Identification of surface wave higher modes using a methodology based on seismic noise and coda waves
Dispersion analysis of Rayleigh waves is performed to assess the velocity of complex structures such as sedimentary basins. At short periods several modes of the Rayleigh waves are often exited. To perform a reliable inversion of the velocity structure an identification of these modes is thus requir...
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Veröffentlicht in: | Geophysical journal international 2015-11, Vol.203 (2), p.856-868 |
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