Back Matter (PDF)

Total Page:16

File Type:pdf, Size:1020Kb

Back Matter (PDF) General Index This excludes references to place names and stratigraphic unit names as these are covered in separate lists. Pages numbers in italics refer to Figures and Tables abbreviations in names 7 basement boudinage 276, 288 Abeloya 83 Bjornoya 219-20 boundary faults 316 acritarchs 233-4, 248 sequences 32 brachiopods 272, 327, 379 Admiralty 16 structures 27 Breibogen Fault 48, 148, 301,305 Admiralty chart 16 see also proto-basement Breibogen Fault Zone 26, 316 Adriabukta folding (HSDT) 33 Bashkirian-Moscovian events 330-1 Brentskardhaugen Bed 58, 363, 373, 374 aerial photography 18 basic igneous petrography 76 Broggerhalvoya structure 168 aeromagnetic survey 422-3 basic layers 106 Bruce, W. S. 16 Agardhbukta Lineament 344 Bathonian transgression 363 bryophytes Albert I Land 299-300 Bathonian-Tithonian events 381-2 fossil 394 Albian-Aptian events 382 bathymetric chart sheet lines 14 living 11 ammonite zonation 369-71,354, 378 bathymetry 7-8, 420 bryozoans 327-8, 355 AMOSEAS 20 bay ice 8 Byrd, R. 19 amphibolites 123, 165, 283-4 Bear Island see Bjornoya Amundson, R. 19 belemnites 371-2, 378-9 13C plot 249 Andr~e Land-Dickson Land Terrane (ADLT) 32, bentonite 454 calc-alkalic basites 106 33, 147-8, 285, 301 Berriasian stage 369 calcite 189 anhydrite 67, 310, 454 Berzeliustinden 203 Caledonian (Ny Friesland) Orogeny 33, 34, 36, Anisian environments 358 Bibliography of Svalbard 20 151, 192, 219, 288 anoxia, Early Siberian 260 Billefjorden Fault Zone (BFZ) 26, 70, 129, 146-7, structures 204 anoxic facies 356-7 285, 301-3, 303-5, 316, 409 vergencies 278, 280 angiosperms 11 Billefjorden Lineament 53, 363 Calypsobyen coal 388 annelid worms Billefjorden Trough 70, 315, 344 Calypsostranda Basin 180, 449 fossil 379 biota Cambrian living 10 living 10 basal unconformity 266 anthracite 227, 450 fossil early diastrophism 266 aplite dykes 106, 142 Paleogene 393-4 lithic units 116-17, 192 Aptian-Albian events 382 Jurassic-Cretaceous 378-80 time scale 259, 260 Arc of Meridian Project 16 Triassic 353-6 see also Cambro-Ordovician Arc of Meridian Surveys 76, 96 Carboniferous-Permian 324-8 Cambridge Arctic Shelf Programme (CASP) 22 Archean 151,229 Devonian 291-6 Cambridge University expeditions 18, 389 Arktikugol 13 Silurian 272 Cambridgebreen Shear Zone 129, 305 arthropods Cambro-Ordovician 260-4 Cambro-Ordovician fossil 293, 394 Vendian 248-9 biotas 260-2 living 10, Pre-Vendian 231-5 correlation within Svalbard 262-4 Artinskian events 333 birds 10 palinspastics 268-70 Asselian Sakmarian events 332-3 Biskayerfonna Horst 149 sedimentary environments 264-6 Atomfjella antiform 27, 124 Biskayerfonna-Holtedahlfonna Horst 148 tectonic environments 266-8 Atomfjella arch 123 Biskayerfonna-Holtedahlfonna terrane (BHFT) tectonothermal events 270-1 Atomfjella Complex 123 32, 33, 148-50, 230, 285, 300-1 terranes 268-70 augen gneiss 283 bivalves 294, 372, 379, 394 Carnian environments 358-60 Austfjorden tectonothermal event 33 Bjornoya 212 Carboniferous Austfonna 96 biota biota 324-8 Axel Heiberg Island 36 Cambro-Ordovician 260 economic deposits 310, 450 Vendian 248 history of research 310 coal 450 lithic units 312-14 Backlund, H. G. 18, 76 cover sequences 36 Bjernoya 212, 215-17 baked sediment 85 lithic units 210, 257 Central Basin 66-73 Balliolbreen Fault 112, 305 Paleozoic 212-19 Spitsbergen, NE 77, 112 Baltica 253-4, 287 pre-Vendian 231 Spitsbergen, NW 134-5 Bangenhuken anticline 27 Triassic 212-13, 350, 361 Spitsbergen, SW 183-7 Bangenhuk granitoid 124 palinspastic reconstructions 269 lithostratigraphic scheme 313 Barents craton/Barentsia 108, 287 structure 219-22 palinspastics 335 Barents Sea 5, 8, 209, 350, 368 tectonic setting sedimentary environments 318-23 Barents shelf 7, 424, 427-8 Cambro-Ordovician 266 structural frame 314-16 petroleum potential 20 Silurian 280 tectonic