Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1525
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dc.contributor.authorallPapazachos, C. B.; Institute of Engineering Seismology and Earthquake Engineering (ITSAK), Foinikas, Thessaloniki, Greeceen
dc.contributor.authorallNolet, G.; Department of Geological and Geophysical Sciences, Princeton University, Princeton, USAen
dc.date.accessioned2006-09-11T07:48:20Zen
dc.date.available2006-09-11T07:48:20Zen
dc.date.issued1997-01en
dc.identifier.urihttp://hdl.handle.net/2122/1525en
dc.description.abstractThe use of 1D or pseudo- 3D ray tracing techniques in linearized tomographic problems leads to solutions for which it is difficult to assess the true resolution and error distribution. For this reason, we employ a revised 3D bending algorithm (Moser et al., 1992) and show that it can be used efficiently for a non-linear inversion in a stepwise scheme. Initial paths are determined from graph theory in order to avoid local minima in bending. The importance of 3D ray tracing in inversion studies and the limitations of the standard 1D approach are demonstrated through synthetic examples. The speed of the ray tracing and the simple scaling scheme allow for an implementation in large-scale tomographic problems.en
dc.format.extent3743308 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.relation.ispartofseries1/40 (1997)en
dc.subjectnon-linear inversionen
dc.subjectarrival timesen
dc.subjectgraph theoryen
dc.subjectbendingen
dc.subject3D ray tracingen
dc.titleNon-linear arrival time tomographyen
dc.typearticleen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.07. Tomography and anisotropyen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorPapazachos, C. B.en
dc.contributor.authorNolet, G.en
dc.contributor.departmentInstitute of Engineering Seismology and Earthquake Engineering (ITSAK), Foinikas, Thessaloniki, Greeceen
dc.contributor.departmentDepartment of Geological and Geophysical Sciences, Princeton University, Princeton, USAen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptITSAK/AUTH-Geolab, Thessaloniki, Greece-
crisitem.author.deptDepartment of Geological and Geophysical Sciences, Princeton University, Princeton, USA-
crisitem.classification.parent04. Solid Earth-
Appears in Collections:Annals of Geophysics
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