DOCSLIB.ORG

Regional Geology Publications European and UK Geology

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Regional Geology Publications European and UK Geology Regional Geology Publications European and UK Geology For full details visit the online bookshop: www.geolsoc.org.uk/bookshop The Geology of Central Petroleum Geology of Tectonostratigraphic Europe – paperback set NW Europe: 50 Years of Atlas of the Northeast (2 volumes) Learning – Proceedings Atlantic Region T. McCann of the 8th Petroleum John R. Hopper, Thomas Funck, Martyn Stoker, This two-volume set provides Geology Conference Uni Arting, Gwenn Peron- the first comprehensive account M. Bowman and B. Levell Pinvidic, Hans Doornebal in English of the geology of The 8th Conference on the and Carmen Gaina Central Europe. Written by Petroleum Geology of NW more than 200 scientists from Europe was held in September The NAG-TEC Atlas provides universities and research 2015 and marked the a comprehensive review of centres spread across Europe 50th anniversary of the first geological and geophysical and North America, the 21 commercial discovery offshore information over the north- chapters are based on the main in the North Sea (West Sole, east Atlantic region. The main stratigraphic periods. Individual in September 1965). Its focus focus was to investigate the chapters outline the evolution was ‘50 Years of Learning – a tectonic evolution of the region of the region divided into a Platform for Present Value and with a particular emphasis on variety of sections which include Future Success’ and its objective basin evolution along conjugate overviews of the stratigraphic was to provide an update on margins. framework, climate, sea-level discoveries, developments, variations, palaeogeography and technologies and geological magmatic activity. Available in concepts from the region. separate volumes. ISBN: 978-1-86239-246-5 ISBN: 978-1-78620-277-2 ISBN: 978-8-77871-378-0 Publisher: GSL Publisher: PGC distributed by GSL Publisher: Geological Survey of August 2008 February 2018 Denmark and Greenland 1,552 Pages Paperback 646 pages Hardback September 2014 List price: £90.00 List price: £150.00 338 pages Hardback Fellows’ price: £65.00 Fellows’ price: £75.00 List price: £175.00 Other societies: £65.00 Other societies: £75.00 Buy online: Buy online: Buy online: www.geolsoc.org.uk/NTATL www.geolsoc.org.uk/CE1P2P www.geolsoc.org.uk/PGC8 The Geological Society’s Lyell Collection: journals, Special Publications 1 and books online. Visit www.lyellcollection.org European and UK Geology For full details visit the online bookshop: www.geolsoc.org.uk/bookshop Lyell Collection Content Late Neoproterozoic to Early Palaeozoic palaoegeography of the Holy Cross Mountains (Central Europe): an Geology of Ireland: Volcanoes of Europe, integrated approach A Field Guide Second edition J. Nawrocki, J, Dunlap, Z. Pat Meere, Ivor McCarthy, (paperback) Pecskay, L. Krzeminski, John Reavy, Allistair Allen Dougal Jerram, Alwyn Scarth A. Zylinska, M. Fanning, & Ken Higgs and Jean-Claude Tanguy W. Jozlowsi, S. Salwa, Z. Szczepanik and W. Trela Studying geology in the field will Volcanoes are intimately tied draw anyone curious about how Read online at: http://jgs. to the history of humanity, they lyellcollection.org/content/164/2/405 our planet works into the field help forge the Earth's crust time and time again. Ireland and atmosphere, and they are Active faulting in a is endowed with a spectacular very much an active feature variety of geology. The rocks populated low-strain of today. The archaeology of setting (Lower Rhine that make up the island of most ancient civilizations of Ireland offer a unique window Europe preserves the imprint Graben, Central into a 2-billion-year history. of spectacular and volcanic Europe) identified phenomena while, in modern by geomorphic, times life is still affected by geophysical and large eruptions from Europe’s geological analysis active volcanic systems. J. Kubler, R. Streich, E. Luck, M. Hoffmann, A.M. Friedrich and