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  • 1
    Publication Date: 2021-04-13
    Description: This paper presents a joint analysis of instrumental and macroseismic data regarding the 19 July 2019, Greece Mw5.1 earthquake occurred west of Athens. This earthquake ruptured a blind, south-dipping normal fault, 23 km WNW of the center of Athens, while its relocated epicentre lies in close vicinity to the one of the 1999 Mw6.0 earthquake. The maximum macroseismic intensity of the 2019 mainshock reached IEMS98 = 7.5. Scarce damage and intensities up to 5–6 were reported in the epicentral area. Higher intensities were observed at larger distances, 12–15 km east and ESE of the epicentre, alongside the banks of Kifissos River, likely related to ground motion amplification due to soft alluvial formations. Similar selectivity of increased ground motions to the east of the epicentre with respect to other azimuths, also observed during the 1981 and 1999 earthquakes, supports eastward rupture directivity of the 2019 mainshock, an effect that is possibly common for the region’s fault system. Damping of seismic effects was observed east of Aegaleo Mountain, a structure suggested to impose a stopping phase in the time histories of the 1999 and 2019 earthquakes (Fig. A1).
    Print ISSN: 1383-4649
    Electronic ISSN: 1573-157X
    Topics: Geosciences , Physics
    Published by Springer
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  • 2
    Publication Date: 2021-06-14
    Description: Here, we present the source mechanism and rupture process for the destructive 24 January 2020 Mw 6.7 Doğanyol–Sivrice earthquake at the East Anatolian Fault Zone (EAFZ, Turkey), obtained from seismological waveform analysis and space geodetic observations. Multi-data analyses and modelling in the present study provide fundamental data and strong constraints for retrieving complex source mechanism of an earthquake and its spatiotemporal slip characteristics along the ruptured segment of fault. The acquired slip model of this earthquake reveals heterogeneous slip distribution along strike N244°E of the fault plane dipping NW (68°) with duration of the source time function (STF) and low stress drop value (Δσ) of ~25 s and ~ 6 bars, respectively. Back-projection analysis validates fault length (L) stretching along strike for a distance of ~75 km and supports predominant south-westerly bilateral rupture propagation with a variable rupture velocity (Vr) of ~2.3–3.4 km/s along with two main patches, presumably a sequence of two asperities being ruptured following the surface trace of the EAFZ. The distribution of aftershocks based on the analysis of two months long data consistently confirms spreading of seismicity along the ruptured fault. The evaluation of Interferometric Synthetic Aperture Radar (InSAR) data reveals that left-lateral co-seismic slip and significant deformation extends for ~20 km on either side of the fault with evident post-seismic displacement. Yet, no significant vertical offsets were observed as GNSS stations detected only horizontal motions. Coda-wave analysis as an independent tool also confirms moment magnitude of Mw 6.7. Our results highlight a case of a damaging earthquake and enhance our understanding of earthquake mechanics, continental deformation and augmented earthquake risk on the EAFZ.
    Type: info:eu-repo/semantics/article
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  • 3
    Publication Date: 2023-06-29
    Description: We present a comprehensive analysis of geodetic data, including InSAR imagery and GNSS observations, to assess the pattern of ground motions of the Paliki peninsula in western Cephalonia, Greece. Paliki is prone to frequent, strong earthquakes, due to its close proximity to the right-lateral Cephalonia Transform Fault (CTF), a 140 km long strike-slip fault that accommodates the relative motion between the Apulian and Aegean lithospheric plates. Our analysis covers the period from 2016 to 2022 and leverages the LiCSBAS, an open-source package, for InSAR time series analysis with the N-SBAS method. We combined the InSAR results with the GNSS observations. The results indicate that active faults on the Paliki peninsula are oriented approximately N-S and exhibit slip rates between 2-5 mm/yr in the line-of-sight direction. The horizontal component of movement is dominant, providing initial evidence of right-lateral strike-slip faulting on the peninsula. The InSAR data also indicate possible post-seismic motion along the fault plane that ruptured on the 3 February 2014 M5.9 earthquake in the northwest part of the peninsula. Moreover, we have identified other possible active structures, including both strike-slip and thrust faults, confirmed by field geological data. The coastal town of Lixouri undergoes uplift, as evidenced by positive line-of-sight displacement values in both imaging geometries. Velocity cross-sections reveal several discontinuities, possibly bounded by active faults and/or crustal flexure. The integration of geodetic data with seismological and field geological data provides a valuable tool for the monitoring of interseismic behaviour of active faults.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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