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
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10505 - Geology
Result continuities
Project
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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