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LIBRO GEOLOGIA 30.Qxd:Maquetaciûn 1
Trabajos de Geología, Universidad de Oviedo, 29 : 278-283 (2010) From ductile to brittle deformation – the structural development and strain variations along a crustal-scale shear zone in SW Finland T. TORVELA1* AND C. EHLERS1 1Åbo Akademi University, Department of geology and mineralogy, Tuomiokirkontori 1, 20500 Turku, Finland. *e-mail: [email protected] Abstract: This study demonstrates the impact of variations in overall crustal rheology on crustal strength in relatively high P-T conditions at mid- to lower mid-crustal levels. In a crustal-scale shear zone, along-strike variations in the rheological competence result in large-scale deformation partition- ing and differences in the deformation style and strain distribution. Keywords: shear zone, deformation, strain partitioning, terrane boundary, Finland, Palaeoproterozoic. The structural behaviour of the crustal-scale Sottunga- several orogenic periods from the Archaean to the Jurmo shear zone (SJSZ) in SW Finland is described. Caledonian orogen 450-400 Ma ago (Fig. 1; e.g. The shear zone outlines a significant crustal disconti- Nironen, 1997; Lahtinen et al., 2005). The bulk of nuity, and it probably also represents a terrain bound- the shield (central and southern Finland, central and ary between the amphibolite-to-granulite facies, dome- northern Sweden) was formed during the and-basin-style crustal block to the north and the Palaeoproterozoic orogeny, ca. 2.0-1.85 Ga ago, amphibolite facies rocks with dominantly steeply dip- which is often referred to in literature as the ping structures to the south. The results of this study Svecofennian orogeny (Gaál and Gorbatschev, 1987). also imply that the late ductile structures (~1.80-1.79 The main direction of convergence against the Ga) can be attributed to the convergence of an Archaean nucleus to the NE (Fig. -
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? .... -
The North-Subducting Rheic Ocean During the Devonian: Consequences for the Rhenohercynian Ore Sites
Published in "International Journal of Earth Sciences 106(7): 2279–2296, 2017" which should be cited to refer to this work. The north-subducting Rheic Ocean during the Devonian: consequences for the Rhenohercynian ore sites Jürgen F. von Raumer1 · Heinz-Dieter Nesbor2 · Gérard M. Stampfli3 Abstract Base metal mining in the Rhenohercynian Zone activated Early Devonian growth faults. Hydrothermal brines has a long history. Middle-Upper Devonian to Lower Car- equilibrated with the basement and overlying Middle-Upper boniferous sediment-hosted massive sulfide deposits Devonian detrital deposits forming the SHMS deposits in the (SHMS), volcanic-hosted massive sulfide deposits (VHMS) southern part of the Pyrite Belt, in the Rhenish Massif and and Lahn-Dill-type iron, and base metal ores occur at sev- in the Harz areas. Volcanic-hosted massive sulfide deposits eral sites in the Rhenohercynian Zone that stretches from the (VHMS) formed in the more eastern localities of the Rheno- South Portuguese Zone, through the Lizard area, the Rhen- hercynian domain. In contrast, since the Tournaisian period ish Massif and the Harz Mountain to the Moravo-Silesian of ore formation, dominant pull-apart triggered magmatic Zone of SW Bohemia. During Devonian to Early Carbonif- emplacement of acidic rocks, and their metasomatic replace- erous times, the Rhenohercynian Zone is seen as an evolv- ment in the apical zones of felsic domes and sediments in ing rift system developed on subsiding shelf areas of the the northern part of the Iberian Pyrite belt, thus changing the Old Red continent. A reappraisal of the geotectonic setting general conditions of ore precipitation. -
The Mediterranean Region—A Geological Primer
