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  • Books  (369)
  • Online Books  (369)
  • 1985-1989  (369)
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  • Books  (369)
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  • 1
    Journal available for loan
    Journal available for loan
    Tübingen : Mohr Siebeck ; 1.1884 - 48.1931; N.F. 1.1932/33 - 10.1943/44(1945),3; 11.1948/49(1949) -
    Call number: ZS 22.95039
    Type of Medium: Journal available for loan
    Pages: Online-Ressource
    ISSN: 1614-0974 , 0015-2218 , 0015-2218
    Language: German , English
    Note: N.F. entfällt ab 57.2000. - Volltext auch als Teil einer Datenbank verfügbar , Ersch. ab 2000 in engl. Sprache mit dt. Hauptsacht.
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  • 2
    Call number: 9783638376723 (ebook)
    Type of Medium: 12
    Pages: 1 Online Ressource (13 Seiten)
    ISBN: 9783638376723
    Language: German
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  • 3
    facet.materialart.12
    Berlin, Heidelberg : Springer
    Call number: doi:10.1007/BFb0011581
    Type of Medium: 12
    Pages: VI, 499 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 3540190864 , 0387190864 , 978-3-540-19086-8 , 978-3-540-39104-3
    Series Statement: Lecture notes in earth sciences 15
    Parallel Title: Digitalisierte Ausg.: The Atlas system of Morocco
    Language: English
    Note: Pages 1-9, Geodynamic evolution of the Atlas system, Morocco: An introduction, Volker Jacobshagen --- Pages 11-17, The Anti-Atlas system: An overview, Eckard Wallbrecher --- Pages 19-42, A ductile shear zone in the Panafrican basement on the northwestern margin of the West African Craton (Sirwa Dome, Central Anti-Atlas, Eckard Wallbrecher --- Pages 43-60, Tectonothermal evolution of the late Panafrican Orogeny in the central Anti-Atlas (Southern Morocco), Yannis Bassias, Eckard Wallbrecher, Alexander Willgallis --- Pages 61-80, A plate tectonic model for the Panafrican Orogeny in the Anti-Atlas, Morocco, Peteralv M. Brabers --- Pages 81-90, The Precambrian/Cambrian boundary in the Anti-Atlas (Morocco) discussion and new results, Werner Buggisch, Erik Flügel --- Pages 91-106, The base of the Cambrian in Morocco, K. Sdzuy, G. Geyer --- Pages 107-121, Paleogeography and facies of the ‘gres terminaux’ (uppermost Lower Cambrian, Anti-Atlas/Morocco), Werner Buggisch, Rainer Siegert --- Pages 123-128, Diagenesis and very low-grade metamorphism of the Lower Cambrian rocks in the Anti-Atlas (Morocco), Werner Buggisch --- Pages 129-138, Deformation of igneous dikes in and around the Tichka granite, high Atlas — Morocco, Jean-Paul Schaer --- Pages 139-168, Synthesis of late paleozoic and triassic redbed sedimentation in Morocco, John C. Lorenz --- Pages 169-199, Jurassic carbonate facies of the Central and Eastern High Atlas rift, Morocco, John E. Warme --- Pages 201-217, Jurassic sediments of the Central High Atlas of Morocco: Deposition, burial and erosian history, Y.A. Brechbühler, R. Bernasconi, J. -P. Schaer --- Pages 219-244, Aspects of Western High Atlas tectonics, Nikolaus Froitzheim, Johannes Stets, Paul Wurster --- Pages 245-271, Structure and post-Palaeozoic evolution of the central High Atlas, Volker Jacobshagen, Rainald Brede, Manfred Hauptmann, Werner Heinitz, Renate Zylka --- Pages 273-291, Structural evolution of the southern and northern Central High Atlas in paleogene and Mio-Pliocene times, Cyril Fraissinet, Mustapha El Zouine, Jean-Luc Morel, André Poisson, Jean Andrieux… --- Pages 293-320, Recent data on the geology of the Middle-Atlas (Morocco), Renaud du Dresnay --- Pages 321-337, Synsedimentary tectonics in the Northern Middle Atlas (Morocco) during the late Cretaceous and Tertiary, Hans-Georg Herbig --- Pages 339-357, Geophysical studies of the earth's crust and upper mantle in the Atlas system of Morocco, Gerhard Schwarz, Peter J. Wigger --- Pages 359-404, The uplift of the central High Atlas as deduced from neogene continental sediments of the Ouarzazate province, Morocco, Konrad Görler, Friedrich-Franz Helmdach, Pieter Gaemers, Kurt Heißig, Winfried Hinsch… --- Pages 405-432, The ostracode fauna of the Ait Kandoula region, systematic description, Friedrich-Franz Helmdach --- Pages 433-444, Geomorphological aspects of the quaternary evolution of the Ouarzazate Basin, Southern Morocco, Gerhard Stäblein --- Pages 445-462, Rates of scarp retreat: A means of dating Neotectonic activity, Karl-Heinz Schmidt --- Pages 463-480, Evolution of the Alboran block margin from early Mesozoic to early Miocene time, M. Durand-Delga, Ph. Olivier --- Pages 481-499, Geodynamic evolution of the Atlas system (Morocco) in post-palaeozoic times, Volker Jacobshagen, Konrad Görler, Peter Giese
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  • 4
    Unknown
    Tokyo : TERRAPUB
    Keywords: space plasmas ; computer simulations ; particle simulations ; MHD simulations
