Quaternary of Western Lithuania:From the Pleistocene Glaciations to Theevolution of the Baltic Sea

Total Page:16

File Type:pdf, Size:1020Kb

Quaternary of Western Lithuania:From the Pleistocene Glaciations to Theevolution of the Baltic Sea THE QUATERNARY OF WESTERN LITHUANIA: FROM THEPLEISTOCENE GLACIATIONS TO THE EVOLUTION OF THE BALTIC SEA The INQUA Peribaltic Group Field Symposium May 27- June 02, 2007, Plateliai, Lithuania PROCEEDINGS VILNIUS, 2007 The Quaternary of Western Lithuania: from the Pleistocene Glaciations to the PROCEEDINGS Evolution of the Baltic Sea, May 27 – June 02, 2007, Plateliai, Lithuania TTHHEE QQUUAATTEERRNNAARRYY OOFF WWEESSTTEERRNN LLIITTHHUUAANNIIAA:: FFRROOMM TTHHEE PPLLEEIISSTTOOCCEENNEE GGLLAACCIIAATTIIOONNSS TTOO TTHHEE EEVVOOLLUUTTIIOONN OOFF TTHHEE BBAALLTTIICC SSEEAA PROCEEDINGS The INQUA Peribaltic Group Field Symposium May 27 – June 02, 2007, Plateliai, Lithuania SPONSORS: KKKAAAUUUNNNOOO HHHIIIDDDRRROOOGGGEEEOOOLLLOOOGGGIIIJJJAAA VILNIUS, 2007 1 The Quaternary of Western Lithuania: from the Pleistocene Glaciations to the Evolution of the Baltic Sea, May 27 – June 02, 2007, Plateliai, Lithuania PROCEEDINGS UDK [551.79: 551.33: 551.8] (100): 061.3 (474.5) Qu‐09 The Quaternary of Western Lithuania: from the Pleistocene glaciations to the evolution of the Baltic Sea: Proceedings: The INQUA Peribaltic Group Field Symposium, May 27 – June 02, 2007, Plateliai, Lithuania / Eds.: R. Guobytė, M. Stančikaitė; Lithuanian Geological Survey, Institute of Geology and Geography. – Vilnius: LGT, 2007. – 107, [1] p.: iliustr. – ISBN 978‐9986‐623‐45‐8 SSSYYYMMMPPPOOOSSSIIIUUUMMM PPPRRROOOGGGRRRAAAMMMMMMEEE May 28th Paper and poster session May 29th Stops 1–2, 4–6, Samogitian Upland Stops 8–9, Venta Plain May 30th Stops 3, 16–19, south‐western Samogitian Plain May 31th Stops 20–24, Curonian Spit June 1th Stops 7, 10–15, north‐western Samogitian Plain The Symposium Venue – Hotel LINELIS (Plateliai) ORGANIZERS: Section of Quaternary Geology of the Lithuanian Geological Society Lithuanian Geological Survey Institute of Geology and Geography Coastal Research and Planning Institute of Klaipėda University The Peribaltic Group (INQUA Sub‐commission on Glaciation) Friends of Baltic Quaternary THE SYMPOSIUM HELD UNDER AUSPICE AND FINANCIAL SUPPORT OF THE: Baltic Sea Region INTERREG III B Project Adaptation Strategies to Climate Change in the Baltic Sea Region (ASTRA), Lithuanian State Science and Studies Foundation ORGANIZING COMMITTEE: Albertas Bitinas, Rimantė Guobytė, Aldona Damušytė, Alma Grigienė (Lithuanian Geological Survey) Miglė Stančikaitė, Petras Šinkūnas (Institute of Geology and Geography) Saulius Gulbinskas, Nerijus Blažauskas (Coastal Research and Planning Institute of Klaipėda University) CCCooommmpppiiillleeeddd bbbyyy::: A. Damušytė EEEdddiiittteeeddd bbbyyy::: R. Guobytė, M. Stančikaitė LLLaaayyyooouuuttt aaannnddd cccooovvveeerrr dddeeesssiiigggnnn::: R. Norvaišienė (Pagramantis outcrop. Photo by P. Aleksa) Circulation: 100 copies ©Lietuvos geologijos tarnyba ©Geologijos ir geografijos institutas 2 The Quaternary of Western Lithuania: from the Pleistocene Glaciations to the PROCEEDINGS Evolution of the Baltic Sea, May 27 – June 02, 2007, Plateliai, Lithuania CONTENTS LITHIC‐ AND POLLEN STRATIGRAPHY OF THE MIDDLE NEOPLEISTOCENE IN THE NORTH OF THE EUROPEAN RUSSIA ................................................................................................................................................... 