Principles of Seismology
Kaup valmöguleikar
The second edition of Principles of Seismology has been extensively revised and updated to present a modern approach to observation seismology and the theory behind digital seismograms. It includes: a new chapter on Earthquakes, Earth's structure and dynamics; a considerably revised chapter on instrumentation, with new material on processing of modern digital seismograms and a list of website hosting data and seismological software; and 100 end-of-chapter problems.
The fundamental physical concepts on which seismic theory is based are explained in full detail with step-by-step development of the mathematical derivations, demonstrating the relationship between motions recorded in digital seismograms and the mechanics of deformable bodies. With chapter introductions and summaries, numerous examples, newly drafted illustrations and new color figures, and an updated bibliography and reference list, this intermediate-level textbook is designed to help students develop the skills to tackle real research problems.
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- Cambridge University Press
- 9781108547451
- 9781107138698
- ePub
- 2
- Agustín Udías; Elisa Buforn
- English
- 2017-12-21
- 10
Kaflar
- Cover
- Half title
- Title page
- Imprints page
- Contents
- Preface and Acknowledgments
- 1 Seismology, the science of earthquakes
- 1.1 The historical development
- 1.2 Seismology, a multidisciplinary science
- 1.3 Divisions of seismology
- 1.4 Theory and observations
- 1.5 International cooperation
- 1.6 Books, journals, and websites
- 1.7 Summary
- 2 Earthquakes, Earth structure, and dynamics
- 2.1 Earthquakes: natural disasters
- 2.2 Size of earthquakes
- 2.3 Earthquakes and faults
- 2.4 Spatial distribution of earthquakes
- 2.5 Temporal distribution of earthquakes
- 2.6 Earth’s structure: crust, mantle, and core
- 2.7 Plate tectonics
- 2.8 Earthquake risk, prediction, and prevention
- 2.9 Summary
- 3 Instrumentation and digital data processing
- 3.1 The historical evolution of seismographs
- 3.2 The theory of the seismometer
- 3.3 Recording systems, magnification, and dynamic range
- 3.4 Electromagnetic seismographs
- 3.5 Digital seismographs
- 3.6 Processing digital seismograms
- 3.6.1 Data acquisition
- 3.6.2 Radial and transverse components
- 3.6.3 Removing the instrumental response
- 3.6.4 Spectral analysis
- 3.6.5 Filtering seismograms
- 3.7 Accelerographs
- 3.8 Other types of seismologic instruments
- 3.9 Summary
- 3.10 Problems
- 4 Basic concepts and equations of an elastic medium
- 4.1 Displacement, strain, and stress
- 4.1.1 Eigenvalues and eigenvectors
- 4.2 Elasticity coefficients
- 4.3 The influence of temperature
- 4.4 Work, energy, and heat considerations
- 4.5 Equations of continuity and motion
- 4.5.1 The equations of continuity of mass and energy
- 4.5.2 The equation of motion or momentum
- 4.6 The Lagrangian formulation
- 4.7 Potential functions of displacements and forces
- 4.8 The Green and Somigliana functions of elastodynamics
- 4.9 Theorems of reciprocity and representation
- 4.10 Summary
- 4.11 Problems
- 5 Waves in an infinite elastic medium
- 5.1 Wave equations for an elastic medium
- 5.2 Solutions of the wave equation
- 5.2.1 Wave fronts and rays
- 5.2.2 Waves of several frequencies
- 5.3 Displacement, velocity, and acceleration
- 5.4 The propagation of energy
- 5.4.1 Phase and group velocities
- 5.5 The effect of gravity on wave propagation
- 5.6 Plane waves
- 5.7 The geometry of Ρ and S wave displacements
- 5.8 Particular forms of the potentials
- 5.9 Spherical waves
- 5.10 Cylindrical waves
- 5.11 Summary
- 5.12 Problems
- 6 Reflection and refraction
- 6.1 Snell’s law
- 6.2 Reflection and refraction in two liquid media
- 6.2.1 Normal incidence
- 6.2.2 Critical incidence
- 6.2.3 Inhomogeneous waves
- 6.2.4 Reflected and transmitted energy
- 6.2.5 Reflection on a free surface
- 6.3 Reflection and refraction in elastic media
- 6.3.1 Incident SH waves
- 6.3.2 Critical incidence and inhomogeneous waves
- 6.3.3 Incident Ρ and SV waves
- 6.4 Reflection on a free surface
- 6.4.1 Incident SH waves
- 6.4.2 Incident Ρ waves
- 6.4.3 Incident SV waves
- 6.4.4 Critical reflection of SV waves
- 6.4.5 The partition of energy
- 6.5 Motion at the free surface
- 6.5.1 Incident Ρ waves
- 6.5.2 Incident S waves
- 6.5.3 Apparent angles of incidence and polarization
- 6.6 Summary
- 6.7 Problems
- 7 Body wave propagation in layered media
- 7.1 Wave propagation in the (x, z) plane
- 7.2 The equation for the displacement–stress vector
- 7.3 The propagator matrix
- 7.4 A layered medium with constant parameters
- 7.4.1 Eigenvalues and eigenvectors
- 7.4.2 The propagator matrix for SH motion
- 7.5 SH motion in an elastic layer over a half-space
- 7.6 The general problem
- 7.6.1 SH motion
- 7.6.2 P–SV motion
- 7.7 Summary
- 7.8 Problems
- 8 Ray theory. Media of constant velocity
- 8.1 The eikonal equation
- 8.1.1 The condition of validity
- 8.2 Ray trajectories
- 8.3 Ray trajectories and travel times. A homogeneous half-space
- 8.4 A layer over a half-space with constant velocities
- 8.5 The dipping layer
- 8.6 A plane-layered medium
- 8.7 Summary
- 8.8 Problems
- 9 Ray theory. Media of variable velocity
- 9.1 A variable velocity with depth
- 9.2 The Lagrangian formulation
- 9.3 The change of distance with the ray parameter
- 9.4 The velocity distribution with ζ constant
- 9.5 A linear increase of velocity with depth
- 9.6 Distributions of velocity with depth
- 9.6.1 A gradual increase of velocity
- 9.6.2 A rapid increase in velocity
- 9.6.3 A decrease of velocity. A low-velocity layer
- 9.7 Travel times for deep foci
- 9.8 Reflected rays
- 9.9 Determination of the velocity distribution
- 9.10 The energy propagated by ray beams. Geometrical spreading
- 9.11 Summary
- 9.12 Problems
- 10 Ray theory. Spherical media
- 10.1 The geometry of ray trajectories and displacements
- 10.2 A sphere of constant velocity
- 10.3 A sphere with a velocity that is variable with the radius
- 10.3.1 The change of distance with the ray parameter
- 10.4 A velocity distribution with ζ constant
- 10.5 Rays with circular trajectory
- 10.6 Distribution of the velocity with the radius
- 10.6.1 A normal distribution
- 10.6.2 A rapid increase in velocity
- 10.6.3 A decrease in velocity. A low-velocity layer
- 10.7 Determination of velocity distribution
- 10.8 Energy propagation by ray beams. Geometric spreading
- 10.9 Summary
- 10.10 Problems
- 11 Travel times and the structure of the Earth
- 11.1 Observations and methods
- 11.1.1 Refraction and wide-angle reflection
- 11.1.2 Vertical reflection
- 11.1.3 Seismic tomography
- 11.1.4 Receiver functions
- 11.2 Distribution of velocity, elasticity coefficients, and density
- 11.3 The crust
- 11.3.1 The mineralogical composition of the crust
- 11.4 The upper mantle
- 11.4.1 The lithosphere and the asthenosphere
- 11.5 The lower mantle
- 11.6 The core
- 11.7 Summary
- 11.8 Problems
- 12 Surface waves
- 12.1 Rayleigh waves in a half-space
- 12.1.1 Displacements of Rayleigh waves
- 12.2 A liquid layer over a rigid half-space. Guided waves
- 12.2.1 Constructive interference
- 12.2.2 The dispersion equation and curves
- 12.2.3 Displacements
- 12.3 An elastic layer over a half-space. Love waves
- 12.3.1 Constructive interference
- 12.3.2 Dispersion curves
- 12.3.3 Displacements
- 12.4 An elastic layer over a half-space. Rayleigh waves
- 12.5 Surface waves in layered media
- 12.5.1 Love waves in a layer over a half-space
- 12.6 Surface waves in a spherical medium
- 12.7 Stoneley waves
- 12.8 Summary
- 12.9 Problems
- 13 Wave dispersion. Phase and group velocities
- 13.1 Phase and group velocities
- 13.2 Groups of waves
- 13.3 The principle of a stationary phase
- 13.4 Characteristics of dispersed waves
- 13.5 Determination of group and phase velocities. Instantaneous frequencies
- 13.5.1 The group velocity
- 13.5.2 The phase velocity
- 13.6 Determination of phase and group velocities. Fourier analysis
- 13.6.1 Fourier analysis of seismograms
- 13.6.2 The phase velocity
- 13.6.3 The group velocity
- 13.7 Dispersion curves and the Earth’s structure
- 13.7.1 Observations
- 13.7.2 Interpretation
- 13.8 Summary
- 13.9 Problems
- 14 Free oscillations of the Earth. Theory and observations
- 14.1 Standing waves and modes of vibration
- 14.2 Vibrations of an elastic string of finite length
- 14.3 Vibrations of an elastic rod
- 14.3.1 Longitudinal vibrations
- 14.3.2 Torsional vibrations
- 14.4 The general problem. The Sturm–Liouville equation
- 14.5 Free oscillations of a homogeneous liquid sphere
- 14.6 Free oscillations of an elastic sphere
- 14.7 Toroidal modes
- 14.8 Spheroidal modes
- 14.9 Effects on free oscillations
- 14.10 Observations
- 14.11 Summary
- 14.12 Problems
- 15 Anelasticity and anisotropy
