1st Croatian Conference on Earthquake Engineering 2021
DOI: 10.5592/co/1crocee.2021.248
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Strong ground motion records of the Zagreb earthquake of 22 March 2020

Abstract: In the morning of 22 March 2020 at 5:24 (UTC) a damaging earthquake struck Zagreb, the capital of Croatia. This shallow local magnitude 5,5 earthquake was the strongest instrumentally recorded earthquake in the NW part of Croatia since 1908 when the first seismological station was installed in Zagreb. The strongest aftershock of local magnitude 4,9 happened at 6:01 (UTC) on the same day. Both events were recorded by two strong motion stations in the City of Zagreb, located close to the epicentres (10 km).

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Cited by 4 publications
(12 citation statements)
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“…4 (case 2) and Fig. 7b are similar to those predicted by the USGS shake map (https://earthquake.usgs.gov/data/shakemap/) and strong motions records (Prevolnik et al, 2021). Except of direct comparison of EQL modelled PGA surf (amplification factor at zero period) with empirical strong motions records (QUHS and QARH), it is interesting to compare 2D model of variation of PGA surf (Fig.…”
Section: Sitesupporting
confidence: 70%
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“…4 (case 2) and Fig. 7b are similar to those predicted by the USGS shake map (https://earthquake.usgs.gov/data/shakemap/) and strong motions records (Prevolnik et al, 2021). Except of direct comparison of EQL modelled PGA surf (amplification factor at zero period) with empirical strong motions records (QUHS and QARH), it is interesting to compare 2D model of variation of PGA surf (Fig.…”
Section: Sitesupporting
confidence: 70%
“…1-10) following both input rock motion scenarios with detailed site param eters (V S30 , fundamental frequency, estimated bedrock depth). Prevolnik et al (2021) presented strong motion records of the M L 5.5 Zagreb earthquake record ed on two stations located close to the epicentres (approx. 10 km distant): station QARH to be 0.20 g and station QUHS to be 0.22 g with presumable classification of ground type C by Eurocode 8 (EN1998-1).…”
Section: Resultsmentioning
confidence: 99%
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“…If site amplification [14] is considered, we can estimate that resulting peak ground acceleration was between 0.03 and 0.11 g. Again, if we consider a distance of about 40-50 km from the location of the Zagreb 2020 earthquake to the Trakošćan site, estimated peak ground acceleration using attenuation relation for the rock is about 0.03 g [22]. With accounted site amplification [14], ground shaking can be assumed between 0.06 and 0.10 g. We compared these assumed values with recorded ground motions-accelerations for the Zagreb 2020 event recorded on stations 10 km distant from the epicenter were about 0.20 g on alluvial sediment sites [23], whereas six accelerometric stations in Zagreb recorded the Petrinja 2020 event on different local sites in a range of 0.04 g up to 0.25 g (see analysis of accelerogram for Petrinja earthquake, [24]).…”
Section: Ambient Vibration Measurements: Pre-and Post-earthquakesmentioning
confidence: 99%