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Velocity model of the Hronov-Poříčí Fault Zone from Rayleigh wave dispersion

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    SYSNO ASEP0434502
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleVelocity model of the Hronov-Poříčí Fault Zone from Rayleigh wave dispersion
    Author(s) Kolínský, Petr (USMH-B)
    Valenta, Jan (USMH-B) RID, ORCID
    Málek, Jiří (USMH-B) RID, ORCID, SAI
    Source TitleJournal of Seismology. - : Springer - ISSN 1383-4649
    Roč. 18, č. 3 (2014), s. 617-635
    Number of pages19 s.
    Publication formPrint - P
    Languageeng - English
    CountryNL - Netherlands
    KeywordsBohemian Massif ; surface waves ; phase-velocity ; dispersion curve
    Subject RIVDB - Geology ; Mineralogy
    R&D ProjectsGA205/09/1244 GA ČR - Czech Science Foundation (CSF)
    LM2010008 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    Institutional supportUSMH-B - RVO:67985891
    UT WOS000337087600019
    EID SCOPUS84902013602
    DOI10.1007/s10950-014-9433-4
    AnnotationThe Hronov-Poříčí Fault Zone (HPFZ) is an active tectonic area with regularly occurring shallow earthquakes up to magnitude 5. For their exact locations, at least an average velocity model of the area is needed. A method of measuring local phase velocities of surface waves using the array of stations deployed permanently in the HPFZ is introduced. Seven regional and teleseismic events are selected to represent different backazimuths of propagation. Applicable range of periods is estimated for each event. The coherency of the waves reaching the array is constraining the short period range. The dimension of the array is a limiting factor for the long-periods. A dispersion curve of Rayleigh wave phase velocity measured at the vertical component and characterizing 1D properties of the target area is determined using the seven measurements for the interval from 1 to 40 s. An isometric method is used to invert the determined dispersion curve for shear and longitudinal velocity distribution from the surface to the depth of 65 km.
    WorkplaceInstitute of Rock Structure and Mechanics
    ContactIva Švihálková, svihalkova@irsm.cas.cz, Tel.: 266 009 216
    Year of Publishing2015
Number of the records: 1  

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