DOCSLIB.ORG

Dissertation Thomas Wiedl 08.10.2015

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Dissertation Thomas Wiedl 08.10.2015 The middle Miocene Leitha Mountains carbonate platform (Vienna Basin, Austria) – a palaeoenvironmental archive at the margin of the tropical reef belt by Bak. rer. nat. Mag. rer. nat. Thomas Wiedl A thesis submitted to the Institute of Earth Sciences Karl-Franzens University of Graz In partial fulfilment of the requirements for the degree of Doctor of Natural Sciences (Dr. rer. nat.) Graz, October 2015 2 Supervisor O. Univ.-Prof. Dr. phil. Werner Piller University of Graz Institute of Earth Sciences Heinrichstraße 26 8010 Graz Austria Co-supervisor Priv. Doz. Mag. Dr. Mathias Harzhauser Head of Department Geological-Paleontological Department Natural History Museum Vienna Burgring 7 1010 Wien Austria 3 4 Contents Preface .................................................................................................................................... 9 Chapter I ............................................................................................................................... 11 Introduction to the study area ..................................................................................... 11 1.1 The Leitha platform in the southern Vienna Basin .............................................. 11 1.2 Tectonic and geological setting of the study area ............................................... 13 1.3 Stratigraphy ................................................................................................................ 14 1.4 References ................................................................................................................. 16 Chapter II ...........................................................................................................21 Facies and synsedimentary tectonics on a Badenian carbonate platform in the southern Vienna Basin (Austria, Central Paratethys) ......................21 2.1 Abstract ....................................................................................................................... 21 2.2 Introduction ................................................................................................................ 22 2.2.1 Study area ........................................................................................................ 24 2.3 Material and methods ............................................................................................... 25 2.4 Section description ................................................................................................... 25 2.4.1 Section I ............................................................................................................ 26 2.4.2 Section II ........................................................................................................... 28 2.4.3 Tectonics ........................................................................................................... 43 2.5 Facies analysis and interpretation .......................................................................... 44 2.5.1 Basal breccia facies ........................................................................................ 44 2.5.2 Cross-bedded gravel facies ........................................................................... 44 2.5.3 Bioclastic corallinacean facies ....................................................................... 45 2.5.4 Acervulina -rhodolith subfacies ...................................................................... 46 2.5.5 Mollusc subfacies ............................................................................................ 48 2.5.6 Amphistegina subfacies .................................................................................. 52 2.5.7 Bryozoan subfacies ......................................................................................... 53 2.5.8 Coral debris subfacies .................................................................................... 53 2.5.9 Pholadomya subfacies .................................................................................... 54 2.5.10 Pinna subfacies ............................................................................................. 55 2.5.11 Rhodolith facies ............................................................................................. 59 2.6 Facies succession and synsedimentary tectonics ............................................... 61 5 2.7 Conclusions ............................................................................................................... 64 2.8 Acknowledgments ..................................................................................................... 65 2.9 References ................................................................................................................. 66 Chapter III .............................................................................................76 Ecospace variability along a carbonate platform at the northern boundary of the Miocene reef belt (Upper Langhian, Austria) ...............................76 3.1 Abstract ....................................................................................................................... 76 3.2 Introduction ................................................................................................................ 77 3.2.1 Study area ........................................................................................................ 78 3.3 Materials and methods ............................................................................................. 80 3.4 Sedimentary facies ................................................................................................... 80 3.4.1 Section A ........................................................................................................... 80 3.4.2 Section B ........................................................................................................... 83 3.4.3 Section C .......................................................................................................... 83 3.4.4 Section D .......................................................................................................... 84 3.5 Stratigraphy ................................................................................................................ 86 3.6 Facies analysis and interpretation .......................................................................... 88 3.6.1 Bioclastic coralline algal–mollusc facies ...................................................... 88 3.6.2 Hyotissa facies ................................................................................................. 89 3.6.3 Isognomon facies ............................................................................................ 91 3.6.4 Bryozoan facies ............................................................................................... 92 3.6.5 Rhodolith facies ............................................................................................... 92 3.6.6 Coral facies ....................................................................................................... 93 3.6.7 Terrigenous sand facies ................................................................................. 95 3.7 Discussion .................................................................................................................. 99 3.7.1 Ecospace modulation – variation under different set-ups ....................... 100 3.7.2 Cyclic sedimentation patterns ..................................................................... 101 3.7.3 The northern boundary of the Langhian Peri-Mediterranean reef belt . 102 3.8 Conclusion ............................................................................................................... 104 3.9 Acknowledgements ................................................................................................. 105 3.10 References ............................................................................................................. 106 6 Chapter IV...........................................................................................120 From biologically to hydrodynamically controlled carbonate production by tectonically induced palaeogeographic rearrangement (Middle Miocene, Pannonian Basin)................................................................................120 4.1 Abstract ..................................................................................................................... 121 4.2 Introduction .............................................................................................................. 122 4.2.1 Study area and geological setting ............................................................... 124 4.3 Material and methods ............................................................................................. 126 4.4 Stratigraphy .............................................................................................................. 126 4.5 Sedimentary facies ................................................................................................. 127 4.5.1 Winden A ........................................................................................................ 127 4.5.2 Winden B ........................................................................................................ 128 4.5.3 Winden C ........................................................................................................ 129 4.5.4 Winden D .......................................................................................................
