Possible mode conversion between Love and Rayleigh waves at a continental margin

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Global anisotropic phase velocity maps for higher mode Love and Rayleigh waves

S U M M A R Y It is well established that the Earth’s uppermost mantle is anisotropic, but there are no clear observations of anisotropy in the deeper parts of the mantle. Surface waves are well suited to observe anisotropy since they carry information about both radial and azimuthal anisotropy. Fundamental mode surface waves, for commonly used periods up to 200 s, are sensitive to structure in...

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Comparative analysis on sensitivities of Love and Rayleigh waves

Love waves are generally less employed than Rayleigh waves in near-surface shear-wave (S-wave) investigations because acquiring S-wave data is not as easy as acquiring P-wave data. The dispersion of Love waves, however, is independent of Poisson’s ratio. This character can be the valuable basis to improve the S-wave velocity imaging. The sensitivity of earth properties to the dispersion curve o...

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Supershear Rayleigh waves at a soft interface.

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Reply to comment by S. Crampin on ‘Global anisotropic phase velocity maps for higher mode Love and Rayleigh waves’

S U M M A R Y We thank Stuart Crampin for his interest in our recent paper but respectfully disagree when he argues that our measurements are not appropriate for inferring mantle anisotropy. The approximations we made are common and perfectly acceptable for the considered frequency band. The comment ignores a large part of the literature which investigated this. We will discuss the validity of ...

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ژورنال

عنوان ژورنال: Geophysical Journal International

سال: 1978

ISSN: 0956-540X,1365-246X

DOI: 10.1111/j.1365-246x.1978.tb06759.x