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  • 1
    Online Resource
    Online Resource
    Cambridge :Cambridge University Press,
    Keywords: Geophysics. ; Electronic books.
    Description / Table of Contents: Focusing on the relationships between geophysical observations and the underlying physical properties of rocks, this book provides practical solutions to problems in geophysical data interpretation. With over 40% new material and MATLAB® routines for implementing rock physics formulas, this second edition is a vital resource for reservoir geophysicists and engineers.
    Type of Medium: Online Resource
    Pages: 1 online resource (525 pages)
    Edition: 2nd ed.
    ISBN: 9780511539039
    DDC: 552/.06
    Language: English
    Note: Cover -- Half-title -- Title -- Copyright -- Contents -- Preface to the Second Edition -- 1 Basic tools -- 1.1 The Fourier transform -- Synopsis -- Evenness and oddness -- Convolution theorem -- Energy spectrum -- Phase spectrum -- Sampling theorem -- Numerical details -- Spectral estimation and windowing -- Fourier transform theorems -- 1.2 The Hilbert transform and analytic signal -- Synopsis -- Causality -- 1.3 Statistics and probability -- Synopsis -- Regression -- Variogram and covariance function -- Distributions -- Monte Carlo simulations -- Bootstrap -- Statistical classification -- 1.4 Coordinate transformations -- Synopsis -- Assumptions and limitations -- 2 Elasticity and Hookes law -- 2.1 Elastic moduli isotropic form of Hookes law -- Synopsis -- Assumptions and limitations -- 2.2 Anisotropic form of Hookes law -- Synopsis -- Voigt notation -- Voigt stiffness matrix structure for common anisotropy classes -- Isotropic: two independent constants -- Cubic: three independent constants -- Hexagonal or transversely isotropic: five independent constants -- Orthorhombic: nine independent constants -- Monoclinic: 13 independent constants -- Phase velocities for several elastic symmetry classes -- Kelvin notation -- Elastic eigentensors and eigenvalues -- Poissons ratio defined for anisotropic elastic materials -- Assumptions and limitations -- 2.3 Thomsens notation for weak elastic anisotropy -- Synopsis -- Uses -- Assumptions and limitations -- 2.4 Tsvankin's extended Thomsen parameters for orthorhombic media -- Uses -- Assumptions and limitations -- 2.5 Third-order nonlinear elasticity -- Synopsis -- Uses -- Assumptions and limitations -- 2.6 Effective stress properties of rocks -- Synopsis -- Uses -- Assumptions and limitations -- 2.7 Stress-induced anisotropy in rocks -- Synopsis -- Uses -- Assumptions and limitations. , 2.8 Strain components and equations of motion in cylindrical and spherical coordinate systems -- Synopsis -- Uses -- Assumptions and limitations -- 2.9 Deformation of inclusions and cavities in elastic solids -- Synopsis -- General pore deformation -- Effective dry compressibility -- Stress-induced pore pressure: Skempton's coefficient -- Saturated stress-induced pore-volume change -- Low-frequency saturated compressibility -- Three-dimensional ellipsoidal cavities -- Spherical cavity -- Penny-shaped crack: oblate spheroid -- Needle-shaped pore: prolate spheroid -- Two-dimensional tubes -- Plane strain -- Two-dimensional thin cracks -- Ellipsoidal cracks of finite thickness -- Deformation of spherical shells -- Uses -- Assumptions and limitations -- 2.10 Deformation of a circular hole: borehole stresses -- Synopsis -- Hollow cylinder with internal and external pressures -- Circular hole with principal stresses at infinity -- Stress concentration around an elliptical hole -- Stress around an inclined cylindrical hole -- Stress around a vertical cylindrical hole in a poroelastic medium -- Uses -- Assumptions and limitations -- Extensions -- 2.11 Mohr's circles -- Synopsis -- Three-dimensional Mohr's circle -- Two-dimensional Mohr's circle -- Uses -- 2.12 Static and dynamic moduli -- Assumptions and limitations -- 3 Seismic wave propagation -- 3.1 Seismic velocities -- Synopsis -- Assumptions and limitations -- 3.2 Phase, group, and energy velocities -- Synopsis -- Assumptions and limitations -- 3.3 NMO in isotropic and anisotropic media -- Synopsis -- NMO in an anisotropic Earth -- VTI symmetry with horizontal reflector -- Vertical symmetry axis with dipping reflector -- Tilted TI symmetry with dipping reflector -- Orthorhombic symmetry with horizontal reflector -- NMO in a horizontally layered anisotropic Earth -- Synopsis. , 3.4 Impedance, reflectivity, and transmissivity -- Synopsis -- Simple band-limited inverse of reflectivity time series -- Rough surfaces -- Uses -- Assumptions and limitations -- 3.5 Reflectivity and amplitude variations with offset (AVO) in isotropic media -- Synopsis -- AVO: amplitude variations with offset -- Approximate forms -- Assumptions and limitations -- 3.6 Plane-wave reflectivity in anisotropic media -- Synopsis -- Transversely isotropic media: VTI -- Transversely isotropic media: HTI -- Orthorhombic media -- Arbitrary anisotropy -- Assumptions and limitations -- 3.7 Elastic impedance -- Elastic impedance expressions: isotropic -- Elastic impedance expressions: VTI anisotropic -- Elastic impedance expressions: orthorhombic x1-x3 symmetry plane -- Elastic impedance expressions: orthorhombic x2-x3 symmetry plane -- Uses -- Assumptions and limitations -- 3.8 Viscoelasticity and Q -- Synopsis -- Uses -- Assumptions and limitations -- 3.9 Kramers-Kronig relations between velocity dispersion and Q -- Synopsis -- Uses -- Assumptions and limitations -- 3.10 Waves in layered media: full-waveform synthetic seismograms -- Synopsis -- Uses -- Assumptions and limitations -- 3.11 Waves in layered media: stratigraphic filtering and velocity dispersion -- Synopsis -- Uses -- Assumptions and limitations -- 3.12 Waves in layered media: frequency-dependent anisotropy, dispersion, and attenuation -- Synopsis -- One-dimensional layered poroelastic medium -- Uses -- Assumptions and limitations -- 3.13 Scale-dependent seismic velocities in heterogeneous media -- Synopsis -- Layered (one-dimensional) media -- Uses -- Assumptions and limitations -- 3.14 Scattering attenuation -- Synopsis -- Uses -- Assumptions and limitations -- 3.15 Waves in cylindrical rods: the resonant bar -- Synopsis -- Torsional waves -- Longitudinal waves -- Flexural waves -- Bar resonance. , Porous, fluid-saturated rods -- Uses -- Assumptions and limitations -- 3.16 Waves in boreholes -- Synopsis -- Isotropic elastic formation -- Transversely isotropic (TI) elastic formation -- Isotropic, poroelastic, permeable formation -- Uses -- Assumptions and limitations -- Extensions -- 4 Effective elastic media: bounds and mixing laws -- 4.1 Hashin-Shtrikman-Walpole bounds -- Synopsis -- Uses -- Assumptions and limitations -- 4.2 Voigt and Reuss bounds -- Synopsis -- Uses -- Assumptions and limitations -- 4.3 Woods formula -- Synopsis -- Uses -- Assumptions and limitations -- 4.4 Voigt-Reuss-Hill average moduli estimate -- Synopsis -- Uses -- Assumptions and limitations -- 4.5 Composite with uniform shear modulus -- Synopsis -- Uses -- Assumptions and limitations -- 4.6 Rock and pore compressibilities and some pitfalls -- Synopsis -- More on