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Surface waves are waves that are essentially confined to the surface of the Earth, in that their amplitudes decrease with depth in some way. This chapter covers the basic theory of such waves, as well as the theory of normal modes, which are waves confined to a surface layer, and are similar to waves in an organ pipe or the motions of a ...
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Such waves are called head waves, and the refraction method involves their interpretation. From a plot of travel time as a function of source–Geophone distance, the number, thicknesses, and velocities of rock layers present can be determined for simple situations.
Published by: University of Toronto Press. View. summary. Head waves – also called refraction arrivals, lateral waves, or conical waves – have been used extensively in near-earthquake studies, geophysical prospecting, and deep-crustal seismological investigations.
Such waves are called head waves, and the refraction method involves their interpretation. From a plot of travel time as a function of source–Geophone distance, the number, thicknesses, and velocities of rock layers present can be determined for simple situations.
17 de mar. de 2018 · Head waves are important in exploration and crustal seismology as they indicate the existence of an interface and the velocity of the generating wave. Head waves have been described in the literature for isotropic media but the extension to anisotropic media seems to be lacking.
