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The lateral variation in phase velocities estimated by surface wave analysis mainly reflects lithological differences (most sensitive to differences in S-wave velocities) (e.g., Fig. 3a c and MBMTL; Fig. 7d).
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Surface wave analysis generally neglects amplitude information, instead using phase information to delineate near-surface S-wave velocity structures.
The S-wave velocity structure derived from surface wave analysis is frequently used to characterize shallow lithology.
Although amplitude information is usually neglected in surface wave analysis, the amplitude of surface waves contains important information for characterizing lithology.
The first to turn up is the P-wave, followed by the S-wave and finally by surface waves.
NVT triggered by surface waves below western Shikoku is considered.
With the patient sitting and resting his/her arm on a rigid surface, pulse wave analysis will be performed with a sensor in the radial artery, using mathematical transformation to estimate the aortic pulse wave and CAIx.
With the patient sitting and resting his/her arm on a rigid surface, pulse wave analysis will be performed with a sensor in the radial artery, using mathematical transformation to estimate the aortic pulse wave.
The polarisation curves were analysed by logarithmic wave analysis.
Central hemodynamics were assessed by pulse wave analysis.
The capabilities of two promising methods, spectral analysis of surface waves and spectral analysis of lamb waves, are discussed in combination with bottlenecks that need to be passed.
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