6 ANDREICHEVA, L. N. THE WEST‐EAST CLIMATE GRADIENT IN GLACIAL HISTORY OF EURASIA.................................................. 9 ASTAKHOV, V. PECULIARITIES OF THE ENVIRONMENT AND DEVELOPMENT OF VEMBŪTAI PLATEAU AND HILL FORT, WESTERN LITHUANIA ................................................................................................................................ 11 BALTRŪNAS, V., KARMAZA, B., STANČIKAITĖ, M., PUKELYTĖ, V. DILATANCY IN UNCONSOLIDATED SEDIMENTS............................................................................................. 13 BRUJ, M. HOLOCENE PALEOGEOGRAPHY RECONSTRUCTION OF THE UPPER VYCHEGDA RIVER DEPOSITS..... 14 BURAVSKAYA, M. N., GOLUBEVA, YU. V. WATER CHESTNUT TRAPA NATANS MACROFOSSILS AND POLLEN FROM PLEISTOCENE INTERGLACIAL AND HOLOCENE DEPOSITS IN LATVIA................................................................................. 16 CERINA, A., KALNINA, L., ZVAGINA, I. THE MISTIC “BURBOT‘S CITY“ IN THE PLATELIAI LAKE – AN UNDERWATER OUTCROP OF INTERGLACIAL SEDIMENTS ................................................................................................................................. 18 DAMUŠYTĖ, A., GUOBYTĖ, R., GRIGIENĖ, A., ŠEIRIENĖ, V. SEDIMENTATION CONDITIONS OF THE UPPER DNIEPER VALLEY IN THE LATE GLACIAL AND HOLOCENE (ORSHA‐ROGACHEV PLOT, BELARUS) .......................................................................................... 20 DROZD, A., BADIAY, V. APPLICATION OF MACROSCOPIC IDENTIFICATION METHODS OF INDICATOR ERRATICS TO LOCATE SOURCE AREA OF ŁUKÓW JURASSIC GLACIAL RAFTS.................................................................................... 22 GAŁĄZKA, D. NEOTECTONIC FAULTING EXPRESSED IN THE QUATERNARY LANDSCAPE IN DENMARK .................... 24 JAKOBSEN, P. R. THE DIVERSITY OF MELTWATER CHANNELS REPRESENTING DIFFERENT STAGES OF DEGLACIATION ON THE FELLS OF OUNASSELKÄ, FINLAND....................................................................................................... 26 JOHANSSON, P., LEHTINEN, K. & SARALA, P. THE STRATIGRAPHY AND PALAEOENVIRONMENT OF THE NORTHERN PART OF THE CURONIAN SPIT BASED ON NEW POLLEN, DIATOM, MOLLUSCS AND CARBONATE ANALYSIS DATA .............................. 28 KABAILIENĖ, M., VAIKUTIENĖ, G., DAMUŠYTĖ, A., RUDNICKAITĖ, E. THE NORTH LITHUANIAN ICE MARGINAL MORAINE RIDGE: STRUCTURE, ORIGIN AND RELATIONSHIP OF SURFACE FORMS WITH PRE‐QUATERNARY STRUCTURES .......................................... 30 KARMAZIENĖ, D. GEOTECHNICAL PROPERTIES OF GLACIODYNAMIC STRUCTURES AT OUTCROP OF ULMALE ............. 32 KARPOVIČS, A., LŪSE, I. TRACE FOSSILS AND SEDIMENTATION OF UPPER PLEISTOCENE GLACIOLACUSTRINE CLAY IN LITHUANIA............................................................................................................................................................... 34 KAZAKAUSKAS, V., UCHMAN, A., GAIGALAS, A. MARINE AND LAND DEPOSITS IN THE SOUTHERN BALTIC AND ORLOWO CLIFF (GDANSK BAY) ON THE LIGHT OF QUARTZ GRAINS SEM STUDIES ................................................................................................ 