M.R. Strecker Read online at: http://sp. lyellcollection.org/content/432/1/127 The Variscan orogeny ISBN: 978-1-84889-166-1 ISBN: 978-1-78046-042-0 in Central Europe: Publisher: The Collins Press Publisher: Dunedin, distributed by GSL April 2013 February 2017 construction and 372 pages Paperback 384 pages Paperback collapse List price: £17.99 List price: £29.99 Buy online: Fellows’ price: £26.99 Wolfgang Franke www.geolsoc.org.uk/MPBIE Buy online: Read online at: http://mem. www.geolsoc.org.uk/MVOEUP lyellcollection.org/content/32/1/333 The Geological Society’s Lyell Collection: journals, Special Publications and books online. Visit www.lyellcollection.org 2 Geology of Scotland For full details visit the online bookshop: www.geolsoc.org.uk/bookshop Geology and landscapes The Geology of Scotland, Volcanoes and the of Scotland, 2nd edition 4th Edition (Paperback) Making of Scotland, (Paperback) N. H Trewin 2nd edition Con Gillen This 4th edition of The Geology Brian Upton The Geology and landscapes of Scotland is greatly expanded Scotland's mountains and glens of Scotland takes the reader from the previous edition with retain the secrets of the long on a tour of each of these 34 authors contributing to 20 and frequently violent geological regions in turn, starting with the chapters. A new format has history that has gone into their Northwest Highlands and Outer been adopted to provide a making. Volcanoes have played Hebrides, which contain some different perspective on the a major role in the creation of the oldest rocks on Earth, geology of Scotland. Scotland is of Scotland and while the through the mountain terrains constructed from a number of youngest, a mere sixty million of the Highlands and Uplands terranes that finally combined in years old, were responsible for to the Lowlands and then the roughly their present positions much of the scenic splendour fringes of the North Sea. A prior to about 410 million of the Inner Hebrides, the rocks section describes the volcanic years ago. Thus the geology composing many of the famous provinces of Scotland; another of each terrane is described Scottish landforms as, for deals with the effects of the Ice up the time of amalgamation, example, those of Glencoe and Ages while a final section looks providing chapters on the the Edinburgh district are also at Scotland's natural resources. Southern Uplands, Midland the direct result of volcanism. Valley, Highlands, Grampian and Hebridean terranes. ISBN: 978-1-78046-009-3 ISBN: 1-86239-126-2 ISBN: 978-1-78046-056-7 Publisher: Dunedin Academic Press Publisher: GSL Publisher: Dunedin Academic Press distributed by GSL February 2003 distributed by GSL July 2013 550 pages Paperback August 2015 254 Pages Paperback List price: £35.00 248 Pages Hardback List price: £24.99 Fellows’ price: £27.50 List price: £24.99 Fellows’ price: £22.49 Other societies: £27.50 Fellows’ price: £22.49 Buy online: Buy online: Buy online: www.geolsoc.org.uk/MPBST www.geolsoc.org.uk/GOS4P www.geolsoc.org.uk/MPBVO2 The Geological Society’s Lyell Collection: journals, Special Publications 3 and books online. Visit www.lyellcollection.org Geology of Scotland For full details visit the online bookshop: www.geolsoc.org.uk/bookshop Lyell Collection Content A sauropod-dominated tracksite from Rubha nam Brathairean (Brothers’ Point), Isle of Skye, Scotland The Dalradian of A Geological Excursion Paige E. dePolo, Stephen Scotland Guide to the Stirling L. Brusatte, Thomas J. Jack Treagus and Perth Area Challands, Davide Foffa, Dugald A. Ross, Mark M.A.E Browne and C. Gillen This new guide has itineraries Wilkinson and Hong-yu Yi grounded in a well understood The Stirling and Perth area Read online at: http://sjg. and documented stratigraphy comprises some wonderfully lyellcollection.org/content/54/1/1 that spans all periods from Pre- varied geology, from the Cambrian through to Triassic Dalradian metamorphic rocks Petroleum generation and covers lithologies from in the southern Highlands and migration in the volcanic tuffs and lavas through to a range