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dc.contributor.authorTassis, Georgios
dc.contributor.authorRønning, Jan Steinar
dc.contributor.authorRohdewald, Siegfried
dc.date.accessioned2020-07-15T07:17:13Z
dc.date.available2020-07-15T07:17:13Z
dc.date.issued2018
dc.identifier.issn0800-3416
dc.identifier.urihttps://hdl.handle.net/11250/2664209
dc.description.abstractThis report continues our work on refraction seismic modeling in Rayfract\u00AE and explores new possibilities offered by the software to create reliable starting models for Wave Eikonal Traveltime (WET) inversion. For this purpose, we used two complex models based on traditional interpretations from Knappe tunnel survey i.e. P1-1 (120 m) and P1-6\/7 (240 m). The first model contains three vertical fracture zones below a thin overburden and the second involves a pair of fracture zones overlain by a thick overburden basin.
dc.language.isoeng
dc.relation.ispartofseriesNGU-Rapport (2018.015)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSPREKKESONE
dc.subjectGEOFYSIKK
dc.subjectREFRAKSJONSSEISMIKK
dc.subjectMODELLERING
dc.titleTomographic inversion of synthetic refraction seismic data using various starting models in Rayfract® software
dc.typeReport
dc.description.localcode66233
dc.source.pagenumber45
dc.relation.project(329500) ForForUT, Forbedrede Forundersøkelser UTbygning


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