Load more

Recommended publications
  • Facies and Synsedimentary Tectonics on a Badenian Carbonate Platform in the Southern Vienna Basin (Austria, Central Paratethys)
    Facies DOI 10.1007/s10347-011-0290-0 ORIGINAL ARTICLE Facies and synsedimentary tectonics on a Badenian carbonate platform in the southern Vienna Basin (Austria, Central Paratethys) Thomas Wiedl • Mathias Harzhauser • Werner E. Piller Received: 7 July 2011 / Accepted: 13 December 2011 Ó Springer-Verlag 2012 Abstract The Mannersdorf quarries at the northeastern limestones on a tectonic-caused flexure indicates syn-tec- edge of the Leitha Mountains (Lower Austria) preserve a tonical movements. Paleostress analyses verify a normal- record of pre-, syn- and post-tectonical phases of a Bade- fault reactivated as a dextral strike-slip fault. The temporal nian carbonate platform in the Vienna Basin. The pre-tec- character of this fault is indicated by a post-tectonical phase tonic phase is reported by a marine transgression with the with a marine transgression, a burial of the fault and nep- development of a coastal slope scree and subsequent pro- tunian dyke development. grading of a Gilbert-type fan delta, overlain by very heter- ogeneous corallinacean limestones. A fault divides the Keywords Miocene Á Langhian Á Central Paratethys Á study area into two independent tectonic blocks, which have Vienna Basin Á Depositional environments Á been logged and subjected to detailed investigation and Synsedimentary tectonics Á Facies sampling. The corallinacean limestones of the first block indicate shallow-water environments (i.e., seagrass mead- ows) and gradual transitions from shallower to deeper Introduction environments, while the second block shows an unconfor- mity, which is linked to a rapid facies change from rela- The Vienna Basin between the Eastern Alps and the tively deeper environments (i.e., indicated by the abundance Western Carpathians is one of the most studied basins—in of in situ Pholadomya) to shallow waters (indicated by terms of both structural and sedimentary geology (e.g., corals).