control of sedimentation 328-32 structural elements 26 volcanic rocks 252 time scale 316 Barents, W 16 Bjornoya Basement Terrane (BOBT) 32, 34 Cenomanian-Maastrichtian events 382-3, 386 Barentsburg 13, 388 Bjornoya Basin 315-16 Central basement terranes 32, 33-4 Barentsoya Bjornoya Platform Terrane (BOPT) 32, 36 Central Basin biostratigraphy 89-91 Black Carbonate Pelite (BCP) 167 coal 449 ice cover 436 Blomstrand, C. B. 16 geomorphology 48 igneous bodies 91 Blomstrandhalvoya graben-syncline 27 lithic units 48-72, 390-1 lithic units 87-9, 350 Blomstrandhalvoya Basins 150-1,300 structural development 73-4, 409 Barentsoya Edgeoya Platform Terrane (BEPT) Bonnia-Holmia faunas 259, 264 structural setting 48, 344 32, 36 bornite 189 Central Basin Terrane (CBT) 32, 35 barite 454 Botniahalvoya 103 Central East Greenland Province 38 Barremian events 382 Botniahalvoya unconformity (NAWT) 32 Central Spitsbergen 73-4 basalts 76, 84, 85 Botonian-Toyonian faunas 259, 264 Central Svalbard terranes 38 516 GENERAL INDEX Central Province (Vendian) 254-5 sedimentary record 296-9 Fairbairn, P. E. 18 central terrane palinspastics 268-70 sequence of events 306-9 Falcon, N. L. 18 central terranes (SW Spitsbergen) 199-200 tectonics 299-303 Famennian events 309 Central vent volcanics (Quaternary) 423 time scale 289 faults 172-3 Central West Fault Zone 48, 316 dextral transpression/transtension, Paleogene boundary 316 Centralwestern Spitsbergen see Spitsbergen 410-11 lineaments 26 chalcocite 189 diamictites 21, 100, 118 major zones 25, 27 chalcopyrite 154, 189, 197, 454 Dickson Land 62 strike-slip 38, 303, 306 Challinor's sections 389-90, 400, 402-8 dinoflagellates 380, 394 dextral 173-4, 390 charts, hydrographic 14 dinosaurs 20 sinistral 204 Changxingian stage 351 footprints fauna, living 10 chromium-rich dolostone 158 carnosaur 55 feldspathite 31,283 chronometric scale 26-7, 29, 30 Iguanodon 20, 58, 380 ferns see pteridophytes chronostratic scale 25-6 Dirksodden Nappe 129 Festningen section (Festungs Profil) 18, 49, 62, 343 Chydeniusbreen granite 113 Dirksodden Thrust 129 Finnmarkian phase 36 cirripedes 379 discontinuities (faults and unconformities) 23, 26 fish claims 11 discovery of Svalbard 5, 11 fossil 137, 138, 291-3, 295, 353, 394 climate records 444-5 dolerites 76, 106, 112 living 10 glacial 436 dolostone 31, 67, 70, 158, 163, 169-70, 265 fission track analysis 398 Jurassic-Cretaceous 380-1 Dragon Oil p.l.c. 94 fjords 4, 48 Vendian 249 Duvefjorden Complex 104, 108 Fleming, W. L. S. 18 coal 37, 47, 51, 72, 73, 216, 217, 310, 363 Duvefjorden granites 106 flint concretions 70 coal fields 50, 51, 154, 389 dykes and sills 76, 106, 112, 113, 377-8 flora see plants coal mining 11,209 Floraberget anticline 27 coccoliths 372, 379 East Spitsbergen Basin 315 flower structure 177 Colesbukta well 58, 451, 452 East Greenland aulacogen 242-3 flowering plants 11 collisional orogeny 288 East Spitsbergen current 8 fluid springs 424-6 compressional tectonics 38 East Svalbard terranes 38 fold and thrust front 48 conchostraca 294 East Svalbard Vendian Province 254 fold-thrust belt 400 conodonts 354 Eastern basement terranes 32-3 foraminifers 326-7, 372, 379 continental drift 21, 37-8 Eastern Svalbard Platform (ESP) 32, 75-7, 315, Forlandsundet Basin 175-6 continental shelf 12 344 coal 449 convection polygon 433 Barentsoya 86-91 origin 176-7 convergence, tectonic 38 Edgeoya 86-91 Forlandsundet Graben 268 Conway, Sir Martin 5, 16, 189, 340 Hopen 91-3 Paleogene 157-8, 388, 391,399, 402-9 copper minerals 454 Kong Karls Land 83-6 Forlandsundet Graben Terrane (FSGT) 32, 34 corals 272, 327, 379 NE Spitsbergen 77-80 formation, stratigraphic 29 covellite 189 SW Nordaustlandet 80-3 Frasnian Famennian events 309 cover sequences 21 Tusenoyane 86-91 Frebold, H. 18, 363 Bjornoya 220-2 echinoderms freeze-thaw processes 433-4 NE Spitsbergen 112 fossil 279, 379 frozen ground 10 cover terranes 32, 35-6 living 10 fuchsite 158 Cretaceous eclogite 165 age estimation 371-2 economic geology biotas 372, 378-80 coal mining 449-51 galena 189, 197, 210 climates 380-1 metalliferous mining 453-4 Garwood, E. J. 16, 18 coal 363, 450 non-metaliferous mining 454 gastropods history 363 petroleum 451-2 fossil 328, 379, 394 igneous activity 363-5, 377-8 Edgeoya 86 7 living 10 lithic units 52, 374-7 biostratigraphy 89-91 geochemistry 102, 126-7 sedimentary environments 382-3 ice cover 436 geographical nomenclature 5 sedimentary sequences 386-7 igneous bodies 91 geological maps stratal scheme 366 lithic units 87-8 outcrops stratigraphy 366-8 oil exploration 93-5 Neogene-Quaternary 419 structural frame 365 Edgeoya-Barentsoya monocline 344 Paleogene 50, 389 tectonic environments 383 Ediacara biota 167 Jurassic-Cretacous 364 time scale 371-2 Ediacara epoch 244 Triassic 341 cryoturbation 433 Edmonds, J. M. 18 Carboniferous-Permian 311 crystalline rocks see igneous also metamorphic Eidembreen tectonics 34, 36, 154, 169, 266-8 Devonian 290 Eifelian-Givetian events 308-9 Silurian 273 Danskoya Basin 153 Ellesmere Island 253, 255, 306 Cambro-Ordovician 258 daylight 8 Ellesmerian (M'Clintock) orogeny 38, 270-1 Proterozoic 228, 245 decoupling in transpression/transtension 410 ellipsoids, deformed 112 regions de Geer, G. 16, 18, 340, 388, 389 Ellsworth, L. 19 Bjornoya 211 deformation events 151-2 Emsian events 308 Central Basin 47, 54, 55, 56, 58 delta complexes 58, 87 environmental regulations 12-13 Nordauslandet 101 desiccation cracks 434 Eoarchean 28 Oscar II Land 58, 156 Devonian Eocene events 415-17 Prince Karls Forland 156 biostratigraphy and correlation 289-91 Eolusletta Shear Zone 130 Spitsbergen NW 133, 139 biota 291-5 escape tectonics 38, 277 Spitsbergen SW 181 coal 450 evaporites 67, 70 geomorphology 48, 431-4 history 289 exploration history 16 geotectonic
Recommended publications
  • Handbok07.Pdf
    - . - - - . -. � ..;/, AGE MILL.YEAR$ ;YE basalt �- OUATERNARY votcanoes CENOZOIC \....t TERTIARY ·· basalt/// 65 CRETACEOUS -� 145 MESOZOIC JURASSIC " 210 � TRIAS SIC 245 " PERMIAN 290 CARBONIFEROUS /I/ Å 360 \....t DEVONIAN � PALEOZOIC � 410 SILURIAN 440 /I/ ranite � ORDOVICIAN T 510 z CAM BRIAN � w :::;: 570 w UPPER (J) PROTEROZOIC � c( " 1000 Ill /// PRECAMBRIAN MIDDLE AND LOWER PROTEROZOIC I /// 2500 ARCHEAN /(/folding \....tfaulting x metamorphism '- subduction POLARHÅNDBOK NO. 7 AUDUN HJELLE GEOLOGY.OF SVALBARD OSLO 1993 Photographs contributed by the following: Dallmann, Winfried: Figs. 12, 21, 24, 25, 31, 33, 35, 48 Heintz, Natascha: Figs. 15, 59 Hisdal, Vidar: Figs. 40, 42, 47, 49 Hjelle, Audun: Figs. 3, 10, 11, 18 , 23, 28, 29, 30, 32, 36, 43, 45, 46, 50, 51, 52, 53, 54, 60, 61, 62, 63, 64, 65, 66, 67, 68, 69, 71, 72, 75 Larsen, Geir B.: Fig. 70 Lytskjold, Bjørn: Fig. 38 Nøttvedt, Arvid: Fig. 34 Paleontologisk Museum, Oslo: Figs. 5, 9 Salvigsen, Otto: Figs. 13, 59 Skogen, Erik: Fig. 39 Store Norske Spitsbergen Kulkompani (SNSK): Fig. 26 © Norsk Polarinstitutt, Middelthuns gate 29, 0301 Oslo English translation: Richard Binns Editor of text and illustrations: Annemor Brekke Graphic design: Vidar Grimshei Omslagsfoto: Erik Skogen Graphic production: Grimshei Grafiske, Lørenskog ISBN 82-7666-057-6 Printed September 1993 CONTENTS PREFACE ............................................6 The Kongsfjorden area ....... ..........97 Smeerenburgfjorden - Magdalene- INTRODUCTION ..... .. .... ....... ........ ....6 fjorden - Liefdefjorden................ 109 Woodfjorden - Bockfjorden........ 116 THE GEOLOGICAL EXPLORATION OF SVALBARD .... ........... ....... .......... ..9 NORTHEASTERN SPITSBERGEN AND NORDAUSTLANDET ........... 123 SVALBARD, PART OF THE Ny Friesland and Olav V Land .. .123 NORTHERN POLAR REGION ...... ... 11 Nordaustlandet and the neigh- bouring islands........................... 126 WHA T TOOK PLACE IN SVALBARD - WHEN? ....