35 KENIG, K. STRATIGRAPHICAL PROBLEMS OF THE PLEISTOCENE SEDIMENTS IN THE PAJŪRIS LOWLAND, WEST LITHUANIA............................................................................................................................................................... 37 KONDRATIENĖ, O. 3 The Quaternary of Western Lithuania: from the Pleistocene Glaciations to the PROCEEDINGS Evolution of the Baltic Sea, May 27 – June 02, 2007, Plateliai, Lithuania MORPHOTECTONIC PATTERN OF THE KOLA PENINSULA ............................................................................. 39 KORSAKOVA, O. P., KOLKA, V. V. SILICEOUS ROCKS AS RAW MATERIAL OF PREHISTORIC ARTEFACTS IN ENVIRONS OF BIRŽULIS LAKE, WESTERN LITHUANIA ................................................................................................................................ 41 KULBICKAS, D. VARYING PRESSURES OF THE ICE SHEETS AS A FACTOR OF THE PLEISTOCENE ACTIVITY OF THE POLOTSK‐KURZEME AND THE SMALAND‐BLEKINGE DEFORMATION ZONES.......................................... 43 KURLOVICH, D. M. THE GLACIATION HISTORY OF THE BELARUSIAN POOZERIE AREA (AS BASED ON 3D GIS‐MODELS OF THE GLACIAL/INTERGLACIAL PALEOSURFACES) ............................................................................................ 45 KURLOVICH, D. M., KURLOVICH, O. A EVALUATION OF NEOTECTONIC MOVEMENTS IN ANTARCTICA ................................................................ 47 LASTOCHKIN, A. N., KROTOVA‐PUTINTSEVA, A. Y. A NEW PALAEOENTOMOLOGICAL AND PALAEOBOTANICAL DATA FROM THE LATE GLACIAL DEPOSITS IN THE RAUNIS SECTION ................................................................................................................... 49 LUKŠEVICA, L., LUKŠEVICS, J., CERINA, A., KALNINA, L., BARŠEVSKIS, A. MORPHOLOGY, INTERNAL STRUCTURE AND GENETIC INTERPRETATION OF THE MORAINE RIDGE AT CĒRE, CENTRAL PART OF THE NORTHERN KURSA UPLAND, NW LATVIA............................................ 51 MARKOTS, A., STRAUTNIEKS, I., ZELČS, V. MICROELEMENTS OF QUATERNARY SEDIMENTS –MAIN SOIL – FORMING ROCKS OF THE NORTH‐ WEST RUSSIA ........................................................................................................................................................... 53 MATINIAN, N. N. IR‐OSL DATING OF DEPOSITS FROM THE NEW LATE PLEISTOCENE SECTION AT THE VOKA SITE, NORTH‐EASTERN ESTONIA .................................................................................................................................. 55 MOLODKOV, A. FACIES AND DEPOSITIONAL HISTORY OF THE LATE WEICHSELIAN TILL AT THE SECTION KOZŁOWO, THE LOWER VISTULA VALLEY, NORTHERN POLAND...................................................................................... 57 NARLOCH, W., WYSOTA, W. DEVELOPMENT HISTORY OF THE GLACIAL LAKES IN NORTHERN VIDZEME, LATVIA ........................... 59 NARTIŠS, M., ZELČS, V. ENVIRONMENT DYNAMICS IN THE LATEST PHASE OF THE EEMIAN (MIKULINO) INTRGLACIAL IN THE CENTRAL AND NORTH‐WESTRN OF THE EAST EUROPEAN PLAIN ...................................................... 61 NOVENKO, E. YU., FAUSTOVA, M. A., CHEPURNAYA, A. A. SUBGLACIAL TUNNEL SPACING INFERRED FROM THE DISTRIBUTION OF BEDROCK VALLEYS IN ESTONIA...................................................................................................................................................................
