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Analysis of Local Site Effects in the Medjimurje Region (North Croatia) and Its Consequences Related to Historical and Recent Earthquakes (CROSBI ID 314605)

Prilog u časopisu | izvorni znanstveni rad | međunarodna recenzija

Stanko, Davor ; Sović, Ivica ; Belić, Nikola ; Markušić, Snježana Analysis of Local Site Effects in the Medjimurje Region (North Croatia) and Its Consequences Related to Historical and Recent Earthquakes // Remote sensing, 14 (2022), 4831, 23. doi: 10.3390/rs14194831

Podaci o odgovornosti

Stanko, Davor ; Sović, Ivica ; Belić, Nikola ; Markušić, Snježana

engleski

Analysis of Local Site Effects in the Medjimurje Region (North Croatia) and Its Consequences Related to Historical and Recent Earthquakes

The Medjimurje region (North Croatia), situated between the Drava and Mura rivers with a slightly elevated hilly area, can be generally characterized as a low-seismicity area. However, macroseismic observations from historical and recent earthquakes indicate that some localities in this region are more prone to damage than others. Significant damage and the observed higher intensities in the Medjimurje region after the historical earthquakes of 1738 MLm5.1 (Medjimurje) and 1880 ML6.3 (Zagreb), and events that occurred in the instrumental era, 1938 ML5.6 (Koprivnica), 1982 ML4.5 (Ivanec), and the most recent 2020 ML5.5 Zagreb and 2020 ML6.2 Petrinja earthquakes, point to the influence of local site effects. There is a reasonable indication that these earthquakes involved several localized site effects that could explain the increased intensity of half a degree or even up to one degree at certain localities compared to macroseismic modeling for rock condition. To better understand the influence of local site effects in the Medjimurje region, the single-station microtremor Horizontal-to-Vertical Spectral Ratio (HVSR) method for subsurface characterization was used. Based on individual measurements, microzonation maps were derived for the Medjimurje region to better understand the behavior of ground motion and the influence of local site conditions in comparison to macroseismic intensities and past damage observations. Several local site effects could be interpreted as a main contribution to site amplification and resonance effects due to variations in deep soft-deposit thicknesses overlayed on hard deposits and directional variations in topographical areas that could localize earthquake damage patterns. Correlations of microtremor analysis with intensity observations from historical earthquakes as well with recent earthquakes could help to distinguish local site zones prone to the possible occurrence of higher earthquake damage from nearby and distant earthquakes.

Medjimurje ; ambient noise measurements ; local site effects ; macroseismic intensity ; microzonation

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Podaci o izdanju

14

2022.

4831

23

objavljeno

2072-4292

10.3390/rs14194831

Trošak objave rada u otvorenom pristupu

Povezanost rada

Geofizika, Geologija

Poveznice
Indeksiranost