Last edited by Kigazuru
Thursday, July 9, 2020 | History

9 edition of Seismic Ray Theory found in the catalog.

Seismic Ray Theory

by V. Cerveny

  • 10 Want to read
  • 17 Currently reading

Published by Cambridge University Press .
Written in English

    Subjects:
  • Vulcanology & seismology,
  • Science/Mathematics,
  • Seismology,
  • Science,
  • Seismic waves,
  • Earth Sciences - Geology,
  • General,
  • Geophysics,
  • Science / Geology,
  • Seismic waves--Mathematical models,
  • Applied,
  • Mathematical Models

  • The Physical Object
    FormatHardcover
    Number of Pages722
    ID Numbers
    Open LibraryOL7738305M
    ISBN 100521366712
    ISBN 109780521366717

    Seismic tomography is a group of seismic inversion methods based on data prediction via solution of a wave equation. This chapter discusses seismic tomography based on ray theory, which essentially is a high frequency approximation to the wave equation. Free 2-day shipping. Buy Seismic Ray Theory (Hardcover) at

      Seismic inversion aims to reconstruct a quantitative model of the Earth subsurface, by solving an inverse problem based on seismic measurements. There are at least three fundamental issues to be solved simultaneously: non-linearity, non-uniqueness, and instability. This book covers the basic theory and techniques used in seismic inversion, corresponding to Author: Yanghua Wang.   The book is therefore tutorial in the sense that a student could learn about seismic ray theory by reading it, but it is also something of a technical manual for the seismologist to consult to find the best way to do this or that and the algorithms to do the : J Hudson.

    Description: Seismic Ray Theory presents a comprehensive treatment of the seismic ray method. This method plays an important role in seismology, seismic exploration, and in the interpretation of seismic measurements. Many concepts which extend the possibilities and increase the efficiency of the seismic ray method are included.   Chapter 10 Seismic ray-impedance inversion Acoustic and elastic impedances Ray impedance Workflow of ray-impedance inversion Ray-impedance inversion with a model constraint Chapter 11 Seismic tomography based on ray theory Seismic tomography Velocity-depth ambiguity in tomography Author: Yanghua Wang.


Share this book
You might also like
Freud, appraisals and reappraisals

Freud, appraisals and reappraisals

The lyar

The lyar

Taste of Columbus V

Taste of Columbus V

navy list for the year 1814.

navy list for the year 1814.

compendious and complete Hebrew and Chaldee lexicon to the Old Testament

compendious and complete Hebrew and Chaldee lexicon to the Old Testament

The Post Office

The Post Office

An elegy [...] the memory of Mason and Alpheus, sons of Mr. Elisha Hale, of Douglas

An elegy [...] the memory of Mason and Alpheus, sons of Mr. Elisha Hale, of Douglas

Industrial Statistics Yearbook, 1986

Industrial Statistics Yearbook, 1986

Private Practice in Communication Disorders

Private Practice in Communication Disorders

Evidence on income redistribution by governments

Evidence on income redistribution by governments

The alphabet

The alphabet

Spiritual Manna - Daily Devotions Through the Year

Spiritual Manna - Daily Devotions Through the Year

Seismic Ray Theory by V. Cerveny Download PDF EPUB FB2

Seismic Ray Theory presents the most comprehensive treatment of the method available. Many new concepts that extend the possibilities and increase the method's efficiency are included. The book has a tutorial character: derivations start with a relatively simple problem, in which the main ideas are easier to explain, and then advance to more Cited by: Seismic Ray Theory presents an entire treatment of the seismic ray method.

This system performs an important place in seismology, seismic exploration, and inside the interpretation of seismic measurements. Many concepts which delay the probabilities and enhance the effectivity of the seismic ray method are included.

Seismic Ray Theory presents the most comprehensive treatment of the seismic ray method available. This method plays an important role in seismology, seismic exploration, and in the interpretation of seismic measurements. Many new concepts which extend the possibilities and increase the efficiency of the method are included.5/5(4).

Seismic Ray Theory will prove to be an invaluable advanced textbook and reference volume in all academic institutions in which seismology is taught or researched.

It will also be an invaluable resource in the research and explo-ration departments of the Cited by: Seismic Ray Theory presents the most comprehensive treatment of the method available. Many new concepts that extend the possibilities and increase the method's efficiency are included.

The book has a tutorial character: derivations start with a relatively simple problem, in which the main ideas are easier to explain, and then advance to more.

