Neuromeerage assessment of magnitudes and parameters of localization earthquake sources by initial characters recording a seismic signal
Journal Title: Геофизический журнал - Year 2019, Vol 41, Issue 1
Abstract
The article is devoted to an extremely important topic of searching for a short-term warning of the entry of destructive vibrations in the territory of Ukraine by assessing in real-time conditions the characteristics of the seismic process — magnitude and localization parameters of the earthquake source, using the mathematical apparatus of neural network modeling. To solve the problem of estimating the parameters characterizing the zone of the excitation source and the geometry of the source-station system, the authors use the initial, least distorted P-sections of seismic signals, examining the postulate that by recording a seismic signal lasting several seconds after its entry, it is possible in real time it is sufficient to accurately predict the bypass of the expected signal (and, therefore, to estimate the magnitude) of the occurring earthquake. The simulation algorithm on networks of artificial neurons uses to determine the time, extremely dangerous from the point of view of seismic risk, the recording of earthquakes in the restricted zone of the sources of the Vrancea zone using the example of one seismic station “Odessa”. Magnitude prediction estimates are demonstrated on various components of earthquake records for time windows of various lengths. The authors also summarize the considered approach, extending it to the network of “Odessa”, “Skvira”, “Poltava” stations and those recorded on them, possibly dangerous later, seismic events at an epicentral distance of up to 12°. Estimates of the prediction of magnitude, depth of the source and the coordinates of the epicenter are demonstrated on the various components of earthquake records for time windows of various lengths. The proposed algorithms can be applied both in the automatic processing of seismic information and the seismic hazard prediction, which provides for direct operational intervention of seismological services in the seismic hazard assessment.
Authors and Affiliations
M. A. Lazarenko, O. A. Gerasimenko, N. M. Ostapchuk, N. L. Shipko
Zones of decompaction of the Earth crust of the central part of the Ukrainian Shield (according to materials of petrophysical and seismogravitational modeling)
P-wave velocity and density of rocks depend considerably on temperature and pressure who¬se influence must be taken into consideration in calculating these parameters at different depths. For the first time, this paper p...
Isostasy and seismisity
A model of the Earth crust structure formed by gravitation of the planet has been considered. An important role in this structure is given to isostasy processes. Analysis of results of seismic exploration by reflected wa...
On substantiation of mechanism of lateral extrusion of the crust of the Mountain Crimea
Numerical modeling of the crust deformations in the section of the Southwest Crimea subjected to rear indentor compression from the side of the East-Black Sea depression has been fulfilled taking into account regularitie...
Possibility of the use of data of infrasonic monitoring for identification of the nature of seismic events
The paper considers the possibility of the use of infrasound measurements conducted in Ukraine to verify the recorded seismic events and the use of infrasound data as one of the criteria for their identification. Registr...
Deep seismogenic zone Vrancea as an indicator of geodynamic processes
Tectonophysical interpretation of 80 mechanisms of earthquake sources (80—172 km deep) during 1940—2011 has been performed for seismogenic zone Vranchea. Functioning nodal planes of mechanisms have been identified as the...