of sedimentary fossiliferous marine and Cambro-Ordovician and igneous rocks within the Laurentian margin fluviatile sediments to aeolian Midland Valley. The eighteen sandstones. The authors hope excursions in this book guide succession of NW to share their thrill of finding the reader to the best geology Scotland that the older classic areas that this region has to offer, John Parnell, Stephen of Shropshire still have the from complex metamorphic Bowden and Darren Mark capacity to inspire. rocks around Dunkeld, Read online at: http://jgs. through the terrestrial old red lyellcollection.org/content/175/1/33 sandstone around Perth, to the younger and more varied Archibald Geike and Carboniferous sedimentary the establishment of rocks south of Stirling. the Scottish Oil Shale Industry John Richard Underhill and ISBN: 978-0-90071-785-7 ISBN: 978-1-90526-788-0 Publisher: GA Guides Publisher: Edinburgh Geological Jonathon Craig January 2010 Society distributed by GSL. Read online at: http:// 202 Pages Paperback March 2015 sp.lyellcollection.org/content/ List price: £17.00 232 pages Paperback early/2019/02/08/SP480-2018-55 GA/GSL Fellows’ price: £14.00 List price: £15.99 Buy online: Fellows’ price: £14.40 www.geolsoc.org.uk/GA067 Buy online: www.geolsoc.org.uk/MPSPA The Geological Society’s Lyell Collection: journals, Special Publications and books online. Visit www.lyellcollection.org 4 Geology of Scandinavia For full details visit the online bookshop: www.geolsoc.org.uk/bookshop Special Publication 344 Special Publication 390 Special Publication 434 Fjord Systems and New Perspectives on Mesozoic Biotas of Archives the Caledonides of Scandinavia and its J.A. Howe, W.E.N Austin, Scandinavia and Arctic Territories M. Forwick and M. Paetzel Related Areas B.P. Kear, J. Lindgren, J.H. Fjords are glacially over- F. Corfu, D. Gasser and Hurum, J Milan and V. Vajda deepened, semi-enclosed D.M. Chew Scandinavia and its Arctic marine basins, but are often The Caledonides are a major territories of Svalbard neglected as a sedimentary orogenic belt that stretches and Greenland represent realm.
Load more

Recommended publications
  • Resolving the Variscan Evolution of the Moldanubian Sector of The
    Journal of Geosciences, 52 (2007), 9–28 DOI: 10.3190/jgeosci.005 Original paper Resolving the Variscan evolution of the Moldanubian sector of the Bohemian Massif: the significance of the Bavarian and the Moravo–Moldanubian tectonometamorphic phases Fritz FINGER1*, Axel GERDEs2, Vojtěch JANOušEk3, Miloš RENé4, Gudrun RIEGlER1 1University of Salzburg, Division of Mineralogy, Hellbrunnerstraße 34, A-5020 Salzburg, Austria; [email protected] 2University of Frankfurt, Institute of Geoscience, Senckenberganlage 28, D-60054 Frankfurt, Germany 3Czech Geological Survey, Klárov 3, 118 21 Prague 1, Czech Republic 4Academy of Sciences, Institute of Rock Structure and Mechanics, V Holešovičkách 41, 182 09 Prague 8, Czech Republic *Corresponding author The Variscan evolution of the Moldanubian sector in the Bohemian Massif consists of at least two distinct tectonome- tamorphic phases: the Moravo–Moldanubian Phase (345–330 Ma) and the Bavarian Phase (330–315 Ma). The Mora- vo–Moldanubian Phase involved the overthrusting of the Moldanubian over the Moravian Zone, a process which may have followed the subduction of an intervening oceanic domain (a part of the Rheiic Ocean) beneath a Moldanubian (Armorican) active continental margin. The Moravo–Moldanubian Phase also involved the exhumation of the HP–HT rocks of the Gföhl Unit into the Moldanubian middle crust, represented by the Monotonous and Variegated series. The tectonic emplacement of the HP–HT rocks was accompanied by intrusions of distinct magnesio-potassic granitoid melts (the 335–338 Ma old Durbachite plutons), which contain components from a strongly enriched lithospheric mantle source. Two parallel belts of HP–HT rocks associated with Durbachite intrusions can be distinguished, a western one at the Teplá–Barrandian and an eastern one close to the Moravian boundary.
