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| Series Preface | ||
| Preface | ||
| 1 | Introduction | 1 |
| 2 | Heterogeneity in the Lithosphere | 7 |
| 3 | Phenomenological Modeling of Coda-Wave Excitation | 41 |
| 4 | Born Approximation for Wave Scattering in Inhomogeneous Media | 87 |
| 5 | Attenuation of High-Frequency Seismic Waves | 109 |
| 6 | Synthesis of Three-Component Seismogram Envelopes for Earthquakes Using Scattering Amplitudes from the Born Approximation | 149 |
| 7 | Envelope Synthesis Based on the Radiative Transfer Theory: Multiple Scattering Models | 173 |
| 8 | Diffraction and Broadening of Seismogram Envelopes | 229 |
| 9 | Summary and Epilogue | 269 |
| Appendix | 277 | |
| Glossary of Symbols | 279 | |
| References | 283 | |
| Subject Index | 303 |
| Price | Condition | Delivery | Seller | Action |
| $174.24 | Digital |
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Add Seismic Wave Propagation and Scattering in the Heterogeneous Earth, Seismic waves — generated both by natural earthquakes and by man-made sources — have produced an enormous amount of information about the Earth's interior. In classical seismology, the Earth is modeled as a sequence of uniform horizontal layers (or speric, Seismic Wave Propagation and Scattering in the Heterogeneous Earth to the inventory that you are selling on WonderClubX
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Add Seismic Wave Propagation and Scattering in the Heterogeneous Earth, Seismic waves — generated both by natural earthquakes and by man-made sources — have produced an enormous amount of information about the Earth's interior. In classical seismology, the Earth is modeled as a sequence of uniform horizontal layers (or speric, Seismic Wave Propagation and Scattering in the Heterogeneous Earth to your collection on WonderClub |