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  • 1
    Call number: ZSP-760/A-15
    In: Terra Antartica reports, No. 15
    Type of Medium: Series available for loan
    Pages: 15 Seiten , Illustrationen , 8 Kartenbeilagen, 1 CD-ROM
    ISBN: 978-88-88395-12-8
    Series Statement: Terra Antartica reports 15
    Language: English
    Note: 1 Kartenbeilage unter dem Titel: Mount Melbourne Quadrangle (Victoria Land) 2012 / P. C. Pertusati, G. Musumeci, R. Carosi, M. Meccheri 〈1 : 250.000〉 aus der Antarctic Geological 1:250.000 Map Series , 1 Kartenbeilage unter dem Titel: Reeves Névé Quadrangle (Victoria Land) 2012 / R. Casnedi, P. C. Pertusati, F. Salvini 〈1 : 250.000〉 aus der Antarctic Geological 1:250.000 Map Series , 1 Kartenbeilage unter dem Titel: Mount Murchison Quadrangle (Victoria Land) 1997 / G. Capponi, M. Meccheri & P. C. Pertusati 〈1 : 250.000〉 aus der Antarctic Geological 1:250.000 Map Series , 1 Kartenbeilage unter dem Titel: Mount Joyce Quadrangle (Victoria Land) 1999 / G. Capponi, L. Crispini, M. Meccheri, G. Musumeci & P. C. Pertusati 〈1 : 250.000〉 aus der Antarctic Geological 1:250.000 Map Series , 1 Kartenbeilage unter dem Titel: Relief Inlet Quadrangle (Victoria Land) 1999 / G. Capponi, L. Crispini, M. Meccheri, G. Musumeci & P. C. Pertusati 〈1 : 250.000〉 aus der Antarctic Geological 1:250.000 Map Series , 1 Kartenbeilage unter dem Titel: Coulman Island Quadrangle (Victoria Land) 1997 / G. Capponi, M. Meccheri & G. Oggiano 〈1 : 250.000〉 aus der Antarctic Geological 1:250.000 Map Series , 1 Kartenbeilage unter dem Titel: Sequence Hills Quadrangle (Victoria Land) 2012 / R. Carosi, M. Meccheri, G. Musumeci, P. C. Pertusati 〈1 : 250.000〉 aus der Antarctic Geological 1:250.000 Map Series , 1 Kartenbeilage unter dem Titel: Freyberg Mountains Quadrangle (Victoria Land) 2012 / G. Capponi, M. Meccheri, P. C. Pertusati 〈1 : 250.000〉 aus der Antarctic Geological 1:250.000 Map Series
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  • 2
    Call number: MR 90.0240
    Type of Medium: Series available for loan
    Pages: 87 S.
    Language: German
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  • 3
    Call number: S 99.0054(91) ; ZSP-320(B,91)
    In: Geologisches Jahrbuch : Reihe B, Regionale Geologie Ausland, Heft 91
    In: Polar issue, No. 7
    Type of Medium: Series available for loan
    Pages: 773 Seiten , Illustrationen , 1 Kartenbeilage, 1 Errata
    ISBN: 3510958349 , 3-510-95834-9
    ISSN: 0341-6402
    Series Statement: Geologisches Jahrbuch : Reihe B, Regionale Geologie Ausland 91
    Classification:
    Regional Geology
    Language: English
    Note: Contents INTRODUCTION Objectives of the Investigations / FRANZ TESSENSOHN ARCHITECTURE OF THE FOLD-AND-THRUST BELT Northern Segment Explanatory Notes to the Geological Map of Brøggerhalvøya and Blomstrandhalvøya 1 : 40,000 / FRIEDHELM THIEDIG, KERSTIN SAALMANN & KARSTEN PIEPJOHN Nappe Stacking on Brøggerhalvøya, NW Spitsbergen / KARSTEN PIEPJOHN, FRIEDHELM THIEDIG & GEOFF M. MANBY Foreland-Thrust Belt Relationships SE of Kongsfjorden and the Function of the Pretender Fault / FRANZ TESSENSOHN, KARSTEN PIEPJOHN & FRIEDHELM THIEDIG Emergence of Basement-Dominated Nappes in Oscar II Land: Implications for Shortening Estimates / GEOFF M. MANBY & NIKOS LYBERIS The Southern Margin of the Belt of Emergent Thrusting on the North Coast of Isfjorden / KARSTEN PIEPJOHN & WERNER VON GOSEN Permo-Carboniferous Slivers Infolded in the Basement of Western Oscar II Land / FRANZ TESSENSOHN, WERNER VON GOSEN & KARSTEN PIEPJOHN Central Segment Basement-Cored Folds in Nordenskiold Land / NIKOS LYBERIS & GEOFF M. MANBY Involvement of Basal Tertiary Strata in the Fold-Belt Deformation in Nordenskiold Land / WERNER VON GOSEN, HANS-JURGEN PAECH & KARSTEN PIEPJOHN Thrust Tectonics North of Van Keulenfjorden / WERNER VON GOSEN & KARSTEN PIEPJOHN Structure of the West Spitsbergen Fold-and-Thrust Belt in Wedel Jarlsberg Land / GEOFF M. MANBY & NIKOS LYBERIS Southern Segment Polyphase Deformation in the Eastern Hornsund Area / WERNER VON GOSEN & KARSTEN PIEPJOHN Decollement Structures in the Triassic South of Hornsund / FRANZ TESSENSOHN, FRIEDHELM THIEDIG, GEOFF M. MANBY & NIKOS LYBERIS Involvement of the Hornsund High in the Fold-Belt Deformation / FRIEDHELM THIEDIG, GEOFF M. MANBY & KARSTEN PIEPJOHN Structural Setting of the West Spitsbergen Fold-and-Thrust Belt in Southern Sørkapp Land / WERNER VON GOSEN, KARSTEN PIEPJOHN & HANS-JÜRGEN PAECH Stress Patterns in the West Spitsbergen Fold-and-Thrust Belt / GEOFF M. MANBY & NIKOS LYBERIS Role of the Tertiary Compressive Structures in the Central Basin, Spitsbergen / HANS-JÜRGEN PAECH The Relationship of the Ny-Alesund Tertiary to the West Spitsbergen Fold-and-Thrust Belt / KARSTEN PIEPJOHN, KERSTIN SAALMANN, FRIEDHELM THIEDIG & HANS-JÜRGEN PAECH Structures in the Tertiary Sediments of the Forlandsundet Graben / WERNER VON GOSEN & HANS-JÜRGEN PAECH Coalification in Post-Caledonian Sediments on Spitsbergen / HANS-JÜRGEN PAECH & JOACHIM KOCH TIMING Paleontology Paleogene Calcareous Nannofossils from the Firkanten and Sarsbukta Formations on Spitsbergen / PAVEL CEPEK Conflicting Interpretations of the Tertiary Biostratigraphy of Spitsbergen and New Palynological Results / PAVEL CEPEK & WILFRIED KRUTZSCH New Biostratigraphic Data from West Spitsbergen Based on Conodonts / FRIEDRICH W. LUPPOLD Conodont Stratigraphy of the Carboniferous and Permian Strata from Brøggerhalvøya and the Billefjorden Trough / WERNER BUGGISCH, MICHAEL JOACHIMSKI, HARALD LÜTZNER, FRIEDHELM THIEDIG & HEIKO HÜNEKE An Upper Cretaceous Microflora from Spitsbergen / WILFRIED KRUTZSCH Isotope Geochronology K/Ar Dating Attempts on Rocks from the West Spitsbergen Fold-and-Thrust Belt and the Central Basin / FRANZ TESSENSOHN, FRIEDHELM HENJES-KUNST & STEFAN KRUMM CONCLUSION The Evolution of the West Spitsbergen Fold-and-Thrust Belt / CASE TEAM , Zusammenfassungen in englischer, deutscher und russischer Sprache
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  • 4
    Call number: S 99.0054(85)
    In: Geologisches Jahrbuch
    In: Polar issue
    Type of Medium: Series available for loan
    Pages: 444 S. , Ill., graph. Darst., Kt. , 1 Kt.-Beil. (1 Bl.) , 24 cm
    ISBN: 3510959159
    Series Statement: Geologisches Jahrbuch : Reihe B, Regionale Geologie Ausland 85
    Classification:
    Regional Geology
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  • 5
    Call number: AWI G9-06-0036 ; AWI G9-10-0040
    Description / Table of Contents: Sixty articles arranged in eight thematic sections refer to most recent geological and geophysical results of Antarctic research. The Precambrian of the East Antarctic shield and its geological history is considered as well as sub-ice topography, geophysics and stratigraphy, sedimentology and geophysics of the surrounding Southern Ocean. Particular emphasis is given to the connection of the Antarctic and the surrounding continents when forming part of Gondwana.
