Opportunities of Re-Establishing Underground Mining in the Borsod Coal Basin in North-Eastern Hungary

Total Page:16

File Type:pdf, Size:1020Kb

Opportunities of Re-Establishing Underground Mining in the Borsod Coal Basin in North-Eastern Hungary DOI 10.2478/ntpe-2019-0057 Opportunities of re-establishing underground mining in the borsod coal basin in north-eastern Hungary 2019 József Molnár, Ákos Debreczeni, Richárd Tompa Volume 2 Institution of Mining and Geotechnical Engineering, Issue 1 University of Miskolc, Hungary pp. 532-540 Date of submission to the Editor: 05/2019 Date of acceptance by the Editor: 08/2019 CADASTRE OF HUNGARIAN COAL RESERVES Significant coal reserves remained in Hungary despite mine closures, and these could be taken into account when considering future fuel and raw material demand of the country. So Mining and Geological Survey of Hungary (MBFSZ) contributed a new cadastre of Hungarian coal deposits of greater or less reserves throughout the country which is available in electronic digital form (https://map.mbfsz.gov.hu/coal_cadastre/). Geological information that can be obtained using the database in question is of essential importance in mine design. Coal basins of Hungary are showed by Figure 1. Fig. 1 Coal basins of Hungary Source: Mining and Geological Survey of Hungary – MBFSZ DEMAND FOR NEW BROWN COAL SOURCES A special research took place in the past years analyzing possibility of establishing coal chemical industry in the Borsod region in question especially József MOLNÁR, Ákos DEBRECZENI, Richárd TOMPA 533 for methanol production. So reserves of brown coal were taken into consideration such as near Kazincbarcika (Tardona), Edelény (Szendrő), and Putnok (Dubicsány and Sajómercse II). Coal demand of chemical utilization should be considered a lucky situation from mining point of view. On the one hand such a plant needs coal of constant quantity and quality as raw material and on the other hand opening a new mine of economic output requires one or more major industrial consumers. Chemical industry which has similar remarkable traditions in the region as mining can be the only major buyer as utilization of coal for power generation is not preferred this time. Although there are several brown coal deposits in the Borsod region, we focus on the Dubicsány and Sajómercse II ones (Figure 2). Both coal deposits are close the Sajó river at town of Putnok. Sajómercse II consists of the eastern remains of the former Putnok underground coal mine south of Sajó furthermore some 10 million tons of east of it. The Dubicsány deposit which is north of the river is totally untouched as no production operations were in it in the past. Main properties of mining point of view of both deposits are described in the paper published by MBFSZ (Debreczeni et al. 2018). Institution of Mining and Geotechnical Engineering was participant in preparing mining plans. Fig. 2 Location of the Dubicsány and Sajómercse II coal deposits in the Borsod coal basin Source: Mining and Geological Survey of Hungary – MBFSZ The Dubicsány brown coal deposit 262 boreholes were sunk on the 23.58 km2 area of the Dubicsány brown coal deposit. Both core sampling and geophysical analysis were done for the vast majority of the holes. Two coal seams (IV and V) are available. Seam IV is thin, not mineable and can be found only on a small part of the deposit. Seam V is mineable and can be found over the whole area. Thickness and mean calorific value of Seam V was determined for all boreholes throughout the whole deposit. Valuating thickness and specific heat content enabled more accurate determination of the borders of the parts of the mine (as 534 New