Seismic Ray Theory presents the most comprehensive treatment of the seismic ray method available. This method plays an important role in seismology, seismic exploration, and in the interpretation of seismic measurements.

Many new concepts which extend the possibilities and increase the efficiency of the method are included.

This book will prove to be an invaluable. Seismic Ray Theory presents a comprehensive treatment of the seismic ray method available. It will prove to be an invaluable advanced textbook and reference volume in all academic institutions in which seismology is taught or researched, and an invaluable resource in the petroleum industry and geological surveys.

The ray theory belongs to the methods most frequently used in seismology and seismic exploration for forward and inverse modeling of high-frequency seismic body waves. In smoothly varying media with smooth interfaces, it can provide useful approximate solutions of the elastodynamic equation of satisfactory accuracy.

Seismic Ray Theory presents a comprehensive treatment of the seismic ray method. This method plays an important role in seismology, seismic exploration, and in the interpretation of seismic measurements. Many concepts which extend the possibilities and increase the efficiency of the seismic ray method are included.

The seismic ray method plays an important role in seismology, seismic exploration, and in the interpretation of seismic measurements. Seismic Ray Theory presents the.

Seismic ray tracing aims to find a ray trajectory satisfying Fermat's principle of stationary travel time on the basis of ray theory (e.g., Lee and Stewart, ; Cerveny, ).

To describe the. Seismology and the Earth’s Deep Interior Body Waves and Ray Theory Body Waves and Ray TheoryBody Waves and Ray Theory • Ray theory: basic principles Wavefronts, Huygens principle, Fermat’s principle, Snell’s Law Seismic phases in the Earth, nomenclature, travel-time curves for teleseismic phases.

The full text of the book is also available —here—, via the Seismic Waves in Complex 3-D Structures (SW3D) consortium. Reader notes on this item Reflection/Transmission Coefficients (p) There are: displacement R/T coefficients, potential R/T. Seismic Ray Theory presents a comprehensive treatment of the seismic ray method.

This method plays an important role in seismology, seismic exploration, and in the interpretation of seismic measurements. Many concepts which extend the possibilities and increase the efficiency of the seismic ray method are included.

Seismic Ray Theory presents a comprehensive treatment of the seismic ray method. This method plays an important role in seismology, seismic exploration, and in the interpretation of seismic measurements. Many concepts which extend the possibilities and increase the efficiency of the seismic ray method are included.

The book has a tutorial. Building on the basic theory of linear inverse problems, the methodologies of seismic inversion are explained in detail, including ray-impedance inversion and waveform tomography etc.

The application methodologies are categorised into convolutional and wave-equation based groups. Following the brief introductory chapter, the book is organized into five topics, with a single chapter devoted to each topic.

These topics are 1) the equations of elastodynamics, 2) seismic rays and traveltimes, 3) dynamic ray tracing and paraxial ray methods, 4) ray amplitudes, and 5) ray-based synthetic by: Seismic ray theory This chapter provides a background on seismic ray theory.

The emphasis is placed on explanation and interpretation of the basic ingredients, rather than on the derivation of equations, which are well covered in existing literature. The most complete account of seismic ray theory available is the monograph by Cerveny´ˇ ().

Ray theory Introduction However, if the scale length of variations in λ and µ are large compared to the seismic wavelength, then P and S can be treated separately and the elastic wave equation is simplified.

Even so, solving the elastic wave equation requires exhaustive computational effort. Ray theory is an alternative approach in which a File Size: KB. Seismic Ray Theory presents a comprehensive treatment of the seismic ray method available. It will prove to be an invaluable advanced textbook and reference volume in all academic institutions in which seismology is taught or researched, and an invaluable resource in the petroleum industry and geological s: 4.

The simplest, yet very powerful, example of these HF methods is the seismic ray method (Babich, ; Karal and Keller, ). The great significance of the seismic ray method is its universality, effectiveness, conceptual clarity, and its ability to investigate various seismic body waves independently of other waves.We define tomography as an imaging technique which generates a cross-sectional picture (a tomogram) of an object by utilizing the object's response to the nondestructive, probing energy of an external source.

Seismic tomography makes use of sources that generate seismic waves which probe a geological target of interest. Figure 1(a) is an example configuration for. Summary. Seismic ray theory is developed ab initio (apart from one or two standard elementary results) with special emphasis on the variables ζ and a, where ζ = d log υ/d log r and α = 2/(1 — ζ).

Travel-time-distance relations are examined for a variety of types of velocity distribution, including the case α constant and cases where α and υ change Cited by: