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dc.contributor.authorKong, L.
dc.contributor.authorGurevich, Boris
dc.contributor.authorMüller, T.
dc.contributor.authorWang, Y.
dc.contributor.authorYang, H.
dc.contributor.editorEAGE
dc.date.accessioned2017-01-30T14:11:39Z
dc.date.available2017-01-30T14:11:39Z
dc.date.created2015-02-02T20:00:46Z
dc.date.issued2013
dc.identifier.citationKong, L. and Gurevich, B. and Müller, T. and Wang, Y. and Yang, H. 2013. Effect of fracture fill on elastic waves in fractured porous rocks, in Proceedings of the Second International Workshop on Rock Physics, Aug 4-9 2013. Southampton: EAGE.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/38066
dc.description.abstract

When a porous medium is permeated by open fractures, wave-induced flow between pores and fractures can cause attenuation and dispersion of the passing wave. Most studies of this phenomenon assume that pores and fractures are saturated with the same fluid. Here we develop a model for wave propagation in a porous medium with aligned fractures where pores and fractures are filled with different fluids. The model is based on the theory of wave propagation in a periodically layered poroelastic medium. The results are consistent with earlier studies when both pores and fractures are saturated with liquids, but also show significant dispersion and attenuation when the pores are filled with a liquid while the fractures are dry or gas-saturated.

dc.publisherEAGE
dc.relation.urihttp://earthdoc.eage.org/publication/publicationdetails/?publication=73426
dc.titleEffect of fracture fill on elastic waves in fractured porous rocks
dc.typeConference Paper
dcterms.source.titleSecond International Workshop on Rock Physics
dcterms.source.seriesSecond International Workshop on Rock Physics
dcterms.source.conferenceSecond International Workshop on Rock Physics
dcterms.source.conference-start-dateAug 4 2013
dcterms.source.conferencelocationSouthampton
dcterms.source.placeThe Netherlands
curtin.departmentDepartment of Exploration Geophysics
curtin.accessStatusFulltext not available


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