Trends in Production Engineering – Volume 2, issue 1, 2019 shown fields North I, North II, South I and South II on Figure 3). Steadier seam thickness and calorific value in a mine field is more advantageous from mining engineering point of view. 755000 755500 756000 756500 757000 757500 758000 758500 759000 759500 760000 760500 761000 761500 P-40 333000 333000 P-3812.21P-35 Du-23 11.43 8.64 2.13 North II Du-46 Dö-5 Dö-7 P-15 P-33 P-24 11.51 7.37Du-51 Du-28 Dö-4 Dö-8 P-31 P-14 Dö-3 332500 P-31/a 11.93 332500 Du-55 11.51 3.47 11.28 11.98 P-32 Du-43 Sg-41 10.89 Dö-9 P-39 P-29 Du-47 10.59Du-45 11.41 11.37 11.65 Sg-34 12.60 11.52P-28 Sg-13 Dö-6 P-37 12.93Du-2911.08 Sg-14 North I Du-42 12.22 11.66 J-46 332000 P-30 11.86 Sg-44 Sg-38 Sk-244 332000 0.59 J-57 9.05 P-22 Du-4810.92 11.22 Sk-287 Sk-263 J-54 12.11Du-50 Sg-50 10.87 Sg-40 P-23 11.68 Sg-12 10.26 J-53 P-21 11.41 11.34 Sg-46 10.97Sk-303 J-52 P-5 Du-53 Du-44 11.77 Sg-16 9.99 8.20 Sg-51 Sg-11 12.59 9.85 Sk-265Sk-264 Du-26 11.06 Sk-295 J-50/aJ-5010.41 331500 11.82 10.81 Sk-286 331500 P-25/aP-25 P-20 Du-13 11.24 Sg-33 8.21 7.45 J-49 P-19/aP-19/bP-19/cP-19 14.30Du-39 Du-49 Sg-49 Sg-37 Sk-301 9.52P-62/H 12.97 Du-35 Du-38 Sk-299 13.38 11.59 11.56 10.78 12.17 Sk-302 10.46 Du-11 Sg-48 Sg-6 Sg-32 Sk-302/a P-27 13.83Du-36 12.13 10.00 Sk-252 P-48 Du-379.75 Sg-53 10.46 13.1110.58 P-26 Du-33 10.55 Sk-285 Sk-300 10.47 331000 13.37 13.23 Sg-47 Sg-54 Sk-298 331000 P-46 10.89 10.49 12.72Du-52 9.98Du-8 9.83 Sk-293 P-13 3.42 Du-41 10.42 9.77Sg-19 Sk-296 Sk-304 P-11 Sg-31 Sg-63 10.66Sk-276 13.79 Du-15 10.61 10.94 P-47 13.26 9.88 10.30 10.91Sk-297 Pu-57 P-34 Du-54 Du-40 9.14 Sg-30Sg-62 Sk-284 12.82 11.05 P-45 D-7 11.20Sg-18Sg-29 11.28 330500 14.00Pu-50 13.22 Du-67 11.69 9.79 10.00Sk-291 330500 Du-21 Du-62 Sg-57 Sk-253 13.55P-44 Du-12 10.67 12.2010.87 Sg-27 Sk-294 12.54P-43 Du-34 Sg-42 11.48 Pu-53 Du-71 10.49 10.03 10.13 Sg-26/ASg-26 12.48 Du-68 Du-70 Du-57 Du-65 11.43 11.66 Sg-35 Sg-25 11.83 13.38 Du-32 P-42/BP-42 12.65 12.42 P-8 P-42/A 13.35 10.60 9.81 8.65 Sg-36 12.16 Pu-60 Du-74 Du-60 Du-24 10.32 12.91Du-20 Du-90 Du-58 Sg-43 Sk-283 330000 12.90 Sg-1514.82 330000 11.50 P-49 8.65 9.46 9.93 Sg-39 Pu-58 13.31 12.58 Du-85 8.80 11.13 12.12 12.62 Du-89 Du-75 Du-66 11.83 Pu-51 Du-73D-6 Sg-28/ASg-28 Sg-52 Pu-61 12.58 10.09 9.51 Sg-4 P-9 10.84 P-6 Du-81 8.76 10.08 11.23 9.21 Du-18 9.42 Du-14 Du-63 5.91 Pu-52 Du-78 Sg-9 329500 12.19 12.42 7.94 8.53 Sg-55 Sg-45 329500 Pu-56 Du-84 Du-76 8.79 10.79Pu-54 Du-61 7.15 Du-83 10.00 7.25 Du-16 Du-56 10.17 P-7 10.79 8.67 South II 10.47 8.00 8.24Du-77 Sg-10 Du-59 Du-86 8.18 Du-88 Du-64 8.82Sg-56 10.17 Du-72/BDu-72/ADu-72 8.10 Pu-55 8.04 7.69 7.42 Du-798.39 9.45 9.96 Du-87 D-3 Du-10 329000 8.93P-310.92 Du-69 Du-17 Sg-60 329000 Du-92 9.06 7.53 7.78 Sg-5 Pu-59 9.16Du-94 Du-97 Du-91 Du-82 Du-80 Sg-58 7.45 8.32 Du-1910.69 5.97 6.97 7.80 6.66 Sg-59 Du-96 Du-99 Du-95 Du-25 Du-93 1.94 6.90 328500 5.96 7.53 10.74 Sg-17 328500 Du-101 Du-100 Du-98 Sg-61 6.66 6.50 Sg-7 5.66 Sg-20 9.73 328000 DUBICSÁNY BROWN COAL DEPOSIT 328000 AVERAGE CALORIFIC VALUE OF THE COAL (MJ/kg) AND BORDERS OF South I THE PARTS OF THE MINE (SEAM V) 327500 327500 1:20000 755000 755500 756000 756500 757000 757500 758000 758500 759000 759500 760000 760500 761000 761500 Fig. 3 Average calorific value of the coal (MJ/kg) and borders of the parts of the Dubicsány mine. Faults are highlighted by red lines Source: Molnár (editor-in-chief), 2018 Total thickness of layers between the two seams (mostly sand) is of 70-72 m at average. Coal reserve of the Dubicsány deposit is concentrated in Seam V. Its thickness is 5-6 m on the vast majority of the deposit except on the south- western part and near the border of the seam.
