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Abstract

This paper compares the velocity of shear and compressional elastic wave of some various rock samples (Granite, Calcareous Phyllite and Shale) in laboratory. Then for these rock samples the measured velocity values were compared with the calculated values based on Hudson (1981) theory.

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/content/papers/10.3997/2214-4609.201408363
1998-06-08
2024-03-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408363
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