- 15.1 Anelasticity and damping
- 15.1.1 Anelasticity
- 15.1.2 Harmonic excitation of a Maxwellian body
- 15.1.3 Damped harmonic motion. The Q coefficient
- 15.2 Wave attenuation
- 15.3 The attenuation of body and surface waves
- 15.3.1 Body waves
- 15.3.2 Surface waves
- 15.4 The attenuation of free oscillations
- 15.5 The attenuation of coda waves
- 15.6 Attenuation in the Earth
- 15.7 Anisotropy
- 15.8 Wave propagation in anisotropic media
- 15.8.1 Body waves
- 15.8.2 Surface waves
- 15.9 Anisotropy in the Earth
- 15.10 Summary
- 15.11 Problems
- 16 Focal parameters of earthquakes
- 16.1 Location of an earthquake focus
- 16.1.1 Macroseismic determination of epicenter locations
- 16.1.2 Instrumental determination. Graphical methods
- 16.1.3 Numerical methods
- 16.2 Joint hypocenter determination
- 16.3 Seismic intensity
- 16.3.1 Isoseismal or intensity maps
- 16.4 Magnitude
- 16.4.1 Scales of magnitude
- 16.4.2 The saturation of magnitude scales
- 16.5 Seismic energy
- 16.6 The seismic moment, stress drop, and average stress
- 16.7 Summary
- 16.8 Problems
- 17 Basic theory of earthquake mechanism
- 17.1 Earthquakes and faults
- 17.2 Equivalent forces. Point sources
- 17.2.1 Formulation using Green’s function
- 17.2.2 Single and double couples
- 17.3 Fractures and dislocations
- 17.4 The Green function for an infinite medium
- 17.4.1 The radial force
- 17.4.2 An impulsive force in an arbitrary direction
- 17.5 The separation of near and far fields
- 17.5.1 The near field
- 17.5.2 The far field
- 17.6 A shear dislocation or fracture. The point source
- 17.6.1 The radiation pattern
- 17.6.2 The geometry of a shear fracture
- 17.7 The source time function
- 17.8 The equivalence between forces and dislocations
- 17.9 Summary
- 17.10 Problems
- 18 The seismic moment tensor
- 18.1 Definition of the moment tensor
- 18.2 The moment tensor and elastic dislocations
- 18.2.1 An explosive source
- 18.2.2 Shear fracture
- 18.3 Eigenvalues and eigenvectors
- 18.4 Types of sources and separation of the moment tensor
- 18.5 Displacements due to a point source
- 18.6 The temporal dependence
- 18.7 The centroid moment tensor
- 18.8 Inversion of the moment tensor
- 18.9 Summary
- 18.10 Problems
- 19 Simple models of fracture
- 19.1 Source dimensions. Kinematic models
- 19.2 Rectangular faults. Haskell’s model
- 19.3 Circular faults. Brune’s model
- 19.4 Nucleation, propagation, and arrest of a rupture
- 19.5 Dynamic models of fracture
- 19.5.1 The static problem
- 19.5.2 The dynamic problem
- 19.6 Friction models of fracture
- 19.7 The complexity of a fracture
- 19.7.1 The cohesive zone
- 19.7.2 Barriers and asperities
- 19.7.3 Acceleration spectra
- 19.8 Summary
- 19.9 Problems
- 20 Methods of determination of source mechanisms
- 20.1 Parameters and observations
- 20.2 P wave first motion polarities. Fault plane solutions
- 20.2.1 Graphical methods
- 20.2.2 Numerical methods
- 20.3 Wave-form modeling
- 20.4 Inversion of the moment tensor
- 20.4.1 The inversion of Rayleigh waves
- 20.5 Amplitude spectra of seismic waves
- 20.6 Determination of the slip distribution over the fault plane
- 20.7 Summary
- 20.8 Problems
- 21 Seismicity, seismotectonics, seismic risk, and prediction
- 21.1 The spatial distribution of earthquakes
- 21.2 The temporal distribution of earthquakes
- 21.3 Seismic cycles
- 21.4 The distribution of magnitudes
- 21.5 Models of the occurrence of earthquakes
- 21.6 Seismotectonics
- 21.7 Seismic hazard and risk
- 21.8 The prediction of earthquakes
- 21.9 Summary
- Appendices
- Appendix 1 Vectors and tensors
- A1.1 Definitions
- A1.2 Operations with vectors and tensors
- A1.3 Vector and tensor calculus
- Appendix 2 Cylindrical and spherical coordinates
- A2.1 Cylindrical coordinates
- A2.2 Spherical coordinates
- Appendix 3 Bessel and Legendre functions
- A3.1 Bessel functions
- A3.2 Spherical Bessel functions
- A3.3 Legendre functions
- A3.4 Associate Legendre functions
- Appendix 4 Fourier and Laplace transforms
- A4.1 Periodic functions
- A4.2 Non-periodic functions
- A4.3 Convolution and correlation
- A4.4 Sampled functions of finite duration
- A4.5 Laplace transform
- Appendix 5 Parameters of the Earth
- Appendix 6 The interior of The Earth
- Appendix 7 Important earthquakes
- Bibliography
- General seismology textbooks
- Special topics in seismology
- Elasticity and wave mechanics
- References
- Index