Recommended publications
  • Act Cciii of 2011 on the Elections of Members Of
    Strasbourg, 15 March 2012 CDL-REF(2012)003 Opinion No. 662 / 2012 Engl. only EUROPEAN COMMISSION FOR DEMOCRACY THROUGH LAW (VENICE COMMISSION) ACT CCIII OF 2011 ON THE ELECTIONS OF MEMBERS OF PARLIAMENT OF HUNGARY This document will not be distributed at the meeting. Please bring this copy. www.venice.coe.int CDL-REF(2012)003 - 2 - The Parliament - relying on Hungary’s legislative traditions based on popular representation; - guaranteeing that in Hungary the source of public power shall be the people, which shall pri- marily exercise its power through its elected representatives in elections which shall ensure the free expression of the will of voters; - ensuring the right of voters to universal and equal suffrage as well as to direct and secret bal- lot; - considering that political parties shall contribute to creating and expressing the will of the peo- ple; - recognising that the nationalities living in Hungary shall be constituent parts of the State and shall have the right ensured by the Fundamental Law to take part in the work of Parliament; - guaranteeing furthermore that Hungarian citizens living beyond the borders of Hungary shall be a part of the political community; in order to enforce the Fundamental Law, pursuant to Article XXIII, Subsections (1), (4) and (6), and to Article 2, Subsections (1) and (2) of the Fundamental Law, hereby passes the following Act on the substantive rules for the elections of Hungary’s Members of Parliament: 1. Interpretive provisions Section 1 For the purposes of this Act: Residence: the residence defined by the Act on the Registration of the Personal Data and Resi- dence of Citizens; in the case of citizens without residence, their current addresses.
    [Show full text]
  • Case Studies from Borsod-Abauj-Zemplén County, North Hungary
    Carpathian Journal of Earth and Environmental Sciences, July 2017, Vol. 12, No. 2, p. 473 - 483 LONG-TERM CHANGES OF LAND USE/LAND COVER PATTERN IN HUMAN TRANSFORMED MICROREGIONS – CASE STUDIES FROM BORSOD-ABAUJ-ZEMPLÉN COUNTY, NORTH HUNGARY László SÜTŐ1, Zoltán DOBÁNY2, TiborJózsef NOVÁK3, Balázs ADORJÁN4, 3 5 József INCZE & Péter RÓZSA 1Department of Environmental Geography and Geoinformatics, Eszterházy Károly University, 3300 Eger, Eszterházy tér 1., Hungary; [email protected] 2Institute of Tourism and Geography, University of Nyíregyháza, 4400 Nyíregyháza Sóstói 31/b. Hungary; [email protected] 3Department of Landscape Protection and Environmental Geography, University of Debrecen, 4032 Debrecen Egyetem tér 1., Hungary; [email protected]; [email protected] 4Department of Botany, University of Debrecen, 4032 Debrecen Egyetem tér 1., Hungary; [email protected] 5Department of Mineralogy and Geology, University of Debrecen, 4032 Debrecen Egyetem tér 1., Hungary, [email protected] Abstract: Using historical geographic and landscape ecological methods three North Hungarian landscape units that underwent different types of anthropic impact were studied. Viticulture in the Nagy Hill of Tokaj was founded more than eight centuries ago, however, due to economic crises and the phylloxera epidemic extension of the vineyards has fallen to less than one-half during 250 years; wetlands and grassland of the Taktaköz were changed by arable lands after river regulation and flood prevention performed in the second half of the 19th century; and traditional land use/land cover pattern of the East Borsod Coal Basin has been transformed by coal mining and industrialization from the end of the 19th century.