160 Article by William Cavazza1 and Forese Carlo Wezel2 The Mediterranean region—a geological primer 1 Dept. of Earth and Geoenvironmental Sciences, Univ. of Bologna, Italy. [email protected] 2 Institute of Environmental Dynamics, University of Urbino, Italy. [email protected] The last twenty-five years of geological investigation of the Mediterranean region have disproved the traditional Introduction notion that the Alpine-Himalayan mountain ranges Many important ideas and influential geological models have been originated from the closure of a single, albeit complex, developed based on research undertaken in the Mediterranean oceanic domain—the Tethys. Instead, the present-day region. For example, the Alps are the most studied orogen in the geological configuration of the Mediterranean region is world, their structure has been elucidated in great detail for the most part and has served as an orogenic model applied to other collisional the result of the creation and ensuing consumption of orogens. Ophiolites and olistostromes were defined and studied for two major oceanic basins—the Paleotethys and the the first time in this region. The Mediterranean Sea has possibly the Neotethys—and of additional smaller oceanic basins highest density of DSDP/ODP sites in the world, and extensive within an overall regime of prolonged interaction research on its Messinian deposits and on their on-land counterparts has provided a spectacular example for the generation of widespread between the Eurasian and the African-Arabian plates. basinal evaporites. Other portions of this region are less well under- In greater detail, there is still some debate about exactly stood and are now the focus of much international attention. -
Iberian Plate-Kinematics in Paleomagnetic and Mantle Reference Frames, Gondwana Research (2016), Doi: 10.1016/J.Gr.2016.03.006
ÔØ ÅÒÙ×Ö ÔØ Cretaceous slab break-off in the Pyrenees: Iberian plate-kinematics in paleo- magnetic and mantle reference frames Reinoud L.M. Vissers, Douwe J.J. van Hinsbergen, Douwe G. van der Meer, Wim Spakman PII: S1342-937X(16)30053-3 DOI: doi: 10.1016/j.gr.2016.03.006 Reference: GR 1599 To appear in: Gondwana Research Received date: 21 September 2015 Revised date: 2 March 2016 Accepted date: 3 March 2016 Please cite this article as: Vissers, Reinoud L.M., van Hinsbergen, Douwe J.J., van der Meer, Douwe G., Spakman, Wim, Cretaceous slab break-off in the Pyrenees: Iberian plate-kinematics in paleomagnetic and mantle reference frames, Gondwana Research (2016), doi: 10.1016/j.gr.2016.03.006 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. ACCEPTED MANUSCRIPT Cretaceous slab break-off in the Pyrenees: Iberian plate- kinematics in paleomagnetic and mantle reference frames Reinoud L.M. Vissers1, Douwe J.J. van Hinsbergen1, Douwe G. van der Meer1,2, Wim Spakman1,3 1 Department of Earth Sciences, Utrecht University, Budapestlaan 4, Utrecht 3584 CD, Netherlands 2 Nexen Petroleum UK Ltd, 97 Oxford Road, Uxbridge, Middlesex UB8 1LU, UK 3 Center for Earth Evolution and Dynamics (CEED), University of Oslo, Sem Saelands vei 24, NO-0316 Oslo, Norway corresponding author: Reinoud L.M. -
Metamorphic Evolution of Relict Eclogite-Facies Rocks in the Paleoproterozoic Nagssugtoqidian Orogen, South-East Greenland”
“Metamorphic evolution of relict eclogite-facies rocks in the Paleoproterozoic Nagssugtoqidian Orogen, South-East Greenland” Von der Fakultät für Georessourcen und Materialtechnik der Rheinisch-Westfälischen Technischen Hochschule Aachen zur Erlangung des akademischen Grades eines Doktors der Naturwissenschaften genehmigte Dissertation vorgelegt von M.Sc. Geowissenschaften Sascha Müller aus Münster Berichter: PD Annika Dziggel Ph.D. Prof. Dr. Jochen Kolb Tag der mündlichen Prüfung: 14. Dezember 2018 Diese Dissertation ist auf den Internetseiten der Universitätsbibliothek online verfügbar. Foreword and Acknowledgements The following thesis was written over the course of 5 years, starting in August 2013, in the framework of the joint GEUS-MMR “SEGMENT (South-East Greenland Mineral Endowment