{"refrec":{"BRefID":324577,"RR":"<b>Vardy, M.E.; Bull, J.M.; Dix, J.K.; Henstock, T.J.; Plets, R.M.K.; Gutowski, M.; Hogarth, P.</b> (2011). The geological Hubble: a reappraisal for shallow water. <i>Lead. Edge (Tulsa Okla.) 30(2)</i>: 154-159. <a href=\"https://dx.doi.org/10.1190/1.3555325\" target=\"_blank\">https://dx.doi.org/10.1190/1.3555325</a>","BEntID":318053,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Lead. Edge (Tulsa Okla.) 30(2)</i>: 154-159. <a href=\"https://dx.doi.org/10.1190/1.3555325\" target=\"_blank\">https://dx.doi.org/10.1190/1.3555325</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Vardy, M.E.; Bull, J.M.; Dix, J.K.; Henstock, T.J.; Plets, R.M.K.; Gutowski, M.; Hogarth, P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Vardy, M.E. <i>et al.</i>","Englishabstract":"Traditional two-dimensional (2D) seismic acquisition techniques image the subsurface using a grid of orthogonal lines. Dips are recorded only in the along-track direction, limiting migration to a 2D along-track approximation of the inherently 3D wavefields. This produces profiles that are often complicated by out-of-plane reflections and with resolution (for structural interpretation) constrained by the line spacing rather than the source wavelength. 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