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Seismic moment tensor and focal mechanism for earthquake of February 22, 2024 in eastern Slovakia (12:54:15 UTC, 21.75E°E, 49.03°N, depth 9 km, ML3.0)

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F25%3A00619350" target="_blank" >RIV/67985891:_____/25:00619350 - isvavai.cz</a>

  • Result on the web

    <a href="https://doi.org/10.24028/gj.v47i2.322470" target="_blank" >https://doi.org/10.24028/gj.v47i2.322470</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.24028/gj.v47i2.322470" target="_blank" >10.24028/gj.v47i2.322470</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Seismic moment tensor and focal mechanism for earthquake of February 22, 2024 in eastern Slovakia (12:54:15 UTC, 21.75E°E, 49.03°N, depth 9 km, ML3.0)

  • Original language description

    The accuracy of the focal mechanism solution can depend very significantly on the number of stations used, especially in the case of weak earthquakes and sparse networks. We describe the procedure for retrieving the seismic moment tensor for the earthquake of February 22, 2024, which happened in Eastern Slovakia, using a limited number of seismic stations. We use records from only two stations of the Slovakian network: sk19 (49.25 degrees N, 21.93 degrees E) and sk20 (49.21 degrees N, 21.61 degrees E). The moment tensor inversion of high-frequency seismogram data in this study is based on a point source approach using the matrix method for the direct waves. The process involves generating records in displacements using the frequency and wave-number integration technique for an elastic horizontally layered medium. Amethod is presented for moment tensor inversion of only direct P-and S-waves, which is less sensitive to path effects modelling than reflected and converted waves, significantly improving the method's accuracy and reliability. The location and origin time of the event are considered known. Based on forward modelling, a numerical technique is developed for the inversion of observed waveforms for the of moment tensor M(t) components obtained by generalized inversion.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10505 - Geology

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2025

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Geofizičeskij žurnal

  • ISSN

    0203-3100

  • e-ISSN

    2524-1052

  • Volume of the periodical

    47

  • Issue of the periodical within the volume

    2

  • Country of publishing house

    UA - UKRAINE

  • Number of pages

    6

  • Pages from-to

    110-115

  • UT code for WoS article

    001469781800015

  • EID of the result in the Scopus database

    2-s2.0-105002991742