دورية أكاديمية
Coseismic Ground Displacement after the Mw6.2 Earthquake in NW Croatia Determined from Sentinel-1 and GNSS CORS Data
| العنوان: | Coseismic Ground Displacement after the Mw6.2 Earthquake in NW Croatia Determined from Sentinel-1 and GNSS CORS Data |
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| المؤلفون: | Bjelotomic Orsulic, Olga, Markovinovic, Danko, Varga, Matej, Bašić, Tomislav |
| المصدر: | Geosciences, 11 (4) |
| بيانات النشر: | MDPI |
| سنة النشر: | 2021 |
| المجموعة: | ETH Zürich Research Collection |
| مصطلحات موضوعية: | 29 December 2020 hazardous earthquake, Mw 6.2 earthquale in Croatia, Sentinel-1, SAR processing, coseismic ground displacement, GNSS |
| الوصف: | At the very end of the year 2020, on 29 December, a hazardous earthquake of Mw = 6.2 hit the area of Petrinja and its surroundings, in the NW of Croatia. The earthquake was felt across the area of 400 km, leaving an inconceivable damage in the vicinity of the epicenter, devastated towns and ruined lives. In order to map the spreading of earthquake waves and to determine the coseismic ground displacement after the mainshock, we have analyzed open satellite radar images of Sentinel-1 and the GNSS data from the nearest CORS station related to the epicenter, along with the seismic faults. In this paper, we addressed and mapped the displacement linear surface ruptures detected by the SAR interferometry. The results show the vertical ground displacement to the extent of -12 cm in the southern area and up to 22 cm in the north-western part of a wide area struck by the earthquake impact, related to the epicenter. Subsidence and uplift in a range of +/- 5 cm over a wider affected area indicate a spatial extent and hazardous impact made by the earthquake. The ground displacement of 30 cm to the West and 40 cm to the East has been identified considering the intersection of Pokupsko and Petrinja strike-slip fault system in the seismic zone of Pannonian basin. Accordingly, we obtained matching results of 5 cm south-easting shift and -3 cm subsidence on Sisak GNSS CROPOS station, addressing the tectonic blocks movement along the activated complex fault system. The results compared with the geology data confirm the existence of two main faults; the Pokupsko and the Petrinja strike-slip faults and interpret the occurrence of secondary post-seismic events over the observed area. ; ISSN:2076-3263 |
| نوع الوثيقة: | article in journal/newspaper |
| وصف الملف: | application/application/pdf |
| اللغة: | English |
| العلاقة: | info:eu-repo/semantics/altIdentifier/wos/000643075600001; http://hdl.handle.net/20.500.11850/494981Test |
| DOI: | 10.3929/ethz-b-000494981 |
| الإتاحة: | https://doi.org/20.500.11850/494981Test https://doi.org/10.3929/ethz-b-000494981Test https://doi.org/10.3390/geosciences11040170Test https://hdl.handle.net/20.500.11850/494981Test |
| حقوق: | info:eu-repo/semantics/openAccess ; http://creativecommons.org/licenses/by/4.0Test/ ; Creative Commons Attribution 4.0 International |
| رقم الانضمام: | edsbas.32C7E151 |
| قاعدة البيانات: | BASE |
| DOI: | 10.3929/ethz-b-000494981 |
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