    [Show full text]
  • Uppony Mountains: High Geomorphological Diversity Within a Small Area
    Chapter 20 Uppony Mountains: High Geomorphological Diversity Within a Small Area Gábor Demeter and Katalin Szalai Abstract Merely of 454 m maximum elevation, the geologically and geomorphologically diverse and still dynamic Uppony Mountains is relatively rich in geomorphic features (caves, pseudo- caverns, gorges, horsts, scarps, landslides, karren, natural outcrops) created by diverse processes (valley incision, derasion, mass movements, karst formation, periglacial, pedimentation). This small mountainous area with its intricate geological structure is ideal either for field investigations in order to obtain broader knowledge on the evolution of North- Hungary or to study both convergent and divergent evolution of forms generated on different rocks. Using a comparative approach, with an outlook to its environs, the quantification and numeric analysis of morphometric and lithological features combined with the traditional descriptive geomorphic approach promotes a better understanding of the area so important in the paleoenvironmental, paleogeographical reconstruction of North-Hungary. Keywords: Paleozoic massif • Piedmont • Imbrication • Gorges • Landslides • Caverns G. Demeter Institute of History, Hungarian Academy of Sciences, H-1014 Budapest, Országház út 30. E-mail: [email protected] K. Szalai Department of Tourism, Kodolányi János University of Applied Sciences, H-8000 Székesfehérvár, Fürd ő út 1. E-mail: [email protected] 20.1 Introduction The Uppony Mountains of 240 km 2 area are located in northeastern Hungary, in the Bükk Mountains northern foreland. It is mainly composed of slightly metamorphosed Paleozoic siliciclastic rocks and limestones with distant Alpine contacts, surrounded by semi- consolidated Neogene marine sediments. Its uniqueness is primarily due to the particular geology: both karstic and non-soluble, as well as highly diagenized and semi-consolidated sediments occur in the area.
    [Show full text]
  • Maps -- by Region Or Country -- Eastern Hemisphere -- Europe
    G5702 EUROPE. REGIONS, NATURAL FEATURES, ETC. G5702 Alps see G6035+ .B3 Baltic Sea .B4 Baltic Shield .C3 Carpathian Mountains .C6 Coasts/Continental shelf .G4 Genoa, Gulf of .G7 Great Alföld .P9 Pyrenees .R5 Rhine River .S3 Scheldt River .T5 Tisza River 1971 G5722 WESTERN EUROPE. REGIONS, NATURAL G5722 FEATURES, ETC. .A7 Ardennes .A9 Autoroute E10 .F5 Flanders .G3 Gaul .M3 Meuse River 1972 G5741.S BRITISH ISLES. HISTORY G5741.S .S1 General .S2 To 1066 .S3 Medieval period, 1066-1485 .S33 Norman period, 1066-1154 .S35 Plantagenets, 1154-1399 .S37 15th century .S4 Modern period, 1485- .S45 16th century: Tudors, 1485-1603 .S5 17th century: Stuarts, 1603-1714 .S53 Commonwealth and protectorate, 1660-1688 .S54 18th century .S55 19th century .S6 20th century .S65 World War I .S7 World War II 1973 G5742 BRITISH ISLES. GREAT BRITAIN. REGIONS, G5742 NATURAL FEATURES, ETC. .C6 Continental shelf .I6 Irish Sea .N3 National Cycle Network 1974 G5752 ENGLAND. REGIONS, NATURAL FEATURES, ETC. G5752 .A3 Aire River .A42 Akeman Street .A43 Alde River .A7 Arun River .A75 Ashby Canal .A77 Ashdown Forest .A83 Avon, River [Gloucestershire-Avon] .A85 Avon, River [Leicestershire-Gloucestershire] .A87 Axholme, Isle of .A9 Aylesbury, Vale of .B3 Barnstaple Bay .B35 Basingstoke Canal .B36 Bassenthwaite Lake .B38 Baugh Fell .B385 Beachy Head .B386 Belvoir, Vale of .B387 Bere, Forest of .B39 Berkeley, Vale of .B4 Berkshire Downs .B42 Beult, River .B43 Bignor Hill .B44 Birmingham and Fazeley Canal .B45 Black Country .B48 Black Hill .B49 Blackdown Hills .B493 Blackmoor [Moor] .B495 Blackmoor Vale .B5 Bleaklow Hill .B54 Blenheim Park .B6 Bodmin Moor .B64 Border Forest Park .B66 Bourne Valley .B68 Bowland, Forest of .B7 Breckland .B715 Bredon Hill .B717 Brendon Hills .B72 Bridgewater Canal .B723 Bridgwater Bay .B724 Bridlington Bay .B725 Bristol Channel .B73 Broads, The .B76 Brown Clee Hill .B8 Burnham Beeches .B84 Burntwick Island .C34 Cam, River .C37 Cannock Chase .C38 Canvey Island [Island] 1975 G5752 ENGLAND.
