{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,3,23]],"date-time":"2026-03-23T11:27:19Z","timestamp":1774265239455,"version":"3.50.1"},"reference-count":77,"publisher":"MDPI AG","issue":"6","license":[{"start":{"date-parts":[[2021,3,13]],"date-time":"2021-03-13T00:00:00Z","timestamp":1615593600000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"DOI":"10.13039\/501100004488","name":"Hrvatska Zaklada za Znanost","doi-asserted-by":"publisher","award":["IP-2016-06-1854"],"award-info":[{"award-number":["IP-2016-06-1854"]}],"id":[{"id":"10.13039\/501100004488","id-type":"DOI","asserted-by":"publisher"}]},{"DOI":"10.13039\/501100004488","name":"Hrvatska Zaklada za Znanost","doi-asserted-by":"publisher","award":["IP-2020-02-3531"],"award-info":[{"award-number":["IP-2020-02-3531"]}],"id":[{"id":"10.13039\/501100004488","id-type":"DOI","asserted-by":"publisher"}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>On 28 December 2020, seismic activity in the wider Petrinja area strongly intensified after a period of relative seismological quiescence that had lasted more than 100 years (since the well-known M5.8 Kupa Valley earthquake of 1909, which is known based on the discovery of the Mohorovi\u010di\u0107 discontinuity). The day after the M5 foreshock, a destructive M6.2 mainshock occurred. Outcomes of preliminary seismological, geological and SAR image analyses indicate that the foreshocks, mainshock and aftershocks were generated due to the (re)activation of a complex fault system\u2014the intersection of longitudinal NW\u2013SE right-lateral and transverse NE\u2013SW left-lateral faults along the transitional contact zone of the Dinarides and the Pannonian Basin. According to a survey of damage to buildings, approximately 15% of buildings were very heavily damaged or collapsed. Buildings of special or outstanding historical or cultural heritage significance mostly collapsed or became unserviceable. A preliminary analysis of the earthquake ground motion showed that in the epicentral area, the estimated peak ground acceleration PGA values for the bedrock ranged from 0.29 to 0.44 g. In the close Petrinja epicentral area that is characterized by the superficial deposits, significant ground failures were reported within local site effects. Based on that finding and building damage, we assume that the resulting peak ground acceleration (PGAsite) values were likely between 0.4 and 0.6 g depending on the local site characteristics and the distance from the epicentre.<\/jats:p>","DOI":"10.3390\/rs13061095","type":"journal-article","created":{"date-parts":[[2021,3,14]],"date-time":"2021-03-14T23:52:06Z","timestamp":1615765926000},"page":"1095","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":63,"title":["Destructive M6.2 Petrinja Earthquake (Croatia) in 2020\u2014Preliminary Multidisciplinary Research"],"prefix":"10.3390","volume":"13","author":[{"ORCID":"https:\/\/orcid.org\/0000-0003-1836-4809","authenticated-orcid":false,"given":"Snje\u017eana","family":"Marku\u0161i\u0107","sequence":"first","affiliation":[{"name":"Department of Geophysics, Faculty of Science, University of Zagreb, 10000 Zagreb, Croatia"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-1829-0862","authenticated-orcid":false,"given":"Davor","family":"Stanko","sequence":"additional","affiliation":[{"name":"Faculty of Geotechnical Engineering, University of Zagreb, 42000 Vara\u017edin, Croatia"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-7539-4639","authenticated-orcid":false,"given":"Davorin","family":"Penava","sequence":"additional","affiliation":[{"name":"Faculty of Civil Engineering and Architecture Osijek, Josip Juraj Strossmayer University of Osijek, 31000 Osijek, Croatia"}]},{"given":"Ines","family":"Ivan\u010di\u0107","sequence":"additional","affiliation":[{"name":"Department of Geophysics, Faculty of Science, University of Zagreb, 10000 Zagreb, Croatia"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-9796-3094","authenticated-orcid":false,"given":"Olga","family":"Bjelotomi\u0107 Or\u0161uli\u0107","sequence":"additional","affiliation":[{"name":"IGEA d.o.o., 42000 Vara\u017edin, Croatia"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-7494-7377","authenticated-orcid":false,"given":"Tvrtko","family":"Korbar","sequence":"additional","affiliation":[{"name":"Department of Geology, Croatian Geological Survey, 10000 Zagreb, Croatia"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-5748-7679","authenticated-orcid":false,"given":"Vasilis","family":"Sarhosis","sequence":"additional","affiliation":[{"name":"Faculty of Engineering and Physical Sciences, School of Civil Engineering, University of Leeds, Leeds LS2 9JT, UK"}]}],"member":"1968","published-online":{"date-parts":[[2021,3,13]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","unstructured":"Stanko, D., Marku\u0161i\u0107, S., Korbar, T., and Ivan\u010di\u0107, J. 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