    [Show full text]
  • Reefs and Coral Carpets in the Miocene Paratethys (Badenian, Leitha Limestone, Austria) Bernhard Riegl Nova Southeastern University, [email protected]
    Nova Southeastern University NSUWorks Marine & Environmental Sciences Faculty Department of Marine and Environmental Sciences Proceedings, Presentations, Speeches, Lectures 2000 Reefs and Coral Carpets in the Miocene Paratethys (Badenian, Leitha Limestone, Austria) Bernhard Riegl Nova Southeastern University, [email protected] W. E. Piller Institut fur Palaontologie der Universitat Wien Follow this and additional works at: https://nsuworks.nova.edu/occ_facpresentations Part of the Marine Biology Commons, and the Oceanography and Atmospheric Sciences and Meteorology Commons NSUWorks Citation Riegl, Bernhard and Piller, W. E., "Reefs and Coral Carpets in the Miocene Paratethys (Badenian, Leitha Limestone, Austria)" (2000). Marine & Environmental Sciences Faculty Proceedings, Presentations, Speeches, Lectures. 111. https://nsuworks.nova.edu/occ_facpresentations/111 This Article is brought to you for free and open access by the Department of Marine and Environmental Sciences at NSUWorks. It has been accepted for inclusion in Marine & Environmental Sciences Faculty Proceedings, Presentations, Speeches, Lectures by an authorized administrator of NSUWorks. For more information, please contact [email protected]. i Proceedings 9 ° International Coral Reef Symposium, Bali, Indonesia 23-27 October 2000. Vol. I Reefs and coral carpets in the Miocene paratethys (Badenian, Leitha Limestone, Austria) B. Riegl i: 2 and W. E. Paler ) ABSTRACT Biohermal (reefs) and biostromal (coral carpets) facies were studied in the Austrian Middle Miocene Leitha Lime- stone. In the Vienna Basin ("Fenk quarry") non-framebuilding and framebuilding biostromal coral communities were found. In the Styrian Basin, well developed patch reefs were observed besides coral carpets. In the Fenk quarry, 2 coral carpet types, four non-framework coral communities, and one bivalve/coral community were found.
    [Show full text]
  • The Danube River Basin District
    / / / / a n ï a r k U / /// ija ven Slo /// o / sk n e v o l S / / / / a r o G a n r C i a j i b r S / / / / a i n â m o R / / / / a v o d l o M / / / / g á z s r ro ya ag M The /// a / blik repu Danube River Ceská / Hrvatska //// osna i Hercegovina //// Ba˘lgarija /// / B /// Basin District h ic e River basin characteristics, impact of human activities and economic analysis required under Article 5, Annex II randr Annex III, and inventory of protected areas required under Article 6, Annex IV of the EU Water Framework Directivee (2000/60/EC) t s Part A – Basin-wide overviewÖ / / Short: “Danube Basin Analysis (WFD Roof Report 2004)” / / d n a l h c s t u e D / / / / The complete report consists of Part A: Basin-wide overview, and Part B: Detailed analysis of the Danube river basin countries 18 March 2005, Reporting deadline: 22 March 2005 Prepared by International Commission for the Protection of the Danube River (ICPDR) in cooperation with the countries of the Danube River Basin District. The Contracting Parties to the Danube River Protection Convention endorsed this report at the 7th Ordinary Meeting of the ICPDR on December 13-14, 2004. The final version of the report was approved 18 March 2005. Overall coordination and editing by Dr. Ursula Schmedtje, Technical Expert for River Basin Management at the ICPDR Secretariat, under the guidance of the River Basin Management Expert Group. ICPDR Document IC/084, 18 March 2005 International Commission for the Protection of the Danube River Vienna International Centre D0412 P.O.
    [Show full text]
  • Δ88sr/86Srsrm987 and Elemental Pattern to Characterise Groundwater and Recharge of Saline Ponds in a Clastic Aquifer in East Austria
    Final Draft of the original manuscript: Tchaikovsky, A.; Häusler, H.; Kralik, M.; Zitek, A.; Irrgeher, J.; Prohaska, T.: Analysis of n(87Sr)/n(86Sr), δ88Sr/86SrSRM987 and elemental pattern to characterise groundwater and recharge of saline ponds in a clastic aquifer in East Austria. In: Isotopes in Environmental and Health Studies. Vol. 55 (2019) 2, 179 - 198. First published online by Taylor & Francis: 24.03.2019 DOI: 10.1080/10256016.2019.1577832 https://dx.doi.org/10.1080/10256016.2019.1577832 87 86 δ88 86 Analysis of n( Sr)/n( Sr), Sr/ SrSRM987 and elemental pattern to characterise groundwater and recharge of saline ponds in a clastic aquifer in East Austria Anastassiya Tchaikovskya, Hermann Häuslerb, Martin Kralikb, Andreas Ziteka, Johanna Irrgeherc,d and Thomas Prohaskaa,d aVIRIS Laboratory, Department of Chemistry, University of Natural Resources and Life Sciences Vienna, Tulln, Austria; bDepartment of Environmental Geosciences, University of Vienna, Vienna, Austria; cDepartment for Marine Bioanalytical Chemistry, Helmholtz Centre for Materials and Coastal Research, Institute for Coastal Research, Geesthacht, Germany; dChair of General and Analytical Chemistry, Montanuniversität Leoben, Leoben, Austria Abstract Elemental and isotopic pattern of n(87Sr)/n(86Sr) and δ88Sr/86SrSRM987 were used to characterise groundwater and recharge of saline ponds in a clastic aquifer in East Austria. Therefore, shallow, artesian and thermal groundwaters of the investigated aquifer along with rainfall and rivers were analysed using (MC) ICP-MS. The n(87Sr)/n(86Sr) ratio and elemental pattern changed with aquifer depth as a result of progressing bedrock leaching and dissolution with increasing groundwater residence time. The n(87Sr)/n(86Sr) ratio of shallow groundwater below saline ponds of 0.71019 ± 0.00044 was significantly different from thermal groundwater of 0.71205 ± 0.00035 (U, k = 2).
