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  • 2005-2009
  • 1995-1999  (5)
  • 1995  (5)
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  • 2005-2009
  • 1995-1999  (5)
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  • 1
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    Unknown
    Selbstverlag Fachbereich Geowissenschaften, FU Berlin
    In:  Herausgeberexemplar
    Publication Date: 2024-04-17
    Description: REITNER, Joachim & KOHRING, Rolf: Prof. Dr. Gundolf ERNST zum 65. Geburtstag. Eine kritische Würdigung des Jubilars ... 5 ; VOIGT, Ehrhard & GORDON, Dennis P.: Ascancestor and Confusocella - two new genera of cheilostomate Bryozoa from the Upper Cretaceous with transitional frontal-shield morphologies ... 15 ; KENNEDY, William J. & KAPLAN, Ulrich: Pseudojacobites farmeryi (CRICK, 1905), ein seltener Ammonit des westfälischen und englischen Ober-Turon ... 25 ; SEIBERTZ, Ekbert & SPAETH, Christian: Die Kreide-Belemniten von Mexiko II. Belemniten des Turon Nord-Mexikos ... 45 ; WIESE, Frank & WILMSEN, Markus: Erstnachweis aus Europa von Litophragmatoceras incomptum (Ammonoidea, Kreide) aus dem Mittel-Cenoman von Liencres (Kantabrien, Nordspanien) ... 53 ; WIESE, Frank: Das mittelturone Romaniceras kallesi-Event im Raum Santander (Nordspanien): Lithologie, Stratigraphie, laterale Veränderung der Ammonitenassoziationen und Paläobiogeographie ... 61 ; KRÜGER, Fritz J.: Leere Oberkretazische Echiniden-Coronen als Habitat benthonischer Organismen ... 79 ; MEHL, Dorte & NIEBUHR, Birgit: Diversität und Wachstumsformen bei Coeloptychium (Hexactinellida, Lychniskosa) der Meiner Mulde (Untercampan, NW-Deutschland) und die Palökologie der Coeloptychidae ... 91 ; REHFELD, Ursula & OTTO, Armin: Distribution and preservation of siliceous sponges of the rhythmically bedded spongiolitic rocks in the Lower Campanian of northern Spain (Cantabria, Santander area): Response to autecology and sea level development ... 109 ; FECHNER, Glenn G.: Phytoplankton und Sporomorphen aus dem Cenoman-Basiskonglomerat von Bochum (Nordrheinwestfalen, Deutschland) ... 129 ; KEUPP, Helmut: Die kalkigen Dinoflagellaten-Zysten aus dem Ober-Alb der Bohrung Kirchrode 1/91 (zentrales Niedersächsisches Becken, NW-Deutschland) ... 155 ; VOIGT, Silke: Verbreitung humider und arider Klimate der nördlichen Hemisphäre während der Oberkreide ... 201 ; HORNA, Frank: Komplexer Nachweis einer Tufflage im Turon von Hoppenstedt ... 207 ; WRAY, David S. & WOOD, Christopher J.: Geochemical identification and correlation of tuff layers in Lower Saxony, Germany ... 215 ; MUTTERLOSE, Jörg & WIEDENROTH, Kurt: Die Bio- und Lithofazies der Unterkreide (Hauterive bis Apt) in NW-Deutschland ... 227 ; TRÖGER, Karl-Armin & VOIGT, Thomas: Event-und Sequenzstratigraphie in der Sächsischen Kreide... 255 ; SEIBERTZ, Ekbert: Towards the single-species boundary definition - a concept proposal with application to the Turonian-Coniacian stage boundary (Upper Cretaceous) ... 269 ; WOOD, Christopher J. & MORTIMORE, Rory N.: An anomalous Black Band succession (Cenomanian - Turonian boundary interval) at Melton Ross, Lincolnshire, eastern England and its international significance ... 277 ; KUTZ, Andreas: Kalk-Mergel-Rhythmite der Oberkreide (Campan und Maastricht) am Massiv von Oroz Betelu (N-Spanien, Provinz Navarra). Ein Exkursionsführer ... 289 ; WOLF, Ernst-Otto.: Sedimentologie, Paläogeographie und Faziesentwicklung der Allochthonite des Campan von Beckum/Zentrales Münsterland ... 305 ; KRIWET, Jürgen & GLOY, Uwe: Zwei mesopelagische Raubfische (Actinopterygii: Euteleostei) aus dem Unterturon der Kronsberg-Mulde bei Hannover / Misburg (NW-Deutschland) ... 335 ; RAUHUT, Oliver W.M.: Zur systematischen Stellung der afrikanischen Theropoden Carcharodontosaurus STROMER 1931 und Bahariasaurus STROMER 1934 ... 357 ; WERNER, Christa: Neue Funde von mesozoischen Wirbeltieren in Äthiopien... 377 ;