    [Show full text]
  • Petroleum, Coal and Research Drilling Onshore Svalbard: a Historical Perspective
    NORWEGIAN JOURNAL OF GEOLOGY Vol 99 Nr. 3 https://dx.doi.org/10.17850/njg99-3-1 Petroleum, coal and research drilling onshore Svalbard: a historical perspective Kim Senger1,2, Peter Brugmans3, Sten-Andreas Grundvåg2,4, Malte Jochmann1,5, Arvid Nøttvedt6, Snorre Olaussen1, Asbjørn Skotte7 & Aleksandra Smyrak-Sikora1,8 1Department of Arctic Geology, University Centre in Svalbard, P.O. Box 156, 9171 Longyearbyen, Norway. 2Research Centre for Arctic Petroleum Exploration (ARCEx), University of Tromsø – the Arctic University of Norway, P.O. Box 6050 Langnes, 9037 Tromsø, Norway. 3The Norwegian Directorate of Mining with the Commissioner of Mines at Svalbard, P.O. Box 520, 9171 Longyearbyen, Norway. 4Department of Geosciences, University of Tromsø – the Arctic University of Norway, P.O. Box 6050 Langnes, 9037 Tromsø, Norway. 5Store Norske Spitsbergen Kulkompani AS, P.O. Box 613, 9171 Longyearbyen, Norway. 6NORCE Norwegian Research Centre AS, Fantoftvegen 38, 5072 Bergen, Norway. 7Skotte & Co. AS, Hatlevegen 1, 6240 Ørskog, Norway. 8Department of Earth Science, University of Bergen, P.O. Box 7803, 5020 Bergen, Norway. E-mail corresponding author (Kim Senger): [email protected] The beginning of the Norwegian oil industry is often attributed to the first exploration drilling in the North Sea in 1966, the first discovery in 1967 and the discovery of the supergiant Ekofisk field in 1969. However, petroleum exploration already started onshore Svalbard in 1960 with three mapping groups from Caltex and exploration efforts by the Dutch company Bataaffse (Shell) and the Norwegian private company Norsk Polar Navigasjon AS (NPN). NPN was the first company to spud a well at Kvadehuken near Ny-Ålesund in 1961.
    [Show full text]
  • Terrestrial Inputs Govern Spatial Distribution of Polychlorinated Biphenyls (Pcbs) and Hexachlorobenzene (HCB) in an Arctic Fjord System (Isfjorden, Svalbard)*
    Environmental Pollution 281 (2021) 116963 Contents lists available at ScienceDirect Environmental Pollution journal homepage: www.elsevier.com/locate/envpol Terrestrial inputs govern spatial distribution of polychlorinated biphenyls (PCBs) and hexachlorobenzene (HCB) in an Arctic fjord system (Isfjorden, Svalbard)* * Sverre Johansen a, b, c, Amanda Poste a, Ian Allan c, Anita Evenset d, e, Pernilla Carlsson a, a Norwegian Institute for Water Research, Tromsø, Norway b Norwegian University of Life Sciences, Ås, Norway c Norwegian Institute for Water Research, Oslo, Norway d Akvaplan-niva, Tromsø, Norway e UiT, The Arctic University of Norway, Tromsø, Norway article info abstract Article history: Considerable amounts of previously deposited persistent organic pollutants (POPs) are stored in the Received 20 July 2020 Arctic cryosphere. Transport of freshwater and terrestrial material to the Arctic Ocean is increasing due to Received in revised form ongoing climate change and the impact this has on POPs in marine receiving systems is unknown This 11 March 2021 study has investigated how secondary sources of POPs from land influence the occurrence and fate of Accepted 13 March 2021 POPs in an Arctic coastal marine system. Available online 17 March 2021 Passive sampling of water and sampling of riverine suspended particulate matter (SPM) and marine sediments for analysis of polychlorinated biphenyls (PCBs) and hexachlorobenzene (HCB) was carried out Keywords: Particle transport in rivers and their receiving fjords in Isfjorden system in Svalbard. Riverine SPM had low contaminant < S e Terrestrial runoff concentrations ( level of detection-28 pg/g dw PCB14,16 100 pg/g dw HCB) compared to outer marine Environmental contaminants sediments 630-880 pg/g dw SPCB14,530e770 pg/g dw HCB).
