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dc.contributor.authorSong, Jin
dc.contributor.authorStovas, Alexey
dc.date.accessioned2019-06-11T08:54:34Z
dc.date.available2019-06-11T08:54:34Z
dc.date.created2018-09-24T11:44:57Z
dc.date.issued2018
dc.identifier.citationGeophysical Prospecting. 2018, 66 (6), 1123-1137.nb_NO
dc.identifier.issn0016-8025
dc.identifier.urihttp://hdl.handle.net/11250/2600421
dc.description.abstractAcoustic transversely isotropic models are widely used in seismic exploration for P‐wave processing and analysis. In isotropic acoustic media only P‐wave can propagate, while in an acoustic transversely isotropic medium both P and S waves propagate. In this paper, we focus on kinematic properties of S‐wave in acoustic transversely isotropic media. We define new parameters better suited for S‐wave kinematics analysis. We also establish the travel time and relative geometrical spreading equations and analyse their properties. To illustrate the behaviour of the S‐wave in multi‐layered acoustic transversely isotropic media, we define the Dix‐type equations that are different from the ones widely used for the P‐wave propagation.nb_NO
dc.language.isoengnb_NO
dc.publisherEuropean Association of Geoscientists and Engineers (EAGE)nb_NO
dc.titleS-wave kinematics in acoustic transversely isotropic media with a vertical symmetry axisnb_NO
dc.typeJournal articlenb_NO
dc.typePeer reviewednb_NO
dc.description.versionacceptedVersionnb_NO
dc.source.pagenumber1123-1137nb_NO
dc.source.volume66nb_NO
dc.source.journalGeophysical Prospectingnb_NO
dc.source.issue6nb_NO
dc.identifier.doi10.1111/1365-2478.12635
dc.identifier.cristin1612889
dc.description.localcodeThis is the peer reviewed version of an article, which has been published in final form at [http://dx.doi.org/10.1111/1365-2478.12635]. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Self-Archiving.nb_NO
cristin.unitcode194,64,90,0
cristin.unitnameInstitutt for geovitenskap og petroleum
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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