Article ID Journal Published Year Pages File Type
4741226 Journal of Applied Geophysics 2006 9 Pages PDF
Abstract

Multichannel analysis of surface waves is a developing method widely used in shallow subsurface investigations. The field procedures and related parameters are very important for successful applications. Among these parameters, the source–receiver offset range is seldom discussed in theory and normally determined by empirical or semi-quantitative methods in current practice. This paper discusses the problem from a theoretical perspective. A formula for quantitatively evaluating a layered homogenous elastic model was developed. The analytical results based on simple models and experimental data demonstrate that the formula is correct for surface wave surveys for near-surface applications.

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Physical Sciences and Engineering Earth and Planetary Sciences Geophysics
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