    [Show full text]
  • Checklist of Lichenicolous Fungi and Lichenicolous Lichens of Svalbard, Including New Species, New Records and Revisions
    Herzogia 26 (2), 2013: 323 –359 323 Checklist of lichenicolous fungi and lichenicolous lichens of Svalbard, including new species, new records and revisions Mikhail P. Zhurbenko* & Wolfgang von Brackel Abstract: Zhurbenko, M. P. & Brackel, W. v. 2013. Checklist of lichenicolous fungi and lichenicolous lichens of Svalbard, including new species, new records and revisions. – Herzogia 26: 323 –359. Hainesia bryonorae Zhurb. (on Bryonora castanea), Lichenochora caloplacae Zhurb. (on Caloplaca species), Sphaerellothecium epilecanora Zhurb. (on Lecanora epibryon), and Trimmatostroma cetrariae Brackel (on Cetraria is- landica) are described as new to science. Forty four species of lichenicolous fungi (Arthonia apotheciorum, A. aspicili- ae, A. epiphyscia, A. molendoi, A. pannariae, A. peltigerina, Cercidospora ochrolechiae, C. trypetheliza, C. verrucosar- ia, Dacampia engeliana, Dactylospora aeruginosa, D. frigida, Endococcus fusiger, E. sendtneri, Epibryon conductrix, Epilichen glauconigellus, Lichenochora coppinsii, L. weillii, Lichenopeltella peltigericola, L. santessonii, Lichenostigma chlaroterae, L. maureri, Llimoniella vinosa, Merismatium decolorans, M. heterophractum, Muellerella atricola, M. erratica, Pronectria erythrinella, Protothelenella croceae, Skyttella mulleri, Sphaerellothecium parmeliae, Sphaeropezia santessonii, S. thamnoliae, Stigmidium cladoniicola, S. collematis, S. frigidum, S. leucophlebiae, S. mycobilimbiae, S. pseudopeltideae, Taeniolella pertusariicola, Tremella cetrariicola, Xenonectriella lutescens, X. ornamentata,
    [Show full text]
  • Foraminifera1 Stratigraphy of Raised Marine Deposits, Representing Isotope Stage 5, Prins Karls Forland, Western Sval Bard
    Foraminifera1 stratigraphy of raised marine deposits, representing isotope stage 5, Prins Karls Forland, western SVal bard HELENE BERGSTEN. TORBJORN ANDERSON and OLAFUR INGOLFSSON Bergsten, H., Andersson. T. & Ingolfsson, 0. 1998: Foraminiferd stratigraphy of raised marine deposits, representing isotope stage 5. Prins Karls Forland, western Svalbard. Polar Research 17(1). 81-91. Two raised marine sequences from Prim Karls Forland, western Svalbard, interpreted to have been deposited during part of isotope substage Se (Eemian) and substage 5a, were studied for foraminifera content. Time constraints are given by I4C ages, infrared stimulated luminescence age estimates and amino acid ratios in suhfossil marine molluscs. A diamicton (unit B) separates the two marine sequences and reflects an advancement of local glaciers sometime late in isotope stage 5. The two marine sequences contain diverse benthic foraminifera1 faunas, indicating periods of a relatively warm and seasonally ice-free marine shelf environment. Compared to the lowermost sequence (unit A), the upper marine sequence (unit C) seems to reflect a more shallow environment that could have resulted from the global lowering of the sea level towards the end of isotope stage 5. Our results further emphasise the problem of biostratigraphic distinction between interglacial and interstadial deposits at high latitudes, with temperature conditions for substage Sa close to those of substage 5e and present conditions. Helene Bergsten, Torbjorn Andersson and Olufur Ingdlfsson, Earth Sciences Centre, Goteborg University, Box 460, S-405 30 Goteborg, Sweden. Introduction Chronology and glacial history The Poolepynten site is situated on Prins Karls Sediments in the Poolepynten sections are ex- Forland, western Svalbard at N78'27'El l"40' posed in up to 10 metre high coastal cliffs over a (Fig.