    [Show full text]
  • Magyarország Közigazgatási Helynévkönyve, 2014. Január 1
    Magyarország közigazgatási helynévkönyve 2014. január 1. Gazetteer of Hungary 1st January, 2014 Központi Statisztikai Hivatal Hungarian Central Statistical Office Budapest, 2014 © Központi Statisztikai Hivatal, 2014 © Hungarian Central Statistical Office, 2014 ISSN 1217-2952 Felelős szerkesztő – Responsible editor: Waffenschmidt Jánosné főosztályvezető – head of department További információ – Contact person: Nagy Ferenc Andrásné szerkesztő – editor (tel: 345-6366, e-mail: [email protected]) Internet: http://www.ksh.hu [email protected] 345-6789 (telefon), 345-6788 (fax) Borítóterv – Cover design: Nyomdai kivitelezés – Printed by: Xerox Magyarország Kft. – Táskaszám: 2014.076 TARTALOM ÚTMUTATÓ A KÖTET HASZNÁLATÁHOZ ............................................................................................................... 5 KÓDJEGYZÉK ..................................................................................................................................................................... 11 I. ÖSSZEFOGLALÓ ADATOK 1. A helységek száma a helység jogállása szerint ............................................................................................................................................................ 21 2. A főváros és a megyék területe, lakónépessége és a lakások száma ........................................................................................................................... 22 3. A települési önkormányzatok főbb adatai ..................................................................................................................................................................
    [Show full text]
  • Ministry of Agriculture and Rural Development PROGRAMME
    Ministry of Agriculture and Rural Development PROGRAMME-COMPLEMENT (PC) to the AGRICULTURE AND RURAL DEVELOPMENT OPERATIONAL PROGRAMME (ARDOP) (2004-2006) Budapest June 2009 ARDOP PC modified by the ARDOP MC on 7 March 2006 and by written procedures on 18 August, 29 September 2006 and on 14 August 2007, revised according to the comments of the European Commission (ref.:AGRI 004597of 06.02.2007, AGRI 022644 of 05.09.07 and AGRI 029995 of 22.11 07.) 2 TABLE OF CONTENTS I. INTRODUCTION .............................................................................................................. 5 I.1 PROGRAMME COMPLEMENT....................................................................... 5 I.2 THE MANAGING AUTHORITY for ARDOP.................................................. 6 I.2.1 General description......................................................................................... 6 I.2.2 The MANAGING AUTHORITY in Hungary................................................ 6 I.2.3 Monitoring ...................................................................................................... 6 I.2.4 Financial Management and Control Arrangements ........................................ 6 I.2.5 Monitoring the capacities................................................................................ 6 I.3 THE PAYING AUTHORITY............................................................................. 6 I.4 THE INTERMEDIATE BODY .......................................................................... 6 I.5 THE FINAL BENEFICIARIES.........................................................................