Task)”-project. During the course of this study, I had the opportunity to witness the beautiful scenery and outstanding geology of Greenland firsthand during a one-month fieldtrip to the area around Tasiilaq in June and August of 2014, for which I greatly appreciate funding by the Geological Survey of Denmark and Greenland (GEUS) and the Ministry of Mineral Resources of Greenland (MMR). Regular funding was provided by the Deutsche Forschungsgemeinschaft from 2013 to 2016, with additional funding until late 2017 by employment at the Institute of Applied Mineralogy and Economic Geology at RWTH Aachen. At first, I want to thank my supervisor Annika Dziggel for her great support and guidance, but also for initiating this interesting project in the first place. Thank you for your support during fieldwork, for encouraging me to keep a sharp mind during analysis and interpretation and for teaching me how to properly present my data. Many thanks also go out to my Co-Supervisor Sven Sindern for his support during the countless hours I spent in the laboratory, as well as with the whole-rock data and isotopic dating. -
The Geology of England – Critical Examples of Earth History – an Overview
The Geology of England – critical examples of Earth history – an overview Mark A. Woods*, Jonathan R. Lee British Geological Survey, Environmental Science Centre, Keyworth, Nottingham, NG12 5GG *Corresponding Author: Mark A. Woods, email: [email protected] Abstract Over the past one billion years, England has experienced a remarkable geological journey. At times it has formed part of ancient volcanic island arcs, mountain ranges and arid deserts; lain beneath deep oceans, shallow tropical seas, extensive coal swamps and vast ice sheets; been inhabited by the earliest complex life forms, dinosaurs, and finally, witnessed the evolution of humans to a level where they now utilise and change the natural environment to meet their societal and economic needs. Evidence of this journey is recorded in the landscape and the rocks and sediments beneath our feet, and this article provides an overview of these events and the themed contributions to this Special Issue of Proceedings of the Geologists’ Association, which focuses on ‘The Geology of England – critical examples of Earth History’. Rather than being a stratigraphic account of English geology, this paper and the Special Issue attempts to place the Geology of England within the broader context of key ‘shifts’ and ‘tipping points’ that have occurred during Earth History. 1. Introduction England, together with the wider British Isles, is blessed with huge diversity of geology, reflected by the variety of natural landscapes and abundant geological resources that have underpinned economic growth during and since the Industrial Revolution. Industrialisation provided a practical impetus for better understanding the nature and pattern of the geological record, reflected by the publication in 1815 of the first geological map of Britain by William Smith (Winchester, 2001), and in 1835 by the founding of a national geological survey. -
Early Identification and Prevention of Difficulties in Learning to Read - a Global Perspective University of Jyväskylä & Niilo Mäki Institute, Finland
Heikki Lyytinen, UNESCO professor & GraphoLearn and Jyväskylä Longitudinal study of Dyslexia (JLD) teams Early identification and prevention of difficulties in learning to read - a global perspective University of Jyväskylä & Niilo Mäki Institute, Finland .. or how I am trying to approach the goal of my present duty as UNESCO Chair/professor On Inclusive Literacy Learning for All For more, see …GraphoLearn.info and for our related publications, heikki.lyytinen.info Compromised reading skill Biological reasons (% of population) » Global > 5% » Finland > 3% (and other transparent languages) Educational reasons » Global - up to 90% (in developing some countries) » Finland – 0% » >500 