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Seismic waves and rays in elastic media /

This book seeks to explore seismic phenomena in elastic media and emphasizes the interdependence of mathematical formulation and physical meaning. The purpose of this title - which is intended for senior undergraduate and graduate students as well as scientists interested in quantitative seismology...

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Detalles Bibliográficos
Clasificación:Libro Electrónico
Autor principal: Slawinski, M. A. (Michael A.), 1961-
Formato: Electrónico eBook
Idioma:Inglés
Publicado: Oxford : Pergamon, 2003.
Edición:1st ed.
Colección:Handbook of geophysical exploration. Seismic exploration ; v. 34.
Temas:
Acceso en línea:Texto completo
Texto completo

MARC

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100 1 |a Slawinski, M. A.  |q (Michael A.),  |d 1961- 
245 1 0 |a Seismic waves and rays in elastic media /  |c by M.A. Slawinski. 
250 |a 1st ed. 
260 |a Oxford :  |b Pergamon,  |c 2003. 
300 |a 1 online resource (xxi, 401 pages) :  |b illustrations, portraits (some color) 
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490 1 |a Handbook of geophysical exploration. Section I, Seismic exploration,  |x 0950-1401 ;  |v v. 34 
520 |a This book seeks to explore seismic phenomena in elastic media and emphasizes the interdependence of mathematical formulation and physical meaning. The purpose of this title - which is intended for senior undergraduate and graduate students as well as scientists interested in quantitative seismology - is to use aspects of continuum mechanics, wave theory and ray theory to describe phenomena resulting from the propagation of waves. The book is divided into three parts: Elastic continua, Waves and rays, and Variational formulation of rays. In Part I, continuum mechanics are used to describe the material through which seismic waves propagate, and to formulate a system of equations to study the behaviour of such material. In Part II, these equations are used to identify the types of body waves propagating in elastic continua as well as to express their velocities and displacements in terms of the properties of these continua. To solve the equations of motion in anisotropic inhomogeneous continua, the high-frequency approximation is used and establishes the concept of a ray. In Part III, it is shown that in elastic continua a ray is tantamount to a trajectory along which a seismic signal propagates in accordance with the variational principle of stationary travel time. 
504 |a Includes bibliographical references (pages 359-373) and index. 
588 0 |a Print version record. 
505 0 |a Front Cover; Seismic Waves and Rays in Elastic Media; Copyright Page; Contents; Part I: Elastic continua; Introduction to Part I; Chapter 1. Deformations; Chapter 2. Forces and balance principles; Chapter 3. Stress -- strain equations; Chapter 4. Strain energy; Chapter 5. Material symmetry; Part II: Waves and rays; Introduction to Part II; Chapter 6. Equations of motion: Isotropic homogeneous continua; Chapter 7. Equations of motion: Anisotropic inhomogeneous continua; Chapter 8. Hamilton' s ray equations; Chapter 9. Lagrange's ray equations; Chapter 10. Christoffel' s equations 
546 |a English. 
650 0 |a Seismic waves. 
650 0 |a Continuum mechanics. 
650 0 |a Seismology  |x Mathematics. 
650 6 |a Ondes sismiques.  |0 (CaQQLa)201-0038514 
650 6 |a M�ecanique des milieux continus.  |0 (CaQQLa)201-0022033 
650 7 |a NATURE  |x Earthquakes & Volcanoes.  |2 bisacsh 
650 7 |a SCIENCE  |x Earth Sciences  |x Seismology & Volcanism.  |2 bisacsh 
650 7 |a Continuum mechanics  |2 fast  |0 (OCoLC)fst00876787 
650 7 |a Seismic waves  |2 fast  |0 (OCoLC)fst01111285 
650 7 |a Seismology  |x Mathematics  |2 fast  |0 (OCoLC)fst01111317 
776 0 8 |i Print version:  |a Slawinski, M.A. (Michael A.), 1961-  |t Seismic waves and rays in elastic media.  |b 1st ed.  |d Oxford : Pergamon, 2003  |z 0080439306  |z 9780080439303  |w (OCoLC)52621447 
830 0 |a Handbook of geophysical exploration.  |n Section I,  |p Seismic exploration ;  |v v. 34.  |x 0950-1401 
856 4 0 |u https://sciencedirect.uam.elogim.com/science/book/9780080439303  |z Texto completo 
856 4 0 |u https://sciencedirect.uam.elogim.com/science/handbooks/09501401/34  |z Texto completo