dry-rock compressibility -- Assumptions and limitations -- 4.7 Kuster and Toksöz formulation for effective moduli -- Synopsis -- Assumptions and limitations -- 4.8 Self-consistent approximations of effective moduli -- Synopsis -- Assumptions and limitations -- 4.9 Differential effective medium model -- Synopsis -- Modified DEM with critical porosity constraints -- Uses -- Assumptions and limitations -- 4.10 Hudson's model for cracked media -- Synopsis -- Special cases of crack distributions -- Heavily faulted structures -- Uses -- Assumptions and limitations -- 4.11 Eshelby-Cheng model for cracked anisotropic media -- Synopsis -- Uses -- Assumptions and limitations -- Extensions -- 4.12 T-matrix inclusion models for effective moduli -- Synopsis -- Uses -- Assumptions and limitations -- 4.13 Elastic constants in finely layered media: Backus average -- Synopsis -- Uses -- Assumptions and limitations -- 4.14 Elastic constants in finely layered media: general layer anisotropy -- 4.15 Poroelastic Backus average. , Synopsis -- Uses -- Assumptions and limitations -- 4.16 Seismic response to fractures -- Synopsis -- Quasi-static fracture compliance -- Dynamic response -- Use -- Assumptions and limitations -- 4.17 Bound-filling models -- Synopsis -- Uses -- Assumptions and limitations -- 5 Granular media -- 5.1 Packing and sorting of spheres -- Synopsis -- Packings of identical spheres -- Porosity -- Coordination number -- Binary mixtures of spheres -- Other practical parameters affecting packing -- Uses -- Assumptions and limitations -- 5.2 Thomas-Stieber model for sand-shale systems -- Synopsis -- Assumptions and limitations -- Extensions -- 5.3 Particle size and sorting -- Synopsis -- Particle size -- Sorting -- 5.4 Random spherical grain packings: contact models and effective moduli -- Synopsis -- Contact stiffnesses and effective moduli -- The Hertz-Mindlin Model -- The Walton model -- The Digby model -- The Jenkins et al. model -- The Brandt model -- The Johnson et al. model -- The cemented-sand model -- The uncemented (soft) sand model -- The stiff-sand and intermediate stiff-sand models -- Caveat on the use of effective medium models for granular media -- Uses -- Assumptions and limitations -- Extensions -- 5.5 Ordered spherical grain packings: effective moduli -- Synopsis -- Simple cubic packing -- Hexagonal close packing -- Face-centered cubic packing -- Uses -- Assumptions and limitations -- 6 Fluid effects on wave propagation -- 6.1 Biots velocity relations -- Synopsis -- Slow S-wave -- Uses -- Assumptions and limitations -- Extensions -- 6.2 Geertsma-Smit approximations of Biots relations -- Synopsis -- Uses -- Assumptions and limitations -- 6.3 Gassmann's relations: isotropic form -- Synopsis -- Compressibility form -- Reuss average form -- Linear form -- P-wave modulus form -- Velocity form -- Pore stiffness interpretation -- Biot coefficient. , VP but no VS.
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  • 2
    Online Resource
    Online Resource
    Newark :John Wiley & Sons, Incorporated,
    Keywords: Seismology-Mathematics. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (259 pages)
    Edition: 1st ed.
    ISBN: 9781119086192
    DDC: 622.338015118
    Language: English
