1887

Abstract

Kjartansson constant Q attenuation model was used to show that intrinsic dispersion of seismic velocities in absorbing media is one of the main reasons leading to discrepancies of the rock elastic constants measured by dynamic and static methods. Young's,

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/content/papers/10.3997/2214-4609.201400045
2009-06-08
2024-04-20
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400045
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