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  • 1
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : American Geophysical Union
    Associated volumes
    Call number: MR 90.0965 ; 4/M 92.1327/15 ; ILP/M 06.0118
    In: Geodynamics series
    In: Publication of the International Lithosphere Programme
    Type of Medium: Monograph available for loan
    Pages: xi, 153 S. : graph. Darst.
    ISBN: 0875905153
    Series Statement: Geodynamics series 15
    Classification:
    Oceanology
    Language: English
    Location: Upper compact magazine
    Location: Reading room
    Location: Reading room
    Branch Library: GFZ Library
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Academic Pr.
    Call number: M 480
    Type of Medium: Monograph available for loan
    Pages: 263 S. : Ill., graph. Darst.
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: AWI G1-96-0290
    Description / Table of Contents: Contents: 1 Introduction. - Why lecturing? Why this Textbook? Why Physical Principles? Why a Readable Textbook? 2 Sorting Out And Mixing. - Bulk Minerals - Heavy Minerals - Size and Sorting Exclusion Principle 3 Grains Settle. - Stokes' Law - why Derivation - Dimensional Analysis Fluid Resistance - Reynolds Number - Resistance Coefficient Lacustrine Varves. - 4 Sediments Are Moved. - Turbidity Currents - Chezy's Equation - Stream Transport Shield's Diagram - Hjulström's Curve. - 5 Rocks Fall. - Sediment - Gravity Flows - Elm Landslide - Grand Banks Slide Speed of Slides - Debris Flows - Sand Avalanches Mud Slide - Olistostrome. - 6 Suspensions Flow. - Suspension Current - Auto-suspension - Bagnold's Criterion - Chezy-Kuenen Equation - Keulegan's Law Energy Line. - 7 Sand Waves Migrate. - Froude Number - Richardson Number - Model Theory - Bedform Point-Bar Sequence - Faciès Models. - 8 Oceans Are Ventilated. - Ocean Currents - Bernoulli's Theorem - Darcy-Weisbach Equation Contourites. - 9 Groundwater Circulates. - Darcy Equation - Poiseuille Law - Hydrodynamic Potential Permeability - Compaction - Diffusion. - 10 Components Equilibrate. - Mass-Action Law - Gibbs Criteria of Chemical Equilibrium - First and Second Law of Thermodynamics - Lewis Concept of Chemical Activity - Carbonate Equilibria Metastable Phases - Calcite Dissolution. - 11 Evaporation Pumps. - Dolomite - Dolomite Solubility Material Transfer in Open Systems Seepage Refluxing - Evaporative Pumping - Flood Recharge. - 12 Isotopes Fractionate. - Isotopes - Isotope Tracers - Paleotemperature - Paleoproductivity - Strangelove Ocean. - 13 Basins Subside. - Isostasy - Airy Model - Crustal Thinning - Mantle Heterogeneity Lithospheric Stresses. - 14 Why Creativity in Geology?. - Appendix I. - Appendix II. - References. - Index.
    Description / Table of Contents: Physical principles of sedimentology is a textbook devoted to the physics of sedimentological processes. The applicability of fundamental principles, such as Newton's Three Laws of Motion, the Law of Conservation of Energy, the First and Second Laws of Thermodynamics, and of other physical relations in hydraulics and groundwater hydrology is illustrated by discussions of natural processes which form sediments or sedimentary rocks. The author's educational background as a major in physics and geology, and his 40-year experience in teaching and research have enabled him to bring together physics and geology in this enjoyable and highly readable text.
    Type of Medium: Monograph available for loan
    Pages: X, 233 S. : Ill., graph. Darst., Kt.
    ISBN: 3540512683
    Branch Library: AWI Library
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  • 4
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    The @island arc 1 (1992), S. 0 
    ISSN: 1440-1738
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Abstract Large petroliferous basins in the continental interior are characterized by very thick sedimentary sequences. It is suggested that these are not intracratonic basins, but areas underlain by oceanic crust. These include the Western Siberian, Pre-Caspian, South Caspian, North and South Kara Basins of the Commonwealth of Independent States, and Tarim, junggar and Qaidam Basins of China. The relict ocean basins are distinguished by their basement topography, by their magnetic signatures and by their elevated Moho. Their sedimentary history is distinguished by an abrupt subsidence, followed by isostastic subsidence under sedimentary load. Two circumstances have contributed to the genesis of giant hydrocarbon deposits in these basins: (1) the geochemical environment in those basins was at one time oxygen-deficient as they evolved from the open marine, through restricted marine to become inland alluvial basins; and (2) the sedimentary in-fill provide thick reservoir beds. Oil has accumulated in older structures, folds, faults, unconformities etc. on the margin of the basins, trapping early migrated hydrocarbons.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 23 (1976), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Three series of density-current experiments were performed in a 5.76 m flume. In the first series, the flume was horizontal, and in the second and third, it was inclined with a positive slope and negative slope, respectively. Energy relations during successive stages of density-current movement were computed from observed data, which showed an appreciable frictional energy dissipation. The computed friction factors of our experimental density-flows were compared to the friction factors for pipe flows (Moody diagram), and while the calculated friction factor increases with increasing Reynold's number within the range of our experiments (Re 2 × 103−2 × 104), it is concluded that with increasing Reynold's number above about 5 × 104 the friction factor decreases. For natural turbidity currents, the Moody diagram gives a reasonable estimate of the friction factor between the current and sediment bed. The value of the friction factor for the interface between the current and overlying water was found to be about 0.2 times the friction factor for the current and flume. However, due to errors inherent in measuring the depth of the current, a value of 0.4 would be more reasonable for density-currents in our range of Reynold's number. Friction tends to decrease the value of the dimensionless coefficient in Keulegan's law of saline front and to decrease the thickness of the flow. In contrast, the presence of a slope in the direction of flow tends to compensate the effect of friction. The angle θc that provides the potential energy to exactly offset the energy losses incurred during movement by the density-currents in our experiments has a calculated value of 31′. An empirical formula φ= 0.935θ—0·57 relating friction, in terms of the hydraulic gradient φ, to the slope angle θ was obtained. Since the thickness of the current can be computed from the relationship between φ and θ, we estimated the thickness of naturally occurring density-currents in Swiss lakes. The results suggest the applicability of our experimental results to small turbidity currents in nature. Our analysis further indicates that large turbidity currents have a small φ and can be expected to flow very long distances on a flat abyssal plain.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 31 (1984), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Experiments were carried out in a 10 × 6 m basin to simulate turbidity currents generated by the Horgen Slumping Events of 1875. The conditions for kinematic similarity were satisfied and the experiments gave further insight into the mechanics of transport triggered by the Horgen slumps. The experimental turbidity currents laid down thick deposits on a subaqueous fan, and thin sheets of turbidite on the floor of the elongate basin through longitudinal transport, comparable with the simulated deposits in Lake Zurich. It is concluded that longitudinal transport is a general phenomenon of turbidity currents.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 33 (1986), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 20 (1973), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 24 (1977), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 285 (1980), S. 201-203 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Evidence is presented indicating that the extinction, at the end of the Cretaceous, of large terrestrial animals was caused by atmospheric heating during a cometary impact and that the extinction of calcareous marine plankton was a consequence of poisoning by cyanide released by the fallen comet ...
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