    Note: Cover -- Title Page -- Copyright Page -- Contents -- Preface -- Acknowledgments -- Chapter 1 Review of Probability and Statistics -- 1.1 Introduction to Probability and Statistics -- 1.2 Probability -- 1.3 Statistics -- 1.3.1 Univariate Distributions -- 1.3.2 Multivariate Distributions -- 1.4 Probability Distributions -- 1.4.1 Bernoulli Distribution -- 1.4.2 Uniform Distribution -- 1.4.3 Gaussian Distribution -- 1.4.4 Log-Gaussian Distribution -- 1.4.5 Gaussian Mixture Distribution -- 1.4.6 Beta Distribution -- 1.5 Functions of Random Variable -- 1.6 Inverse Theory -- 1.7 Bayesian Inversion -- Chapter 2 Rock Physics Models -- 2.1 Rock Physics Relations -- 2.1.1 Porosity - Velocity Relations -- 2.1.2 Porosity - Clay Volume - Velocity Relations -- 2.1.3 P-Wave and S-Wave Velocity Relations -- 2.1.4 Velocity and Density -- 2.2 Effective Media -- 2.2.1 Solid Phase -- 2.2.2 Fluid Phase -- 2.3 Critical Porosity Concept -- 2.4 Granular Media Models -- 2.5 Inclusion Models -- 2.6 Gassmann's Equations and Fluid Substitution -- 2.7 Other Rock Physics Relations -- 2.8 Application -- Chapter 3 Geostatistics for Continuous Properties -- 3.1 Introduction to Spatial Correlation -- 3.2 Spatial Correlation Functions -- 3.3 Spatial Interpolation -- 3.4 Kriging -- 3.4.1 Simple Kriging -- 3.4.2 Data Configuration -- 3.4.3 Ordinary Kriging and Universal Kriging -- 3.4.4 Cokriging -- 3.5 Sequential Simulations -- 3.5.1 Sequential Gaussian Simulation -- 3.5.2 Sequential Gaussian Co-Simulation -- 3.6 Other Simulation Methods -- 3.7 Application -- Chapter 4 Geostatistics for Discrete Properties -- 4.1 Indicator Kriging -- 4.2 Sequential Indicator Simulation -- 4.3 Truncated Gaussian Simulation -- 4.4 Markov Chain Models -- 4.5 Multiple-Point Statistics -- 4.6 Application -- Chapter 5 Seismic and Petrophysical Inversion -- 5.1 Seismic Modeling -- 5.2 Bayesian Inversion. , 5.3 Bayesian Linearized AVO Inversion -- 5.3.1 Forward Model -- 5.3.2 Inverse Problem -- 5.4 Bayesian Rock Physics Inversion -- 5.4.1 Linear - Gaussian Case -- 5.4.2 Linear - Gaussian Mixture Case -- 5.4.3 Non-linear - Gaussian Mixture Case -- 5.4.4 Non-linear - Non-parametric Case -- 5.5 Uncertainty Propagation -- 5.6 Geostatistical Inversion -- 5.6.1 Markov Chain Monte Carlo Methods -- 5.6.2 Ensemble Smoother Method -- 5.6.3 Gradual Deformation Method -- 5.7 Other Stochastic Methods -- Chapter 6 Seismic Facies Inversion -- 6.1 Bayesian Classification -- 6.2 Bayesian Markov Chain Gaussian Mixture Inversion -- 6.3 Multimodal Markov Chain Monte Carlo Inversion -- 6.4 Probability Perturbation Method -- 6.5 Other Stochastic Methods -- Chapter 7 Integrated Methods -- 7.1 Sources of Uncertainty -- 7.2 Time-Lapse Seismic Inversion -- 7.3 Electromagnetic Inversion -- 7.4 History Matching -- 7.5 Value of Information -- Chapter 8 Case Studies -- 8.1 Hydrocarbon Reservoir Studies -- 8.1.1 Bayesian Linearized Inversion -- 8.1.2 Ensemble Smoother Inversion -- 8.1.3 Multimodal Markov Chain Monte Carlo Inversion -- 8.2 CO2 Sequestration Study -- Appendix: MATLAB Codes -- A.1 Rock Physics Modeling -- A.2 Geostatistical Modeling -- A.3 Inverse Modeling -- A.3.1 Seismic Inversion -- A.3.2 Petrophysical Inversion -- A.3.3 Ensemble Smoother Inversion -- A.4 Facies Modeling -- References -- Index -- EULA.
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  • 3
    Online Resource
    Online Resource
    Cambridge :Cambridge University Press,
    Keywords: Earth sciences--Information services. ; Electronic books.
    Description / Table of Contents: This book presents a unified framework for assessing the value of potential data gathering schemes by integrating spatial modelling and decision analysis, with a focus on the Earth sciences. Real datasets and MATLAB codes are provided online, making this an invaluable reference for students, researchers, and industry professionals.
    Type of Medium: Online Resource
    Pages: 1 online resource (402 pages)
    Edition: 1st ed.
