1887

Abstract

Spectral ratio methods are used to investigate the attenuation of p-waves in a clay rich shale as a function of confining pressure. A generalised standard linear solid (GSLS) model is then fitted to the data. The attenuation of the fast axis p-wave is found to be relatively indepenent of confining pressure and is in good agreement with the GSLS model.

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/content/papers/10.3997/2214-4609.20145374
2010-04-26
2021-10-17
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20145374
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