Recommended publications
  • Geological Setting and Tectonic Framework in Denmark
    DANMARKS OG GRØNLANDS GEOLOGISKE UNDERSØGELSE RAPPORT 2010/124 Low- and intermediate level radioactive waste from Risø, Denmark. Location studies for potential disposal areas. Report no. 3 Geological setting and tectonic framework in Denmark Stig A. Schack Pedersen & Peter Gravesen GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF CLIMATE AND ENERGY G E U S DANMARKS OG GRØNLANDS GEOLOGISKE UNDERSØGELSE RAPPORT 2010/124 Low- and intermediate level radioactive waste from Risø, Denmark. Location studies for potential disposal areas. Report no. 3 Geological setting and tectonic framework in Denmark Stig A. Schack Pedersen & Peter Gravesen GEOLOGICAL SURVEY OF DENMARK AND GREENLAND ~ MINISTRY OF CLIMATE AND ENERGY G E U S 1. INTRODUCTION 4 1.1 The aim of this report ............................................................................................... 5 2. GEOLOGICAL SETTING OF DENMARK 6 2.1 The pre-Quaternary Geology of Denmark ............................................................... 7 3. GEOLOGICAL – TECTONIC FRAMEWORK 10 3.1 The geotectonic margins of the Danish Basin ....................................................... 10 3.2 Deep-seated tectonic structures ............................................................................ 12 4. SALT DIAPIRS 13 4.1 The salt provinces in Denmark ............................................................................... 14 5. TECTONICS OF CRETACEOUS AND TERTIARY DEPOSITS 17 6. TECTONICS OF BORNHOLM: BASEMENT, BLOC TECTONICS AND INVERSION 18 7. THE PRE-QUARTERNY SURFACE
    [Show full text]
  • Low-And Intermediate Level Radioactive Waste from Risoe
    1. INTRODUCTION 5 2. DATA AND DATABASES 7 2.1 Distribution of rocks and sediments, environment and age ...................... 7 2.2 Field investigations .......................................................................................... 8 2.3 Field inspections ............................................................................................ 10 2.4 Borehole data ................................................................................................. 11 2.4.1 Well data archive and Jupiter database. ................................................ 11 2.5 Shallow geophysical data ............................................................................. 14 2.6 Groundwater data .......................................................................................... 16 2.7 Rock and sediment mineralogy and chemistry ......................................... 17 2.7.1 Redox processes ....................................................................................... 17 2.7.2 Mineralogical and chemical composition of rocks and sediments ..... 18 2.8 Data from the National Groundwater mapping ......................................... 18 2.8.1 Drinking water areas ................................................................................. 18 2.8.2 Groundwater mapping............................................................................... 19 2.9 Earth quake data ........................................................................................... 22 3. MAPS 24 3.1 Quaternary Maps in scale 1:50.000
    [Show full text]
  • The East Greenland Rifted Volcanic Margin
    GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN 24 • 2011 The East Greenland rifted volcanic margin C. Kent Brooks GEOLOGICAL SURVEY OF DENMARK AND GREENLAND DANISH MINISTRY OF CLIMATE, ENERGY AND BUILDING 1 Geological Survey of Denmark and Greenland Bulletin 24 Keywords East Greenland, North Atlantic, rifted volcanic margin, large igneous province, LIP, Palaeogene, basalt, syenite, nephelinite, carbona- tite, uplift. Cover Sundown over the nunataks in the Main Basalts (Skrænterne Fm) to the south of Scoresby Sund. Camped on the glacier, the 1965 Ox- ford University East Greenland Expedition travelled and collected from this area on foot, manhauling equipment on the sledge to the left. The expedition results were published in Fawcett et al. (1973). Frontispiece: facing page Mountains of horizontally layered basalt flows rising to about 2000 m on the south side of Scoresby Sund. Typical trap topography as found throughout most of the Kangerlussuaq–Scoresby Sund inland area. Chief editor of this series: Adam A. Garde Editorial board of this series: John A. Korstgård, Department of Geoscience, Aarhus University; Minik Rosing, Geological Museum, University of Copenhagen; Finn Surlyk, Department of Geography and Geology, University of Copenhagen Scientific editor of this volume: Adam A. Garde Editorial secretaries: Jane Holst and Esben W. Glendal Referees: Dennis K. Bird (USA) and Christian Tegner (DK) Illustrations: Eva Melskens with contributions from Adam A. Garde Digital photographic work: Benny Schark Graphic production: Kristian A. Rasmussen Printers: Rosendahls · Schultz Grafisk A/S, Albertslund, Denmark Manuscript received: 1 March 2011 Final version approved: 20 September 2011 Printed: 22 December 2011 ISSN 1604-8156 ISBN 978-87-7871-322-3 Citation of the name of this series It is recommended that the name of this series is cited in full, viz.