    [Show full text]
  • 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.
    [Show full text]
  • Pre-Mesozoic Geology of Saxo-Thuringia from the Cadomian Active Margin to the Variscan Orogen
    GEOLOGICA CARPATHICA, FEBRUARY 2011, 62, 1, 42 BOOK REVIEW Pre-Mesozoic Geology of Saxo-Thuringia From the Cadomian Active Margin to the Variscan Orogen Editors: ULF LINNEMANN & ROLF L. ROMER 26–28 April 2010 2010. Schweizerbart Science Publishers, Stuttgart. 488 pages, 190 figures, 6 tables, 1 Sheet Map, 1 DVD, 1 foldout, 25x 17 cm, 1400 g. Language: English ISBN 978-3-510-65259-4, bound, price: 84.90 EUR The monographic work is a summary of results of a wider team of authors, who have contributed to the five dominant Parts, each of which consists of several Chapters focused on individual problems of the Saxo-Thuringian Region, its geological structure and its development in time and space. It is a classical analysis of the development of the Pre-Mesozoic stage from the Cadomian Active Margin to the Variscan Orogene. Saxo-Thuringia represents a very important region displaying development of the Variscides in one part of the Pangea supercontinent. The first chapter of the first part (Introduction) of the book is absolutely devoted to the location of this region of Saxo-Thuringia in the context of the Pangea supercontinent, followed by detailed recapitulation of the geological maps and results from geological mapping in historical survey from oldest documents to almost present- day works, which are well preserved and represent for the reader the classical and modern shool of regional geology of this region. The third chapter of this part completely untraditionally, but in a very interesting way shows the region of Saxo- Thuringia from the point of view of geochemical potential.
    [Show full text]
  • Crystalline Complexes in the Southern Parts O.F the Bohemian Massif and in the Eastern Alps by G
    INTERNATIONAL GEOLOGICAL CONGRESS XXIII SESSION PRAGUE 1968 Guide to Excursion 32 C Austria Crystalline Complexes in the Southern Parts o.f the Bohemian Massif and in the Eastern Alps by G. Frasl, H. G. Scharbert, H. Wieseneder PUBLISHED BY THE GEOLOGICAL SURVEY OF AUSTRIA Excursion 32 C / Aug. 31.-Sept. 3, 1968 Excursion Leaders and Authors of the Excursion-guide: G. FRASL Universität Salzburg, Institut für Geologie und Paläontologie - Salzburg, Porsdie­ straße 8. H. G. ScHARBER T Universität Wien, Mineralogisch-Petrographisches Institut - Wien I, Dr.-Karl-Lueger­ ring 1. H. WIESENEDER Universität Wien, Mineralogisch-Petrographisches Institut - Wien 1, Dr.-Karl-Lueger­ ring 1. All rights reserved. Copyright, 1968, © by Geologische Bundesanstalt, Wien III. Printed in Austria. Contents I. The Bohernian Massif in Austria, Moldanubian Zone. H. G. ScHARBERT (First day) . 5 Introduction . 5 The excursion (Stop 1/1-stop I/6) 9 II. The Bohemian Massif in Austria, Moravian Zone. G. FRASL (Second day) . 13 General remarks . 13 The excursion (Stop II/1-stop II/9) 17 III. The eastern End of the Central Alps. H. WIESENEDER (Third and fo*th day) 25 General geology of the area . 25 The Wechsel unit . 25 The "grobgneiss" formation . 26 Permo-Mesozoic . 28 Metamorphism in the Semmering-Wechsel area . 30 The excursion (Stop III/1-stop III/11) . 30 Selected literature within ead1 article 1 (First day) The Bohemian Massif in Austria The Moldanubian Zone By H. G. ScHARBERT With 1 figure Introduction The Bohemian Massif is a deeply eroded cratogenic block having re­ ceived its last tectonic coining during the Variscian orogeny.
