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IN SITU MEASUREMENTS OF SHEAR‐WAVE VELOCITY IN SEDIMENTS WITH HIGHER‐MODE RAYLEIGH WAVES *
Author(s) -
GABRIELS P.,
SNIEDER R.,
NOLET G.
Publication year - 1987
Publication title -
geophysical prospecting
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.735
H-Index - 79
eISSN - 1365-2478
pISSN - 0016-8025
DOI - 10.1111/j.1365-2478.1987.tb00812.x
Subject(s) - rayleigh wave , geology , shear (geology) , love wave , phase velocity , amplitude , dispersion (optics) , shear velocity , shear waves , rayleigh scattering , seismology , surface wave , wave propagation , geophysics , longitudinal wave , mechanics , mechanical wave , optics , turbulence , physics , petrology
A seismic survey was carried out on a tidal flat in the SW‐Netherlands in order to determine shear‐wave velocities in sediments by means of higher‐mode Rayleigh waves. The dispersion properties of these Rayleigh waves were measured in the 2‐D amplitude spectrum–or f, k ‐spectrum–and resulted in phase velocities for six different modes as a function of frequency (5–30 Hz). These observed phase velocities were inverted for a nine‐layer model for the shear‐wave velocity to a depth of 50 m.

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