Seismic velocity changes caused by an overburden stress

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Seismic velocity changes caused by an overburden stress

An increase in seismic velocity with depth is a common rock property, one that can be encountered practically everywhere. Overburden pressure increases vertical stress, producing a nonlinear elastic response. Application of a conventional nonlinear theory to this problem leads to transverse isotropy...

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Bibliographic Details
Main Authors:	Korneev, V., Glubokovskikh, Stanislav
Format:	Journal Article
Published:	2013
Online Access:	http://hdl.handle.net/20.500.11937/13665

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