    Description: commemorativepublication
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; Paläobiologie
    Language: German , English
    Type: doc-type:book
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  • 2
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    Unknown
    Selbstverlag Fachbereich Geowissenschaften, FU Berlin
    In:  Herausgeberexemplar
    Publication Date: 2024-04-17
    Description: SCHUDACK, Michael E.: Neue mikropaläontologische Beiträge (Ostracoda, Charophyta) zum Morrison-Ökosystem (Oberjura des Western Interior, USA) ... 389 ; BARTHOLDY, Jan, BELLAS, Spyridon M., MERTMANN, Dorothee, MACHANIEC, Elsbieta & MANUTSOGLU, Emmanuil: Fazies- Entwicklung und Biostratigraphie einer Sequenz eozäner Sedimente im Steinbruch Pod Capkami, Tatra-Gebirge, Polen ... 409 ; SCHULZ, Eberhard: Palynologische Untersuchungen des marinen Mittelrhäts im Creuzburger Graben bei Eisenach (W-Thüringen) ... 427 ; KRUTZSCH, Wilfried: Verbreitung der Trockenzonen im Kainophytikum - Eine Skizze ... 439 ; KOHRING, Rolf & SCHLÜTER, Thomas: Erhaltungsmechanismen känozoischer Insekten in fossilen Harzen und Sedimenten ... 457 ; ZILS, Wolfgang, WERNER, Christa, MORITZ, Andrea & SAANANE, Charles: Orientierende Tendaguru-Expedition 1994 ... 483 ; KIENEL, Ulrike, REHFELD, Ursula & BELLAS, Spyridon M.: The Miocene Blue Clay Formation of the Maltese Islands: Sequence-stratigraphic and palaeoceanographic implications based on calcareous nannofossil stratigraphy ... 533 ; SOUJON, Andr6, MANUTSOGLU, Emmanuil, REITNER, Joachim & JACOBSHAGEN, Volker: Lithistide Demospongiae aus der metamorphen Plattenkalk-Serie der Trypali Ori (Kreta/Griechenland) … 559 ; BARON-SZABO, Rosemarie C.: Taxonomy and Palaeoecology of Late Miocene corals of NW-Crete (Gramvoüssa, Roka- and Koukounaras- Fms.) ... 569 ; MANUTSOGLU, Emmanuil, MERTMANN, Dorothee, SoujON, Andre, DORNSIEPEN, Ulrich Friedrich & JACOBSHAGEN, Volker: Zur Nomenklatur der Metamorphite auf der Insel Kreta, Griechenland ... 579 ; FRYDAS, D., KONTOPOULOS, N., STAMATOPOULOS, L., GUERNET, C. & VOLTAGGIO, M.: Middle-Late Pleistocene sediments in the northwestern Peloponnesus, Greece. A combined study of biostratigraphical, radiochronological and sedimentological results ... 589 ; BECKER, R. Thomas: Taxonomy and Evolution of Late Famennian Tornocerataceae (Ammonoidea) ... 607 ; GRÖSCHKE, Manfred & KAPILIMA, Saldi: Ammoniten aus dem Septarienmergel (Kimmeridgium) des Mandawa-Mahokondo-Gebietes bei Nchia, Südtansania ... 645 ; KEUPP, Helmut & RIEDEL, Frank: Nautilus pompilius in captivity: a case study of abnormal shell growth ... 663 ; KRIWET, Jürgen: Beitrag zur Kenntnis der Fisch-Fauna des Ober-Jura (unteres Kimmeridge) der Kohlengrube Guimarota bei Leiria, Mittel-Portugal: 1 . Asteracanthus biformatus n. sp. (Chondrichthyes: Hybodontoidea) ... 683 ; MARTIN, Thomas: Incisor enamel microstructure and phylogenetic interrelationships of Pedetidae and Ctenodactyloidea (Rodentia) ... 693 ; ERESKOVSKY, Alexander V.: Materials to the Faunistic Study of the White and Barents seas sponges. 5. Quantitative Distribution ... 709 ; ERESKOVSKY, Alexander V.: Materials to the Faunistic Study of the White and Barents seas sponges. 6. The origin of the White and Barents seas sponge faunas ... 715 ; WÖRHEIDE, Gert: Bi- und multivariate Analyse borealer und mediterraner Populationen der Echinocardium cordatum - Gruppe (Echinoidea; Spatangoida) ... 731 ; HILBRECHT, Heinz: Computergestützte Methoden in der Morphometrie ... 765 ; CLAUSING, Andreas: Some critical notes on qualitative versus quantitative analysis in terrestrial palaeoecology ... 781 ; GLOY, Uwe: Bibliographie 1994, Institut für Paläontologie, Freie Universität Berlin ... 787 ;
