and mineral water occurencesoccurences.. 1. Dacian Dacianbasi basin;n; 2. Carpat Carpathhoo--balkanidbalkanideses;; 3. SSerboerbo--mamaccedonedoniiaannmasmasss;; 4. Vardar zonzonee;; 5. Dinarides Dinaridesof W.Serbia; 6. Pann Pannonioniananbasi basin.n. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 1. GeologyGeologyofof Serbia HG unit Water Groups Total bodies of water WB and bodies GWB Quaternary Neogene Karst+fract Quaternary Neogene Karst+fractur ured ed Bačka and 510 00 06 Banat Srem, 411 01 07 Mačva, Pos- Tamnava Central 663 03 523 Serbia E. Serbia 341400 324 SW Serbia 006 00 17 W. Serbia 103 00 48 Total1912270 4 1375 Distribution of gw bodies (58 WB and 92 GWB). October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 1. GeologyGeologyofof Serbia Catchment Status Good Bad NA Danube 531 Sava 111 Kolubara 220 Drina 502 V. Morava 720 W. Morava 610 S. Morava 10 0 0 Nišava 520 Lim 801 Ibar 600 Timok 611 Tamiš 010 Tisa 020 Total60166 Present status of gw bodies. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 1. GeologyGeologyofof Serbia GW impact assessment on ecosystems in Serbia has been performed from the two viewpoints: Quantitative impact caused by gw tapping Gw chemical effects on surface water bodies. Conclusion: there are no gw quantitative and chemical effects on ecosystems and such situation can be expected till 2015. However, further investigation is needed. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 2. Vojvodina –Pannonian basin Depth to the basin bottom varies in the wide range, predominantly 800-4,000m. Early Miocene sediments formed under marine conditions (sea water salinity over 300 g/l; in Sarmatian formations within brackish facies – approx. 14 g/l). Tortonian formation is the main formation for oil and gas reservoirs. Pliocene sediments are with several horizons containing thermomineral and mineral water. Numerous fault structures. Geological crosscross--sectionsection DanubeDanube--TisaTisa--Kikinda.Kikinda. 1. crystalline schists, 2-2-6.6. Mesozoic sediments, 77--8.8. marly sandstones, 99--10.10. sandsand-- clayey sediments, 11. fault, 12. borehole. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 2. Vojvodina –Pannonian basin Confined geological structures are present not only in Triassic limestones, but also in MioPliocene deposits. That is why gas reservoirs are numerous. Geological crosscross--sectionsection of a gas reservoir. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 2. Vojvodina –Pannonian basin Methane is predominant gas. Strong methane eruptions have been recorded in Bečej borehole, and water and gas in borehole close to Melenci. No. Borehole T (0C) % volume Gas He (+Ne) locality predomin % volume ant in % volume N2 CO2 O2 CH4 N2 - 64 0.0030 1. Novi Sad 24.0 64.34 1.50 2.50 30.76 CH4 - 53 0.0071 2. Temerin 27.0 43.16 3.00 0.50 53.00 CH4 – 82 0.0077 3. Stari Bečej 37.0 8.37 2.50 7.00 82.00 CH4 – 57 0.0071 4. Ovča 18.0 40.62 0.70 1.10 57.00 N2 - 96 0.0516 5. Omoljica 36.8 96.10 2.00 0.50 - Content of gas in gw of Pannonian basin. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 2. Vojvodina –Pannonian basin Banatski dvor gas field is the first gas storage in Serbia (Lower Pontian sandstones). Geological model of Banatski dvor gas storage. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 2. Vojvodina –Pannonian basin Gw bodies in Bačka and Banat (6(6).). Gw bodies in Srem and Mačva (7). October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 2. Vojvodina –Pannonian basin High mineralization (17.0-29.5 g/l) – wells in Bavaniste, Velika Greda, Ovca, Boka, Torda, etc. and high iodine content (16-25 mg/l) - wells in Kikinda, Backo Petrovo selo, Itebej, Novosadska banja and Maglic. Methane brines have not been investigated, as well as their effects on gw, except close to the wells, but they were probably formed in bays of Miocene sea. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 2. Vojvodina –Pannonian basin Aquifers of Pannonian basin are without CO2, and so - effects to ecosystems are not existent. Slano Kopovo. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 2. Vojvodina –Pannonian basin Regarding seismic activity, Pannonian basin is not so active. That is why fluid migration to the surface can’t be registered. Seismological map of Pannonian basin. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 3. Central Serbia The oldest geological formations are Precambrian schists, covered by Tertiary sediments, up to 4,000m thick. Numerous regional faults are present. Geological crosscross--sectionsection inin the area of KrusKrusevacevac town. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 3. Central Serbia According to oil&gas exploration, confined structures rich in thermomineral water are known. For HC deposits, Sarmatian sandstone and limestone formations are the most important environment. Map of TertiarTertiaryy formation thickness in Pomoravlje. CrossCross--sectionsection for Pomoravlje region. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 3. Central Serbia Oil & gas field Ostrovo and other reservoirs could be interesting for CO2 geological storage. Structural map of Ostrovo reservoir. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 3. Central Serbia Content of minerals in gw of the oil field is over 16 g/l (Jugovo, near Smederevo – 26 g/l). Palanacki kiseljak, Djavola varos and Tularska banja have more than 6 g/l. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 3. Central Serbia Gw at 22 localities are rich in CO2 (> 1000 mg/l). No. Locality T % Gas He (+Ne) (0C) volume predominant % volume in % volume N2 CO2 O2 H2S 1. Sijerinska 67.0 30.50 62.55 7.00 - CO2 – 62 - banja 2. Vranjska banja 68.5 69.04 15.55 14.00 0.45 N2 – 70 0.0031 3. Tulare 19.5 5.91 88.00 6.00 Yes CO2 – 88 0.0031 4. Smed. Palanka 33.0 8.87 78.90 11.00 1.10 CO2 – 80 0.0010 5. Ribarska banja 33.0 91.13 5.40 1.60 1.60 N2 – 91 0.0951 6. Lomnica 14.0 12.82 72.00 - CO2 - 72 0.0004 Content of gas in mineral waters of Serbian crystalline basement. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 3. Central Serbia As a result of deep thermometamorphic processes in rocks, high concentrations of CO2 are present at the top formations of crystalline schists. Gw migrates along faults to the surface, enriching alluvial deposits (W. Morava alluvial plain near Krusevac town, Kubrsnica near Smed. Palanka, etc.), or discharging through numerous springs or into Neogene aquifers. That is why effects of CO2 on ecosystems should be investigated more. October 17-19, 2011 2nd CGS Europe Knowledge Sharing Workshop Maria Laach, Germany Natural Analogues 3. Central Serbia Influence of salty springs and brines to the ecosystems of Central Serbia has not be registered yet. However, water from the Djavolja varos well is very aggressive for plants and animals (pH=3.5). Đavolja varoš. October 17-19, 2011 2nd CGS Europe Knowledge
Load more

Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Urban Climate Monitoring System Suitability for Intra-Urban Thermal Comfort Observations in Novi Sad (Serbia) – with 2014 Ex
    ICUC9 - 9th International Conference on Urban Climate jointly with 12th Symposium on the Urban Environment Urban climate monitoring system suitability for intra-urban thermal comfort observations in Novi Sad (Serbia) – with 2014 examples Dragan D. Milošević Dragan D. Milošević1, Stevan M. Savić1, János Unger2, Tamás Gál2 1 Climatology and Hydrology Research Centre, Faculty of Science, University of Novi Sad, Trg Dositeja Obradovića 3, 21000 Novi Sad, Serbia, [email protected], [email protected] 2 Department of Climatology and Landscape Ecology, University of Szeged, P.O. Box 653, 6701 Szeged, Hungary, [email protected], [email protected] dated: 12 June 2015 Abstract In 2014, urban climate monitoring systems were established in two neighboring European cities (Novi Sad, Serbia; Szeged, Hungary) based on Local Climate Zones (LCZ) classification system, GIS model calculations and fieldwork. Seven built LCZ types in the built-up area of Novi Sad (112 km2) and two LCZ land cover types in nonurban environment in the vicinity of the city were delineated. Urban climate monitoring system in Novi Sad consists of 27 stations equipped with air temperature and relative humidity sensors distributed across all LCZs. This system provided 10-minute measured air temperature and relative humidity data since June 2014. Human comfort observations in different LCZs of the city and its surroundings were investigated for warmest (tropical) and coldest (icy) day in 2014 in Novi Sad. Thermal comfort was assessed with the application of the Physiologically Equivalent Temperature (PET) thermal index. Differences in PET index amongst LCZs can be as high as 10-12 ºC during nocturnal hours when comparing built-up areas of the city (e.
    [Show full text]
  • Pannex, a GEWEX Regional Hydroclimate Project (RHP) Over the Pannonian Basin
    PannEx, A GEWEX Regional Hydroclimate project (RHP) over the Pannonian Basin White Book J anuary 2019 WCRP Publication No.: 03/2019 Bibliographic information This report should be cited as: PannEx White Book, A GEWEX Regional Hydroclimate Project (RHP) over the Pannonian Basin (2019). WCRP Report 3/2019, World Climate Research Programme (WCRP): Geneva, Switzerland, 108 pp. Contact information All enquiries regarding this report should be directed to [email protected] or: World Climate Research Programme c/o World Meteorological Organization 7 bis, Avenue de la Paix Case Postale 2300 CH-1211 Geneva 2 Switzerland Cover image credit Cover page image courtesy of Katarina Stefanović Copyright notice This report is published by the World Climate Research Programme (WCRP) under a Creative Commons Attribution 3.0 IGO License (CC BY 3.0 IGO, www.creativecommons.org/licenses/by/3.0/igo) and thereunder made available for reuse for any purpose, subject to the license’s terms, including proper attribution. Authorship and publisher’s notice PannEx (the Pannonian Basin Experiment) is a Regional Hydroclimate Project (RHP) of the Global Energy and Water Exchanges project (GEWEX) Hydroclimatology Panel (GHP) which aims to achieve a better understanding of the Earth system components and their interactions in the Pannonian Basin. The international efforts in PannEx provide scientific support and involve the international research community in an integrated approach towards identifying and increasing adaptation capacity in the face of climate change in the Pannonian Basin. The WCRP Core Project on Global Energy and Water Exchanges (GEWEX) is an integrated program of research, observations, and science activities that focuses on the atmospheric, terrestrial, radiative, hydrological, coupled processes, and interactions that determine the global and regional hydrological cycle, radiation and energy transitions and their involvement in global changes.
    [Show full text]
  • Potentials of Renewable Energy Sources in the Republic of Serbia
    POTENTIALS OF RENEWABLE ENERGY SOURCES IN THE REPUBLIC OF SERBIA WITH A DETAILED REVIEW OF THE EXPLOITATION OF GEOTHERMAL RESOURCES IN THE AUTONOMOUS PROVINCE OF VOJVODINA Zoran Stipi ć City of Subotica Urban Planning Institute, Trg Republike 16, Subotica, Serbia [email protected] Slobodan Vidovi ć Tehnoproing , Gogoljeva 13,Novi Sad, Serbia, [email protected] Mom čilo Spasojevi ć Faculty of Technical Sciences, Trg D.Obradovi ća 6, Novi Sad, Serbia, [email protected] Abstract: Energy supply is one of the basic issues in the contemporary world’s sustainable development. By adopting the Kyoto Protocol and implementing its mechanisms, it is expected that the use of conventional energy sources shall stabilise and decrease on global level. The European Union’s legal framework, through its appropriate directives, sets very clear objectives for the use of renewable energy sources for member states. Serbia is a country with significant potentials in renewable energy sources, which are, regretfully, underused. Renewable energy source potentials are featured by very favourable indicators in matters of both capacity and distribution. The status is especially favourable in the field of geothermal energy potentials in the Autonomous Province of Vojvodina, situated in the Pannonian Basin, where there are significant sources of this fuel. The paper presents the basic forms and characteristics of renewable energy sources in Serbia and provides an overview of the possibilities for their use. Key words: Renewable energy sources, potentials, capacities, resources, geothermal energy, Serbia, Vojvodina. 1. INTRODUCTION Solving global energy problems implies an interdisciplinary approach and considering the issues from different perspectives. Decreasing overall energy consumption, increasing energy efficiency, modernising the installation, using alternative energy sources and adopting and implementing a number of legal regulations and international covenants are the points of departure in solving this exceptionally complex issue.
    [Show full text]
  • DANUBEPARKS Strategy on Conservation and Navigation
    1 Danube Delta Biosphere Reserve 2 Srebarna Nature Reserve 3 Kalimok-Brushlen Protected Site 4 Rusenski Lom Nature Park 5 Persina Nature Park 6 Djerdap National Park 7 Gornje Podunavlje Special Nature Reserve 8 Kopački rit Nature Park 9 Lonjsko Polje Nature Park 10 Duna-Dráva National Park 11 Duna-Ipoly National Park 12 Dunajské luhy Protected Landscape Area 13 Záhorie Protected Landscape Area 14 Donau-Auen National Park 15 Donauauwald Neuburg Ingolstadt DANUBEPARKS Strategy on ConServation Author: Alexander Zinke, and navigation Zinke Environment Consulting for Central and Eastern Europe, Vienna network of protected areas Acknowledgements This document has been prepared under the ETC-SEE Project Danube Parks Work Package 3 (EU number SEE EoI/A/064/2.3/X), coordinated by the project manager, Georg Frank from the National Park Danube Floodplains in Orth/Austria. The document has been drafted by Alexander Zinke, Zinke Environment Consulting for Central and Eastern Europe, Vienna. Technical advise has kindly been provided by Carl Manzano and Christian Baumgartner (National Park Danube Floodplains), Erika Schneider (WWF Institute for Floodplains Ecology at the Karlsruhe Institute of Technology in Germany), Georg Rast (WWF Germany) and Helmut Habersack (Institute of Water Management, Hydrology and Hydraulic Engineering at the University of Natural Resources and Life Sciences, Vienna). Various comments on the draft document have been provided from experts of the DANUBEPARKS network during and after its ETC-SEE project Task Force meetings and international workshops in January 2010 (Bratislava/SK), November 2010 (Ingolstadt/DE) and May 2011 (Orth/AT). Photographies have been provided by Alexander Zinke and Christian Baumgartner.
    [Show full text]
  • Growth of Pike (Esox Lucius L.) in the Section of the Tisza River at Tiszafüred
    Tiscia (Szeged) Vol. XVIII, pp. 103—112 (1983) GROWTH OF PIKE (ESOX LUCIUS L.) IN THE SECTION OF THE TISZA RIVER AT TISZAFÜRED Á. HARKA Kossuth Lajos Secondary School, Tiszafüred (Received January 25, 1981) Abstract On the basis of measurements on 204 fish specimens the following relationship was established between the standard body length and body weight of pike: lg W = -4.811+2.9301gLc, where W=body weight in g, Lc = body length in mm. The following relation was found between standard body length and total body length: Lt = 5.651+1.110 Lc The determination of the age of pike as well as its body length in the single years was per- formed on the basis of the growth-rings of scales. Growth can be well described by Bertalanffy's equation: 01695 t + 0 5 1,= 1008.6E1 — e- < ' >]x, where l, = standard body length of pike at the age of "t", e = the base of natural logarithm. · Introduction Pike has been a very important fish species especially in the tributaries and stagnant waters of the Tisza, and with the establishing of reservoirs it has become increasingly frequent also in the main branch of the river. Therefore it may be impor- tant from economical aspect to obtain knowledge about its growth which has not been studied to date Hungarian waters. This paper reports on growth studies performed on behalf of the Fisheries Research Institute, Szarvas in the section of the Tisza in the water storage area of Kisköre, and presents at the same time the first information in connection with the growth of pike in Hungary.
    [Show full text]
  • 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.
    [Show full text]
  • Technical Report and Preliminary Economic Assessment for the Piskanja Borate Project, Serbia
    TECHNICAL REPORT AND PRELIMINARY ECONOMIC ASSESSMENT FOR THE PISKANJA BORATE PROJECT, SERBIA REPORT PREPARED IN ACCORDANCE WITH THE GUIDELINES OF NATIONAL INSTRUMENT 43-101 AND ACCOMPANYING DOCUMENTS 43-101.F1 AND 43-101.CP. Prepared For Erin Ventures Inc. Report Prepared by SRK Consulting (UK) Limited UK5932 Effective Date: 1st September 2014 QPs: Dr Mikhail Tsypukov (FIMMM) Dr Mike Armitage C.Eng C.Geol Mark Campodonic MSc, FGS, MAusIMM(CP) SRK Consulting Piskanja– Table of Contents Main Report Table of Contents 1 SUMMARY .......................................................................................................... 1 1.1 Introduction .............................................................................................................................. 1 1.2 Licence Status ......................................................................................................................... 1 1.3 Geology .................................................................................................................................... 2 1.4 Exploration Data ...................................................................................................................... 3 1.5 Mineral Resource Estimate ...................................................................................................... 3 1.6 Preliminary Economic Assessment ......................................................................................... 4 1.7 Interpretation and conclusions ................................................................................................