    ISBN: 9781316437803
    DDC: 550.01/156
    Language: English
    Note: Cover -- Half-title -- Title page -- Copyright information -- Table of contents -- Preface -- Acknowledgments -- 1 Introduction -- 1.1 What is the value of information? -- 1.2 Motivating examples from the Earth sciences -- 1.3 Contributions of this book -- 1.4 Organization -- 1.5 Intended audience and prerequisites -- 1.6 Bibliographic notes -- 2 Statistical models and methods -- 2.1 Uncertainty quantification, information gathering, and data examples -- 2.2 Notation and probability models -- 2.2.1 Univariate probability distributions -- 2.2.2 Multivariate probability distributions -- 2.3 Conditional probability, graphical models, and Bayes' rule -- 2.3.1 Conditional probability -- 2.3.2 Graphical models -- 2.3.3 Bayesian updating from data -- 2.3.4 Examples -- Treasure Island: The pirate example -- Gotta get myself connected: Bayesian network example -- Never break the chain: Markov chain example -- For whom the bell tolls: Gaussian projects example -- 2.4 Inference of model parameters -- 2.4.1 Maximum likelihood estimation -- 2.4.2 Examples -- I love rock and ore: mining oxide grade example -- Never break the chain: Markov chain example -- 2.5 Monte Carlo methods and other approximation techniques -- 2.5.1 Analysis by simulation -- 2.5.2 Solving integrals -- 2.5.3 Sampling methods -- 2.5.4 Example -- Risky business: petroleum prospect risking example -- 2.6 Bibliographic notes -- Models -- Estimation and sampling -- 3 Decision analysis -- 3.1 Background -- 3.2 Decision situations: terminology and notation -- 3.2.1 Decisions, uncertainties, and values -- 3.2.2 Utilities and certain equivalent -- 3.2.3 Maximizing expected utility -- 3.2.4 Examples -- Treasure island: the pirate example -- For whom the bell tolls: Gaussian projects example -- 3.3 Graphical models -- 3.3.1 Decision trees -- 3.3.2 Influence diagrams -- 3.3.3 Examples. , For whom the bell tolls: Gaussian projects example -- MacKenna's gold: oil and gold example -- Time after time: time-lapse seismic example -- Value from 4-D seismic monitoring -- Influence diagrams for 4-D seismic monitoring -- Observable property nodes -- Reservoir property nodes -- Seismic property nodes -- 3.4 Value of information -- 3.4.1 Definition -- 3.4.2 Perfect versus imperfect information -- 3.4.3 Relevant, material, and economic information -- 3.4.4 Examples -- Treasure island: the pirate example -- For whom the bell tolls: Gaussian projects example -- 3.5 Bibliographic notes -- Decision analysis fundamentals -- Graphical models -- VOI fundamentals -- VOI for canonical problems -- Computational issues and application reviews -- 4 Spatial modeling -- 4.1 Goals of stochastic modeling of spatial processes -- 4.2 Random fields, variograms, and covariance -- 4.3 Prediction and simulation -- 4.3.1 Spatial prediction and Kriging -- 4.3.2 Common geostatistical stochastic simulation methods -- 4.4 Gaussian models -- 4.4.1 The spatial regression model -- 4.4.2 Optimal spatial prediction: Kriging -- 4.4.3 Multivariate hierarchical spatial regression model -- 4.4.4 Examples -- Norwegian wood: forestry example -- I love rock and ore: mining oxide grade example -- 4.5 Non-Gaussian response models and hierarchical spatial models -- 4.5.1 Skew-normal models -- 4.5.2 Spatial generalized linear models -- 4.5.3 Example -- We will rock you: rock hazard example -- 4.6 Categorical spatial models -- 4.6.1 Indicator random variables -- 4.6.2 Truncated Gaussian and pluri-Gaussian models -- 4.6.3 Categorical Markov random field models -- 4.6.4 Example -- Black gold in a white plight: reservoir characterization example -- 4.7 Multiple-point geostatistics -- 4.7.1 Algorithms -- 4.7.2 Example -- Go with the flow: petroleum simulation example -- 4.8 Bibliographic notes. , Traditional geostatistics books describing variogram methods, Kriging, and simulation -- Sequential simulation techniques and related topics -- Spatial statistics -- Non-Gaussian response models -- Markov random fields -- Multiple-point geostatistics -- Spatiotemporal models -- 5 Value of information in spatial decision situations -- 5.1 Introduction -- 5.1.1 Spatial decision situations -- 5.1.2 Information gathering in spatial decision situations -- 5.1.3 Overview of models -- 5.2 Value of information: a formulation for static models -- 5.2.1 Prior value -- 5.2.2 Posterior value -- Perfect information -- Imperfect information -- 5.2.3 Special cases: an overview -- 5.3 Special case: low decision flexibility and decoupled value -- 5.3.1 Prior value -- 5.3.2 Posterior value -- 5.3.3 Computational notes -- 5.3.4 Example -- Norwegian wood: forestry example -- Framing the decision situation -- Information gathering -- Modeling -- VOI analysis -- 5.4 Special case: high decision flexibility and decoupled value -- 5.4.1 Prior value -- 5.4.2 Posterior value -- 5.4.3 Computational notes -- 5.4.4 Examples -- Never break the chain: Markov chain example -- Framing the decision situation -- Information gathering -- Modeling -- VOI analysis -- The tree amigos: conservation biology example -- Framing the decision situation -- Information gathering -- Modeling -- VOI analysis -- Norwegian wood: forestry example -- Framing the decision situation -- Information gathering -- Modeling -- VOI analysis -- 5.5 Special case: low decision flexibility and coupled value -- 5.5.1 Prior value -- 5.5.2 Posterior value -- 5.5.3 Computational notes -- 5.5.4 Example -- Go with the flow: petroleum simulation example -- Framing the decision situation -- Information gathering -- Modeling -- VOI analysis -- 5.6 Special case: high decision flexibility and coupled value. , 5.6.1 Prior value -- 5.6.2 Posterior value -- 5.6.3 Computational notes -- 5.6.4 Example -- Frozen: hydropower example -- Framing the decision situation -- Information gathering -- Modeling -- VOI analysis -- 5.7 More complex decision situations -- 5.7.1 Generalized risk preferences -- 5.7.2 Additional constraints -- The tree amigos: conservation biology example -- 5.7.3 Sequential decision situations -- Gotta get myself connected: Bayesian network example -- 5.8 Sequential information gathering -- For whom the bell tolls: Gaussian projects example -- 5.9 Other information measures -- 5.9.1 Entropy -- 5.9.2 Prediction variance -- Norwegian wood: forestry example -- 5.9.3 Prediction error -- The tree amigos: conservation biology example -- 5.10 Bibliographic notes -- Low decision flexibility and decoupled value -- Low decision flexibility and coupled value -- High decision flexibility and decoupled value -- High decision flexibility and coupled value -- More complex decision situations -- Other information measures -- 6 Earth sciences applications -- 6.1 Workflow -- 6.2 Exploration of petroleum prospects -- 6.2.1 Gotta get myself connected: Bayesian network example -- Framing the decision situation -- Information gathering -- Modeling -- VOI analysis -- 6.2.2 Basin street blues: basin modeling example -- Framing the decision situation -- Information gathering -- Modeling -- VOI analysis -- 6.2.3 Risky business: petroleum prospect risking example -- Framing the decision situation -- Information gathering -- Modeling -- VOI analysis -- 6.3 Reservoir characterization from geophysical data -- 6.3.1 Black gold in a white plight: reservoir characterization example -- Framing the decision situation -- Information gathering -- Modeling -- VOI analysis -- 6.3.2 Reservoir dogs: seismic and electromagnetic data example -- Framing the decision situation. , Information gathering -- Modeling -- VOI analysis -- 6.4 Mine planning and safety -- 6.4.1 I love rock and ore: mining oxide grade example -- Framing the decision situation -- Information gathering -- Modeling -- VOI analysis -- 6.4.2 We will rock you: rock hazard example -- Framing the decision situation -- Information gathering -- Modeling -- VOI analysis -- 6.5 Groundwater management -- 6.5.1 Salt water wells in my eyes: groundwater management example -- Framing the decision situation -- Information gathering -- Modeling -- VOI analysis -- 6.6 Bibliographic notes -- Petroleum -- Mining planning and safety -- Groundwater, hydrology, and geothermal resources -- Environmental applications -- Biological conservation, forestry, and fishing -- Agriculture and climate forecasting -- 7 Problems and projects -- 7.1 Problems and tutorial hands-on projects -- 7.1.1 Problem sets -- 7.1.2 Hands-on projects -- The tree amigos: conservation biology example -- Part I: parameter specification -- Part II: value of information -- Go with the flow: petroleum simulation example -- Part I: downloading realization outputs -- Part II: generate realizations from geologic scenario -- Part III: VOI analysis using approximate Bayesian computing -- Frozen: hydropower example -- Time after time: time-lapse seismic example -- Norwegian wood: forestry example -- Part I: parameter estimation and Kriging -- Part II: VOI analysis and spatial design -- 7.2 Hands on: exploration of petroleum prospects -- 7.2.1 Gotta get myself connected: Bayesian network example -- Part I: small network -- Part II: North Sea network with 25 segments -- 7.2.2 Basin street blues: basin modeling example -- 7.2.3 Risky business: petroleum prospect risking example -- 7.3 Hands on: reservoir characterization from geophysical data -- 7.3.1 Black gold in a white plight: reservoir characterization example. , Part I: modeling and prediction from seismic amplitude versus offset data.