    [Show full text]
  • Freiberg Online Geoscience FOG Is an Electronic Journal Registered Under ISSN 1434-7512
    FOG Freiberg Online Geoscience FOG is an electronic journal registered under ISSN 1434-7512 2016, VOL 46 Christoph Breitkreuz and Uwe Kroner (conveners) Workshop on “Late Paleozoic magmatism in the Erzgebirge / Krušné hory: Magma genesis, tectonics, geophysics, and mineral deposits” - Abstracts - 42 pages, 23 contributions Content Preface .......................................................................................................................................................... 3 Vertical evolution of the Cínovec granite cupola – chemical and mineralogical record (Breiter) ............... 4 The Late Paleozoic volcanic centres in Central Europe – What do we know and what we need to know! (Breitkreuz) ................................................................................................................................................... 7 The initial phase of the Late Carboniferous Altenberg-Teplice Volcanic Complex: Volcanosedimentary evolution of the Schönfeld–Altenberg Depression Complex (Breitkreuz et al.) .......................................... 9 Reprocessing of deep seismic reflection profiles from the Erzgebirge / Krušné hory area (Buske et al.) .. 11 Correlating the lithofacies schemes of the Late Paleozoic Teplice Rhyolite, Central-European Variscides (German-Czech border) (Casas-García et al.) ........................................................................................... 13 The exhumation channel of the Erzgebirge: From heat advection to the emplacement of Sn-W enriched granites (Hallas et
    [Show full text]
  • Geological Survey of Denmark and Greenland Bulletin 1, 145-216
    DENMARK, SOUTHERN SWEDEN AND THE NETHERLANDS Previous page: Jurassic sediments exposed in a clay-pit at Bagå on Bornholm, Denmark – see Michelsen et al. (2003, this volume). Photo: Peter K. Warna-Moors. Jurassic lithostratigraphy and stratigraphic development onshore and offshore Denmark Olaf Michelsen, Lars H. Nielsen, Peter N. Johannessen, Jan Andsbjerg and Finn Surlyk A complete updated and revised lithostratigraphic scheme for the Jurassic succession of the onshore and offshore Danish areas is presented together with an overview of the geological evo- lution. The lithostratigraphies of Bornholm, the Danish Basin and the Danish Central Graben are described in ascending order, and a number of new units are defined. On Bornholm, the Lower–Middle Jurassic coal-bearing clays and sands that overlie the Lower Pliensbachian Hasle Formation are referred to the new Sorthat Formation (Lower Jurassic) and the revised Bagå Formation (Middle Jurassic). In the southern Danish Central Graben, the Middle Jurassic succession formerly referred to the Lower Graben Sand Formation is now included in the revised Bryne Formation. The Lulu Formation is erected to include the uppermost part of the Middle Jurassic succession, previously referred to the Bryne Formation in the northern Danish Central Graben. The Upper Jurassic Heno Formation is subdivided into two new members, the Gert Member (lower) and the Ravn Member (upper). The organic-rich part of the upper Farsund Formation, the for- mer informal ‘hot unit’, is established formally as the Bo Member. Dominantly shallow marine and paralic deposition in the Late Triassic was succeeded by wide- spread deposition of offshore marine clays in the Early Jurassic.