    [Show full text]
  • Part II Excursions
    © Österreichische Geologische Gesellschaft/Austria; download unter www.geol-ges.at/ und www.biologiezentrum.at Excursions 85 (1992) p. 97-239 Mitt. Osterr. Geol. Ges. Wien, September 1992 Guidebook 154 Abb. Part II Excursions EXCURSION 1 100 Stop 1/1: Baden-Sooß 101 Stop 1/2: Steinbrunn 102 Stop 1/3: Großhöflein 112 Stop 1/4: St. Georgen near Eisenstadt 118 Stop 1/5: St. Margareten 126 Stop 1/6: Wolfsthal 132 EXCURSION 2 138 Stop 2/1: ÖMV-AG, Zenrum Gewinnung 139 Stop 2/2: Ernstbrunn 140 Stop 2/3: Au bei Klement 149 Stop 2/4: Au bei Klement 153 Stop 2/5: Staatz 154 Stop 2/6: Steinberg Ridge 156 EXCURSION 3 161 Stop 3/1: Bisamberg 161 Stop 3/2: Königsstetten 168 Stop 3/3: Königsstetten , 170 Stop 3/4: Dopplerhütte 172 Stop 3/5: Greifenstein 174 EXCURSION 4 177 Stop 4/1: Kaltenleutgeben 179 Stop 4/2: Hinterbrühl 193 Stop 4/3: Hinterbrühl 199 Stop 4/4: Gaaden 201 Stop 4/5: Talhof 203 Stop 4/6: Agydigraben 203 Stop 4/7: Neuhaus 206 Stop 4/8: Weißenbach 212 Stop 4/9: Berndorf 213 EXCURSION 5 218 Stop 5/1: Hohe Wand 218 Stop 5/2: Odenhof 222 Stop 5/3: Sierning 226 Stop 5/4: Florianikogel 231 Stop 5/5: Rax Mountain 234 © Österreichische Geologische Gesellschaft/Austria; download unter www.geol-ges.at/ und www.biologiezentrum.at 98 Guidebook to Excursions in the Vienna Basin etc. m i l /«.-~.,_1 ^ *""W«jf YCSi V\A IX» ROUTES OF EXCURSIONS 1-5 HodoninsafV 2" n © Österreichische Geologische Gesellschaft/Austria; download unter www.geol-ges.at/ und www.biologiezentrum.at Part II - Excursions 99 GEOLOGIC FRAME OF EXCURSIONS 1 • 5 50 100 150km <k.