million compromised readers! The development of reading accuracy (% correct) during the 1. Grade in Finland Procentage Procentage 36 100 36 100 80 of correct items 27 75 of correct 27 orrect 60 18 18 50 itmes 40 items36 from correct 9 9 25 20 Onumber Number items from 36 0 0 0 0 School +10 vk 1.Gr ends School +10 vk. 1.Gr entry +5 week +15 week entry ends +5 week +15 week Individual development The average development Aro et al., 2004 Early identification - Jyväskylä Longitudinal study of Dyslexia (JLD) & Graphogame – our tool for the prevention of RDs The Jyväskylä Longitudinal study of Dyslexia (JLD): An intensive follow-up of children at familial risk for dyslexia from birth > JLD 1994- Timo Ahonen, Mikko Aro, Kenneth Eklund, Jane Erskine, Tomi Guttorm, Leena Holopainen, Jarmo Hämäläinen, Ritva Ketonen, Marja-Leena Laakso, Seija Leinonen, Paavo Leppänen, -
Full Issue Vol. 2 No. 4
Swedish American Genealogist Volume 2 | Number 4 Article 1 12-1-1982 Full Issue Vol. 2 No. 4 Follow this and additional works at: https://digitalcommons.augustana.edu/swensonsag Part of the Genealogy Commons, and the Scandinavian Studies Commons Recommended Citation (1982) "Full Issue Vol. 2 No. 4," Swedish American Genealogist: Vol. 2 : No. 4 , Article 1. Available at: https://digitalcommons.augustana.edu/swensonsag/vol2/iss4/1 This Full Issue is brought to you for free and open access by Augustana Digital Commons. It has been accepted for inclusion in Swedish American Genealogist by an authorized editor of Augustana Digital Commons. For more information, please contact [email protected]. Swedish American Genea o ist A journal devoted to Swedish American biography, genealogy and personal history CONTENTS The Emigrant Register of Karlstad 145 Swedish American Directories 150 Norwegian Sailor Last Survivor 160 Norwegian and Swedish Local Histories 161 An Early Rockford Swede 171 Swedish American By-names 173 Literature 177 Ancestor Tables 180 Genealogical Queries 183 Index of Personal Names 187 Index of Place Names 205 Index of Ships' Names 212 Vol. II December 1982 No. 4 I . Swedish Americanij Genealogist ~ Copyright © I 982 S1tiedish Amerh·an Geneal,,gtst P. 0 . Box 2186 Winte r Park. FL 32790 !I SSN 0275-9314 ) Editor and P ub lisher Nils Will ia m Olsson. Ph.D .. F.A.S.G. Contributing Editors Glen E. Brolardcr. Augustana Coll ege . Rock Island. IL: Sten Carls,on. Ph.D .. Uppsala Uni versit y. Uppsala . Sweden: Carl-Erik Johans,on. Brigham Young Univ ersity.J>rovo. UT: He nn e Sol Ib e . -
Mapping a Hidden Terrane Boundary in the Mantle Lithosphere with Lamprophyres
ARTICLE DOI: 10.1038/s41467-018-06253-7 OPEN Mapping a hidden terrane boundary in the mantle lithosphere with lamprophyres Arjan H. Dijkstra 1 & Callum Hatch1,2 Lamprophyres represent hydrous alkaline mantle melts that are a unique source of information about the composition of continental lithosphere. Throughout southwest Britain, post-Variscan lamprophyres are (ultra)potassic with strong incompatible element enrich- 1234567890():,; ments. Here we show that they form two distinct groups in terms of their Sr and Nd isotopic compositions, occurring on either side of a postulated, hitherto unrecognized terrane boundary. Lamprophyres emplaced north of the boundary fall on the mantle array with εNd −1 to +1.6. Those south of the boundary are enriched in radiogenic Sr, have initial εNd values of −0.3 to −3.5, and are isotopically indistinguishable from similar-aged lamprophyres in Armorican massifs in Europe. We conclude that an Armorican terrane was juxtaposed against Avalonia well before the closure of the Variscan oceans and the formation of Pangea. The giant Cornubian Tin-Tungsten Ore Province and associated batholith can be accounted for by the fertility of Armorican lower crust and mantle lithosphere. 