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  • 1
    Call number: 9/M 07.0421(381)
    In: Geological Society special publication
    Description / Table of Contents: The volume highlights developments in our understanding of the palaeogeographical, palaeobiological, palaeoclimatic and cryospheric evolution of Antarctica. It focuses on the sedimentary record from the Devonian to the Quaternary Period. It features tectonic evolution and stratigraphy, as well as processes taking place adjacent to, beneath and beyond the ice-sheet margin, including the continental shelf.The contributions in this volume include several invited review papers, as well as original research papers arising from the International Symposium on Antarctic Earth Sciences in Edinburgh, in July 2011. These papers demonstrate a remarkable diversity of Earth science interests in the Antarctic. Following international trends, there is particular emphasis on the Cenozoic Era, reflecting the increasing emphasis on the documentation and understanding of the past record of ice-sheet fluctuations. Furthermore, Antarctic Earth history is providing us with important information about potential future trends, as the impact of global warming is increasingly felt on the continent and its ocean.
    Type of Medium: Monograph available for loan
    Pages: vi, 506 S.: z.T. farb. Ill., graph. Darst.
    ISBN: 9781862393639
    Series Statement: Special Publication / Geological Society 381
    Classification:
    Historical Geology
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Call number: ZSP-553-19
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 52 S. : Ill., graph. Darst
    ISBN: 8717055628
    ISSN: 0106-1046
    Series Statement: Meddelelser om Grønland : Geoscience 19
    Language: English
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    Boca Raton : CRC Press
    Call number: AWI G7-17-91080
    Type of Medium: Monograph available for loan
    Pages: xliv, 382 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 9781482234404
    Language: English
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    London : The Geological Society
    Associated volumes
    Call number: 9/M 02.0134
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: vi, 344 S.
    ISBN: 186239072X
    Series Statement: Geological Society special publication 176
    Classification:
    A. 3.11.
    Location: Reading room
    Branch Library: GFZ Library
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  • 5
    Description / Table of Contents: The flow of glacier ice can produce structures that are striking and beautiful. Associated sediments,too, can develop spectacular deformation structures, and examples are remarkbly well preserved in Quaternary deposits. Although such features have long been recognized, they are now the subject of new attention from glaciologists and glacial geologists. This collection of papers addresses how the methods for unravelling deformation structures evolved in recent years by structural geologists can be used for glacial materials, and the opportunities offered to structural geologists by glacial materials for studying deformation in rocks.
    Pages: Online-Ressource (360 Seiten)
    ISBN: 9781862390720
    Language: English
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  • 6
    Keywords: Antarctica; glacial geology; paleoclimatology; paleoenvironment; Southern Ocean
    Description / Table of Contents: Introduction --- Antarctic Palaeoenvironments and Earth-Surface Processes in context / Michael J. Hambrey and Bethan J. Davies / Geological Society, London, Special Publications, 381, 1-5, 24 September 2013, https://doi.org/10.1144/SP381.27 --- A. Palaeozoic and Mesozoic evolution of the Antarctic Continent --- The geological and tectonic evolution of the Transantarctic Mountains: a review / David H. Elliot / Geological Society, London, Special Publications, 381, 7-35, 1 July 2013, https://doi.org/10.1144/SP381.14 --- Differential Movement across Byrd Glacier, Antarctica, as indicated by Apatite (U–Th)/He thermochronology and geomorphological analysis / D. J. Foley, E. Stump, M. van Soest, K. X. Whipple and K. V. Hodges / Geological Society, London, Special Publications, 381, 37-43, 6 August 2013, https://doi.org/10.1144/SP381.25 --- Mesozoic to recent evolution of intraplate stress fields under multiple remote stresses: The case of Signy Island (South Orkney Microcontinent, Antarctica) / A. Maestro, J. López-Martínez and F. Bohoyo / Geological Society, London, Special Publications, 381, 45-65, 19 April 2013, https://doi.org/10.1144/SP381.4 --- The Taylor Group (Beacon Supergroup): the Devonian sediments of Antarctica / Margaret A. Bradshaw / Geological Society, London, Special Publications, 381, 67-97, 6 August 2013, https://doi.org/10.1144/SP381.23 --- Late Cretaceous dinosaurs from the James Ross Basin, West Antarctica / Marcelo A. Reguero, Claudia P. Tambussi, Rodolfo A. Coria and Sergio A. Marenssi / Geological Society, London, Special Publications, 381, 99-116, 24 July 2013, https://doi.org/10.1144/SP381.20 --- Palaeobiogeography of Austral echinoid faunas: a first quantitative approach / Thomas Saucede, Benjamin Pierrat, Arnaud Brayard and Bruno David / Geological Society, London, Special Publications, 381, 117-127, 19 April 2013, https://doi.org/10.1144/SP381.6 --- B. Cenozoic glaciation and impacts --- Taxonomic diversity of Eocene Antarctic penguins: a changing picture / Piotr Jadwiszczak / Geological Society, London, Special Publications, 381, 129-138, 24 June 2013, https://doi.org/10.1144/SP381.7 --- Heat-flow determinations of basement age in small oceanic basins of the southern central Scotia Sea / P. F. Barker, L. A. Lawver and R. D. Larter / Geological Society, London, Special Publications, 381, 139-150, 19 April 2013, https://doi.org/10.1144/SP381.3 --- Cenozoic landscape and ice drainage evolution in the Lambert Glacier–Amery Ice Shelf system / Duanne A. White / Geological Society, London, Special Publications, 381, 151-165, 1 July 2013, https://doi.org/10.1144/SP381.15 --- History of the grounded ice sheet in the Ross Sea sector of Antarctica during the Last Glacial Maximum and the last termination / Brenda L. Hall, George H. Denton, John O. Stone and Howard Conway / Geological Society, London, Special Publications, 381, 167-181, 19 April 2013, https://doi.org/10.1144/SP381.5 --- Late Eocene Glaciofluvial to Glaciomarine transition in the Lambert Graben: constraints from lithofacies and mineralogy of ODP Site 1166 sediments, Prydz Bay, Antarctica / K. Strand, J. Köykkä and J. Lamminen / Geological Society, London, Special Publications, 381, 183-197, 30 July 2013, https://doi.org/10.1144/SP381.24 --- The Offshore New Harbour Project: deciphering the Middle Miocene through Late Eocene seismic stratigraphy of Offshore New Harbour, western Ross Sea, Antarctica / Stephen F. Pekar, Marvin A. Speece, Gary S. Wilson, David S. Sunwall and Kirsty J. Tinto / Geological Society, London, Special Publications, 381, 199-213, 19 April 2013, https://doi.org/10.1144/SP381.2 --- Constraints on Antarctic Ice Sheet configuration during and following the Last Glacial Maximum and its episodic contribution to sea-level rise / John B. Anderson, Alexandra E. Kirshner and Alexander R. Simms / Geological Society, London, Special Publications, 381, 215-232, 1 July 2013, https://doi.org/10.1144/SP381.13 --- Glaciomarine sedimentation dynamics of the Abbot glacial trough of the Amundsen Sea Embayment shelf, West Antarctica / Katharina Hochmuth and Karsten Gohl / Geological Society, London, Special Publications, 381, 233-244, 24 July 2013, https://doi.org/10.1144/SP381.21 --- Southern Ocean bioproductivity during the last glacial cycle – new detection method and decadal-scale insight from the Scotia Sea / D. Sprenk, M. E. Weber, G. Kuhn, P. Rosén, M. Frank, M. Molina-Kescher, V. Liebetrau and H.-G. Röhling / Geological Society, London, Special Publications, 381, 245-261, 30 July 2013, https://doi.org/10.1144/SP381.17 --- Palaeoenvironmental records from the West Antarctic Peninsula drift sediments over the last 75 ka / Maryline J. Vautravers, David A. Hodell, James E. T. Channell, Claus-Dieter Hillenbrand, Mike Hall, James Smith and Robert D. Larter / Geological Society, London, Special Publications, 381, 263-276, 5 July 2013, https://doi.org/10.1144/SP381.12 --- Provenance of Pleistocene sediments from Site U1359 of the Wilkes Land IODP Leg 318 – evidence for multiple sourcing from the East Antarctic Craton and Ross Orogen / N. C. Pant, P. Biswas, Prakash K. Shrivastava, S. Bhattacharya, Kamlesh Verma, Mayuri Pandey and Iodp Expedition 318 Scientific Party / Geological Society, London, Special Publications, 381, 277-297, 1 July 2013, https://doi.org/10.1144/SP381.11 --- C. Glacial and periglacial processes --- Geomorphological evidence of cold-based glacier activity in South Victoria Land, Antarctica / C. B. Atkins / Geological Society, London, Special Publications, 381, 299-318, 24 July 2013, https://doi.org/10.1144/SP381.18 --- A review of geomorphic processes and landforms in the Dry Valleys of southern Victoria Land: implications for evaluating climate change and ice-sheet stability / D. R. Marchant, S. L. Mackay, J. L. Lamp, A. T. Hayden and J. W. Head / Geological Society, London, Special Publications, 381, 319-352, 1 July 2013, https://doi.org/10.1144/SP381.10 --- Landscape evolution and ice-sheet behaviour in a semi-arid polar environment: James Ross Island, NE Antarctic Peninsula / Bethan J. Davies, Neil F. Glasser, Jonathan L. Carrivick, Michael J. Hambrey, John L. Smellie and Daniel Nývlt / Geological Society, London, Special Publications, 381, 353-395, 19 April 2013, https://doi.org/10.1144/SP381.1 --- Windows on Antarctic soil–landscape relationships: comparison across selected regions of Antarctica / Megan R. Balks, Jerónimo López-Martínez, Sergey V. Goryachkin, Nikita S. Mergelov, Carlos E. G. R. Schaefer, Felipe N. B. Simas, Peter C. Almond, Graeme G. C. Claridge, Malcolm Mcleod and Joshua Scarrow / Geological Society, London, Special Publications, 381, 397-410, 16 May 2013, https://doi.org/10.1144/SP381.9 --- Sedimentary processes in two different polar periglacial environments: Examples from Schirmacher Oasis and Larsemann Hills, East Antarctica / Rajesh Asthana, Prakash K. Shrivastava, M. Javed Beg, Ashit K. Swain, Amit Dharwadkar, Sandip K. Roy and Hari B. Srivastava / Geological Society, London, Special Publications, 381, 411-427, 30 July 2013, https://doi.org/10.1144/SP381.22 --- Periglacial processes and landforms of the Antarctic: a review of recent studies and directions / Kevin Hall / Geological Society, London, Special Publications, 381, 429-453, 1 July 2013, https://doi.org/10.1144/SP381.16 --- Palaeoshoreline records of glacial isostatic adjustment in the Dry Valleys region, Antarctica / Stephanie A. Konfal, T. J. Wilson and B. L. Hall / Geological Society, London, Special Publications, 381, 455-467, 30 July 2013, https://doi.org/10.1144/SP381.26 --- Characteristic atmosphere–ocean–solid earth interactions in the Antarctic coastal and marine environment inferred from seismic and infrasound recording at Syowa Station, East Antarctica / Masaki Kanao, Alessia Maggi, Yoshiaki Ishihara, Eleonore Stutzmann, Masa-Yuki Yamamoto and Genti Toyokuni / Geological Society, London, Special Publications, 381, 469-480, 16 May 2013, https://doi.org/10.1144/SP381.8 --- Evaluation of Envisat ASAR IMP imagery for snow mapping at varying spatial resolution (Deception Island, South Shetlands – Antarctica) / Carla Mora, Gonçalo Vieira and Miguel Ramos / Geological Society, London, Special Publications, 381, 481-493, 24 July 2013, https://doi.org/10.1144/SP381.19
    Pages: Online-Ressource (VI, 506 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781862396401
    Language: English
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 21 (2002), S. 0 
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: This paper outlines the results of stable isotope (δD-δ18O) analysis of snow and glacier ice undertaken as part of a larger study concerning structural glaciology, debris entrainment and debris transport patterns at Midtre Lovénbreen, Svalbard. Samples of fresh snow were collected from the glacier surface in spring 1999 and samples of surface glacier ice and basal ice samples were collected in summer 1999. When plotted on bivariate co-isotopic diagrams (δD-δ18O), the slopes obtained for snow and unmodified glacier ice (6.4 and 6.9, respectively) are less steep than those for the basal ice layer and transverse ice layers on the ice surface (7.6 and 7.7, respectively). The difference in the slope of these lines is not statistically significant at the sample size (50) used in this study. The results indicate that although stable isotope analysis clearly has potential for studies of debris entrainment, transport and structural glaciology, difficulties remain with applying this technique. It is therefore not possible to apply these isotopic techniques to ice facies of unknown origins. In particular, large sample numbers are required to establish statistical differences and high-resolution sampling of specific ice facies may be necessary to establish isotopic differences.