    [Show full text]
  • Ages of Detrital Zircons
    Elsevier Editorial System(tm) for Precambrian Research Manuscript Draft Manuscript Number: Title: AGES OF DETRITAL ZIRCONS (U/Pb, LA-ICP-MS) FROM THE LATEST NEOPROTEROZOIC - MIDDLE CAMBRIAN(?) ASHA GROUP AND EARLY DEVONIAN TAKATY FORMATION, THE SOUTH- WESTERN URALS: A TEST OF AN AUSTRALIA-BALTICA CONNECTION WITHIN RODINIA Article Type: SI:Precambrian Supercontinents Keywords: Urals, Detrital Zircon, Rodinia, Ediacaran, Baltica Corresponding Author: Prof. Nikolay Borisovich Kuznetsov, Ph.D. Corresponding Author's Institution: Geological Institute of Russian Academy of Science First Author: Nikolay B Kuznetsov, Ph.D. Order of Authors: Nikolay B Kuznetsov, Ph.D.; Josef G Meert, Ph.D.; Tatiana V Romanyuk, Ph.D. Abstract: Results from U/Pb-dating of detrital zircons (dZr) from sandstones of the Basu and Kukkarauk Fms. (Asha Group) of Ediacaran-Middle Cambrian(?) age along with the results obtained from the Early Devonian Takaty Fm. are presented. The age of the Asha Group is traditionally labeled as Upper Vendian in the Russian stratigraphic chart that overlaps with the Ediacaran in the International stratigraphic chart. The dZr whose ages fall within the age-interval of (500-750 Ma) are common in the Basu and Kukkarauk Fm. These ages are typical for crystalline complexes in the Pre- Uralides-Timanides orogen. The identification of zircons with this age range agrees with commonly adopted interpretations for the depositional origin of the Asha Group as a molasse resulting from the erosion of that orogenic belt. Based on the estimates of the youngest ages of dZr along with the tentative identification of inarticulate brachiopods in the Kukkarauk Fm., it appears that the upper part of the Asha Group may extend into the Middle Cambrian.
    [Show full text]
  • Lower Palaeozoic Evolution of the Northeast German Basin/Baltica Borderland
    Originally published as: McCann, T. (1998): Lower Palaeozoic evolution of the NE German Basin/Baltica borderland. - Geological Magazine, 135, 129-142. DOI: 10.1017/S0016756897007863 Geol. Mag. 135 (1), 1998, pp. 129–142. Printed in the United Kingdom © 1998 Cambridge University Press 129 Lower Palaeozoic evolution of the northeast German Basin/Baltica borderland TOMMY MCCANN GeoForschungsZentrum (Projektbereich 3.3 – Sedimente und Beckenbildung), Telegrafenberg A26, 14473 Potsdam, Germany (Received 15 October 1996; accepted 11 July 1997) Abstract – The Vendian–Silurian succession from a series of boreholes in northeast Germany has been pet- rographically and geochemically investigated. Evidence suggests that the more northerly Vendian and Cambrian succession was deposited on a craton which became increasingly unstable in Ordovician times. Similarly, the Ordovician-age succession deposited in the Rügen area indicates a strongly active continental margin tectonic setting for the same period. By Silurian times the region was once more relatively tectoni- cally quiescent. Although complete closure of the Tornquist Sea was not complete until latest Silurian times, the major changes in tectonic regime in the Eastern Avalonia/Baltica area recorded from the Ordovician sug- gest that a significant degree of closure occurred during this time. The precise location of the southwestern edge of 1. Introduction Baltica (that is, that part of Baltica to the south of the The northeast German Basin is situated between the sta- Sorgenfrei-Tornquist Zone) is not known. This is largely ble Precambrian shield area of the Baltic Sea/Scandinavia as a result of masking by younger sediments (Tanner & to the north and the Cadomian/Caledonian/Variscan- Meissner, 1996).
