Number of the records: 1  

Upper crustal structure of the northern part of the Bohemian ­Massif in ­rel­ation­ t­o geological, potential field data and new deep seismic data (Eger/Ohře Rift, Central Europe)

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    SYSNO ASEP0372604
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JOstatní články
    TitleUpper crustal structure of the northern part of the Bohemian ­Massif in ­rel­ation­ t­o geological, potential field data and new deep seismic data (Eger/Ohře Rift, Central Europe)
    Author(s) Skácelová, Z. (CZ)
    Mlčoch, B. (CZ)
    Novotný, Miroslav (GFU-E) RID
    Mrlina, Jan (GFU-E) ORCID, RID
    Source TitleZeitschrift für geologische Wissenschaften - ISSN 0303-4534
    Roč. 39, č. 1 (2011), s. 1-18
    Number of pages18 s.
    Languageeng - English
    CountryDE - Germany
    Keywordsupper crustal structure ; Bohemian Massif ; Eger/Ohře Rift ; Saxothuringian Zone ; Teplá-Barrandian Unit ; Moldanubian Zone
    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)
    AnnotationThe latest international seismic refraction experiment in the Central Europe SUDETES 2003 covered also the territory of the northern part of the Bohemian Massif. The profile S01 follows the SW-NE axis of the Eger/Ohře Rift in Northwestern Bohemia. The dictinct first arrivals of Pg waves were used to derive a 2-D tomographic velocity model with an optimum lateral resolution. The innovative DRTG method was applied in iterative mode to minimize linearized errors of tomographic inversion. The iteration process yielded a fine-grid velocity model with a required level of RMS travel-time fit and the model rouhgness. The time residuals were assessed at single grid depth levels and used to derive the statistical lateral resolution of "lens-shaped" velocity anomalies: for the 95% confidence level and 5% anomalies, one can resolve their lateral sizes from 15 to 40 km at the depths from 0 to 20 km.
    WorkplaceGeophysical Institute
    ContactHana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
    Year of Publishing2012
Number of the records: 1  

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