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)
Identifikátory výsledku
Kód výsledku v 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>
Výsledek na webu
<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>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
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)
Popis výsledku v původním jazyce
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.
Název v anglickém jazyce
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)
Popis výsledku anglicky
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.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10505 - Geology
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2025
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Geofizičeskij žurnal
ISSN
0203-3100
e-ISSN
2524-1052
Svazek periodika
47
Číslo periodika v rámci svazku
2
Stát vydavatele periodika
UA - Ukrajina
Počet stran výsledku
6
Strana od-do
110-115
Kód UT WoS článku
001469781800015
EID výsledku v databázi Scopus
2-s2.0-105002991742