    [Show full text]
  • Tectonic Evolution of the Mesozoic South Anyui Suture Zone, GEOSPHERE; V
    Research Paper GEOSPHERE Tectonic evolution of the Mesozoic South Anyui suture zone, GEOSPHERE; v. 11, no. 5 eastern Russia: A critical component of paleogeographic doi:10.1130/GES01165.1 reconstructions of the Arctic region 18 figures; 5 tables; 2 supplemental files; 1 animation Jeffrey M. Amato1, Jaime Toro2, Vyacheslav V. Akinin3, Brian A. Hampton1, Alexander S. Salnikov4, and Marianna I. Tuchkova5 1Department of Geological Sciences, New Mexico State University, MSC 3AB, P.O. Box 30001, Las Cruces, New Mexico 88003, USA CORRESPONDENCE: [email protected] 2Department of Geology and Geography, West Virginia University, 330 Brooks Hall, P.O. Box 6300, Morgantown, West Virginia 26506, USA 3North-East Interdisciplinary Scientific Research Institute, Far East Branch, Russian Academy of Sciences, Magadan, Portovaya Street, 16, 685000, Russia CITATION: Amato, J.M., Toro, J., Akinin, V.V., Hamp- 4Siberian Research Institute of Geology, Geophysics, and Mineral Resources, 67 Krasny Prospekt, Novosibirsk, 630091, Russia ton, B.A., Salnikov, A.S., and Tuchkova, M.I., 2015, 5Geological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 119017, Russia Tectonic evolution of the Mesozoic South Anyui su- ture zone, eastern Russia: A critical component of paleogeographic reconstructions of the Arctic region: ABSTRACT INTRODUCTION Geosphere, v. 11 no. 5, p. 1530–1564, doi: 10 .1130 /GES01165.1. The South Anyui suture zone consists of late Paleozoic–Jurassic ultra- The South Anyui suture zone (Fig. 1) is a remnant of a Mesozoic ocean Received 19 December 2014 mafic rocks and Jurassic–Cretaceous pre-, syn-, and postcollisional sedimen- basin that separated the Arctic Alaska–Chukotka microplate from Siberia Revision received 2 July 2015 tary rocks.
    [Show full text]
  • The Apennines, the Dinarides, and the Adriatic Sea: Is the Adriatic Microplate a Reality?
    Geogr. Fis. Dinam. Quat. 32 (2009), 167-175, 13 figg. CLIFF D. OLLIER (*) & COLIN F. PAIN (**) THE APENNINES, THE DINARIDES, AND THE ADRIATIC SEA: IS THE ADRIATIC MICROPLATE A REALITY? ABSTRACT: OLLIER C.D. & PAIN C.F., The Apennines, the Dinarides, here called the Dinaride Mountains (which is sometimes and the Adriatic Sea: is the Adriatic Microplate a reality?. (IT ISSN 0391- split into different ranges in different countries, such as the 9838, 2009). Albanides in Albania) as shown in fig. 1. Structurally both The Apennines and the Dinarides consist of nappes thrust towards the Apennines and the Dinarides are thrust towards the the Adriatic Sea, which is underlain by largely undisturbed rocks. Plate tectonic reconstructions are very varied, with supposed subduction in Adriatic. The tectonic position of this area is problematic. many different directions. Besides this there is an over-ruling concept In plate tectonic terms the Dinaride Mountains are that a plate called the Adriatic (or Adria) Plate moved north from Africa usually explained as a result of subduction of a plate under to Europe where its collision helped to create the Alps. Some think the plate is still moving. The total tectonic setting, together with palaeonto- the Dinarides. Similarly the Apennines are commonly ex- logical and seismic data, suggests that the older model of two converging nappe belts meeting a common foreland best fits the observed facts. KEY WORDS: Adriatic, Apennines, Dinarides, Plates, Arcs. RIASSUNTO: OLLIER C.D. & PAIN C.F., Gli Appennini, le Dinaridi e il mare Adriatico: la Microplacca Adriatica è una realtà?. (IT ISSN 0391- 9838, 2009).
