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dc.contributor.authorTsiklauri, Den_US
dc.date.accessioned2016-04-12T12:22:27Z
dc.date.submitted2016-03-23T12:19:42.532Z
dc.identifier.urihttp://qmro.qmul.ac.uk/xmlui/handle/123456789/11779
dc.descriptionRevtex4, 7 postscript figs, submitted to J. Acoust. Soc. Amen_US
dc.descriptionRevtex4, 7 postscript figs, submitted to J. Acoust. Soc. Am
dc.descriptionRevtex4, 7 postscript figs, submitted to J. Acoust. Soc. Amen_US
dc.descriptionRevtex4, 7 postscript figs, submitted to J. Acoust. Soc. Amen_US
dc.description.abstractThis paper has been withdrawn by the author due to the physically inconsistent assumption of constant slip velocity, instead, see a new improved model - physics/0201045.en_US
dc.subjectphysics.geo-phen_US
dc.subjectphysics.geo-phen_US
dc.subjectphysics.flu-dynen_US
dc.subjectphysics.med-phen_US
dc.titleBiot's theory of propagation of elastic waves in a fluid-saturated porous solid revisited: introduction of non-zero boundary slip velocityen_US
dc.typeArticle
pubs.author-urlhttp://arxiv.org/abs/physics/0109007v2en_US
pubs.declined2016-03-23T12:19:21.51+0000
pubs.notesNot knownen_US


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