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Imaging the Mariánské Lázně Fault (Czech Republic) by 3-D ground-penetrating radar and electric resistivity tomography

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    SYSNO ASEP0381710
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleImaging the Mariánské Lázně Fault (Czech Republic) by 3-D ground-penetrating radar and electric resistivity tomography
    Author(s) Fischer, Tomáš (GFU-E) ORCID, RID
    Štěpančíková, Petra (USMH-B) RID, ORCID, SAI
    Karousová, M. (CZ)
    Tábořík, P. (CZ)
    Flechsig, C. (DE)
    Gaballah, M. (EG)
    Source TitleStudia geophysica et geodaetica. - : Geofyzikální ústav AV ČR, v. v. i. - ISSN 0039-3169
    Roč. 56, č. 4 (2012), s. 1019-1036
    Number of pages18 s.
    Publication formPrint - P
    Languageeng - English
    CountryCZ - Czech Republic
    Keywordsfault tectonics ; resistivity tomography ; ground penetrating radar
    Subject RIVDC - Siesmology, Volcanology, Earth Structure
    R&D ProjectsIAA300120905 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    CEZAV0Z30120515 - GFU-E (2005-2011)
    AV0Z30460519 - USMH-B (2005-2011)
    UT WOS000311588500008
    DOI10.1007/s11200-012-0825-z
    AnnotationGeodynamic activity in the area of West Bohemia is typified by the occurrence of earthquake swarms, Quaternary volcanism and high flux of mantle-derived CO2. The highest swarm activity occurs beneath the eastern edge of the Cheb basin, which is delineated by the NW-SE trending morphologically pronounced Mariánské Lázně Fault (MLF) controlling the formation of the basin. The previous trenching survey across the MLF zone has identified several fault strands with possible Quaternary activity. In this paper we present the results of the geophysical survey focused to trace the faults signatures in geophysical sections and to build an image of near surface tectonics. The method of electric resistivity tomography (ERT) along two profiles parallel to the trench identified a strong resistivity contrast between the bodies of sandy gravels in the middle and conductive clayey sands to the west and weathered crystalline basement to the east.
    WorkplaceGeophysical Institute
    ContactHana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
    Year of Publishing2013
Number of the records: 1  

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