    [Show full text]
  • New Data on Geology of the Southern Urals: a Concise Summary of Research After the Period of EUROPROBE Activity
    Solid Earth Discuss., doi:10.5194/se-2016-62, 2016 Manuscript under review for journal Solid Earth Published: 12 May 2016 c Author(s) 2016. CC-BY 3.0 License. 5 New data on geology of the Southern Urals: a concise summary of research after the period of EUROPROBE activity Victor Puchkov Institute of Geology, Ufa Scientific Centre, K.Marx st.16/2, Ufa 450077 Russian Federation. Correspondence to : V.N.Puchkov ( [email protected] ) 10 15 1 Solid Earth Discuss., doi:10.5194/se-2016-62, 2016 Manuscript under review for journal Solid Earth Published: 12 May 2016 c Author(s) 2016. CC-BY 3.0 License. 5 Abstract. The period of an official activity of the EUROPROBE commission was connected in the Urals with implementation of the URALIDES Program, that stimulated many qualified geologists from the Western research institutes and Universities to come to the region and work with local geologists at actual problems of the Uralian geology. The author tries to answer a question: what interesting results 10 had been obtained in the Southern Urals in the last decade, when the most of foreign researchers left the Urals, and how these results correspond to the scientific conclusions that had been done before. Key words: Urals, EUROPROBE, URSEIS−95, stratigraphy, tectonics, ophiolites, HP metamorphism, plumes. 15 20 2 Solid Earth Discuss., doi:10.5194/se-2016-62, 2016 Manuscript under review for journal Solid Earth Published: 12 May 2016 c Author(s) 2016. CC-BY 3.0 License. 5 1. Introduction. The decade between 1992 and 2001 was of a special importance for the geology of the Urals.
    [Show full text]
  • Reconstructing the Alps–Carpathians–Dinarides As a Key to Understanding Switches in Subduction Polarity, Slab Gaps and Surface Motion
    Int J Earth Sci (Geol Rundsch) DOI 10.1007/s00531-014-1060-3 REVIEW ARTICLE Reconstructing the Alps–Carpathians–Dinarides as a key to understanding switches in subduction polarity, slab gaps and surface motion Mark R. Handy · Kamil Ustaszewski · Eduard Kissling Received: 16 September 2013 / Accepted: 13 July 2014 © The Author(s) 2014. This article is published with open access at Springerlink.com Abstract Palinspastic map reconstructions and plate part of the Alpine orogen and induced widespread crust– motion studies reveal that switches in subduction polarity and mantle decoupling, thus facilitating Pannonian extension and the opening of slab gaps beneath the Alps and Dinarides were roll-back subduction of the Carpathian oceanic embayment. triggered by slab tearing and involved widespread intracrustal The second slab-tearing event triggered uplift and peneplaini- and crust–mantle decoupling during Adria–Europe collision. zation in the Eastern Alps while opening a second slab gap, In particular, the switch from south-directed European sub- still present between the Eastern and Central Alps, that was duction to north-directed “wrong-way” Adriatic subduction partly filled by northward counterclockwise subduction of beneath the Eastern Alps was preconditioned by two slab- previously unsubducted Adriatic continental lithosphere. In tearing events that were continuous in Cenozoic time: (1) late Miocene time, Adriatic subduction thus jumped westward Eocene to early Oligocene rupturing of the oppositely dipping from the Dinarides into the heart of the Alpine orogen, where European and Adriatic slabs; these ruptures nucleated along a northward indentation and wedging of Adriatic crust led to trench–trench transfer fault connecting the Alps and Dinar- rapid exhumation and orogen-parallel escape of decoupled ides; (2) Oligocene to Miocene steepening and tearing of the Eastern Alpine crust toward the Pannonian Basin.
