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  • 1
    Online Resource
    Online Resource
    San Diego :Elsevier Science & Technology,
    Keywords: Geological modeling. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (294 pages)
    Edition: 1st ed.
    ISBN: 9780080532561
    Series Statement: Issn Series ; v.Volume 4
    DDC: 550.113
    Language: English
    Note: Front Cover -- Global Optimization Methods in Geophysical Inversion -- Copyright Page -- Contents -- Preface -- Chapter 1. Preliminary Statistics -- 1.1. Random variables -- 1.2. Random numbers -- 1.3. Probability -- 1.4. Probability distribution, distribution function and density function -- 1.5. Joint and marginal probability distributions -- 1.6. Mathematical expectation, moments, variances, and covariances -- 1.7. Conditional probability -- 1.8. Monte Carlo integration -- 1.9. Importance sampling -- 1.10. Stochastic processes -- 1.11. Markov chains -- 1.12. Homogeneous, inhomogeneous, irreducible and aperiodic Markov chains -- 1.13. The limiting probability -- Chapter 2. Direct, Linear and Iterative-linear Inverse Methods -- 2.1. Direct inversion methods -- 2.2. Model based inversion methods -- 2.3. Linear/linearized inverse methods -- 2.4. Iterative linear methods for quasi-linear problems -- 2.5. Bayesian formulation -- 2.6. Solution using probabilistic formulation -- 2.7. Summary -- Chapter 3. Monte Carlo Methods -- 3.1. Enumerative or grid search techniques -- 3.2. Monte Carlo inversion -- 3.3. Hybrid Monte Carlo-linear inversion -- 3.4. Directed Monte Carlo methods -- Chapter 4. Simulated Annealing Methods -- 4.1. Metropolis algorithm -- 4.2. Heat bath algorithm -- 4.3. Simulated annealing without rejected moves -- 4.4. Fast simulated annealing -- 4.5. Very fast simulated reannealing -- 4.6. Mean -- 4.7. Using SA in geophysical inversion -- 4.8. Summary -- Chapter 5. Genetic Algorithms -- 5.1. A classical GA -- 5.2. Schemata and the fundamental theorem of genetic algorithms -- 5.3. Problems -- 5.4. Combining elements of SA into a new GA -- 5.5. A mathematical model of a GA -- 5.6. Multimodal fitness functions, genetic drift -- 5.7. Uncertainty estimates -- 5.8. Evolutionary programming -- 5.9. Summary. , Chapter 6. Geophysical Applications of SA and G A -- 6.1. 1-D Seismic waveform inversion -- 6.2. Pre-stack migration velocity estimation -- 6.3. Inversion of resistivity sounding data for 1-D earth models -- 6.4. Inversion of resistivity profiling data for 2-D earth models -- 6.5. Inversion of magnetotelluric sounding data for 1-D earth models -- 6.6. Stochastic reservoir modeling -- 6.7. Seismic deconvolution by mean field annealing and Hopfield network -- Chapter 7. Uncertainty Estimation -- 7.1. Methods of Numerical Integration -- 7.2. Simulated annealing: The Gibbs' sampler -- 7.3. Genetic algorithm: The parallel Gibbs' sampler -- 7.4. Numerical examples -- 7.5. Summary -- References -- Subject Index.
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  • 2
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Seismic prospecting. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (188 pages)
    Edition: 1st ed.
    ISBN: 9789400908819
    Series Statement: Modern Approaches in Geophysics Series ; v.8
    Language: English
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  • 3
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical prospecting 30 (1982), S. 0 
    ISSN: 1365-2478
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences , Physics
    Notes: Common midpoint data are now being collected with ever increasing source-receiver offsets. For wide aperture seismic data classical methods of interpretation fail, since velocity analyses and signal-to-noise enhancement methods based on hyperbolic traveltime curves are no longer appropriate. Therefore, the goals of increased velocity resolution and signal enhancement, which motivate the increase in offset, are not achieved. Approximate methods, involving higher order traveltime curves or extrapolations, have been developed for velocity analysis but these are ineffective in the presence of refracted arrivals, and lack a physical basis. These problems can be minimized by transforming the observational data to the domain of intercept or vertical delay time τ and horizontal ray parameter p. In this domain headwave refractions are collapsed into points and both near vertical and wide angle reflections can be analyzed simultaneously to derive velocity-depth information, even in the presence of velocity gradients or low velocity zones.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical prospecting 32 (1984), S. 0 
    ISSN: 1365-2478
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences , Physics
    Notes: Almost all ray-tracing methods ignore the analysis of the amplitudes of seismic arrivals and therefore utilize only half of the available information. We propose a method which is a combination of ray-tracing imaging and transformation of the amplitudes of wide-aperture data.Seismic data in the conventional X-T domain are first transformed to the domain of intercept time τ and ray parameter p to recover the plane wave response. The next step is the derivation of a series of plane wave reflection coefficients, which are mapped as a function of τ and p. The reflection coefficients R(τ, p) for two arbitrarily chosen traces can then be used in our inversion method to derive a slowness-depth and a density-depth profile. It is shown that the inclusion of amplitudes of seismic arrivals (in this method, we consider the acoustic case) makes the inverse method highly stable and accurate. In a horizontally stratified medium one can recover separate profiles of velocity and density. Since this method utilizes large-offset data, it can be used for separate recovery of velocity and density to a greater depth.
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Ice streams drain much of the interior West Antarctic Ice Sheet and buffer the main ice reservoir from oceanic influences,. The slow-flowing interior feeds the floating Ross Ice Shelf with ice via fast-flowing ice streams that are believed to modulate sea-level change through their control of ...
    Type of Medium: Electronic Resource
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