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  • 1
    Call number: M 96.0059
    Type of Medium: Monograph available for loan
    Pages: VI, 167 S.
    ISBN: 3432262914
    Classification:
    Tectonics
    Language: German
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Darmstadt : Primus
    Call number: 9/M 07.0427
    Description / Table of Contents: Contents: 1. Kontraktionstheorie, Kontinentverschiebung und Plattentektonik, 2. Plattenbewegungen und ihre geometrischen Beziehungen, 3. Kontinentale Grabenbrüche, 4. Passive Kontinentränder und Tiefseebecken, 5. Mittelozeanische Rücken, 6. Heiße Flecken, 7. Subduktionszonen, Inselbögen und Aktive Kontinentränder, 8. Transformstörungen, 9. Terrane, 10. Plattentektonik im frühen Präkambrium, 11. Plattentektonik und Gebirgsbildung, 12. Alte Gebirge, 13. Junge Gebirge - Alpen und Himalaja.
    Type of Medium: Monograph available for loan
    Pages: 196 S. , Ill., graph. Darst., Kt.
    Edition: 2., aktualisierte Aufl.
    ISBN: 9783896785909
    Classification:
    Tectonics
    Note: Erscheinungsjahr in Vorlageform:2007
    Location: Reading room
    Branch Library: GFZ Library
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  • 3
    Call number: 9783319761022 (e-book)
    Description / Table of Contents: This richly illustrated book presents Germany’s geological evolution in the context of the Earth’s dynamic history. It starts with an introduction to Geology and explains the plate tectonic development, as well as the formation of both ancient and recent mountain belts - namely the Caledonian, Variscan and the modern-day Alps - that formed this part of Europe. A dedicated chapter discusses the origin of earthquakes in Germany, the occurrence of young volcanic rocks and the various episodes of rock deformation and metamorphism at these complex crossroads of plate tectonic history. The book highlights Germany’s diverse geological history, ranging from the origin of the Earth, the formation of deep crystalline rocks, and their overlying sedimentary sequences, to its more recent “ice age” quaternary cover. The last chapter addresses the shaping of the modern landscape. Though the content is also accessible for non-geologists, it is primarily intended for geoscience students and an academic audience
    Type of Medium: 12
    Pages: 1 Online-Ressource (xxxvii, 304 Seiten) , Illustrationen, Diagramme, Karten
    Edition: Online edition Springer eBook Collection. Earth and Environmental Science
    ISBN: 9783319761022 , 978-3-319-76102-2
    ISSN: 2364-6438 , 2364-6446
    Series Statement: Regional Geology Reviews
    Language: English
    Note: Contents 1 Introduction 2 Time and Geological Periods 3 Rocks and the Geological Record 4 The Age of the Rocks 5 Plate Tectonics, the Unifying Theory 6 Tectonics Units of Europe 6.1 Ancestral Europe 6.2 Paleo-Europe 6.3 Meso-Europe 6.4 Neo-Europe 7 Overview of the Plate Tectonic History of Europe 8 The Dynamic Earth, Earthquakes in Germany 9 Early Geological Evolution of Germany 9.1 The Pre-variscan Basement 9.2 Occurrences of Proterozoic and Early Paleozoic Units 9.2.1 Harz Mountains 9.2.2 Rheinisches Schiefergebirge 9.2.3 Lusatia 9.2.4 Elbe Zone 9.2.5 Erzgebirge 9.2.6 Schwarzburg Anticlinorium, Vesser Zone 9.2.7 Bohemian Massif 9.2.8 Black Forest 10 Late Paleozoic of Germany 10.1 The Variscan Orogeny 10.1.1 Rhenohercynian Zone 10.1.2 Saxothuringian Zone 10.1.3 Moldanubian Zone 10.2 Development of the Variscan Orogeny Through Time 10.2.1 Devonian 10.2.2 Carboniferous 10.3 The Variscides in Germany 10.3.1 Regional Geology of the Rhenohercynian 10.3.2 Northern Phyllite Zone 10.3.3 Regional Geology of the Saxothuringian 10.3.4 Saxothuringian (excluding the Mid-German Crystalline Zone) 10.3.5 Regional Geology of the Moldanubian 11 Permian and Mesozoic Geology of Germany 11.1 Post-Variscan History 11.2 Permian 11.2.1 Rotliegend 11.2.2 Zechstein 11.3 Permian/Triassic Boundary 11.4 Triassic 11.4.1 Buntsandstein (Bunter Sandstone) 11.4.2 Muschelkalk 11.4.3 Keuper 11.5 Triassic/Jurassic Boundary 11.6 Jurassic 11.6.1 Early Jurassic 11.6.2 Middle Jurassic 11.6.3 Late Jurassic 11.7 Cretaceous 11.7.1 Early Cretaceous 11.7.2 Late Cretaceous 11.8 Cretaceous/Tertiary Boundary 12 The Evolution of the Alps 12.1 Overview of the Tectonic Structure of the Alps 12.1.1 Helvetic 12.1.2 Penninic 12.1.3 Austroalpine and Southern Alpine Units 12.2 Development of the Alpine Region During the Permian 12.3 The Alpine Triassic 12.4 The Alpine Jurassic 12.5 The Alpine Region in the Cretaceous and Early Tertiary 12.6 The Tectonic Evolution of the Alps 13 Tertiary Basins 13.1 Tertiary Brown Coal Deposits 13.2 The Upper Rhine Graben 13.3 The Northern Alpine Foreland Basin—The Molasse 14 Tertiary and Quaternary Volcanism 14.1 Volcanism in the Eifel 14.2 Westerwald, Siebengebirge, Vogelsberg, Rhön, and Heldburger Gangschar 14.3 Small Chimneys in the Odenwald and the Messel Pit 14.4 Kaiserstuhl 14.5 Tuff Chimneys of Bad Urach, Hegau 14.6 Eger Graben Area, Fichtel Mountains, Vogtland, and Lusatia 15 Asteroid Craters 16 Germany During the Glacial Periods 16.1 Glacial and Interglacial Periods 16.2 Deposits and Erosion Forms of the Glacial Periods 16.3 The Baltic Sea—A Relic from the Last Glaciation Period Appendix References Index