    [Show full text]
  • 1. Introduction
    1. Introduction 1.1. A short introduction to the subject In 186, a young adherent of Darwin’s theories and geology, Charles Lyell (1788–1868), presented the di- researcher into prehistoric cultures named John Lub- vision of the Stone Age into the Palaeolithic and Neo- bock (1834–1913) published his book Pre-historic lithic in the ninth volume of his famous Elements of Times, as Illustrated by Ancient Remains, and the Man- Geology . As a consequence, these terms became ac- ners and Customs of Modern Savages, which gained cepted in the scientific world and gained the status of great popularity in European and American scientific independent epochs; they were later to be joined by circles. A year later an edition in French appeared in a third, the Middle Stone Age or Mesolithic. Paris, and in 1876 a Russian edition was published in Lubbock divided the Palaeolithic from the Neo- Moscow. Lubbock’s book drew the world’s attention to lithic on the basis of technological criteria linked pri- the beginning of a new science – prehistory, or rather marily to techniques of stone tool production. Soon prehistoric archaeology, which in the second half of after, thanks to the development of cultural anthro- the 19th century was regarded as one of the disciplines pology, further criteria were added. This was due of anthropology, then defined more widely (Lubbock to the works of Lewis H. Morgan (1818–1881) and 186; cf. also Niederle 1893). Fate ordained that the Edward Burnett Tylor (1832–1917), the most impor- year in which Lubbock’s work appeared would also tant proponents of evolutionism in cultural anthro- see the death of the important Danish researcher of pology (Tylor 1871; 1881; Morgan 1877).
    [Show full text]
  • Burgenland Winegrowing Area: Hareter Vineyard Wine
    Burgenland Winegrowing area: Austria’s most full-bodied red wines grow under the influence of the continentally warm Pannonian climate in the country’s most eastern state. The Ruster Ausbruch, one of the world’s most famous sweet wines, is a focus of regional wine identity. Right in the south, the Eisenberg offers the best conditions for red wines of the finest minerality and incomparable elegance. Blue Frankish with its exceptional depth of fruit and length grows in the Mittelburgenland and to the north of the Rosalia mountains. A unique terroir for complex white wines is located on the eastern slope of the Leitha mountains. The Blue Zweigelt with its powerful, juicy red wines dominates to the east of Lake Neusiedl, even if Blue Frankish and Sankt Laurent also provide excellent results. Hareter vineyard Thomas Hareter’s organic vineyard is situated in the Weiden am See district on the eastern bank of Lake Neusiedl. The history of the agricultural family-run business goes back to the 18th century. In 2011, Thomas Hareter took over his parents’ business which was certified as organic from 2009 and has been managing it with his wife Claudia ever since. Covering an area of 15 hectares, 50% of the vineyard is covered with red and white vines that benefit from the lake’s own micro-climate and the clayey-gravelly soils. These lend the wines their mineral touch and a cool fresh fruity taste. Thomas Hareter strives to produce harmonious wines that are easy to store from the mostly local vines, such as Zweigelt, Blue Frankish, white Burgundy and Welschriesling.
    [Show full text]
  • And Seewinkel Gravel Beds - Implications of Middle Pleistocene Uplift and Neighboring Subsidence in the Northern Burgenland (Austria) H
    Geophysical Research Abstracts, Vol. 8, 06293, 2006 SRef-ID: 1607-7962/gra/EGU06-A-06293 © European Geosciences Union 2006 The Parndorf- and Seewinkel gravel beds - implications of Middle Pleistocene uplift and neighboring subsidence in the Northern Burgenland (Austria) H. Häusler Center for Earth Sciences, University of Vienna, Austria ([email protected]) The Pleistocene terraces in the Alpine foreland of Austria are characterised by a suc- cession of oldest terraces at highest positions stepwise followed up by younger terraces in deeper positions down to the recent bed of River Danube and its tributaries. Based on this principle (regarding loess cover, palaeo-soils, soil successions, cryoturbation and fossils if any), several terraces in Lower Austria with a basement ranging between 60 and 120 meters above river Danube are supposed to be of Upper Pliocene/Early Pleistocene age. Terraces with a basement at 45 meters above River Danube in gen- eral date as Günz, and at 17-30 meters above this river as Mindel. Around Vienna the so-called Hochterrasse (high terrace; Gänserndorf terrace) with its base at about 16 meters above the River Danube is of Riß age, and the Niederterrasse (low terrace; Prater terrace), which is situated about 8 meters above this river, is of Würmian age. This method of indirect dating of terraces according to their height above River Danube cannot be applied, however, when terraces were tectonically tilted or when gravel beds were deposited in regions of Pleistocene subsidence such as the Little Hungarian Plain (Kisalföld). A new approach of paralleling Pleistocene terraces of the Northern Burgenland (Parndorfer Platte - Seewinkel) with Pleistocene deposits in Northwestern Hungary promotes discussion of Middle Pleistocene palaeogeography related to fault tectonics.
