1887

Abstract

Shear-wave particle motion directions measured in vertical seismie profiles (VSP) are very sensitive to anisotropic properties of the medium; however, in the case of compressional waves this is not true (Crampin 1981). Analyzing polarization diagrams (holograms) to measure these directions can be inaccurate because individual 3-component geophones are subject to interference from ambient noise and ot her coherent signals. An alternative is to investigate polarization characteristics along wavefronts using multicomponent Radon transforms.

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/content/papers/10.3997/2214-4609.201410755
1991-05-28
2020-10-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410755
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