PSPI: streamlining 3D echo-reconstructive imaging

dc.contributor.authorBonomi, Ernesto
dc.contributor.authorBrieger, Leesa
dc.contributor.authorPieroni, Enrico
dc.contributor.authorArienti, Maria Teresa
dc.contributor.authorCazzola, Luca
dc.contributor.authorMarchetti, Paolo
dc.date.accessioned2014-06-17T08:59:45Z
dc.date.available2014-06-17T08:59:45Z
dc.date.issued1999
dc.description.abstractEcho­reconstruction techniques for subsurface imaging, widely used in oil exploration, are based on experiments in which short acoustic impulses, emitted at the surface, illuminate a certain volume and are backscattered by inhomogeneities of the medium. The inhomogeneities act as reflecting surfaces which cause signal echoing; the echoes are then recorded at the surface and processed through a propagation model (which acts as a “computational lens”) to yield an image of those very inhomogeneities. Migration, based on the scalar wave equation, is the standard imaging technique for seismic applications [1]. In the migration process, the recorded pressure waves(called the seismic traces or the seismic section) are used as initial conditions for a wave field governed by the scalar wave equation in an inhomogeneous medium.IT
dc.identifier.urihttp://hdl.handle.net/11050/1035
dc.language.isoenIT
dc.subjectinhomogeneous mediumIT
dc.subjectwave equationIT
dc.subjectseismic applicationsIT
dc.subject3D visualizationIT
dc.subject.een-cordisEEN CORDIS::ELETTRONICA, INFORMATICA E TELECOMUNICAZIONI::Multimedia::Visualizzazione, realtà virtualeIT
dc.subject.een-cordisEEN CORDIS::FISICA E SCIENZE ESATTE::Scienze della terra ::Tettonica, sismologiaIT
dc.titlePSPI: streamlining 3D echo-reconstructive imagingIT
dc.typeReportIT
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