    [Show full text]
  • 4 Strauss Et Al.P65
    GEOLOGICA CARPATHICA, JUNE 2006, 57, 3, 185—197 Sequence stratigraphy in a classic pull-apart basin (Neogene, Vienna Basin). A 3D seismic based integrated approach PHILIPP STRAUSS1, MATHIAS HARZHAUSER2, RALPH HINSCH3 and MICHAEL WAGREICH4 1 OMV, EOP-AUT Exploration, Gerasdorferstrasse 151, 1210 Vienna, Austria; [email protected], 2Natural History Museum Vienna, Geological-Palaeontological Department, Vienna, Austria 3Rohöl-Aufsuchungs AG (RAG), Vienna, Austria 4Department of Geological Sciences, University of Vienna, Vienna, Austria (Manuscript received February 2, 2005; accepted in revised form December 8, 2005) Abstract: This paper presents an improved sequence stratigraphic framework for the southern and central Vienna Basin (Austria) based on the integration of 3D seismic reflection data, well data, surface outcrops and refined biostratigraphy. The 3D survey used for this study is positioned close to the margin of the Vienna Basin, which increases the stratigraphic importance of this analysis. Distal basin facies, so far only known from seismic and well data, are compared and correlated to their proximal equivalents in surface outcrops. The investigated part of the basin is characterized by a syn-sedimentary horst and graben structure, with Badenian (Langhian and Lower Serravallian) platform carbonates on the elevated areas and fine-grained marine clastic sediments in adjacent subbasins. This integrated approach allows the separation of the Neogene sediments in the southern Vienna Basin into five Middle and Upper Miocene 3rd order depositional cycles: the Badenian is separated into three depositional cycles and the Sarmatian (Middle and Upper Serravallian) and the Pannonian (Tortonian) represent one depositional cycle each. The three Badenian cycles are correlated with the TB 2.3., TB 2.4.
    [Show full text]
  • Palaeontological Highlights of Austria
    © Österreichische Geologische Gesellschaft/Austria; download unter www.geol-ges.at/ und www.biologiezentrum.at Mitt. Österr. Geol. Ges. ISSN 0251-7493 92 (1999) 195-233 Wien, Juli 2000 Palaeontological Highlights of Austria WERNER E. PILLER1, GUDRUN DAXNER-HÖCK2, DARYL P DOMNING3, HOLGER C. FORKE4, MATHIAS HARZHAUSER2, BERNHARD HUBMANN1, HEINZ A. KOLLMANN2, JOHANNA KOVAR-EDER2, LEOPOLD KRYSTYN5, DORIS NAGEL5, PETER PERVESLER5, GERNOT RABEDER5, REINHARD ROETZEL6, DIETHARD SANDERS7, HERBERT SUMMESBERGER2 28 Figures and 1 Table Introduction Besides Zeapora gracilis, distinguished by large rounded cortical filaments, Pseudolitanaia graecensis and Pseu­ The oldest known fossils in Austria date back into the dopalaeoporella lummatonensis occur (Fig. 3). Pseudolitan­ Ordovician. From this time on a broadly continuous fossil aia graecensis is built up of straight thalli containing club- record is preserved up to the Holocene. Since an encyclo­ shaped filaments and Pseudopalaeoporella lummatonensis paedic or monographic presentation is impossible within is characterized by a typically poorly-calcified medullar this volume, nine case studies of different stratigraphic lev­ zone and delicate cortical filaments. els (Fig. 1) were selected to call attention to this remarkably There are two localities known with autochthonous algal good fossil documentation. These case studies include occurrences in the Graz Palaeozoic. One is characterized records on invertebrate fossils from several time slices from by Pseudopalaeoporella lummatonensis with dispersed the Late Palaeozoic to the Miocene, as well as on verte­ thalli of Pseudolitanaia. Contrary to all expectations, these brates from the Miocene and Pleistocene and on plant algae are found in marly lithologies suggesting very bad fossils from the Devonian and Early Miocene. This selection environmental conditions for photoautotrophic organisms.