    [Show full text]
  • Kinematics and Extent of the Piemont–Liguria Basin – Implications for Subduction Processes in the Alps
    Solid Earth, 12, 885–913, 2021 https://doi.org/10.5194/se-12-885-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Kinematics and extent of the Piemont–Liguria Basin – implications for subduction processes in the Alps Eline Le Breton1, Sascha Brune2,3, Kamil Ustaszewski4, Sabin Zahirovic5, Maria Seton5, and R. Dietmar Müller5 1Department of Earth Sciences, Freie Universität Berlin, Berlin, Germany 2Geodynamic Modelling Section, German Research Centre for Geosciences, GFZ Potsdam, Potsdam, Germany 3Institute of Geosciences, University of Potsdam, Potsdam, Germany 4Institute for Geological Sciences, Friedrich-Schiller-Universität Jena, Jena, Germany 5EarthByte Group, School of Geosciences, The University of Sydney, Sydney, NSW 2006, Australia Correspondence: Eline Le Breton ([email protected]) Received: 18 September 2020 – Discussion started: 8 October 2020 Revised: 3 March 2021 – Accepted: 5 March 2021 – Published: 21 April 2021 Abstract. Assessing the size of a former ocean of which only 84–35 Ma, 260 km between 35–0 Ma), which greatly exceeds remnants are found in mountain belts is challenging but cru- the width of the ocean. We suggest that at least 63 % of the cial to understanding subduction and exhumation processes. subducted and accreted material was highly thinned conti- Here we present new constraints on the opening and width nental lithosphere and most of the Alpine Tethys units ex- of the Piemont–Liguria (PL) Ocean, known as the Alpine humed today derived from OCT zones. Our work highlights Tethys together with the Valais Basin. We use a regional tec- the significant proportion of distal rifted continental margins tonic reconstruction of the Western Mediterranean–Alpine involved in subduction and exhumation processes and pro- area, implemented into a global plate motion model with vides quantitative estimates for future geodynamic modeling lithospheric deformation, and 2D thermo-mechanical mod- and a better understanding of the Alpine Orogeny.
    [Show full text]
  • Geologic CO2 Storage in Eastern Europe, Caucasus and Central Asia an Initial Analysis of Potential and Policy
    UNITED NATIONS ECONOMIC COMMISSION FOR EUROPE Geologic CO2 storage in Eastern Europe, Caucasus and Central Asia An initial analysis of potential and policy UNITED NATIONS ECONOMIC COMMISSION FOR EUROPE Geologic CO2 storage in Eastern Europe, Caucasus and Central Asia: An initial analysis of potential and policy UNITED NATIONS GENEVA, 2021 ©2021 United Nations All rights reserved worldwide Requests to reproduce excerpts or to photocopy should be addressed to the Copyright Clearance Center at copyright.com. All other queries on rights and licenses, including subsidiary rights, should be addressed to: United Nations Publications, 405 East 42nd St, S-09FW001, New York, NY 10017, United States of America Email: [email protected]; website: https://shop.un.org The findings, interpretations and conclusions expressed herein are those of the author(s) and do not necessarily reflect the views of the United Nations or its officials or member States. The designation employed and the presentation of material on any map in this work do not imply the expression of any opinion whatsoever on the part of the United Nations concerning the legal status of any country, territory, city or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. Mention of any firm, licensed process or commercial products does not imply endorsement by the United Nations. This publication is issued in English and Russian. United Nations publication issued by the United Nations Economic Commission for Europe. Acknowledgements Wolfgang Heidug is the lead author of this report. Filip Neele and Lydia Rycroft of the Netherlands Organisation for Applied Scientific Research (TNO), Luca Taschini of the London School of Economics (LSE) and University of Edinburg Business School, and Colin Ward of the King Abdullah Petroleum Studies and Research Centre (KAPSARC) made sig- nificant contributions to this report.
    [Show full text]