    [Show full text]
  • Narratives, Beliefs, Understanding
    proba.qxd 2020.03.03. 9:59 Page 1 TÖRTÉNELEM ÉS TÁRSADALOMTUDOMÁNYOK XXXI. ÉVFOLYAM 4. SZÁM Narratives, Beliefs, Understanding EDITOR OF THE THEMATIC ISSUE: PÁSZKA, IMRE – MMXIX WINTER – proba.qxd 2020.03.03. 9:59 Page 2 TÖRTÉNELEM ÉS TÁRSADALOMTUDOMÁNYOK Fõszerkesztõ KISS GÁBOR FERENC Szerkesztõbizottság SZEGFÛ LÁSZLÓ (elnök), JANCSÁK CSABA, KISS GÁBOR FERENC, MARJANUCZ LÁSZLÓ, NAGY TAMÁS, NÓTÁRI TAMÁS, PÁSZKA IMRE, RÁCZ LAJOS Tanácsadó testület ANDAHÁZI SZEGHY VIKTOR, BANGÓ JENÕ, CSABA LÁSZLÓ, GARDA DEZSÕ, GEBEI SÁNDOR, JOHN GOODWIN, PAPP SÁNDOR, SZAKÁLY SÁNDOR, SZELÉNYI IVÁN, UTASI ÁGNES, VERES VALÉR Szerkesztõk HALMÁGYI MIKLÓS, KOVÁCS ATTILA, MIKLÓS PÉTER, NAGY GÁBOR DÁNIEL, PLUGOR RÉKA, SZÕTS ZOLTÁN OSZKÁR Munkatársak DÁVID BENJÁMIN, FLOUTIER JEREMY, GATTI BEÁTA, GAUSZ ILDIKÓ, LENGYEL ÁDÁM, SÁNTA TAMÁS Számunk az EIKKA Alapítvány, a Dél-magyarországi Pedagógiai Alapítvány, a Magyar Történelmi Társulat Csongrád Megyei és Szegedi Csoportja, a Nemzeti Kulturális Alap, a Szegedi Tudományegyetem Polgáraiért Alapítvány, az SZTE Bölcsészettudományi Kar, az SZTE Juhász Gyula Pedagógusképzõ Kar, az SZTE Alkalmazott Társadalomismereti és Kisebbségpolitikai Intézet, az SZTE Történettudományi Intézet, az SZTE JGYPK HÖK és a SZEPA Alapítvány támogatásával készült. A Belvedere Meridionale online elérhetõ itt: www.belvedere.meridionale.hu A lap tanulmányokat, interjúkat, ismertetéseket és kritikákat közöl a történelem és a társadalomtudományok körébõl. A közlésre benyújtott cikk még nem publikált és más folyóiratnál elbírálás alatt nem lévõ, eredeti írásmû lehet. A benyújtott és a lap jellegének megfelelõ írásokat két, a szerzõ számára ismeretlen szakmai lektor bírálja el. A két lektor véleményének figyelembevételével a szerkesztõség döntést hoz a megjelentetésrõl, melyet a szerzõvel közöl. A folyóirat megjelenik évente négy alkalommal: tavasszal, nyáron, õsszel és télen. A szerkesztõség címe: 6725 Szeged, Hattyas sor 10.
    [Show full text]
  • Magyar Állami Földtani Intézet Évi Jelentése 1-2.Sz
    RELATIONES ANNUAE INSTITIUTI GEOLOGICI PUBLICI HUNGARICI A MAGYAR ÁLLAMI FÖLDTANI INTÉZET ÉVI JELENTÉSE 1994–1995/I–II. ANNUAL REPORT OF THE GEOLOGICAL INSTITUTE OF HUNGARY BUDAPEST, 2000 © Copyright Geological Institute of Hungary (Magyar Állami Földtani Intézet), 2000 All rights reserved! Minden jog fenntartva! Reviewers — lektorok: LÁSZLÓ BOGNÁR, GÉZA CSÁSZÁR, ENDRE DUDICH, JÁNOS HAAS, MÁRIA HÁMOR-VIDÓ, ÁRON JÁMBOR, EMÕKE JOCHA-EDELÉNYI, ERIKA JUHÁSZ, PÉTER KOVÁCS-PÁLFFY, LÁSZLÓ KORPÁS, MARGIT KORPÁS-HÓDI, BÉLA NAGY, MRS. LÁSZLÓ NAGY †CSABA RAVASZ, ÉVA SZEGÕ, TIBOR ZELENKA Scientific editor — szakszerkesztõ: JÓZSEF KNAUER Linguistic revisor — nyelvi lektor: TAMÁS JASKÓ Technical editor— mûszaki szerkesztõ: DEZSÕ SIMONYI DTP — számítógépes nyomdai elõkészítés: ILDIKÓ TIEFENBACHER Published by the Geological Institute of Hungary — kiadja a Magyar Állami Földtani Intézet Responsible editor — felelõs kiadó: KÁROLY BREZSNYÁNSZKY Director — igazgató HU ISSN 0368–9751 ANN. REP. OF THE GEOLOGICAL INSTITUTE OF HUNGARY, 1994–1995/I–II. (2000) CONTENTS — TARTALOM GAÁL GÁBOR: A Magyar Állami Földtani Intézet mûködési jelentése az 1994–1995. évrõl . 7 BREZSNYÁNSZKY KÁROLY: Búcsú dr. Konda Józseftõl (1929–1995) . 59 †JASKÓ, S.: Quaternary tectonics and sedimentation in North-Eastern Hungary . 69 RÉTI, ZS.: Preliminary report on Miocene vulcanism at the Northern Bükk Foreland . 75 KALMÁR, J. and KNAUER, J.: Initial stage and antecedents of the Lutetian sedimentation in the region of Nyirád (Southern Bakony Mts, Transdanubian Central Range) . 83 KOLLÁNYI, K.: The role of smaller foraminifers in paleoenvironmental reconstruction with relation to the Eocene deposits of the NE Bakony Mts and the flanking zone of the Vértes Mts . 93 BODNÁR, E.: Facies and age of the Upper Cretaceous marine deposits in borehole section Pápakovácsi–1, Bakony Mts, Hungary .