    [Show full text]
  • 6 Workshop on the Neogene
    NEOGENE OF THE PARATETHYAN REGION 6TH WORKSHOP ON THE NEOGENE OF CENTRAL AND SOUTH-EASTERN EUROPE AN RCMNS INTERIM COLLOQUIUM PROGRAMME page 45. ABSTRACTS page 10101. FIELD TRIP GUIDEBOOK page 102124. 31 MAY - 3 JUNE 2015, ORFŰ, HUNGARY Fig. 0.1 Simplified geological map with field stops (map modified from Gyalog (2013)) NEOGENE OF THE PARATETHYAN REGION 6TH WORKSHOP ON THE NEOGENE OF CENTRAL AND SOUTH-EASTERN EUROPE an RCMNS Interim Colloquium Programme Abstracts Field Trip Guidebook 31 May - 3 June 2015, Orfű, Hungary NEOGENE OF THE PARATETHYAN REGION 6 W N C S‐E E an RCMNS Interim Colloquium 31 May ‐ 3 June 2015, Orfű, Hungary PROGRAMME, ABSTRACTS AND FIELD TRIP GUIDEBOOK Organizing Commiee Imre M (MOL Hungarian Oil and Gas Plc. / MTA‐MTM‐ELTE Research Group for Paleontology, Budapest) Ágnes K (Hungarian Geological Society) Orsolya S (Eötvös Loránd University, Budapest) Kriszna S (University of Pécs) Gábor C (Geological and Geophysical Instute of Hungary, Budapest) Alfréd D (Hungarian Natural History Museum, Budapest) György L (University of Miskolc) Ildikó S (Geological and Geophysical Instute of Hungary, Budapest) Emőke T (Eötvös Loránd University, Budapest) Klára P (Geological and Geophysical Instute of Hungary, Budapest) Katalin B (Eötvös Loránd University, Budapest) Lilla T (Eötvös Loránd University, Budapest) Editors István‐Róbert B Ágnes K Imre M Kriszna S Published by Hungarian Geological Society H‐1015 Budapest, Csalogány u. 12. [email protected]‐online.hu www.foldtan.hu Budapest 2015 ISBN 978‐963‐8221‐57‐5 Cover photo: Uppermost part of the Pannonian calcareous marls and their transion to the overlying –sll Pannonian–coarse sands at Pécs‐Danitzpuszta.
    [Show full text]
  • Socio-Economic Analysis of the Carpathian Area
    Socio-economic analysis of the Carpathian area Project co-financed by the EU Pécs 2007 Hungarian Academy of Sciences HAS Centre for Regional Studies Centre for Regional Studies Transdanubian Research Institute Director General: Dr. Gyula Horváth Director: Pálné dr. Ilona Kovács Phone: +36 72 523 800 H-7621 Pécs, Papnövelde u. 22. H-7601 Pécs, P.O. Box 199 Fax: +36 72 523 803 Socio-economic analysis of the Carpathian area Supervisors Iván Illés DSc; Zoltán Gál PhD Technical editor Szilárd Rácz Authors Ferenc Erdősi DSc (chapter 9) István Fodor DSc (chapter 4) Zoltán Gál PhD (chapter 15) Wiktor Glowacki (chapter 5) Zoltán Hajdú DSc (chapter 2, 3) László Hrubi (chapter 11) Iván Illés DSc (chapter 1, 10) Lukasz Kotula (chapter 5) Teréz Kovács PhD (chapter 13) Kinga Kuczynska (chapter 5) Gábor Lux (chapter 12) Péter Póla PhD (chapter 6, 7, 8) Zoltán Raffay PhD (chapter 14) HAS CENTRE FOR REGIONAL STUDIES 1 TRANSDANUBIAN RESEARCH INSTITUTE Socio-economic analysis of the Carpathian area Contents 1. Introduction – The Carpathians: a European macroregion......................................................... 6 1.1. Physical geographic features.............................................................................................. 6 1.2. The analysed area.............................................................................................................. 7 1.3. Demography..................................................................................................................... 10 1.4. Ethnic and religious affiliations
    [Show full text]