Acoustic and Elastic Wave Fields in Geophysics, II
โ Scribed by A.A. Kaufman, A.L. Levshin and K.L. Larner (Eds.)
- Publisher
- Academic Press, Elsevier
- Year
- 2002
- Leaves
- 618
- Series
- Methods in Geochemistry and Geophysics 37
- Category
- Library
No coin nor oath required. For personal study only.
โฆ Table of Contents
Content:
Introduction
Pages vii-viii
Acknowledgments
Page ix
List of symbols
Pages xi-xii
Chapter 1 Principles of geometrical acoustics Original Research Article
Pages 1-98
Chapter 2 Dynamics of high-frequency wave fields Original Research Article
Pages 99-185
Chapter 3 Basics of Kirchhoff migration Original Research Article
Pages 187-238
Chapter 4 Plane waves in layered media (normal incidence) Original Research Article
Pages 239-272
Chapter 5 Plane waves in layered media (oblique incidence) Original Research Article
Pages 273-366
Chapter 6 Spherical waves in the presence of horizontal interface Original Research Article
Pages 367-450
Chapter 7 Propagation of waves inside a layer Original Research Article
Pages 451-496
Chapter 8 Acoustic potential in a medium with a cylindrical interface Original Research Article
Pages 497-518
Appendix A Functions of complex variables
Pages 519-553
Appendix B Hilbert transform
Pages 555-559
Appendix C The saddle point method
Pages 561-577
Appendix D Differential equations
Pages 579-612
References
Pages 613-614
Index
Pages 615-617
๐ SIMILAR VOLUMES
This monograph is the last volume in the series 'Acoustic and Elastic Wave Fields in Geophysics'. The previous two volumes published by Elsevier (2000, 2002) dealt mostly with wave propagation in liquid media. <p> The third volume is dedicated to propagation of plane, spherical and cylindrical ela
Volume One begins with a systematic development of basic concepts (strain, stress, stiffness and compliance, viscous clamping) and coordinate transformations in both tensor and matrix notation. The basic elastic field equations are then written in a form analogous to Maxwell's equations. This analog
<p>45 downwards because (j on the average increases with height; but this conclusion does not follow from (18.3) when the dependency of Kc upon ~o is taken into consideration. s 2 ERTELl and PRIESTLEY and SWINBANK have shown that the upward eddyยญ flux of sensible heat must be larger than indicated b