    [Show full text]
  • National Geological Screening: East Anglia Region
    National Geological Screening: East Anglia region Minerals and Waste Programme Commissioned Report CR/17/100 BRITISH GEOLOGICAL SURVEY MINERALS AND WASTE PROGRAMME COMMISSIONED REPORT CR/17/100 National Geological Screening: East Anglia region M A Woods1, D Schofield1, T Pharaoh2, R Haslam2, E Crane3, J P Bloomfield3, J R Lee4, B Baptie4, R P Shaw5, T Bide5 and F M McEvoy 1Rock type, 2Rock structure, 3Groundwater, 4Natural processes, 5Resources Contributors/editors L P Field, R Terrington, P Williamson, I Mosca, N J P Smith, D E Evans, C Gent, M Barron, A Howard, G Baker, R M Lark, A Lacinska, S Thorpe, H Holbrook, I Longhurst and L Hannaford The National Grid and other Ordnance Survey data © Crown Copyright and database rights 7. Ordnance Survey Licence No. 100021290 EUL. Keywords National geological screening, GDF, East Anglia, rock type, structure, groundwater, natural processes, resources Bibliographical reference WOODS, M A, SCHOFIELD, D, PHARAOH, T, HASLAM, R, CRANE, E, BLOOMFIELD, J P, LEE, J R, BAPTIE, B, SHAW, R P, BIDE T AND F M MCEVOY. 2018. National geological screening: East Anglia region. British Geological Survey Commissioned Report, CR/17/100. 69pp. BRITISH GEOLOGICAL SURVEY The full range of our publications is available from BGS shops at Nottingham, Edinburgh, London and Cardiff (Welsh British Geological Survey offices publications only), See contact details below or shop online at www.geologyshop.com Environmental Science Centre, Keyworth, Nottingham The London Information Office also maintains a reference NG12 5GG collection of BGS publications, including maps, for Tel 0115 936 3100 consultation. We publish an annual catalogue of our maps and other BGS Central Enquiries Desk publications; this catalogue is available online or from any of Tel 0115 936 3143 the BGS shops.
    [Show full text]
  • Exploration for Deep Geothermal Reservoirs in Luxembourg and the Surroundings - Perspectives of Geothermal Energy Use Tom Schintgen
    Schintgen Geothermal Energy (2015) 3:9 DOI 10.1186/s40517-015-0028-2 RESEARCH ARTICLE Open Access Exploration for deep geothermal reservoirs in Luxembourg and the surroundings - perspectives of geothermal energy use Tom Schintgen Correspondence: [email protected] Abstract Helmholtz Centre Potsdam - GFZ German Research Centre for Background: The aim of this paper is to combine different types of information Geosciences, Telegrafenberg, 14473 necessary for a first rather qualitative assessment of deep geothermal reservoirs in the Potsdam, Germany region of Luxembourg. Within the geological framework, the study area encompasses Luxembourg and the surrounding areas of Belgium, Germany, and France. On the one hand, the focus is laid on low-enthalpy hydrothermal reservoirs in Mesozoic aquifers in the Trier-Luxembourg Embayment. On the other hand, petrothermal reservoirs in the Devonian basement of the Ardennes and Eifel regions are considered for exploitation by Enhanced/Engineered Geothermal Systems (EGS). Methods: For geothermal exploration and exploitation purposes, geological, thermal, hydrogeological and structural data are necessary. Results: Among the Mesozoic aquifers, the Buntsandstein aquifer characterized by temperatures of up to 50°C is a suitable hydrothermal reservoir that could be exploited by means of heat pumps or provide direct heat for various applications. The most promising area is the zone of the SE-Luxembourg Graben. The aquifer is the warmest underneath the upper Alzette valley and the limestone plateau in Lorraine, where the Buntsandstein aquifer lies below a thick Mesozoic cover. At the base of an inferred Rotliegend graben in the same area, temperatures of up to 75°C are expected. However, geological and hydraulic conditions are uncertain.
    [Show full text]