Seismic Ray Theory
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Kennett and A. Summary: The region of the Earth of interest far reflection seismology is characterised by rapid fluctuations in properties with depth superimposed on a smoother trend of general increase in seismic velocity with depth, together with significant horizontal variations. Since most hydrocarbon deposits are to be sought in traps formed by lateral contrasts it is most important that modelling techniques should give as accurate a representation of the seismic wave field as possible in a complex medium.
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In deep reflection seismology designed to look at the whole crust, the principal features of interest, such as thrusts, have often to be mapped by their expression in terms of horizontal changes in reflection character. Any successful modelling scheme must therefore be able to cope, at the very least, with major horizontal and vertical variations in seismic properties. Incorporating fine-scale structure is difficult and for the time being may have to be done via the use of one-dimensional models adjusted for appropriate ray paths or by the association of reflection sequences with interfaces.
At 30 Hz a typical P-wavelength would be m, which is larger than the scale on which both horizontal and vertical resolution is desired.
About this book
Many new concepts that extend the possibilities and increase the method's efficiency are included. The book has a tutorial character: derivations start wit The seismic ray method plays an important role in seismology, seismic exploration, and in the interpretation of seismic measurements. 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 complex problems.
Most of the derived equations are expressed in algorithmic form and may be used directly for computer programming. This book will prove to be an invaluable advanced text and reference in all academic institutions in which seismology is taught or researched.
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Seismic Wave and Ray Theory
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