    Description: commemorativepublication
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; Paläobiologie
    Language: German , English
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  • 3
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    Unknown
    Selbstverlag Fachbereich Geowissenschaften, FU Berlin
    In:  Herausgeberexemplar
    Publication Date: 2024-05-02
    Description: In der vorliegenden Arbeit wird die Krustenstruktur im östlichen Andenvorland untersucht. Das Gebiet umfaßt den Nordwesten Argentiniens, zwischen dem 22° und 25° südlichen Breitengrad und dem 66° und 62° westlichen Längengrad. Aus morphologischer Sicht befindet sich das Untersuchungsgebiet im Übergang zwischen dem Subandin (Sierras Subandinas) und der südlichen Ostkordillere zum Chaco Vorland (Llanura Chaqueña). Im Untersuchungsgebiet zeichnet sich ein Wechsel in den tektonischen Strukturen ab, welcher als Interaktion zwischen der tertiären Andenorogenese und kretazischen Riftbildungen gedeutet wird. Dieser als Inversionstektonik bekannte tektonischer Stil hat nicht nur oberflächennahe Strukturen hervorgerufen, sondern auch tiefgreifende Massenveränderungen verursacht. Teile dieser Modifikationen sind in der Signatur des Schwerefeldes erhalten geblieben, und somit ist die Interpretation gravimetrischer Meßergebnisse zusammen mit den geologischen Randbedingungen eine Grundvorraussetzung zur Untersuchung dieser tektonischen Interaktion. Zum Verständnis dieser Strukturen war es notwendig, sowohl den Teil des Beckens zu untersuchen, welcher nicht von der andinen Orogenese betroffen ist, als auch jenen der direkt in die letztere miteinbezogen wurde. Aus gravimetrischer Sicht ist die Bougueranomalie des Gebietes stark vom Effekt der Andenwurzel geprägt. Jedoch deuten einige Abweichungen auf die Existenz lokalerer Störkörper hin, die Ziel der Modellierung waren. Ein solcher Störkörper wurde am südöstlichen Rand des kretazischen Rifts identifiziert. Die Modellierung wurde einerseits zweidimensional durchgeführt um einen Überblick über das Gebiet zu bekommen. Eine regionale 3D Modellierung führte dann zu einer präziseren Interpretation des Gebietes. Insbesondere wurde dabei der Effekt überschobener Riftschollen am Ostrand des Beckens untersucht. Diese Überschiebungen drücken sich im gravimetrischen Restfeld als deutliche positive Anomalie aus. Allerdings kann diese Anomalie nicht direkt mit einem Astenosphärenanstieg, welcher durch Riftbildung entstanden sein könnte, in Einklang gebracht werden - wie von einigen Autoren vermutet wurde. Eine weitere modellierte Struktur bildete die Vortiefe, welche durch die Auflast der andinen Überschiebung enstanden ist. Die dadurch hervorgerufenen negativen Anomalien bilden einen deutlichen Kontrast zu der beschriebenen positiven Anomalie im Vorland, der sich auch im Restfeld als starker Gradient äußert. Die 2D Modellierung erbrachte folgende Ergebnisse: im anorogenen Breich des Untersuchungsgebietes wurde die Existenz einer deutliche Asymmetrie des Beckens bestätigt, mit einer nach Südosten geneigten Riftabscherungsfläche. Die Orogenese hinterließ deutliche Spuren in der Reaktivierung der Abscherungen wobei entlang der südostvergenten Störungen tieferes Krustenmaterial emporgeschoben wurde. Mit einer größeren Dichte wird dieser Vorgang als Ursache der positiven Anomalie intepretiert. Westvergente