    Type of Medium: Monograph available for loan
    Pages: XX, 492 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 3540306730
    ISSN: 3-540-30673-0
    Language: English
    Note: Contents Theme 1 History of Antarctic Research 1.1 The Road to Gondwana via the Early SCAR Symposia / A. B. Ford 1.2 Exploring the Unknown: History of the First German South Polar Expedition 1901–1903 / C. Lüdecke Theme 2 Antarctica – The Old Core 2.1 Characteristics of Metamorphosed Banded Iron Formation and Its Relation to the Magnetic Anomaly in the Mt. Riiser-Larsen Area, Amundsen Bay, Enderby Land, Antarctica / M. Funaki, P. Dolinsky, N. Ishikawa, A. Yamazaki 2.2 Experimental Constraints on the Decompressional P-T Paths of Rundvågshetta Granulites, Lützow-Holm Complex, East Antarctica / T. Kawasaki, Y. Motoyoshi 2.3 Sapphirine – Orthopyroxene – Garnet Granulite from Schirmacher Hills, Central Dronning Maud Land / S. Baba, M. Owada, E. S. Grew, K. Shiraishi 2.4 Genesis of Ferropotassic A-Type Granitoids of Mühlig-Hofmannfjella, Central Dronning Maud Land, East Antarctica / M. J. D’Souza, A. V. K. Prasad, R. Ravindra 2.5 Late Pan-African Fluid Infiltration in the Mühlig-Hofmann- and Filchnerfjella of Central Dronning Maud Land, East Antarctica / A. K. Engvik, S. Elvevold 2.6 Electron Microprobe (EMP) Dating on Monazite from Forefinger Point Granulites, East Antarctica: Implication for Pan-African Overprint / Y. Motoyoshi, T. Hokada, K. Shiraishi 2.7 Tectonic Subdivision of the Prince Charles Mountains: A Review of Geologic and Isotopic Data / E. V. Mikhalsky, A. A. Laiba, B. V. Beliatsky 2.8 Crustal Provinces of the Prince Charles Mountains Region and Surrounding Areas in the Light of Aeromagnetic Data / A. V. Golynsky, V. N. Masolov, V. S. Volnukhin, D. A. Golynsky 2.9 Magnetic Anomalies of the Grove Mountains Region and Their Geological Significance / A. V. Golynsky, D. A. Golynsky, V. N. Masolov, V. S. Volnukhin Theme 3 The Continent Beneath the Ice 3.1 ADMAP – A Digital Magnetic Anomaly Map of the Antarctic / A. V. Golynsky, M. Chiappini, D. Damaske, F. Ferraccioli, C. A. Finn, T. Ishihara, H. R. Kim, L. Kovacs, V. N. Masolov, P. Morris, R. von Frese 3.2 Identifying Major Sedimentary Basins Beneath the West Antarctic Ice Sheet from Aeromagnetic Data Analysis / R. E. Bell, M. Studinger, G. Karner, C. A. Finn, D. D. Blankenship 3.3 Bedrock Plateaus within the Ross Embayment and beneath the West Antarctic Ice Sheet, Formed by Marine Erosion in Late Tertiary Time / D. S. Wilson, B. P. Luyendyk 3.4 Inversion of Airborne Gravity Data Acquired over Subglacial Lakes in East Antarctica / I. Y. Filina, D. D. Blankenship, L. Roy, M. K. Sen, T. G. Richter, J. W. Holt 3.5 Russian Geophysical Studies of Lake Vostok, Central East Antarctica / V. N. Masolov, S. V. Popov, V. V. Lukin, A. N. Sheremetyev, A. M. Popkov 3.6 Morphology of the Subglacial Bed Relief of Lake Vostok Basin Area (Central East Antarctica) Based on RES and Seismic Data / S. V. Popov, A. N. Lastochkin, V. N. Masolov, A. M. Popkov 3.7 Deep Reflection Imaging beneath the Mizuho Plateau, East Antarctica, by SEAL-2002 Seismic Experiment / M. Yamashita, H. Miyamachi, M. Kanao, T. Matsushima, S. Toda, M. Takada, A. Watanabe 3.8 Seismic Anisotropy beneath Northern Victoria Land from SKS Splitting