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  • 4
    Book
    Book
    Cambridge [u.a.] : Cambridge Univ. Press
    Keywords: Petrophysik
    Type of Medium: Book
    Pages: X, 329 S. , graph. Darst. , 26 cm
    Edition: 1. publ., reprint.
    ISBN: 0521620686
    DDC: 552/.06
    RVK:
    RVK:
    Language: English
    Note: Literaturverz. S. 313 - 324
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford BSL : Blackwell Science Ltd
    Geophysical prospecting 47 (1999), S. 0 
    ISSN: 1365-2478
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences , Physics
    Notes: Modelling of AVO signatures for reservoir characterization requires VS estimation from other available logs when shear-wave data are not available. We tested various models for predicting VS from P-wave velocity, porosity and shale volume measured in well logs. Effective medium models which characterize the pore space in terms of ellipsoidal inclusions were compared with statistical VP–VS regressions. The inclusion models were calibrated by non-linear minimization of the difference between model-predicted velocities and actual measured velocities. The quality of the VS prediction was quantified in terms of the rms error by comparison with shear-wave data in wells where both VP and VS were measured. The linear regressions were found to be more robust and the rms error in the prediction was comparable to effective medium model-based predictions.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 146 (1996), S. 393-404 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1573-8868
    Keywords: spatial filtering ; spectral coverage ; cokriging
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract When seismic data and porosity well logs contain information at different spatial scales, it is important to do a scale-matching of the datasets. Combining different data types with scale mismatch can lead to suboptimal results. A good correlation between seismic velocity and rock properties provides a basis for integrating seismic data in the estimation of petrophysical properties. Three-dimensional seismic data provides an unique exhaustive coverage of the interwell reservoir region not available from well data. However, because of the limitations of measurement frequency bandwidth and view angles, the seismic image can not capture the true seismic velocity at all spatial scales present in the earth. The small-scale spatial structure of heterogeneities may be absent in the measured seismic data. In order to take best advantage of the seismic data, factorial kriging is applied to separate the small and large-scale structures of both porosity and seismic data. Then the spatial structures in seismic data which are poorly correlated with porosity are filtered out prior to integrating seismic data into porosity estimation.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Mathematical geology 29 (1997), S. 933-950 
    ISSN: 1573-8868
    Keywords: seismic image response ; Born approximation ; spectral filtering
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract Seismic measurements may be used in geostatistical techniques for estimation and simulation of petrophysical properties such as porosity. The good correlation between seismic and rock properties provides a basis for these techniques. Seismic data have a wide spatial coverage not available in log or core data. However, each seismic measurement has a characteristic response function determined by the source-receiver geometry and signal bandwidth. The image response of the seismic measurement gives a filtered version of the true velocity image. Therefore the seismic image cannot reflect exactly the true seismic velocity at all scales of spatial heterogeneities present in the Earth. The seismic response function can be approximated conveniently in the spatial spectral domain using the Born approximation. How the seismic image response affects the estimation of variogram. and spatial scales and its impact on geostatistical results is the focus of this paper. Limitations of view angles and signal bandwidth not only smooth the seismic image, increasing the variogram range, but also can introduce anisotropic spatial structures into the image. The seismic data are enhanced by better characterizing and quantifying these attributes. As an exercise, examples of seismically assisted cokriging and cosimulation of porosity between wells are presented.
    Type of Medium: Electronic Resource
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