Störungen scheinen nur oberflächennahe Bereiche miteinbezogen haben. Im regionalen 3D Modell wurde ein Ansteigen der Unterkruste unterhalb des Beckens angenommen. Die asymmetrische Anordnung dieses Anstiegs deutet eher auf einen kompressive tektonischen Effekt hin als auf eine residuale Krustenverdünnung. Zusammenfassend kann gesagt werden, daß sich in diesem Breich im Schwerefeld die Effekte des Andengradienten mit denen der überschobenen Basement-Tektonik und der Vorlandtief kombinieren und als solche fur einen starken lokalen Gradienten am Rande des Effekts der Andenwurzel verantwortlich sind.
    Description: In the present study, the structure of the crust beneath the eastern Andean foreland is analyzed. The area comprises part of northwest Argentina, between 22° and 25° S and 66° and 62° W. In terms of morphotectonics, the area studied covers the transition between the Sierras Subandinas (Subandean Ranges) and the southern part of the Cordillera Oriental (Eastern Cordillera) to the Chaco plains (Llanura Chaqueña). In the area, a pervasive change controls the tectonic features, which is interpreted as a consequence of the interaction between the Andean orogeny and preexistent Cretaceous rifting. This inversion tectonics did not only result in a particular suite of near to surface structures but also modified deeply the mass distribution within the crust. This changes in mass distributions and hence density contrasts is evidenced by the gravity field. As such, a careful analysis of gravity data together with the geological boundary conditions are the basis for an analysis of this tectonic interaction. Understanding these structures implied to analyse not only the part of the rift involved in the Andean compressive orogenesis but also that part where original extensional features are still preserved. From a gravimetrical point of view, the Bouguer-anomaly of the area shows a strong overprint related with the Andean root. Some smaller changes in the field however indicate the existence of local sources, which where the target of the modelling. Such a change had been indentified at the southeastern edge of the Cretaceous rift. Modelling was performed towfold. As such, a 2D model was made in order to get an insight into the regional aspects of the area. A more detailed 3D model led to a more precise interpretation of the area. In particular, the effect of the inverted rift tectonics at the eastern edge of the basin was studied. These upthrusts correlate with a readily identifiable positive anomaly within the residual field. The anomaly neverthless cannot be directly related with an astenospheric uprise, preserved since the rifting stage, as suggested by some authors. In addition, the foredeep related with the tectonic load of the Andean overthurst, was modelled. The negative anomalies generated during this process, show a strong contrast in comparison with the positive anomaly described above, depicted also by a prominent gradient in the residual field. 2D modelling led to the following results. In the region, where Creataceous rifting structures were not overprinted by the Andean orogeny an obvious asymmetry of the basin was defined, being the master detachment dipping to the northeast. The orogeny left evidences of reactivation, where the structures of the southeastern edge were the pathways of the uplift if deeper crustal material with a higher density. This process may be responsible for a part of the positive anomaly mentioned. Structures located at the western and northwestern edge of the basin seem to have only involved nearer-to surface structures. The 3D model assumed a slight uprise of the lower crust beneath the basin. The asymmetry in goemetty seem to stand more for a tectonic effect than for a remanent thinned crust. As a summary, the gravity field in this area shows the combined effects of the regional Andean gradient with the more local effects of the basement tectonics (inverted rifting) and the overthrusted foredeep. Hence, at least these three factors seem to be responsible for the strong local gradient in a lateral position of the Andean root.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:550 ; Geophysik