    [Show full text]
  • Geological Survey of Denmark and Greenland Bulletin 14, 78
    Bulletin 14: GSB191-Indhold 04/12/07 14:36 Side 1 GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN 14 · 2007 Quaternary glaciation history and glaciology of Jakobshavn Isbræ and the Disko Bugt region, West Greenland: a review Anker Weidick and Ole Bennike GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF CLIMATE AND ENERGY Bulletin 14: GSB191-Indhold 04/12/07 14:36 Side 2 Geological Survey of Denmark and Greenland Bulletin 14 Keywords Jakobshavn Isbræ, Disko Bugt, Greenland, Quaternary, Holocene, glaciology, ice streams, H.J. Rink. Cover Mosaic of satellite images showing the Greenland ice sheet to the east (right), Jakobshavn Isbræ, the icefjord Kangia and the eastern part of Disko Bugt. The position of the Jakobshavn Isbræ ice front is from 27 June 2004; the ice front has receded dramatically since 2001 (see Figs 13, 45) although the rate of recession has decreased in the last few years. The image is based on Landsat and ASTER images. Landsat data are from the Landsat-7 satellite. The ASTER satellite data are distributed by the Land Processes Distribution Active Archive Center (LP DAAC), located at the U.S. Geological Survey Center for Earth Resources Observation and Science (http://LPDAAC.usgs.gov). Frontispiece: facing page Reproduction of part of H.J. Rink’s map of the Disko Bugt region, published in 1853. The southernmost ice stream is Jakobshavn Isbræ, which drains into the icefjord Kangia; the width of the map illustrated corresponds to c. 290 km. Chief editor of this series: Adam A. Garde Scientific editor of this volume: Jon R. Ineson Editorial secretaries: Jane Holst and Esben W.
    [Show full text]
  • Geological Survey of Denmark and Greenland Bulletin 16, 2008, P 56-66
    Lower Cretaceous units 388 mg HC/g TOC; the interval is thus an excellent poten- In general, the Lower Cretaceous succession of the study tial oil and gas source rock. Similarly, a c. 20 m thick inter- area contains few and relatively thin potential oil source val in the Års-1 well possesses a mixed oil/gas generation rocks. Three wells, the Lavø-1, Sæby-1 and Års-1, contain potential, although the potential is poorer than in Sæby-1 intervals in the Lower Cretaceous (Vedsted Formation or as the HI values range from 210–411 mg HC/g TOC, undifferentiated Lower Cretaceous) with a petroleum gen- averaging 294 mg HC/g TOC. In the Lavø-1 well, a c.18 eration potential. In the Sæby-1 well, a c. 20 m thick m thick potential source-rock interval with HI values from organic-rich interval has TOC contents up to 5.28 wt% 175–242 mg HC/g TOC is present. The Lower Cretaceous and HI values from 320–472 mg HC/g TOC, averaging is, however, thermally immature in all well sections. Potential reservoirs The principal sedimentary units of interest with respect to stones are predominantly well to moderately sorted, fine- potential reservoirs in the Norwegian–Danish Basin are to medium-grained, locally coarse-grained and slightly the sandstones of the Upper Triassic – lowermost Jurassic pebbly. The shoreface sandstones occur as widespread Gassum Formation and the Middle Jurassic Haldager Sand sheets, 4–30 m thick, separated by marine transgressive Formation. The growth of salt pillows caused local topo- mudstones and lagoonal heteroliths.
    [Show full text]
  • Lithostratigraphy of the Palaeogene–Lower Neogene Succession of The
    GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN 12 · 2007 Lithostratigraphy of the Palaeogene – Lower Neogene succession of the Danish North Sea Poul Schiøler, Jan Andsbjerg, Ole R. Clausen, Gregers Dam, Karen Dybkjær, Lars Hamberg, Claus Heilmann-Clausen, Erik P. Johannessen, Lars E. Kristensen, Iain Prince and Jan A. Rasmussen GEOLOGICAL SURVEY OF DENMARK AND GREENLAND DANISH MINISTRY OF THE ENVIRONMENT 1 Geological Survey of Denmark and Greenland Bulletin 12 Keywords Lithostratigraphy, biostratigraphy, North Sea Basin, Palaeogene, Neogene. Cover Complex fabric created by multiple small-scale sand intrusions (light) into dark mudstones – such enigmatic fabrics are commonly associated with the sand-rich units of the Rogaland Group in the Siri Canyon area, offshore Denmark. The illustrated section of core is about 10 cm across and is from the lower Tyr Member (Lista Formation) in the Cecilie-1B well (2346.8 m). Photograph: Jakob Lautrup. Chief editor of this series: Adam A. Garde Editorial board of this series: John A. Korstgård, Geological Institute, University of Aarhus; Minik Rosing, Geological Museum, University of Copenhagen; Finn Surlyk, Department of Geography and Geology, University of Copenhagen Scientific editors of this volume: Jon R. Ineson and Martin Sønderholm Editorial secretaries: Jane Holst and Esben W. Glendal Referees: Paul van Veen (Norway) and Robert O’B. Knox (UK) Illustrations: Stefan Sølberg Digital photographic work: Benny M. Schark Graphic production: Knud Gr@phic Consult, Odense, Denmark Printers: Schultz Grafisk, Albertslund, Denmark Manuscript received: 29 August 2005 Final version approved: 8 September 2006 Printed: 29 June 2007 ISSN 1604-8156 ISBN 978-87-7871-196-0 Geological Survey of Denmark and Greenland Bulletin The series Geological Survey of Denmark and Greenland Bulletin replaces Geology of Denmark Survey Bulletin and Geology of Greenland Survey Bulletin.