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: Well-rounded gravels are described from moraine-mound complexes, diamicton forefields and modern englacial thrusts at the margins of four glaciers on the northern side of Brøggerhalvøya, northwest Spitsbergen. Their shape charcteristics are compared with modern and fossil glacigenic, modern beach and Early Weichselian beach gravels from this peninsula. The best discriminators of the well-rounded gravels have been found to be the percentage-frequency roundness histograms, the roundness mid-point and roundness range diagrams and the sphericity-roundness plots. It is concluded that the gravels have been derived by englacial thrusting from Early Weichselian or last interglacial beaches in the inner parts of the fjord and in the low level cirques when sea level reached at least 50m a.s.l. and deposited the beach gravels. The discrimination between gravel in basal diamictons, proglacial outwash and modern beaches is difficult as the reworking has resulted in little particle shape change. The potential major problem caused by reworking in the glacial environment is emphasised. especially when clast shape comparisons from modern environments to older sediments are used.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Oxford UK : Blackwell Science Ltd
    Sedimentology 49 (2002), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: This paper focuses on the structural glaciology, dynamics, debris transport paths and sedimentology of the forefield of Soler Glacier, a temperate outlet glacier of the North Patagonian Icefield in southern Chile. The glacier is fed by an icefall from the icefield and by snow and ice avalanches from surrounding mountain slopes. The dominant structures in the glacier are ogives, crevasses and crevasse traces. Thrusts and recumbent folds are developed where the glacier encounters a reverse slope, elevating basal and englacial material to the ice surface. Other debris sources for the glacier include avalanche and rockfall material, some of which is ingested in marginal crevasses. Debris incorporated in the ice and on its surface controls both the distribution of sedimentary facies on the forefield and moraine ridge morphology. Lithofacies in moraine ridges on the glacier forefield include large isolated boulders, diamictons, gravel, sand and fine-grained facies. In relative abundance terms, the dominant lithofacies and their interpretation are sandy boulder gravel (ice-marginal), sandy gravel (glaciofluvial), angular gravel (supraglacial) and diamicton (basal glacial). Proglacial water bodies are currently developing between the receding glacier and its frontal and lateral moraines. The presence of folded sand and laminites in moraine ridges in front of the glacier suggests that, during a previous advance, Soler Glacier over-rode a former proglacial lake, reworking lacustrine deposits. Post-depositional modification of the landform/sediment assemblage includes melting of the ice-core beneath the sediment cover, redistribution of finer material across the proglacial area by aeolian processes and fluvial reworking. Overall, the preservation potential of this landform/sediment assemblage is high on the centennial to millennial timescale.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Oxford UK : Blackwell Science Ltd
    Sedimentology 47 (2000), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The Lambert Graben is occupied by the world’s largest fjord system, through which flows the Lambert Glacier, the Amery Ice Shelf and their tributaries. Along the western margin of the graben, in the northern Prince Charles Mountains, remnants of uplifted Miocene and Pliocene strata of the glacigenic fjordal Pagodroma Group total more than 800 m in thickness. These sediments provide evidence for a dynamic East Antarctic ice sheet during the Neogene Period. Each of the four Pagodroma Group formations defined from this region rests unconformably on either Proterozoic or Permo-Triassic rocks. The unconformity surfaces represent parts of the walls and floors of Neogene fjords. For these surfaces to have been eroded, the ice must have been grounded out as far as the continental shelf in Prydz Bay. The Pagodroma Group was deposited by wet-based glaciers discharging into a fjordal setting and includes lithofacies that are quite different from those produced by modern Antarctic ice masses. The principal lithofacies are massive diamicts and soulder gravels, deposited both close to a calving, grounded glacier terminus and from icebergs. The few stratified diamicts are the product of more distal iceberg sedimentation. An ice-transported gravel lithofacies includes rockfall debris derived from palaeofjord walls and mixed with subglacially derived diamicts. Some lithofacies contain evidence of subaquatic slumping and gravity flowage. Volumetrically minor lithofacies include laminites, with some exposures exhibiting large ice-rafted clasts. The laminites represent less proximal, mainly ice-free fjordal sediments, resulting either from tidal-current sorting of suspended sediment originating from subaquatic glaciofluvial discharge, or from turbidity currents derived from unstable subaquatically deposited glacigenic sediment. The Pagodroma Group provides a record of multiple glaciation by dynamic, sliding glaciers carrying large amounts of both basal and supraglacial debris. The closest modern analogues, in terms of the thermal and dynamic characteristics of the Neogene Lambert Glacier, appear to be the fast-flowing tidewater glaciers of East Greenland. These glaciers originate from the interior ice sheet and discharge large volumes of icebergs; the resulting lithofacies are predominantly diamicts.
    Type of Medium: Electronic Resource
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