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|a spa
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|a Stein, Seth
|9 15458
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| 245 |
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|a An introduction to seismology, earthquakes and earth structure /
|c Seth Stein and Michael Wysession
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| 250 |
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|a 11th ed.
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| 260 |
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|a Malden :
|b Blackwell,
|c 2011.
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| 300 |
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|a 498 p. :
|b il., grafs. ;
|c 28 cm.
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| 500 |
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|a Incluye índice analítico
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| 505 |
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|a 1. Introduction. 1.1.1. Overview -- 1.1.2. Models in seismology -- 1.2. Seismology and society -- 1.2.1. Seismic hazards and risks -- 1.2.2. Engineering seismology and earthquake engineering -- 1.2.3. Highways, bridges, dams and pipelines -- 1.2.4. Tsunamis, ladslides and soil liquefaction -- 1.2.5. Earthquake forecasting -- 1.2.6. Earghquake prediction -- 1.2.7. Real-time warnings -- 1.2.8. Nuclear monitoring and treaty verification -- 2. Basic Seismological Theory. 2.1. Introduction -- 2.2. Waves on a string -- 2.2.1. Theory -- 2.2.2. Harmonic wave solution -- 2.2.3. Reflection and transmission -- 2.2.4. Energy in a harmonic wave -- 2.2.5. Normal modes of a sring -- 2.3. Stress and strain -- 2.3.1. Introduction -- 2.3.2. Sress -- 2.3.3. Stress as a tensor -- 2.3.4. Principal stressses -- 2.3.5. Maximum shear stress and faulting -- 2.3.6. Deviatoric stresses -- 2.3.7. Equation of motion -- 2.3.8. Strain -- 2.3.9. constitutive equations -- 2.3.10. Boundary conditions -- 2.3.11. Strain energy -- 2.4. Seismic wavees -- 2.4.1. The seismic wave equation -- 2.4.2. Plane waves -- 2.4.3. spherical waves -- 2.4.4. P and S waves -- 2.4.5. Energy in a plane wave -- 2.5. Snell's law -- 2.5.1. The layered medium approximation -- 2.5.2. Plane wave potentials for a layered medum -- 2.5.3. Angle of incidence and apparent velocity -- 2.5.4. Snell's law -- 2.5.5. critical angle -- 2.5.6. Snell's law for SH slowness -- 2.5.8. Waveguides -- 2.5.9. Fermat's principle and geometric ray theory -- 2.5.10. Huygens'principle and diffraction -- 2.6. Plane wave reflection and transmission coefficients -- 2.6.1. Introducion -- 2.6.2. SH wave reflection and transmission coefficients -- 2.6.3. Energy flux for reflected and transmitted SH waves -- 2.6.4. Postcritical SH waves -- 2.6.5. P-SV waves at a free surface -- 2.6.6. Solid-solid and solid-liquid interfaces -- 2.7. Surface waves -- 2.7.1. Introduction -- 2.7.2. Raryleigh waves in a homogeneous halfspace -- 2.7.3. Love waves in a layer over a halfspace -- 2.7.4. Love wave dispersion -- 2.8. Dispersion -- 2.8.1. Phase and group velocity -- 2.8.2. Disprsive signals -- 2.8.3. Surface wave dispersion studies -- 2.8.4. Tsunami dispersion -- 2.9. Normal modes of the earth -- 2.9.. Motivation -- 2.9.2. Modes of a sphere -- 2.9.3. Spherical harmonics -- 2.9.4. Torsional modes -- 2.9.5. Spheroidal modes -- 2.9.6. Modes and propagating waves -- 2.9.7. Observing normal modes -- 2.9.8. Normal mode synthetic seismograms -- 2.9.9. -- Mode atternation, splitting and coupling -- 3. Seismology and Earth Structure. 