    [Show full text]
  • Secondary Mineralisation Processes in Coal Pit Heaps and Its Impact On
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by University of Debrecen Electronic Archive ACTA GGM DEBRECINA Geology, Geomorphology, Physical Geography Series DEBRECEN Vol. 2, 41–45 2007 Secondary mineralisation processes in coal pit heaps and its impact on the environment in NE Hungary Szénmeddők másodlagos mineralizációs folyamatai és környezeti hatásuk Északkelet-Magyarországon László Sütő1, Miklós Kozák1, Richard W. McIntosh1, Zoltán Püspöki1, Imre Beszeda2 1Department of Mineralogy and Geology, University of Debrecen 4032 Egyetem tér 1. Debrecen, Hungary e-mail: [email protected] 2Department of Solid State Physics, University of Debrecen Abstract – Ottnangian-Karpatian brown coal seams were exploited from the late 19th century producing numerous pit heaps accumulated between 1920 and 1970 in the hilly foreground of the Bükk Mountains, northern Hungary. The aim of this paper was the observation of the processes in the pit heaps and its environmental impacts. The five coal seams were formed in paralic transgressional-progradational swamps. The oxihydration of the pyrite and marcasite content of the coal heap resulted in the production of sulphuric acids that exposed the components of the embedding sediments. Furthermore, the self-combustion of the partly siliceous and fragmented coal material in the pit heap was frequent. In this partly open system with varying temperature, hydrothermal, low-pressure and high-temperature pneumatolitic and thermo-contact micro- environments occurred simultaneously. In remobilising the original elements of the organic and the heap material, the migration of the adsorbed water and the gravitational free water equally played an important role. According to the microscopic, micromorphological electron microscopic, microprobe and X-ray analyses, primarily, sulphates occur in the heaps and the formation of rhombic native sulphur is frequent.
    [Show full text]
  • Magyarország Közigazgatási Helynévkönyve, 2012. Január 1
    Magyarország közigazgatási helynévkönyve 2012. január 1. Gazetteer of Hungary 1st January, 2012 Központi Statisztikai Hivatal Hungarian Central Statistical Office Budapest, 2012 © Központi Statisztikai Hivatal, 2012 © Hungarian Central Statistical Office, 2012 ISSN 1217-2952 Felelős szerkesztő – Responsible editor: Waffenschmidt Jánosné főosztályvezető – head of department További információ – Contact person: Nagy Ferenc Andrásné szerkesztő – editor (tel: 345-6366, e-mail: [email protected]) Internet: http://www.ksh.hu [email protected] 345-6789 (telefon), 345-6788 (fax) Borítóterv – Cover design: Nyomdai kivitelezés – Printed by: Xerox Magyarország Kft. – Táskaszám: 2012. 91 TARTALOM ÚTMUTATÓ A KÖTET HASZNÁLATÁHOZ ............................................................................................................... 5 KÓDJEGYZÉK ..................................................................................................................................................................... 11 I. ÖSSZEFOGLALÓ ADATOK 1. A helységek száma a helység jogállása szerint ........................................................................................................................................................... 17 2. A főváros és a megyék területe, lakónépessége és a lakások száma........................................................................................................................... 18 3. A települési önkormányzatok főbb adatai ..................................................................................................................................................................
