1887

Abstract

The inversion of Rayleigh wave dispersion curves can yield the shear wave velocity profile which<br>gives the image of subsurface. In most of the existing techniques of computing Rayleigh wave dispersion<br>curves, it is assumed that the subsurface consists of horizontally flat layers.

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/content/papers/10.3997/2214-4609-pdb.157.sageep001
2009-03-29
2022-05-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.157.sageep001
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