3.1. Introduction -- 3.2. Refraction seismology -- 3.2.1. Flat layer method -- 3.2.2. Dipping layer method -- 3.2.3. Advanced analysis methods -- 3.2.4. Crustal structure -- 3.2.5. Rocks and minerals -- 3.3. Reflecion seismology .. 3.3.1. Travel time curves for reflections -- 3.3.2. Intercept-slowness forulation for travel times -- 3.3.3. Multichannel data geometry -- 3.3.4. Common midpoint stacking -- 3.3.5. Signal embancement -- 3.3.6. Deconvolution -- 3.3.7. Migration -- 3.3.8. Data processing sequence -- 3.4. Seismic waves in a spherical earht -- 3.4.1. Ray paths and travel times -- 3.4.2.Velocity distributions -- 3.4.3. Travel time curve inversion -- 3.5. Body wave travel time studies -- 3.5.1. Body wave phases -- 3.5.2. Core phases - 3.5.3. Upper mantle structure -- 3.5.4. Lower mantle structure -- 3.5.5. Visualizing body waves -- 3.6. Anisotropic earth structure -- 3.6.1. General considerations -- 3.6.2. Transverse isotropy and azimuthal amisotropy -- 3.6.3. Anisotropy of minerals and rocks -- 3.6.4. Anisotropy of composite structures -- 3.6.5. Anisotropy in the lithosphere and the athenosphere -- 3.6.6. Anisotropy in the mantle and the core -- 3.7. Attenuation and anelasticity -- 3.7.1. Wave atternuation -- 3.7.2. Geometric spreading -- 3.7.3. Multipathing -- 3.7.4. Scattering -- 3.7.5. Instrinsic atternuation -- 3.7.6. Quality factor, Q -- 3.7.7. Spectral resonance peaks -- 3.7.8. Physical dispersion due to amelasticity -- 3.7.9. Physical models for anelasticity -- 3.7.10. Q from rust to inner core -- 3.8. Composition of the mantle and the core -- 3.8.1. Density within the earth -- 3.8.2. Temperature in the earth -- 3.8.3. Composition of the mantle -- 3.8.4. Composition of D'' --- 3.8.5. Composition of the core -- 3.8.6.Seismology and plantera evolution -- 4. Earthquakes. 4.. Introduction -- 4.2. Focal mechanisms -- 4.2.1. Fault geometry -- 4.2.2. First motions -- 4.2.3. Body wave radiation patterns -- 4.2.4. Stereographic fault plane representation -- 4.2.5. Analytical representation of fault geometry -- 4.3. Waveform modeling -- 4.3.1. Basic model -- 4.3.2. Source time function -- 4.3.3. Body wave modeling -- 4.3.4. Surface wave focal mechanism -- 4.3.5. Once and future earghqakes -- 4.4. Moment tensors -- 4.4.1. Equivalent forces -- 4.4.2. Single forces -- 4.4.3. Force couples -- 4.4.4. Double couples -- 4.4.5. Earthquake moment tensors -- 4.4.6. Isotropic and CLVD moment tensors -- 4.4.7. Moment tensor inversion -- 4.4.8. Interpretation of moment tensors -- 4.5. Earthquake geodesy -- 4.5.1. Measuring ground deformation -- 4.5.2. coseismic deformation -- 4.5.3. Joitn geodetic and seismological earthquake studies -- 4.5.4. Interseismic deformation and the seismic cycle -- 4.6. Source parameters -- 4.6.1. Magnitudes and moment -- 4.6.2. Source spectra and scaling laws -- 4.6.3. Stress drop and earthquake energy -- 4.7. Earthquake statistics. 4.7.1. Frequency-magnitude relations -- 4.7.2. Aftershocks -- 4.7.3. Earthquake probabilities -- 5. Seismology and Plate Tectonics. 5.1. Introduction -- 5.2. Plate kinematics -- 5.2.1. Relative plate motions -- 5.2.2. Global plate motions -- 5.2.3. Space-based geodesy -- 5.2.4. Absolute plate motions -- 5.3. Spreading centers -- 5.3.1. Geometry of ridges and transforms -- 5.3.2. Evolutions of the oceanic lithosphere -- 5.3.3. Ridge and transform earthquakes and processes -- 5.4. Subduction zones -- 5.4.1. Thermal models of sbduction -- 5.4.2. Earthquakes in subducting slabs -- 5.4.3. Interplate trench earthquakes -- 5.5. Oceanic intraplae earthquakes and tectonics -- 5.5.1. Locations of oceanic intraplate seismicity -- 5.5.2. Fources and stresses in the oceanic lithosphere -- 5.5.3. Constraints on mantle viscosity -- 5.6. Continental eartquakes and tectonics -- 5.6.1. Continental plate boundary zones -- 5.6.2. Seismic, aseismic, transient and permanent deformation -- 5.6.3. Continental intraplate earthquake -- 5.7. Faulting and deformation in the earth. 