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dc.contributor.authorBharadwaj, Pawan
dc.contributor.authorSchuster, Gerard T.
dc.contributor.authorMallinson, Ian
dc.contributor.authorDai, Wei
dc.date.accessioned2015-05-26T07:06:08Z
dc.date.available2015-05-26T07:06:08Z
dc.date.issued2011-11-10
dc.identifier.citationTheory of supervirtual refraction interferometry 2012, 188 (1):263 Geophysical Journal International
dc.identifier.issn0956540X
dc.identifier.doi10.1111/j.1365-246X.2011.05253.x
dc.identifier.urihttp://hdl.handle.net/10754/555748
dc.description.abstractInverting for the subsurface velocity distribution by refraction traveltime tomography is a well-accepted imaging method by both the exploration and earthquake seismology communities. A significant drawback, however, is that the recorded traces become noisier with increasing offset from the source position, and so accurate picking of traveltimes in far-offset traces is often prevented. To enhance the signal-to-noise ratio (SNR) of the far-offset traces, we present the theory of supervirtual refraction interferometry where the SNR of far-offset head-wave arrivals can be theoretically increased by a factor proportional to; here, N is the number of receiver or source positions associated with the recording and generation of the head-wave arrival. There are two steps to this methodology: correlation and summation of the data to generate traces with virtual head-wave arrivals, followed by the convolution of the data with the virtual traces to create traces with supervirtual head-wave arrivals. This method is valid for any medium that generates head-wave arrivals recorded by the geophones. Results with both synthetic traces and field data demonstrate the feasibility of this method. There are at least four significant benefits of supervirtual interferometry: (1) an enhanced SNR of far-offset traces so the first-arrival traveltimes of the noisy far-offset traces can be more reliably picked to extend the useful aperture of the data, (2) the SNR of head waves in a trace that arrive later than the first arrival can be enhanced for accurate traveltime picking and subsequent inversion by later-arrival traveltime tomography, (3) common receiver-pair gathers can be analysed to detect the presence of diving waves in the first arrivals, which can be used to assess the nature of the refracting boundary, and (4) the source statics term is eliminated in the correlation operations so that the timing of the virtual traces is independent of the source excitation time. This suggests the possibility of applying this method to earthquake data recorded by receivers that are inline with the refraction paths and source locations. © 2011 The Authors Geophysical Journal International © 2011 RAS.
dc.publisherOxford University Press (OUP)
dc.relation.urlhttp://gji.oxfordjournals.org/cgi/doi/10.1111/j.1365-246X.2011.05253.x
dc.rightsArchived with thanks to Geophysical Journal International © The Authors Geophysical Journal International © 2011 RAS
dc.subjectInterferometry
dc.subjectInterface waves
dc.titleTheory of supervirtual refraction interferometry
dc.typeArticle
dc.contributor.departmentCenter for Subsurface Imaging and Fluid Modeling
dc.contributor.departmentEarth Science and Engineering Program
dc.contributor.departmentPhysical Science and Engineering (PSE) Division
dc.identifier.journalGeophysical Journal International
dc.eprint.versionPublisher's Version/PDF
dc.contributor.institutionIndian School of Mines, Dhanbad, India
kaust.personSchuster, Gerard T.
kaust.personDai, Wei
kaust.personBharadwaj, Pawan
kaust.personMallinson, Ian
refterms.dateFOA2018-06-13T10:17:12Z
dc.date.published-online2011-11-10
dc.date.published-print2012-01


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