    Language: English
    Type: doc-type:book
    Format: 136
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  • 4
    Map available for loan
    Map available for loan
    Ontario : Geological Survey of Canada
    Call number: AWI K-00-0105 / Fach 7
    Type of Medium: Map available for loan
    Pages: 1 Kt. : mehrfarb. ; 128 x 94 cm
    Series Statement: Geological Survey of Canada: Map 1880A
    Language: English
    Branch Library: AWI Library
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  • 5
    Call number: M 96.0159 ; M 96.0160 ; AWI G9-96-0124 ; AWI ad G9-96-0124
    In: Petermanns Geographische Mitteilungen : Ergänzungsheft, 289
    Description / Table of Contents: The monograph "The Schirmacher Oasis, Queen Maud Land, East Antarctica, and its surroundings" describes a region lying in a unique geographical position on the edge of East Antarctica. This area plays a key role for geological, paleoenvironmental and ecological studies for the understanding of regional and global changes. The book is the first complex multidisciplinary description of various geospheres within an Antarctic region. It presents a comprehensive summary of the results of two decades of German and three decades of international research efforts in this area, referring extensively also to sources never published before or which are difficult of access. Additionally, the monograph presents a very detailed photographic documentation and various map presentations of this area of East Antarctica, of its land and ice forms, its erosion, deposition and drainage features, its weather and climate as well as of its aurora features. The ozone soundings taken in the Schirmacher Oasis were the only year-round observations of vertical ozone distributions over Antarctica in 1985, the year of the "discovery'' of the "Antarctic Ozone Hole". For students and scientists interested in Antarctic regions and problems related to global change this book will serve as a source of references and as a guide for future expeditions as well.
    Type of Medium: Monograph available for loan
    Pages: 448 Seiten , Illustrationen , Annexes , 25 cm
    Edition: 1. Auflage
    ISBN: 3623007609
    Series Statement: Petermanns Geographische Mitteilungen : Ergänzungsheft 289
    Classification:
    A.0.3.
    Language: English
    Note: Contents Foreword Preface Editors' remarks The authors 1. The Schirmacher Oasis as a part of Queen Maud Land / (D. FRITZSCHE & P. BORMANN) 1.1. About Antarctic oases in general and the geographical setting of the Schirmacher Oasis in particular 1.2. History of discoveries and first investigations in Queen Maud Land 1.3. Systematic investigations of the Schirmacher Oasis and its surroundings since 1959 1.3.1. Contributions of the Norwegian Antarctic Expedition in 1958-59 1.3.2. Investigations of the Soviet Antarctic Expedition 1.3.2.1. The wintering stations Lasarev and Novolazarevskaya - their observatory registrations and field programmes 1.3.2.1.1. Logistical bases 1.3.2.1.2. Regular Soviet observatory programmes 1.3.2.1.3. Field studies in the surroundings of the stations 1.3.2.1.3.1. Glaciological