1 School of Geography, Earth and Environmental Sciences, Plymouth University, Plymouth PL4 8AA, UK. 2 Department of Core Research Laboratories, Natural History Museum, Cromwell Road, London, SW7 5BD UK. Correspondence and requests for materials should be addressed to A.H.D. (email: [email protected]) NATURE COMMUNICATIONS | (2018) 9:3770 | DOI: 10.1038/s41467-018-06253-7 | www.nature.com/naturecommunications 1 ARTICLE NATURE COMMUNICATIONS | DOI: 10.1038/s41467-018-06253-7 ilson’s cycle1 of the opening and closing of ocean typically form 10 cm to m-wide dykes and other types of minor Wbasins throughout Earth history was based on the intrusions cutting across Variscan foliations in Carboniferous and similarity of Early Palaeozoic faunal assemblages in Devonian rocks. -
Stratigraphic Studies on the Precambrian in Finland
STRATIGRAPHIC STUDIES ON THE PRECAMBRIAN IN FINLAND by Ahti Simonen Simonen, A. 1986, Stratigraphie studies on the Preeambrian in Finland. Geological Survey 01 Finland, Bulletin 336, 21-37.3 figures, one table, one appendix. The main historieal outlines of the stratigraphie study of the Preeambrian in Finland are presented. Detailed field work and the applieation of new methods of research have steadily inereased our stratigraphie knowledge, and many reinterpretations of earlier eonelusions have therefore been neeessary. Key words: stratigraphy, basement , Svecokarelides, Preeambrian. research, history , glossary, Finland Prof. Ahti Simonen, Otakllja 3 D 46, 02/50 Espoo /5, Finland CONTENTS Introduction ." , .. " .... "" .. "" .......... , ... ",., ... ",... ... 22 Main historical outlines .",."" .. .... , ... .. , ... ",." ... ... ""... 22 Pre-Svecokarelidic base me nt complex 27 Svecokarelides 28 Karelidic belt 29 Svecofennidic belt ,., ........... ..... , ... "' . ..... , ,, .. .. .. .. , 32 Post-Svecokarelian rocks ... .. , .. ,." .. ", ... ........ .. """, . ", 34 ConcIuding Remarks .... .... .. ............ ..... .. ... ......... .. , 35 References ...... , . ...... .. , ...... , ..... ,......... .. .... .... 35 Appendix: Explanation of the terms (by Ahti Simonen and Carola Eklundh) Geological Survey of Finland, Bulletin 336 22 Ahti Simonen INTRODUCTION The study of the sueeession of events and Finland. Furthermore, the methods suitable the stratigraphie cIassifieation of formations for stratigraphie interpretation of metamorphie -
Ages of Detrital Zircons (U/Pb, LA-ICP-MS) from the Latest
Precambrian Research 244 (2014) 288–305 Contents lists available at ScienceDirect Precambrian Research jo urnal homepage: www.elsevier.com/locate/precamres Ages of detrital zircons (U/Pb, LA-ICP-MS) from the Latest Neoproterozoic–Middle Cambrian(?) Asha Group and Early Devonian Takaty Formation, the Southwestern Urals: A test of an Australia-Baltica connection within Rodinia a,∗ b c Nikolay B. Kuznetsov , Joseph G. Meert , Tatiana V. Romanyuk a Geological Institute, Russian Academy of Sciences, Pyzhevsky Lane, 7, Moscow 119017, Russia b Department of Geological Sciences, University of Florida, 355 Williamson Hall, Gainesville, FL 32611, USA c Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, B. Gruzinskaya ul. 10, Moscow 123810, Russia a r t i c l e i n f o a b s t r a c t Article history: A study of U-Pb ages on detrital zircons derived from sedimentary sequences in the western flank of Received 5 February 2013 Urals (para-autochthonous or autochthonous with Baltica) was undertaken in order to ascertain/test Received in revised form source models and paleogeography of the region in the Neoproterozoic. Samples were collected from the 16 September 2013 Ediacaran-Cambrian(?) age Asha Group (Basu and Kukkarauk Formations) and the Early Devonian-aged Accepted 18 September 2013 Takaty Formation. Available online 19 October 2013 Ages of detrital zircons within the Basu Formation fall within the interval 2900–700 Ma; from the Kukkarauk Formation from 3200 to 620 Ma. Ages of detrital zircons from the Devonian age Takaty For- Keywords: Australia mation are confined to the Paleoproterozoic and Archean (3050–1850 Ma).