5.7.1.Rheology -- 5.7.2. Rock fracture and friction -- 5.7.3. Ductile flow -- 5.7.4. Strength of the lithosphere -- 5.7.5. Earthquakes and rock friction -- 5.7.6. Earthqakes and regional deformaion -- 6. Seismograms as Signals. 6.1. Introduction -- 6.2. Fourier analysis -- 6.2.1. Fourier series -- 6.2.2. Complex Fourier series -- 6.2.3. Fourier transforms -- 6.2.4. Properties of Fourier transforms -- 6.2.5. Delta functions -- 6.3. Linear systems -- 6.3.1. Basic model -- 6.3.2. Convolution and deconvolution modeling -- 6.3.3. Finite length signals -- 6.3.4. Correlation -- 6.4. Discrete time series and transforms -- 6.4.1. Sampling of continuous data -- 6.4.2. The discrete Fourier transforms -- 6.4.3. Properties of DFTs -- 6.4.4. The fast Fourier transform -- 6.4.5. Digital convolution -- 6.5. Stacking -- 6.5.1. Random errors -- 6.5.2. -- 6.6. Seismometers and seismological networks -- 6.6.1. Introduction -- 6.6.2. The dampted harmonic oscillator -- 6.6.3. Earth noise -- 6.6.4. seismometers and seismographs -- 6.6.5. Digital recording -- 6.6.6. Types of networks -- 6.6.7. Global networks -- 6.6.8. Arrays -- 6.6.9. Regiona networks -- 7. Inverse Problems. Inverse problems -- 7.1. Introduction -- 7.2. Earthquake location -- 7.2.1. Theory -- 7.2.2. Eartquake location for a homogeneous medium -- 7.2.3. Errors -- 7.2.4. Earthquake location for more complex geometries -- 7.3. Travel time tomography -- 7.3.1. Theory -- 7.3.2. Generalized inverse -- 7.3.3. Properties of the generalized inverse solution -- 7.3.4. Variants of the solution -- 7.4. Stratified earth structure -- 7.4.1. Earth structure from normal modes -- 7.4.2. Parameter and data space inversions -- 7.4.3. Features of the solutions -- 7.5. Inverting for plate morions -- 7.5.1. Method -- 7.5.2. Testing the results with X2 and F-ratio tests -- Appendix: mathematical and computational background. A.1. Introduction -- A.2. Complex numbers -- A.3. Scalar products -- A.3.. Vector products -- A. 3.5. Index notation -- A.3.6. Vector spaces -- A.4. Mattrix algebra. A.4.1. definitions -- A.4.2. Determinant -- A.4.3. Inverse -- A.4.04. Systems of linear equations -- A.4.5. Systems of linear equations -- A. 4.5. Solving systems of equations on a computer -- A.5. Vector transformations. A.5.1. Cordinate transformations -- A.5.2. Eigenwalues and eigenvectors -- A.5.3. Symmetric matrix eigenvalues, eigenvectors, diagonalization and decomposition -- A.6. Vector calclus. A.6.1. Scalar and vector fields -- A.6.2. Gradient -- A.6.3. Divergence -- A.6.4. Curl -- A.6.5. Laplacian -- A.7. Spherical coordinates -- A.7.1. The spherical coordinate system -- A.7.2. Distance and azimuth -- A.7.3. Choice of axes -- A.7.4. Vector operators in spherical coordinates -- A.8. Scientific programming. A.8.1. Example: synthetic seismogram calculation -- A.8.2. Programming style -- A.8.3. Representation of numbers -- A.8.4. A few pitfalls -- A.8.5. Some philosophical points.
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| 650 |
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0 |
|a Geología
|9 1052
|
| 650 |
|
0 |
|a Sismología
|9 11128
|
| 700 |
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|a Wysession, Michael
|9 15459
|
| 942 |
|
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|2 CDU
|c LIBRO
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