studies at the Lazarev and Novolazarevskaya Ice Shelves 1.3.2.1.3.2. Geophysical investigations 1.3.2.1.3.3 Hydrological studies of lakes within the Schirmacher Oasis 1.3.2.1.3.4. Physico-geographical and geological studies of the Schirmacher Oasis 1.3.2.1.3.5. Biological investigations 1.3.2.2. Major geographic-geological surveys and geophysical and aerophotogrammetric mapping of the eastern mountain region of Queen Maud Land 1.3.3. Investigations of the Indian Antarctic Expedition 1.3.3.1. India 's interest in Antarctica 1.3.3.2. Indian Antarctic Expeditions and main results of investigations in the area of the Schirmacher Oasis and its surroundings 1.3.4. Contributions by German investigators 1.3.4.1. Origin of scientific interest in the Schirmacher Oasis and the establishment of the Georg Forster Station 1.3.4.2. Observational programmes at Georg Forster Station 1.3.4.3. Field observations within and in the surroundings of the Schirmacher Oasis 2. Geophysical investigations / (P. BORMANN, U. SCHÄFER, C. KOPSCH & S. WAGNER) 2.1. Permanent geomagnetic recordings 2.1.1. Recording environment, requirements and facilities 2.1.2. Recording of the total intensity F 2.1.3. Recording of the variation field 2.2. Geophysical field investigations 2.2.1. Review of former geophysical field investigations in Queen Maud Land 2.2.2. Geomagnetic field measurements by GDR teams 2.2.2.1. Measuring of variation differences 2.2.2.2. Geomagnetic mapping of the Schirmacher Oasis and profile measurements in its surroundings: data, results and geological implications 3. Geology / (H.-J. PAECH & W. STACKEBRANDT) 3.1. Geological setting and former investigations / (H.-J. PAECH) 3.2. Schirmacher Oasis 3.2.1. Lithostratigraphy / (W. STACKEBRANDT) 3.2.2. Tectonics / (W. STACKEBRANDT) 3.2.2.1. Planar structures 3.2.2.2. Linear structures 3.2.2.3. Fault structures and dykes 3.2.2.4. Structure and kinematics of the Lake 55 m fault zone by means of petromagnetic fabric analysis / (V. DAMM) 3.2.3. Petrography and petrochemistry 3.2.3.1. Metamorphics / (G. ANDREHS & P. BORMANN) 3.2.3.1.1. Methodology 3.2.3.1.2. Classification of rock types 3.2.3.1.3. Investigation of rock deformation 3.2.3.1.4. Mylonitization in fault zones 3.2.3.1.5. Characterization of metamorphism 3.2.3.1.6. Conclusions 3.2.3.2. Dykes / (U. WAND) 3.2.4. Photogeological indications / (E. BANKWITZ & P. BANKWITZ) 3.2.4.1. Rock series 3.2.4.2. Fault zones 3.3. The Nunatak region / (H.-U. WETZEL) 3.3.1. The Nunatak Metamorphic Complex 3.3.1.1. Nunatak Palets 3.3.1.2. Nunatak Aerodromnaya 3.3.1.3. Nunatak 870 m 3.3.1.4. Nunatak Südnachbar 3.3.1.5. Southern IGA Rocks 3.3.2. The Schirmacher Oasis Metamorphic Complex 3.3.2.1. Nunatak Basisniy 3.3.2.2. Nunatak Kit 3.4. Generalization of the geological history of the Schirmacher Oasis and Nunatak Metamorphic Complexes / (H.-J. PAECH, W. STACKEBRANDT & H.-U. WETZEL) 3.4.1. Lithostratigraphic succession 3.4.2. History of endogenic processes 3.5. Wohlthat Massif / (H. KÄMPF, W. STACKEBRANDT, K. HAHNE, H.-J. PAECH & V. S. LEPIN) 3.5.1. Introduction 3.5.2. Eliseev Anorthosite Complex 3.5.2.1. Introduction 3.5.2.2. Magmatic features 3.5.2.3. Metamorphic structures and textures 3.5.2.4. Chemical composition 3.5.2.5. Fracture tectonics and non-metamorphic dyke rocks 3.5.2.6. Ages and isotopie compositions 3.5.3. Rock assemblages covered by ice / (K. HAHNE, P. VOGLER & R. LEWIS) 3.5.4. Photogeological structures of the basement of the Wohlthat Massif / (P. BANKWITZ & E. BANKWITZ) 3.5.4.1. Structural features 3.5.4.2. Folding and schistosity 3.5.4.3. Fracture tectonics 3.5.4.4. Magmatic veins 3.6. Mineralizations in central Queen Maud Land / (H. KÄMPF) 3.6.1. Mineralization associated with metamorphics 3.6.2. Mineralization associated with anorthosite and gabbro 3.6.3. Mineralizations in granitoids and pegmatites 3.6.4. Hydrothermal mineralizations 3.7. Conclusions on the structure, composition and history of the Earth's crust in central Queen Maud Land / (P. BORMANN, H.