    [Show full text]
  • Download Download
    GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN 25 • 2011 Upper Cretaceous chalk facies and depositional history recorded in the Mona-1 core, Mona Ridge, Danish North Sea Kresten Anderskouv and Finn Surlyk GEOLOGICAL SURVEY OF DENMARK AND GREENLAND DANISH MINISTRY OF CLIMATE, ENERGY AND BUILDING 1 Geological Survey of Denmark and Greenland Bulletin 25 Keywords Upper Cretaceous chalk, Danish North Sea, Mona-1, facies analysis Cover Detail of a shear-deformed, matrix-supported chalk conglomerate representing a deformed debris-flow deposit (Mona-1 polished core, 10890 ft). Such chalk deposits are typical of the Upper Cretaceous succession in the Mona-1 well and exemplify two important processes of redeposition: fluid-like deformation during debris flow and plastic deformation during slumping or the final stages of debris-flow deposition. Photograph courtesy of Wintershall Noordzee B.V. Chief editor of this series: Adam A. Garde Editorial board of this series: John A. Korstgård, Department of Geoscience, Aarhus University; Minik Rosing, Geological Museum, University of Copenhagen; Finn Surlyk, Department of Geography and Geology, University of Copenhagen Scientific editor of this volume: Jon R. Ineson Editorial secretaries: Jane Holst and Esben W. Glendal Referees: Frans van Buchem (DK) and Maurice E. Tucker (UK) Illustrations: Jette Halskov, Britta Munch and Christian Hagen Digital photographic work: Benny M. Schark Graphic production: Kristian A. Rasmussen Printers: Rosendahls . Schultz Grafisk A/S, Albertslund, Denmark Manuscript received: 6 December 2010 Final version approved: 19 October 2011 Printed: 29 December 2011 ISSN 1604-8156 ISBN 978-87-7871-327-8 Citation of the name of this series It is recommended that the name of this series is cited in full, viz.
    [Show full text]
  • Lithostratigraphy of the Upper Oligocene–Miocene Succession Of
    Lithostratigraphy of the upper Oligocene–Miocene succession in Denmark Rasmussen, Erik Skovbjerg; Dybkjær, Karen; Piasecki, Stefan Published in: Bulletin of the Geological Society of Denmark Publication date: 2010 Document version Publisher's PDF, also known as Version of record Citation for published version (APA): Rasmussen, E. S., Dybkjær, K., & Piasecki, S. (2010). Lithostratigraphy of the upper Oligocene–Miocene succession in Denmark. Bulletin of the Geological Society of Denmark, 22. Download date: 30. sep.. 2020 Bulletin 22_ GSB191-Indhold 04/03/11 12.40 Side 1 GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN 22· 2010 Lithostratigraphy of the Upper Oligocene – Miocene succession of Denmark Erik Skovbjerg Rasmussen, Karen Dybkjær and Stefan Piasecki GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF CLIMATE AND ENERGY Bulletin 22_ GSB191-Indhold 04/03/11 12.40 Side 2 Geological Survey of Denmark and Greenland Bulletin 22 Keywords Lithostratigraphy, Miocene, Upper Oligocene, North Sea, Denmark Cover Upper shoreface sands of the Billund Formation in the Addit gravel pit, central Jylland showing prominent burrows (Ophiomorpha isp.); illustrated section is 40 cm high. Photo: Tom Pallesen. Frontispiece Outcrop of the Kolding Fjord Member, Klintinghoved Formation at Hagenør, Lillebælt. The succession is dominated by organic-rich, lagoonal, silty clay and sand beds deposited as washover fans on the back-barrier flat. Photo: Peter Warna-Moors. Chief editor of this series: Adam A. Garde Editorial board of this series: John A. Korstgård, Department of Earth Sciences, University of Aarhus; Minik Rosing, Geological Museum, University of Copenhagen; Finn Surlyk, Department of Geography and Geology, University of Copenhagen Scientific editor of this volume: Jon R.
