EFFICIENCY OF THE SEISMOLOGICAL OBSERVATION SYSTEM AT THE UDINA VOLCANIC COMPLEX IN 2019
1 Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences, Russia, 123242, Moscow, ul. Bolshaya Gruzinskaya, 10, building 1
2 Kamchatka Branch of the Federal Research Center “Geophysical Survey of Russian Academy of Sciences”, Russia, 683006, Petropavlovsk-Kamchatskii, bulv. Piipa 9
Journal: Seismic instruments
Tome: 57
Number: 4
Year: 2021
Pages: 21-32
UDK: 550.34.034
DOI: 10.21455/si2021.4-2
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BURMIN VALERY YURIEVICH., SALTYKOV VADIM ALEKSANDROVICH., KONOVALOVA ANNA ALEKSANDROVNA. EFFICIENCY OF THE SEISMOLOGICAL OBSERVATION SYSTEM AT THE UDINA VOLCANIC COMPLEX IN 2019 // . 2021. Т. 57. № 4. С. 21-32. DOI: 10.21455/si2021.4-2
@article{EFFICIENCY2021,
author = ", BURMINVALERYYURIEVICH. and , SALTYKOVVADIMALEKSANDROVICH. and , KONOVALOVAANNAALEKSANDROVNA.",
title = "EFFICIENCY OF THE SEISMOLOGICAL OBSERVATION SYSTEM AT THE UDINA VOLCANIC COMPLEX IN 2019",
journal = "Seismic instruments",
year = 2021,
volume = "57",
number = "4",
pages = "21-32",
doi = "10.21455/si2021.4-2",
language = "English"
}
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Keywords: SEISMIC STATIONS, EFFICIENCY OF OBSERVATION SYSTEMS, ENERGY CLASS OF AN EARTHQUAKE, MAGNITUDE OF AN EARTHQUAKE, HYPOCENTER
Аnnotation: An assessment of the efficiency of the network of seismic stations on the territory of the Udina volcanic complex (UVC), which consisted of 29 instruments, located irregularly in the territory, was carried out. At different points of the UVC, earthquakes of different minimum energy class and with different accuracy are recorded. The calculation of the minimum energy classes for the seismological network of the UVC of 29 seismic stations shows that with an increase of the stations about 30 thousand, such a network throughout the territory under consideration reliably registers earthquakes equal 7.0 minimum energy classes, which corresponds to a magnitudes of ~2.5. The values of errors in determining the coordinates of earthquake epicenters in latitude (δφ) and longitude (δλ), within the network, do not exceed 0.4 km. The values of errors in determining the depths of earthquake foci ( H ) in the center of such a network does not exceed 0.2 km, and within the entire UVC territory does not exceed 5.0 km. For these calculations, the errors in determining the travel time and propagation velocities of seismic waves were set equal to 0.1 s and 0.1 km/s, respectively, and could be both random and systematic.