    Description / Table of Contents: PART I PARTICLE SIMULATIONS --- INTRODUCTION TO PARTICLE SIMULATION MODELS AND OTHER APPLICATION TO ELECTROSTATIC PLASMA WAVES / Hideo Okuda / pp. 3-41 --- PARTICLE SIMULATION OF ELECTROMAGNETIC WAVES AND ITS APPLICATION TO SPACE PLASMAS / Hiroshi Matsumoto and Yoshiharu Omura / pp. 43-102 --- RELATIVISTIC CODE APPLIED TO RADIATION GENERATION / A. T. Lin / pp. 103-116 --- MODERN DEVELOPMENT IN PARTICLE SIMULATION / J. C. Adam / pp. 117-130 --- PART II MHD SIMULATIONS --- PRINCIPLES OF MAGNETOHYDRODYNAMIC SIMULATION IN SPACE PLASMAS / Tetsuya Sato / pp. 133-153 --- MHD MODELLING OF THE EARTH'S MAGNETOSPHERE / C. C. Wu / pp. 155-177 --- NUMERICALLY-SIMULATED FORMATION AND PROPAGATION OF INTERPLANETARY SHOCKS / S. T. Wu / pp. 179-201 --- ANOMALOUS TRANSPORT BY KELVIN-HELMHOLTZ INSTABILITIES / Akira Miura / pp. 203-224 --- PART III OTHER-METHOD SIMULATIONS --- PARTICLE BEHAVIOR IN THE MAGNETOSPHERE / R. A. Wolf and R. W. Spiro / pp. 227-254 --- HYBRID SIMULATION TECHNIQUES APPLIED TO THE EARTH'S BOW SHOCK / D. Winske and M. M. Leroy / pp. 255-278 --- VLASOV SIMULATION OF ION ACOUSTIC DOUBLE LAYERS / G. Chanteur / pp. 279-301 --- SIMULATION MODELS FOR SPACE PLASMAS AND BOUNDARY CONDITIONS AS A KEY TO THEIR DESIGN AND ANALYSIS / Christian T. Dum / pp. 303-375
    Pages: Online-Ressource (X, 380 Seiten)
    ISBN: 9027719527
    Language: English
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  • 5
    Unknown
    Tokyo : Terra Scientific Publishing Company
    Keywords: equilibrium form ; fine particles ; surface roughening and melting ; step pattern ; crystal morphology ; morphological stability and perfection ; solution growth ; morphology and growth unit ; snow crystals ; minerals
    Pages: Online-Ressource (XX, 690 Seiten)
    ISBN: 4887041029
    Language: English
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  • 6
  • 7
  • 8
    Unknown
    Berlin ; Heidelberg : Springer
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  • 9
    Unknown
    Berlin ; Heidelberg : Springer
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  • 10
    Unknown
    Berlin ; Heidelberg : Springer
    Description / Table of Contents: INTRODUCTION Over the past 18 years the author and several colleagues have developed a mathematical model designed to predict the propagation characteristics of acoustic waves in marine sediments. The model is based on the classical work of Maurice Biot who developed a comprehensive theory for the mechanics of porous, deformable media in a series of papers spanning the time period from 1941 to 1973. Since our objective was to develop a practical working model that could be used as a guide in planning and interpreting experimental work, we began with the simplest possible form of the model and added various complexities only as they were needed to explain new variations in the data that were obtained. Thus the number of material parameters that had to be measured or assumed at any stage in the development of the model was kept to a minimum. Since the first version of the model was introduced in 1970, we have published over twenty technical papers covering various stages of its development and many papers have been published by colleagues who have utilized our work in various ways. This monograph is an attempt to summarize the development and use of the model to date. Acoustic waves in ocean sediments may be considered as a limiting case in the more general category of mechanical waves that can propagate in fluid-saturated porous media. The general problem of wave motion in this kind of material has been studied extensively over the past thirty years by engineers, geophysicists and acousticians for a variety of reasons. In some cases, interest is focused on low-frequency waves of rather large amplitude, such as those that arise near the source of an earthquake or near a building housing heavy, vibrating machinery. At other times, the main interest is in waves of low frequency and amplitude that have traversed long distances through the sediment. In still another category, high-frequency waves that are able to resolve thin layering and other fine structural details are of interest in studying near-bottom sediments. Thus the full spread of frequency and amplitude has been studied for geological materials ranging from soft, unconsolidated sediments to rock. Because of the almost limitless combinations of different types of sediment, stratification and structure, accurate mathematical description of the wave field produced by a particular source can be constructed only if accurate descriptions of the acoustic properties of individual components can be specified. These properties depend on the geological history of the sediment deposit, on the frequency content of the wave field and on a number of other factors that depend on the environment in situ. A survey of the literature suggests that there are a number of parameters that play principal roles in controlling the dynamic response of saturated sediments...
    Pages: Online-Ressource (153 Seiten)
    ISBN: 9780387971919
    Language: English
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