    [Show full text]
  • Evaluation of the Quality, Thermal Maturity and Distribution of Potential Source Rocks in the Danish Part of the Norwegian–Danish Basin
    GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN 16 · 2008 Evaluation of the quality, thermal maturity and distribution of potential source rocks in the Danish part of the Norwegian–Danish Basin Henrik I. Petersen, Lars H. Nielsen, Jørgen A. Bojesen-Koefoed, Anders Mathiesen, Lars Kristensen and Finn Dalhoff GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF CLIMATE AND ENERGY Geological Survey of Denmark and Greenland Bulletin 16 Keywords Norwegian–Danish Basin, source rocks, generation potential, maturation Cover Photomicrograph of alginite-rich organic matter from lacustrine sediments of the Frederikshavn Formation in the Terne-1 well (200–210 m depth; see also Fig. 39); the photograph is taken in fluorescence-inducing blue light. The sub-circular structure (c. 200 µm across) is an algal body that resembles the freshwater green alga Botryococcus. Chief editor of this series: Adam A. Garde Editorial board of this series: John A. Korstgård, Geological Institute, University of Aarhus; Minik Rosing, Geological Museum, University of Copenhagen; Finn Surlyk, Department of Geography and Geology, University of Copenhagen Scientific editor of this volume: Jon R. Ineson Editorial secretaries: Jane Holst and Esben W. Glendal Referees: Anthony M. Spencer (Norway) and an anonymous referee Illustrations: Stefan Sølberg, with contributions from Jette Halskov Digital photographic work: Benny M. Schark Layout and graphic production: Annabeth Andersen Printers: Schultz Grafisk, Albertslund, Denmark Manuscript received: 7 December 2007 Final version approved: 25 August 2008 Printed: 28 November 2008 ISSN 1604-8156 ISBN 978-87-7871-232-5 Geological Survey of Denmark and Greenland Bulletin The series Geological Survey of Denmark and Greenland Bulletin replaces Geology of Denmark Survey Bulletin and Geology of Greenland Survey Bulletin.
    [Show full text]
  • Of the of the Project
    SPBA-Compleet 22-04-10 13:41 Pagina i PetroleumPetroleum GeologicalGeological AtlasAtlas ofof thethe SouthernSouthern PermianPermian BasinBasin AreaArea Southern Permian Basin Atlas Hans Doornenbal and Alan Stevenson (editors) Cover image provided by NASA ©2010 TNO and contributions of individual authors ISBN 978-90-73781-61-0 Doornenbal, J.C. and Stevenson, A.G. (editors), 2010. Petroleum Geological Atlas of the Southern Permian Basin Area. EAGE Publications b.v. (Houten) SPBA-Compleet 22-04-10 13:41 Pagina ii BGS – British Geological Survey British Geological Survey Founded in 1835, the British Geological Survey (BGS) is the world’s oldest national Geological Survey and the United Kingdom’s premier centre for earth science Headquarters Marine Geosciences information and expertise. The BGS client base is drawn from the public and private sectors both in the UK and internationally. The BGS strategy is to focus Keyworth Murchison House its activities on key issues related to energy and environmental change and to address complex environmental challenges requiring decisions in the short- and Nottingham NG12 5GG West Mains Road medium-term, including carbon capture and storage, radioactive waste management, natural hazards, resource security and environmental protection. BGS plays United Kingdom Edinburgh EH9 3LA a major role in the delivery of the Natural Environment Research Council (NERC) strategy – ‘Next Generation Science for Planet Earth’ and the ‘Living With United Kingdom Environmental Change’ (LWEC) programme. BGS enhances its culture of commercial innovation to ensure that its knowledge is shared and exploited to deliver T +44 115 936 3100 T +44 131 667 1000 societal and economic impacts and benefits.
    [Show full text]