    [Show full text]
  • Tertiary Fold-And-Thrust Belt of Spitsbergen Svalbard
    Winfried K. Dallmann • Arild Andersen • Steffen G. Bergh • Harmond D. Maher Jr. • Yoshihide Ohta Tertiary fold-and-thrust belt of Spitsbergen Svalbard ' ~dl... ,, !!~"\\ MEDDELELSER NR.128 9,.~,f OSLO 1993 k ·pOlARll'l'>'\ MEDDELELSER NR. 128 WINFRIED K. DALLMANN, ARILD ANDRESEN, STEFFEN G. BERGH, HARMON D. MAHER Jr. & YOSHIHIDE OHTA Tertiary f old-and-thrust belt of Spitsbergen Svalbard COMPILATION MAP, SUMMARY AND BIBLIOGRAPHY NORSK POLARINSTITUTT OSLO 1993 Andresen, Arild: Univ. Oslo, Institutt for geologi, Pb. 1047 Blindern, N-0316 Oslo Bergh, Steffen G.: Univ. Tromsø, Institutt for biologi og geologi, N-9037 Tromsø Dallmann, Winfried K.: Norsk Polarinstitutt, Pb. 5072 Majorstua, N-0301 Oslo Maher, Harmon D., Jr.: Univ. Nebraska, Dept. of Geography and Geology, Omaha, USA-Nebraska 68182-0199 Ohta, Yoshihide: Norsk Polarinstitutt, Pb. 5072 Majorstua, N-0301 Oslo ISBN 82-7666-065-7 Printed December 1993 Cover photo by W. K. Dallmann: Folded Triassic sandstones and shales within the interior part of the Tertiary fold-and-thrust belt at Curie­ Sklodowskafjellet, Wedel Jarlsberg Land, Svalbard. CONTENTS: Introduction 5 Map data and explanatory remarks 6 Sources, compilation and accuracy of the geological base map 7 Explanation of map elements 7 Stratigraphy 7 Structure 8 Outline of the Tertiary fold-and-thrust belt of Spitsbergen 10 Tectonic setting 10 Dimensions and directions 11 Structural subdivision and characteristics 13 Interior part of foldbelt 13 Western Basement High 15 Forlandsundet Graben 16 Central Tertiary Basin 16 Billefjorden Fault Zone 17 Lomfjorden Fault Zone 17 Structural descriptions (including explanation of cross sections) 17 Sørkapp-Hornsund area 17 Interior Wedel Jarlsberg Land/Torell Land - Bellsund 19 Western and Central Nordenskiold Land 21 Oscar li Land 22 Brøggerhalvøya 24 Billefjorden - Eastern Nordenskiold Land 24 Agardhbukta - Negribreen 25 Bibliography 29 Maps and map descriptions 29 Proceedings of symposia etc.
    [Show full text]
  • ESG Perspectives June 2019 Svalbard Sojourn an Arctic
    June 2019 ESG Perspectives ™ SVALBARD SOJOURN: AN ARCTIC EXPERIENCE by Bob Smith, President & CIO islands are 60% glaciated with some of the world’s fastest-moving glaciers. The balance of the region is 30% barren ground, and 10% is covered with very low ground vegetation. In contrast to other Arctic regions, the Svalbard has no indigenous population and there is no historical evidence that the Vikings settled in the area during their time. In fact, it was the 1596 Dutch expedition of Willem Barents who discovered and drew maps of the region before his ship was crushed by freezing sea ice leading to his untimely death. However, the work of this expedition survived, and it led to the exploration of the region by other European countries over the Photo of Bob Smith in Kungsfjord, Svalbard centuries. This eventually gave rise to the exploitation It is said that what happens in the Arctic doesn’t stay of the natural resources of the region as a destination in the Arctic. That is because this region provides for whalers, fur trappers, and seal hunters, as well as essential global climate regulation and substantial other animal-based products. With the industrialization ecosystem benefits to humanity outside and beyond of Europe and the arrival of steel-hulled ships in the its boundaries. Indeed, the Arctic environment, and early 1900s, this region also eventually became a source human society and its economic activities are deeply for industrial minerals and, in particular, coal. connected to each other, representing a pivotal link in a complex adaptive global ecosystem.