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  • 4
    Call number: 13/N 16.90064
    Type of Medium: Monograph available for loan
    Pages: XXIX, 961 Seiten , Illustrationen, Diagramme
    ISBN: 9789400762398
    Series Statement: Encyclopedia of earth sciences series
    Classification:
    Oceanology
    Parallel Title: Erscheint auch als Encyclopedia of Marine Geosciences
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 42 (1995), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    Terra nova 9 (1997), S. 0 
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Ground-penetrating radar (GPR) is applied to detect subsurface tectonic structures and to map the geometry of faulted blocks. Tectonic interpretations from a profile crossing the graben fault and a grid in a second-order graben structure providing a 3D data set are correlated to the structural inventory of the outcrop. Folded layers of the roll-over anticline are identified by continuous curved reflectors and an increasing dip towards the main graben fault. Faults are indicated by arrays of reflector terminations. Variations in the water and clay content caused by karstification and brecciation on fault planes are displayed by changing amplitudes of the detected signal. The 3D visualization of the second-order graben structure with a grid of GPR profiles illustrates the local stress pattern which coincides with structural observations in the outcrop and photo lineations.
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Distribution patterns of benthic foraminiferal faunas from ODP Leg 170 Sites 1041 and 1042 show that the Costa Rican convergent margin subsided from coastal to abyssal depth from Middle Miocene to Present. This favours the model of a margin undergoing active subduction erosion. We propose that subduction erosion leads to the removal of material from the base of the forearc wedge and, as a consequence, to progressive subsidence of the forearc. A mean subsidence rate is estimated to be approximately 0.4 mm yr−1.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 76 (1987), S. 567-577 
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Abstract The Biscay synclinorium in Northern Spain is interpreted as an asymmetric basin developed by a rift system propagating from NW to SE and subsiding between the anticlockwise rotating Iberian plate and the Biscay block since the Middle to Upper Albian. Turbiditic sediments were deposited from Albian to Lower Tertiary. Paleocurrent directions and facies distribution of these sediments are used to reconstruct the paleogeographic development of the Biscay basin and the area surrounding it. The amount of tectonic deformation in the Basque area increases from W to E. The western region is dominated by brittle deformation and changes toward the E to ductile deformation, evaluated temperatures, and nappe movement. Metamorphosis and the lack of covering layers in the southeastern Biscay synclinorium as well as strong similarities between the sediments of the northwestern Biscay basin and those of the Zumaya basin are explained by a northward transported Zumaya nappe which originally was situated in the southeastern continuation of the Biscay basin and not in the eastern continuation of the Deva basin.
    Abstract: Resumen El sinclinorio de Vizcaya en el norte de España es interpretado como una cuenca asimétrica que resultó de un »rift« que se propagó del NW al SE. Desde el Albense Medio a Superior la cuenca subsidió entre la Placa Ibérica y el Bloque de Vizcaya como consecuencia de la rotación sinistral de la Placa Ibérica. A partir del Albense hasta el Terciário Inferior se depositaron sedimentos de tipo flysch. Se midieron direcciones de paleocorrientes y se determinó la distribución de las facies de los sedimentos para la reconstrucción del desarrollo paleogeográfico de la cuenca de Vizcaya y sus alrededores. El grado de la deformación tectónica en el País Vasco aumenta desde el W con deformación frágil hacia el E con deformación dÚctil, alteración térmica y movimiento de mantos de corrimiento. Ea alteración térmica y la falta de un cubrimiento en el SE del sinclinorio de Vizcaya asi como otras similitudes entre los sedimentos de la cuenca de Zumaya y los de la cuenca de Vizcaya permiten interpretar a la cuenca de Zumaya como un manto de corrimiento que fue transportado hacia el N.
