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Abstract

The dominating waveforms in a borehole seismogram are the dispersive guided boundary waves: the Stoneley wave (tube wave) and the Pseudo-Rayleigh wave modes. An analysis of measured field data with respect to these dispersive waves requires an appropriate dispersion analysis method.

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/content/papers/10.3997/2214-4609.201409524
1995-05-29
2024-03-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409524
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