Analysis / S. Pondrelli, L. Margheriti, S. Danesi Theme 4 Gondwana Margins in Antarctica 4.1 Scouting Craton’s Edge in Paleo-Pacific Gondwana / C. A. Finn, J. W. Goodge, D. Damaske, C. M. Fanning 4.2 The Matusevich Fracture Zone in Oates Land, East Antarctica / G. Kleinschmidt, A. L. Läufer 4.3 Tectonic Model for Development of the Byrd Glacier Discontinuity and Surrounding Regions of the Transantarctic Mountains during the Neoproterozoic – Early Paleozoic / E. Stump, B. Gootee, F. Talarico 4.4 Depositional Environments of the Byrd Group, Byrd Glacier Area: A Cambrian Record of Sedimentation, Tectonism, and Magmatism / B. Gootee, E. Stump 4.5 Late-Ross Structures in the Wilson Terrane in the Rennick Glacier Area (Northern Victoria Land, Antarctica) / A. L. Läufer, G. Kleinschmidt, F. Rossetti 4.6 Style of Uplift of Paleozoic Terranes in Northern Victoria Land, Antarctica: Evidence from K-Ar Age Patterns / C. J. Adams Theme 5 Antarctic Peninsula Active Margin Tectonics 5.1 Patagonia – Antarctica Connections before Gondwana Break-Up / F. Hervé, H. Miller, C. Pimpirev 5.2 Moho Depth along the Antarctic Peninsula and Crustal Structure across the Landward Projection of the Hero Fracture Zone / T. Janik, P. Þroda, M. Grad, A. Guterch 5.3 Crustal Thinning and the Development of Deep Depressions at the Scotia- Antarctic Plate Boundary (Southern Margin of Discovery Bank, Antarctica) / J. Galindo-Zaldívar, J. C. Balanyá, F. Bohoyo, A. Jabaloy, A. Maldonado, J. M. Martínez-Martínez, J. Rodríguez-Fernández, E. Suriñach 5.4 Bransfield Basin Tectonic Evolution / J. Galindo-Zaldívar, L. Gamboa , A. Maldonado, S. Nakao, Y. Bochu 5.5 The Sedimentary Sequences of Hurd Peninsula, Livingston Island, South Shetland Islands: Part of the Late Jurassic–Cretaceous Depositional History of the Antarctic Peninsula / C. Pimpirev, K. Stoykova, M. Ivanov, D. Dimov 5.6 Regional Structures and Geodynamic Evolution of North Greenwich (Fort Williams Point) and Dee Islands, South Shetland Islands / J. F. Dumont, E. Santana, F. Hervé, C. Zapata 5.7 The Eocene Volcaniclastic Sejong Formation, Barton Peninsula, King George Island, Antarctica: Evolving Arc Volcanism from Precursory Fire Fountaining to Vulcanian Eruptions / S. B. Kim, Y. K. Sohn, M. Y. Choe 5.8 Elephant Island Recent Tectonics in the Framework of the Scotia-Antarctic-South Shetland Block Triple Junction (NE Antarctic Peninsula) / J. Galindo-Zaldívar, A. Maestro, J. López-Martínez, C. S. de Galdeano 5.9 Tectonics and Geomorphology of Elephant Island, South Shetland Islands / J. López-Martínez, R. A. J. Trouw, J. Galindo-Zaldívar, A. Maestro, L. S. A. Simões, F. F. Medeiros, C. C. Trouw 5.10 Geodynamical Studies on Deception Island: DECVOL and GEODEC Projects / M. Berrocoso, A. García-García, J. Martín-Dávila, M. Catalán-Morollón, M. Astiz, M. E. Ramírez, C. Torrecillas, J. M. E. de Salamanca Theme 6 Antarctic Rift Tectonics 6.1 Mawson Breccias Intrude Beacon Strata at Allan Hills, South Victoria Land: Regional Implications / D. H. Elliot, E. H. Fortner, C. B. Grimes 6.2 What Supports the Marie Byrd Land Dome? An Evaluation of Potential Uplift Mechanisms in a Continental Rift System / W. E. LeMasurier 6.3 A Multi-Phase Rifting Model for the Victoria Land Basin, Western Ross Sea / F. J. Davey, L. De Santis 6.4 Rift History of the Western Victoria Land Basin: A new Perspective Based on Integration of Cores with Seismic Reflection Data / C. R. Fielding, S. A. Henrys, T. J. Wilson 6.5 Constraints on the Timing of Extension in the Northern Basin, Ross Sea / S. C. Cande, J. M. Stock 6.6 The Structure of the Continental Margin off Wilkes Land and Terre Adélie Coast, East Antarctica / J. B. Colwell, H. M. J. Stagg, N. G. Direen, G. Bernardel, I. Borissova 6.7 Post-Rift Continental Slope and Rise Sediments from 38° E to 164° E, East Antarctica / P. E. O’Brien, S. Stanley, R. Parums Theme 7 Antarctic Neotectonics, Observatories and Data Bases 7.1 On Seismic Strain-Release within the Antarctic Plate / A. M. Reading 7.2 Vertical Crustal Deformation in Dronning Maud Land, Antarctica: Observation versus Model Prediction / M. Scheinert, E. Ivins, R. Dietrich, A. Rülke 7.3 Seismic Activity Associated with Surface Environmental Changes of the Earth System, around Syowa Station, East Antarctica / M. Kanao, K. Kaminuma 7.4 Geodynamic Features and Density Structure of the Earth’s Interior of the Antarctic and Surrounded Regions with the Gravimetric Tomography Method / R. Kh. Greku, V. P. Usenko, T. R. Greku 7.5 Some Recent Characteristics of Geomagnetic Secular Variations in Antarctica / A. Meloni, L. R. Gaya-Piqué, P. De Michelis, A. De Santis 7.6 Topographic and Geodetic Research by GPS, Echosounding and ERS Altimetric, and SAR Interferometric Surveys during Ukrainian Antarctic Expeditions in the West Antarctic / R. Greku, G. Milinevsky, Y. Ladanovsky, P. Bahmach, T. Greku 7.7 Geodetic Research o
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 70 (1981), S. 637-647 
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Abstract In the Antarctic summer of 1979/80 the German Antarctic North Victoria Land Expedition (Ganovex 1979) carried out geoscientific investigations in the northern part of Victoria Land.Landsat satellite images from a section of the northeastern corner of Victoria Land, west of the Ross Sea, are described. These photos represent the first digital image processing for this area. Their value can be discerned already, especially in terms of our knowledge on the glaciology, geomorphology, and geology of this region.
    Abstract: Résumé Au cours de l'été antarctique 1979/1980, l'Expédition Allemande Antarctique de la Terre Victoria (Ganovex 1979) a effectué des recherches géoscientifiques sur la partie nord de la Terre Victoria. Nous présentons ici des images du satelliteLandsat de la partie nord-est de la Terre Victoria à l'ouest de la Mer de Ross. Ces images représentent le premier essai d'un traitement digital par images sur cette région. La valeur de ces essais est déja evidente en glaciologie, géomorphologie et géologie.
    Notes: Zusammenfassung Im antarktischen Sommer 1979/80 führte die Deutsche Antarktis-Expedition Nord-Victorialand (Ganovex 1979) geowissenschaftliche Untersuchungen im nördlichen Victorialand durch. Von einem Teilgebiet an der Nordostecke von Victorialand, westlich des Ross-Meeres, werden Bilder des SatellitenLandsat vorgestellt. Diese Aufnahmen sind die ersten Versuche einer digitalen Bildverarbeitung für dieses Gebiet. Sie lassen aber schon den Wert besonders für die Glaziologie, Geomorphologie und Geologie erkennen.
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 76 (1987), S. 233-243 
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Abstract In the context of Gondwana North Victoria Land forms the Antarctic conjugate terrain to the East Australian Lachlan Fold Belt, where the distinction between S- and I-type granitoids was first worked out (Chappell &White 1974). Thus the area was considered a good testing ground for the hypothesis when the German Antarctic North Victoria Land Expedition (Ganovex) resumed fieldwork there in 1979/80. It was known at that time that there existed a Cambro/Ordovician and a Devonian/Carboniferous granitoid generation, which, in analogy to Australia, were taken to be related to two different orogenetic events. Our geological, petrographical and geochemical investigations, together with radiometric age dating, revealed that this is true only for the older granite generation. The younger generation is in fact anorogenic. At the same time, it became obvious that the S- and I-type classification did not completely fit the observed field data. At this pointPitcher's (1982) subdivision of the I-types into a »Cordilleran« and a »Caledonian« suite offered a solution to account for the observed irregularities. At about the same time, plate tectonic models based on evidence independent from the granite classification were developed for this part of the active Gondwana margin. This offers the opportunity to crosscheck the tectonic environment derived from the granite classification: The characteristics of the older, Cambro/Ordovician granitoids allow a perfect accommodation in the model of an active margin above a subduction zone as derived from other evidence. For the younger (Devonian/Carboniferous) granitoids, however, the postulated tectonic setting (post-collisional uplift and faulting) could not be verified in North Victoria Land. It is concluded thatPitchers classification is applicable in its petrographic and geochemical aspects but that the tectonic environment postulated for the production of »Caledonian« I-type granitoids may not be the same in all investigated areas.
    Abstract: Résumé Dans le contexte du Gondwana, la Terre Victoria est le pendant antarctique de la zone plissée de Lachlan, en Australie Orientale, où la distinction entre granites S et I a été établie pour la première fois (Chappel &White 1974). C'est pourquoi la vérification de cette hypothèse a été portée au programme de l'expédition allemande à la Terre Victoria en 1979–80 (Ganovex). On connaissait à cette époque l'existence d'une génération cambro-ordovicienne et d'une génération dévono-carbonifère de granitoÏdes qui, par analogie avec l'Australie, avaient été rapportées à deux événements orogéniques différents. Nos investigations géologiques, pétrologiques, géochimiques et géochronologiques montrent que cette conclusion n'est vraie que pour les granites de la première génération. La seconde génération est, en fait, anorogénique. Il s'est avéré en mÊme temps que la répartition en types S et I ne correspond pas exactement aux observations de terrain. Par contre, la distinction introduite parPitcher (1982) parmi les granites I entre une série »de Cordillère« et une série »Calédonienne« peut expliquer les irrégularités que nous observons. Environ à cette époque, des modèles géodynamiques basés sur des considérations indépendantes de la classification des granites ont été proposés pour cette partie de la marge active du Gondwana. Ces modèles permettent de recouper les considérations sur l'environnement tectonique des granites, déduites de leur classification: Les caractères des granitoÏdes anciens, cambro-ordoviciens, s'accordent parfaitement au modèle d'une marge active surmontant une subduction. Par contre, pour les granitoÏdes jeunes, dévono-carbonifères, la situation tectonique postulée (soulèvement et fracturation post-collision) n'a pas pu Être confirmée sur la Terre Victoria. En conclusion, la classification dePitcher est applicable dans ses aspects pétrographiques et géochimiques, mais l'environnement tectonique qui préside à la formation de granitoÏdes de type »Calédonien I« n'est pas nécessairement le mÊme dans toutes les régions étudiées.
    Notes: Zusammenfassung Im Gondwana Rahmen bildet Nord Victoria Land das antarktische Pendant zur ostaustralischen Lachlan Mobilzone, wo die Einteilung von Graniten in S- und I-Typen entwickelt wurde (Chappell &White 1974). Deshalb war eine überprüfung dieser neu entwickelten Hypothese eines der Arbeitsziele, als die deutschen Nord Victoria Land Expeditionen (Ganovex) dort 1979 ihre Arbeiten aufnahmen. An den bekannten zwei Granitgenerationen der Region wurden geologische, petrographische und geochemische Untersuchungen sowie Altersbestimmungen durchgeführt, deren Ergebnisse sich folgenderma\en zusammenfassen lassen. Die ältere, kambro-ordovizische Granitfolge steht, analog zur Situation in Australien, in enger Beziehung zu einer bedeutenden Orogenese, während sich zur jüngeren, devonisch-karbonischen Suite kein zugehöriges tektonisches Ereignis finden lie\. Dies steht im Gegensatz zur Situation in Australien/Tasmanien. Die S- und I-Typ Klassifikation, auf Nord Victoria Land angewendet, weist ähnliche Widersprüche auf, wie siePitcher (1982) zur Aufteilung der I-Typen in »kordillere« und »kaledonische« Sippen führten. Plattentektonische Modelle, die in den letzten Jahren für diese Region am mobilen Rand Gondwanas unabhängig von der Granitklassifikation nach geologischen und tektonischen Kriterien entwickelt wurden, erlauben es, die vonPitcher entwickelten tektonischen Bildungsmilieus für verschiedene Granit-Typen zu überprüfen: Die Charakteristiken der älteren (kambro-ordovizischen) Granite erlauben ein widerspruchsloses Einfügen in das aus anderen Kriterien abgeleitete Bild eines aktiven Kontinentalrandes über einer Subduktionszone. Für die jüngeren (devonisch-karbonischen) Granite dagegen, die im Charakter den »kaledonischen« I-TypenPitchers entsprechen, sind die für deren Bildung postulierten Vorgänge, nämlich Hebung und Dehnung nach einer Kollision, in Nord Victoria Land nicht erkennbar. Demnach erscheint zwar die KlassifikationPitchers sinnvoll, da sie in ihrer petrographisch-geochemischen Charakterisierung nachvollziehbar ist, aber das abgeleitete tektonische Milieu für die Bildung der »kaledonischen« Typen bedarf einer weiteren überprüfung.
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 71 (1982), S. 361-369 
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Abstract A late Precambrian turbidite succession is described from North Victoria Land, Antarctica, in its sedimentological, biological and tectonic aspects. Similar sequences occurring across the whole continent along the present Transantarctic Mountains are discussed. The geotectonic significance of this flysch belt is analysed in its relation to the East Antarctic Shield, the Gondwana craton and a proto-Pacific.
    Abstract: Résumé L'auteur décrit, avec ses critères sédimentologiques, biologiques et tectoniques, une série de turbidites du Précambrien supérieur dans le Nord de la Terre Victoria de l'Antarctique. Il discute des séries analogues se présentant dans tout le continent suivant la présente Chaîne transantarctique. Il analyse la signification géotectonique de cette ceinture de flysch dans sa relation avec le bouclier de l'Antarctique oriental, du craton du Gondwana et d'un Proto-Pacifique.
    Notes: Zusammenfassung Aus dem Nord-Viktoria-Land, Antarktis, wird eine spätkambrische Turbiditfolge mit ihren sedimentologischen, biologischen und tektonischen Kriterien beschrieben. Ähnliche Sequenzen, die quer durch den ganzen Kontinent im Zuge des Transantarktischen Gebirges vorkommen, werden diskutiert. Die geotektonische Bedeutung dieses Flysch-Gürtels wird analysiert in seiner Beziehung zum ostantarktischen Schild, zum Gondwana Kraton und zu einem Proto-Pazifik.
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  • 9
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    In:  Geological Society Special Publication 246: 275-291.
    Publication Date: 2007-10-08
    Description: The early Palaeozoic Ross Orogen in northern Victoria Land, Antarctica, consists of three major fault-bounded tectonostratigraphic terranes. Their true nature, fartravelled or local part of the accretionary collage, is under discussion. The inboard Wilson terrane (WT) consists mainly of high-grade metamorphic rocks intruded by the calcalkaline magmatic arc of the Ross Orogen. The terrane nature of the WT is doubtful, as it appears more like the leading edge of the East Antarctic craton. The Bowers terrane (BT) comprises a mixed sedimentary-volcanic succession, beginning with volcanic rocks of island-arc character, followed by turbidites, mudstones, conglomerates and fossiliferous Middle Cambrian shallow-water sediments. The whole sequence is capped by a fluvial to deltaic quartizitic series several kilometres thick, with strong continental affinity. The combination of primitive forearc to back-arc volcanics at the bottom and mature continental sediments at the top poses a problem. The outer Robertson Bay terrane (RBT) is made up of a thick turbidite succession which, in one area, contains allochthonous blocks of fossiliferous Tremadocian limestones. All terrane boundaries appear to be distinct fault zones. The WT/BT boundary forms a deep-reaching continent-ocean suture associated with strongly sheared rock units, ultramafic lenses and high-pressure rocks. Coesite in eclogites of the Lanterman Range indicates a depth of burial of around 90 km. A greenschist-facies schist belt marks the BT/RBT boundary. The terranes contain evidence for subduction at an active margin setting as well as for accretion processes along major faults. The present changes of the Cambrian time-scale, such as younging of the base of the Upper Cambrian by about 30 Ma since the 1980s, allow separation of arc formation and later terrane accretion events.
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  • 10
    Publication Date: 2012-09-30
    Print ISSN: 1860-1804
    Topics: Geography , Geosciences
    Published by Schweizerbart
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