    Notes: Zusammenfassung Das Biskaya-Synklinorium in Nord-Spanien wird als em asymmetrisches Becken interpretiert, das durch ein von NW nach SE propagierendes Rift-System entstand und seit dem Mittelbis Ober-Alb zwischen der im Gegenuhrzeigersinn rotierenden Iberischen Platte und dem Biskaya block einsank. Turbiditische Sedimente wurden vom Alb bis ins Alttertiär abgelagert. Aus Paläoströmungs-Richtungen und Faziesverteilungen wird die paläogeographische Entwicklung des Biskaya-Beckens und seiner Umgebung rekonstruiert. Der Grad der tektonischen Deformation im Gebiet des Baskenlandes nimmt von W nach E von bruchhafter zu duktiler Verformung mit thermischer Beanspruchung und Deckenbewegungen zu. Die thermischen Veränderungen und das Fehlen des Deckgebirges im südöstlichen Biskaya-Synklinorium sowie starke ähnlichkeiten der Sedimente des Biskaya-Beckens mit denen des Zumaya-Beckens werden durch die Annahme einer nach N transportierten Zumaya-Decke erklärt, die ursprünglich die südöstliche Fortsetzung des Biskaya-Beckens und nicht die östliche Fortsetzung des Deva-Beckens bildete.
    Type of Medium: Electronic Resource
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  • 9
    Publication Date: 2009-12-28
    Description: New structural, geochronological, and petrological data highlight which crustal sections of the North American-Caribbean Plate boundary in Guatemala and Honduras accommodated the large-scale sinistral offset. We develop the chronological and kinematic framework for these interactions and test for Palaeozoic to Recent geological correlations among the Maya Block, the Chortis Block, and the terranes of southern Mexico and the northern Caribbean. Our principal findings relate to how the North American-Caribbean Plate boundary partitioned deformation; whereas the southern Maya Block and the southern Chortis Block record the Late Cretaceous-Early Cenozoic collision and eastward sinistral translation of the Greater Antilles arc, the northern Chortis Block preserves evidence for northward stepping of the plate boundary with the translation of this block to its present position since the Late Eocene. Collision and translation are recorded in the ophiolite and subduction-accretion complex (North El Tambor complex), the continental margin (Rabinal and Chuacus complexes), and the Laramide foreland fold-thrust belt of the Maya Block as well as the overriding Greater Antilles arc complex. The Las Ovejas complex of the northern Chortis Block contains a significant part of the history of the eastward migration of the Chortis Block; it constitutes the southern part of the arc that facilitated the breakaway of the Chortis Block from the Xolapa complex of southern Mexico. While the Late Cretaceous collision is spectacularly sinistral transpressional, the Eocene-Recent translation of the Chortis Block is by sinistral wrenching with transtensional and transpressional episodes. Our reconstruction of the Late Mesozoic-Cenozoic evolution of the North American-Caribbean Plate boundary identified Proterozoic to Mesozoic connections among the southern Maya Block, the Chortis Block, and the terranes of southern Mexico: (i) in the Early-Middle Palaeozoic, the Acatlan complex of the southern Mexican Mixteca terrane, the Rabinal complex of the southern Maya Block, the Chuacus complex, and the Chortis Block were part of the Taconic-Acadian orogen along the northern margin of South America; (ii) after final amalgamation of Pangaea, an arc developed along its western margin, causing magmatism and regional amphibolite-facies metamorphism in southern Mexico, the Maya Block (including Rabinal complex), the Chuacus complex and the Chortis Block. The separation of North and South America also rifted the Chortis Block from southern Mexico. Rifting ultimately resulted in the formation of the Late Jurassic-Early Cretaceous oceanic crust of the South El Tambor complex; rifting and spreading terminated before the Hauterivian (c. 135 Ma). Remnants of the southwestern Mexican Guerrero complex, which also rifted from southern Mexico, remain in the Chortis Block (Sanarate complex); these complexes share Jurassic metamorphism. The South El Tambor subduction-accretion complex was emplaced onto the Chortis Block probably in the late Early Cretaceous and the Chortis Block collided with southern Mexico. Related arc magmatism and high-T/low-P metamorphism (Taxco-Viejo-Xolapa arc) of the Mixteca terrane spans all of southern Mexico. The Chortis Block shows continuous Early Cretaceous-Recent arc magmatism.
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  • 10
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