    [Show full text]
  • Transformation of Land Use Pattern in the East Borsod Coal Basin from The
    DOI: 10.21120/LE/10/3-4/16 Landscape & Environment 10 (3-4) 2016. 223-231 TRANSFORMATION OF LAND USE PATTERN IN THE EAST BORSOD COAL BASIN FROM THE BEGINNING OF MINING INDUSTRY TO THE POLITICAL CHANGES LÁSZLÓ SÜTŐ1* – ERIKA HOMOKI2 – ZOLTÁN DOBÁNY3 – PÉTER RÓZSA4 1 Eszterházy Károly University, Department of Environmental Geography and Geoinformatics, H-3300 Eger Eszterházy tér 1. P.O.B. 43. 2University of Nyíregyháza, Institute of Teacher Training, H-4400 Nyíregyháza, Sóstói út 31/b. 3 University of Nyíregyháza, Institute of Tourism and Geography, H-4400 Nyíregyháza, Sóstói út 31/b. 4 University of Debrecen, Department of Mineralogy and Geology, H-4032 Hungary Debrecen, Egyetem tér 1. P.O.B. 9. *E-mail: [email protected] Received 02 August 2016, accepted in revised form 18 September 2016 Abstract Historical geographic studies on land cover may support the understanding of the recent state. Focusing on coal mining, this process was followed and analyzed in the case of the East Borsod Coal Basin from the early 20th century to the political change. The contemporaneous maps and manuscripts concerning the mining were evaluated using geoinformatic techniques. More- over, digitalized topographic map coming from the early and late period of mining (1924 and 1989, respectively) were analyzed. To determine the degree of human disturbance hemerobic of the three military surveys, too. It can be stated that montanogenic subtype of an industrial- relations and changes of the given land cover patches were quantified on the basis of the maps surfaces, however, relative dominance of forest forming the matrix of the landscape remained.
    [Show full text]
  • A Kazincbarcikai Kistérség Válogatott Honismereti Bibliográfiája
    A Kazincbarcikai Kistérség válogatott honismereti bibliográfiája Kazincbarcika 2010 A bibliográfia anyagát válogatta: MÁRKUS ZSUZSANNA (Borsod-Abaúj-Zemplén Megyei Bányászattörténeti Múzeum, Rudabánya) Szerkesztette: HADOBÁS SÁNDOR Megjelent az Oktatási és Kulturális Minisztérium által meghirdetett KÖZKINCS PROGRAM támogatásával Kiadta a Kazincbarcika és Vonzáskörzete Többcélú Önkormányzati Kistérségi Társulás Felelıs kiadó: SZÉKELYNÉ VARGA MÁRIA irodavezetı ISBN 978 963 87929 6 9 Nyomdai munkák: Litoplán Kft., Kazincbarcika. Felelıs vezetı: Tóth Zoltán 2 E L İ S Z Ó A Kazincbarcikai Kistérség érdekes, változatos vidék Borsod-Abaúj- Zemplén Megye északnyugati részén. Területét a Sajó vágja ketté: a fo- lyótól északra a szelíd Borsodi-dombság , délre a vadregényes Bükk hú- zódik. Központjában található a névadó nagyváros, amely minden irány- ból jól megközelíthetı. Legnagyobb múltú települése azonban a több szempontból is hírneves, 2008 óta ismét városi rangot viselı Rudabánya . Községei jobbára a hajdani borsodi bányavidékhez tartoztak, s napjaink- ban a bányabezárások következtében kialakult gazdasági-társadalmi problémákkal küzdenek. Lélekszámuk folyamatosan csökken, jövıbeli ki- látásaik nem túl biztatóak. Van azonban, amire méltán büszkék lehetnek a kistérségben élık: a szép természeti környezetre, az érdekességekben gazdag helytörténetre, a mőemlékekre, az irodalmi hagyományokra, az egykor jelentıs bányászatra, az itt-ott még ma is élı népi kultúrára és a vidékhez kötıdı jeles személyiségekre. A felsoroltak jobb, teljesebb meg- ismerését
    [Show full text]