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Depth-recursive tomography along the Eger Rift using the S01 profile refraction data: tested at the KTB super drilling hole, structural interpretation supported by magnetic, gravity and petrophysical data

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    SYSNO ASEP0330159
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleDepth-recursive tomography along the Eger Rift using the S01 profile refraction data: tested at the KTB super drilling hole, structural interpretation supported by magnetic, gravity and petrophysical data
    Author(s) Novotný, Miroslav (GFU-E) RID
    Skácelová, Z. (CZ)
    Mrlina, Jan (GFU-E) ORCID, RID
    Mlčoch, B. (CZ)
    Růžek, Bohuslav (GFU-E) ORCID, RID
    Source TitleSurveys in Geophysics. - : Springer - ISSN 0169-3298
    Roč. 30, č. 6 (2009), s. 561-600
    Number of pages40 s.
    Languageeng - English
    CountryNL - Netherlands
    Keywordsdepth-recursive refraction tomography ; lateral resolution ; German Continental Deep Drilling Project (KTB) ; Zone Erbendorf-Vohenstrauss (ZEV) ; low-velocity zones
    Subject RIVDC - Siesmology, Volcanology, Earth Structure
    R&D ProjectsIAA300460602 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    SB/630/3/02 GA MŽP - Ministry of Environment (MŽP)
    CEZAV0Z30120515 - GFU-E (2005-2011)
    UT WOS000271119200002
    DOI10.1007/s10712-009-9068-0
    AnnotationThe refraction data from the SUDETES 2003 experiment were used for highresolution tomography along the profile S01. The S01 profile crosses the zone Erbendorf- Vohenstrauss (ZEV) near the KTB site, then follows the SW–NE oriented Eger Rift in the middle part and continues toward the NE across the Elbe zone and the Sudetic structures as far as the Trans-European Suture Zone. To get the best resolution in the velocity image only the first arrivals of Pg waves with minimum picking errors were used.
    WorkplaceGeophysical Institute
    ContactHana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
    Year of Publishing2010
Number of the records: 1  

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