    [Show full text]
  • Poland, Piotr Glowacki
    Piotr GŁOWACKI Associate Professor Title Polish activity in Svalbard – Report from 2016 – ASSW – FARO Meeting, Prague, Czech Republik, 1 April 2017 Polish activity at Svalbard in 2016 Kaffioyra Petunia Calypso Hornsund area Greenlad Sea: (Knipovich Reach) 12 July 2002 Terra/MODIS © NASA “Visible Earth” Polish camp activity in Hornsund area in 2016 Vimsoden Treskelen Werenskiold Hamberbukta Gnalberget Hornsund Station Calypso 12 July 2002 Terra/MODIS © NASA “Visible Earth” Polish Polar Station Hornsund hosted in 2016 • Winter crew – 11 persons x 2 • Technical staff – 13 persons • Polish scientists – 64 persons • Students from Maritime Academy – 8 persons • Foreign scientists – 19 persons (Czech - 4, Spein -2, Germany - 2, Norway - 3, UK - 3, USA - 5) Seasonal station in Petuniabukta owner: Adam Mickiewicz University in Poznan (5 July – 5 September) 16 scientists ; 465 man-days Photo: J. Malecki Seasonal station at Kaffiøyra (Oscar II Land) owner: Nicolaus Copernicus University in Torun (15 – 24 April) and (5 July – 8 September) 16 scientists; 438 man-days Seasonal station BARANOWKA (Wedel Jarlsberg Land) owner: University of Wroclaw (4 July – 6 September) 3 scientists; 130 man-days s/y OCEANIA AREX 2016 (22 June - 14 August) Crew 14 persons + 14 scientists Exchange ca 40 scientists from Poland and Germany (700 person days) Scientific - training vessel Horyzont II on Svalbard in 2016 First trip (26 June – 18 July) Secound trip (11 September - 5 Oktober) 16 crew 16 crew 20 students 20 students 64 members from expeditions 45 members from expedition EDU-ARTIC (2016 – 2019) „Innovative educational program attracting young people to natural sciences and polar research” Grant supported by: Horizon 2020 Coordinator: Institute of Geophysics PAS Partners: • American Systems Ltd.
    [Show full text]
  • Appendix: Economic Geology: Exploration for Coal, Oil and Minerals
    Downloaded from http://mem.lyellcollection.org/ by guest on October 1, 2021 PART 4 Appendix: Economic geology: exploration for coal, oil and Glossary of stratigraphic names, 463 minerals, 449 References, 477 Index of place names, 455 General Index, 515 Alkahornet, a distinctive landmark on the northwest, entrance to Isfjorden, is formed of early Varanger carbonates. The view is from Trygghamna ('Safe Harbour') with CSE motorboats Salterella and Collenia by the shore, with good anchorage and easy access inland. Photo M. J. Hambrey, CSE (SP. 1561). Routine journeys to the fjords of north Spitsbergen and Nordaustlandet pass by the rocky coastline of northwest Spitsbergen. Here is a view of Smeerenburgbreen from Smeerenburgfjordenwhich affords some shelter being protected by outer islands. On one of these was Smeerenburg, the principal base for early whaling, hence the Dutch name for 'blubber town'. Photo N. I. Cox, CSE 1989. Downloaded from http://mem.lyellcollection.org/ by guest on October 1, 2021 The CSE motorboat Salterella in Liefdefjorden looking north towards Erikbreen with largely Devonian rocks in the background unconformably on metamorphic Proterozoic to the left. Photo P. W. Web, CSE 1989. Access to cliffs and a glacier route (up Hannabreen) often necessitates crossing blocky talus (here Devonian in foreground) and then possibly a pleasanter route up the moraine on to hard glacier ice. Moraine generally affords a useful introduction to the rocks to be traversed along the glacial margin. The dots in the sky are geese training their young to fly in V formation for their migration back to the UK at the end of the summer.
    [Show full text]
  • A Contribution to the Knowledge of Bryophytes in Polar Areas Subjected
    Ǘ Digitally signed by Piotr Ǘ Otrba Date: 2018.12.31 18:02:17 Z Acta Societatis Botanicorum Poloniae DOI: 10.5586/asbp.3603 ORIGINAL RESEARCH PAPER Publication history Received: 2018-08-10 Accepted: 2018-11-26 A contribution to the knowledge of Published: 2018-12-31 bryophytes in polar areas subjected to Handling editor Michał Ronikier, W. Szafer rapid deglaciation: a case study from Institute of Botany, Polish Academy of Sciences, Poland southeastern Spitsbergen Authors’ contributions AS: designed and coordinated the study, determined the 1 2 3 moss specimens, wrote the Adam Stebel *, Ryszard Ochyra , Nadezhda A. Konstantinova , manuscript; RO: designed Wiesław Ziaja 4, Krzysztof Ostafin 4, Wojciech Maciejowski 5 the study, determined the 1 Department of Pharmaceutical Botany, Faculty of Pharmacy with Division of Laboratory moss specimens, wrote the Medicine, Medical University of Silesia in Katowice, Ostrogórska 30, 41-200 Sosnowiec, Poland manuscript, contributed 2 Department of Bryology, W. Szafer Institute of Botany, Polish Academy of Sciences, Lubicz 46, the distribution maps; NAK: 31-512 Cracow, Poland determined the liverwort 3 Kola Science Center, Russian Academy of Sciences, 184256, Kirovsk, Murmansk District, Russia specimens, wrote the 4 Institute of Geography and Spatial Management, Jagiellonian University, Gronostajowa 7, manuscript; WZ: collected the 30-387 Cracow, Poland specimens, developed the 5 Institute of the Middle and Far East, Jagiellonian University, Gronostajowa 3, 30-387 Cracow, tables, wrote the manuscript; Poland KO: collected the specimens, developed the tables, * Corresponding author. Email: [email protected] contributed the study area map; WM: conceived and coordinated the study, collected the specimens, developed the Abstract tables, wrote the manuscript, e paper provides a list of 54 species of bryophytes (48 mosses and six liverworts) contributed the study area map collected from Spitsbergen, the largest island of the Arctic Svalbard archipelago Funding (Norwegian Arctic), in 2016.
