| Citation: | Jianghai Xia, Richard D Miller, Yixian Xu, Yinhe Luo, Chao Chen, Jiangping Liu, Julian Ivanov, Chong Zeng. High-Frequency Rayleigh-Wave Method. Journal of Earth Science, 2009, 20(3): 563-579. doi: 10.1007/s12583-009-0047-7
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High-frequency (≥2 Hz) Rayleigh-wave data acquired with a multichannel recording system have been utilized to determine shear (S)-wave velocities in near-surface geophysics since the early 1980s. This overview article discusses the main research results of high-frequency surface-wave techniques achieved by research groups at the Kansas Geological Survey and China University of Geosciences in the last 15 years. The multichannel analysis of surface wave (MASW) method is a non-invasive acoustic approach to estimate near-surface S-wave velocity. The differences between MASW results and direct borehole measurements are approximately 15% or less and random. Studies show that simultaneous inversion with higher modes and the fundamental mode can increase model resolution and an investigation depth. The other important seismic property, quality factor (
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