-J. PAECH & W. STACKEBRANDT) 4. Geomorphology / (W. RICHTER & P. BORMANN) 4.1. Introduction 4.2. Overview of the macro-relief between the ice shelf barrier and the Wegener Inland Ice 4.3. Characterization of landformsin the Schirmacher Oasis 4.3.1. General characterization of landforms 4.3.2. Structural geomorphology 4.3.3. Surface forms due to glacial erosion and deposition 4.3.4. Surface water geomorphology 4.4. Weathering processes 4.4.1. Background and scope 4.4.2. Frost and insolation weathering 4.4.2.1. Measuring programme / (W. KRÜGER) 4.4.2.2. Results / (W. KRÜGER & P. BORMANN) 4.4.2.2.1. Data for bedrock 4.4.2.2.2. Temperature data for unconsolidated rock and soil 4.4.2.2.3. Soil moisture data for unconsolidated rock and soil 4.4.2.2.4. Discussion of results on rock and soil temperature as well as soil moisture measurements with regard to frost and insolation weathering in the Schirmacher Oasis / (W. KRÜGER & P. BORMANN) 4.4.3. Special forms of weathering 4.4.3.1. Chemical weathering and initial processes of pedogenesis 4.4.3.2. Salt efflorescences / (U. WAND) 4.4.3.3. Cavernous weathering / (J. BALKE & W. RICHTER) 4.4.3.4. Wind action (W. RICHTER) 5. Weather and climate / (W. RICHTER & P. BORMANN) 5.1. General climatic conditions 5.2. Local climatic conditions and variability of essential elements of the macro-climate in the Schirmacher Oasis 5.2.1. General peculiarities of oasis climate 5.2.2. Elements of macro-climate in the Schirmacher Oasis and their variability 5.2.2.1. Solar radiation 5.2.2.2. Air temperature 5.2.2.3. Wind direction and velocity 5.2.2.4. Precipitation 5.2.2.5. Humidity 5.2.2.6. Cloudiness 5.3. Isotope variations in atmospheric moisture and precipitation / (P. KOWSKI) 6. The continental ice cover in the surroundings of the Schirmacher Oasis / (W.-D. HERMICHEN) 6.1. Antarctic ice and world climate 6.2. Regional survey 6.3. Survey of former glaciological investigations 6.4. Present structure and dynamics of the regional ice cover 6.5. Isotope studies on the glacio-climatic history of the area 6.6. Some remarkable morphological minor forms of the snow and ice surface / (W. RICHTER) 6.7. Moraines around Lake Untersee - indicators of the Late-Quaternary regional glacial history / (W. STACKEBRANDT) 7. Satellite sea ice observations in the Atlantic sector of the Southern Ocean / (H. GERNANDT) 7.1. General introduction 7.2. Long-term variations of the sea ice edge / (H. GERNANDT, K. DRESCHER & L. THARANG) 7.2.1. Data evaluation 7.2.2. Mean seasonal variations 7.2.3. Anomalies of sea ice distribution 7.2.4. Interannual variations 7.2.5.Conclusions 7.3. The break-up of ice shelf areas / (H. GERNANDT, P. GLÖDE & J. SCHMECHEL) 7.3.1. Introduction 7.3.2. Satellite observations of the Filchner Ice Shelf's break-up 7.4. Typical sea ice distribution as a response to the circulation of the Southern Ocean / (H. GERNANDT & P. GLÖDE) 7.4.1. Data interpretation 7.4.2. Typical sea ice distributions 7.4.3. Discussion 7.4.4. Conclusions 8. Hydrology / (W. RICHTER & P. BORMANN) 8.1. General remarks 8.2. Fundamentals of physical geography 8.2.1. Hydrographic relevance of geol
    Location: Upper compact magazine
    Location: Upper compact magazine
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    Location: AWI Reading room
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