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Seismic waves velocities inferred from the surface waves dispersion in the Malé Karpaty Mountains, Slovakia

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    0517296 - ÚSMH 2020 RIV CZ eng J - Článek v odborném periodiku
    Lukešová, Renata - Fojtíková, Lucia - Málek, Jiří - Kolínský, P.
    Seismic waves velocities inferred from the surface waves dispersion in the Malé Karpaty Mountains, Slovakia.
    Acta geodynamica et geomaterialia. Roč. 16, č. 4 (2019), s. 451-464. ISSN 1214-9705. E-ISSN 2336-4351.
    [Czech - Polish - Slovak Symposium on Mining and Environmental Geophysics /37/ and Conference OVA´19 - New Knowledge and Measurements in Seismology, Engineering Geophysics and Geotechnical Engineering /28/. Rožnov pod Radhoštěm, 28.05.2019-31.05.2019]
    Institucionální podpora: RVO:67985891
    Klíčová slova: Surface waves * Joint inversion of Love and Rayleigh waves * 1-D velocity model * Malé Karpaty
    Obor OECD: Geology
    Impakt faktor: 1.227, rok: 2019
    Způsob publikování: Open access
    https://www.irsm.cas.cz/materialy/acta_content/2019_doi/Lukesova_AGG_2019_0038.pdf

    The study area of Western Carpathians belongs to one of the most seismically active regions in Slovakia, where the available velocity models are not precise enough for accurate location and
    determination of focal mechanism. To improve the uppermost part of the currently used models, seismic surface wave data from two blasts in the quarry Rohožník, recorded at the MKnet local
    seismic network, were analyzed. Group velocity dispersion curves of Rayleigh and Love waves were determined by the frequency-time analysis. A mean group velocity dispersion curve for
    Love and Rayleigh waves for the central part of the MKnet network was settled and consequently joint inversion, for the period range 0.9 – 2.7 s, was performed to obtain a 1-D
    velocity model using the isometric method. The 11-layered model extends to depth of 2.5 km and indicate increase of the velocities from the surface down to the depths of 0.9 km. Then,
    velocities slightly decrease. The minimum of the low-velocity zone is at the depth of 1.8 km s.after which the velocities moderately increase to the velocity of the halfspace with vP = 5.35 km/s
    and vS = 2.96 km/s.
    Trvalý link: http://hdl.handle.net/11104/0302612

     
     
Počet záznamů: 1