    [Show full text]
  • Supplement of Solid Earth, 12, 1025–1049, 2021 © Author(S) 2021
    Supplement of Solid Earth, 12, 1025–1049, 2021 https://doi.org/10.5194/se-12-1025-2021-supplement © Author(s) 2021. CC BY 4.0 License. Supplement of Early Cenozoic Eurekan strain partitioning and decoupling in central Spitsbergen, Svalbard Jean-Baptiste P. Koehl Correspondence to: Jean-Baptiste P. Koehl ([email protected]) The copyright of individual parts of the supplement might differ from the article licence. 1 S1: (a) Photographs in non-polarized and (b) polarized light of a thick section in Devonian sandstone including fractured quartz (qz) crosscut by healed fractures (hf) showing no displacement and by quartz-rich cataclastic fault rock filled with calcite cement (upper part); (c) Photographs in non-polarized and (d) polarized light of cataclased Devonian sandstone comprised of quartz crystals showing mild undulose extinction (ue) and grainsize reduction along the subvertical, east-dipping fault in the gully under the coal mine in Pyramiden (see Figure 2 for the location of the fault). Brittle cracks incorporate clasts of quartz, and a matrix of quartz, calcite and brownish, iron-rich clay minerals. 2 S2: Uninterpreted seismic sections in Sassenfjorden–Tempelfjorden (a–f) and Reindalspasset (g). See Figure 1b for location. 3 S3: Field photograph of steeply east-dipping, partly overturned Lower Devonian dark sandstone near the bottom of the gully below the mine entrance. 4 S4: Uninterpreted field photograph of Figure 3b in Pyramiden. 5 S5: (a) Interpreted and (b) uninterpreted field photograph along the northern shore of Sassenfjorden showing uppermost Pennsylvanian–lower Permian strata of the Wordiekammen and Gipshuken formations thrusted and folded top-west by a low-angle Eurekan thrust.
    [Show full text]
  • Caledonian Anatexis of Grenvillian Crust: a U/Pb Study of Albert I Land, NW Svalbard
    NORWEGIAN JOURNAL OF GEOLOGY Caledonian anatexis of Grenvillian crust 173 Caledonian anatexis of Grenvillian crust: a U/Pb study of Albert I Land, NW Svalbard Per Inge Myhre, Fernando Corfu & Arild Andresen Myhre, P.I., Corfu, F. & Andresen, A.: Caledonian anatexis of Grenvillian crust: a U/Pb study of Albert I Land, NW Svalbard. Norwegian Journal of Geology, Vol. 89, pp. 173-191. Trondheim 2008. ISSN 029-196X. Dating by U-Pb ID-TIMS of zircon, titanite and monazite has been carried out on orthogneiss, granite and migmatite from Albert I Land Terrane, Northwest Svalbard, to investigate the origin of this terrane and its role within the North Atlantic Caledonides. Detrital zircons in a migmatized metasedimentary rock of the Smeerenburgfjorden Complex indicate deposition after about 1070 Ma. Zircon and titanite from orthogneiss within the same complex yield an upper intercept age of 967.9 ± 4.7 Ma interpreted to date crystallization of the igneous protolith. Monazite ages of 419.7 ± 0.5 Ma from the orthogneiss are interpreted to date Caledonian reworking. Other migmatite and granite samples of the Smeerenburgfjorden Com- plex record monazite growth during a 6–8 My long period commencing at c. 430 Ma. This period concluded with the intrusion of granitoids with ages of 421.7 ± 0.6 Ma and 418.8 ± 0.7 Ma. The latter is coeval with the Hornemantoppen Batholith emplaced at 418.4 ± 0.8 Ma. The identification of late Grenvillian (Rigolet) magmatic and Caledonian (Scandian) magmatic and metamorphic events, combined with other stratigraphic analogies, supports a link with Svalbard’s Nordaustlandet Terrane as well as with Laurentian terranes in NE Greenland and the Scandinavian Caledonides.
    [Show full text]