2019
DOI: 10.3390/rs11161848
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On the Segmentation of the Cephalonia–Lefkada Transform Fault Zone (Greece) from an InSAR Multi-Mode Dataset of the Lefkada 2015 Sequence

Abstract: We use Interferometric Synthetic Aperture Radar (InSAR) to study the Cephalonia-Lefkada Transform Fault Zone (CTF) in the Ionian Sea. The CTF separates continental subduction to the north from oceanic subduction to the south, along the Hellenic Subduction Zone. We exploit a rich multi-modal radar dataset of the most recent major earthquake in the region, the 17 November 2015 Mw 6.4 event, and present new surface displacement results that offer additional constraints on the fault segmentation of the area. Based… Show more

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Cited by 6 publications
(3 citation statements)
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“…The mean thickness of the seismogenic layer along the KTFZ is equal to 12 km, with earthquake focal depths ranging between 3 and 15 km [36]. The large earthquakes that occurred in the study area since 2003 (Figure 2; 2003 with M w = 6.2 in the northern part of Lefkada; 2014 with M w = 6.1 and 6.0 in the Paliki Peninsula in Kefalonia; 2015 with M w = 6.5 in the southern part of Lefkada), along with the one that occurred offshore southeast of the Island of Kefalonia in 1983 with M w = 7.0, have attracted research interest ( [37][38][39][40][41][42][43], among others), and thus a detailed segmentation model for KTFZ is available. Each fault segment considered in this study is modeled using the standard source characterization approach, promoting specific fault segments with fixed endpoints [44,45].…”
Section: Fault Segmentation Model Of Kefalonia Transform Fault Zone A...mentioning
confidence: 99%
“…The mean thickness of the seismogenic layer along the KTFZ is equal to 12 km, with earthquake focal depths ranging between 3 and 15 km [36]. The large earthquakes that occurred in the study area since 2003 (Figure 2; 2003 with M w = 6.2 in the northern part of Lefkada; 2014 with M w = 6.1 and 6.0 in the Paliki Peninsula in Kefalonia; 2015 with M w = 6.5 in the southern part of Lefkada), along with the one that occurred offshore southeast of the Island of Kefalonia in 1983 with M w = 7.0, have attracted research interest ( [37][38][39][40][41][42][43], among others), and thus a detailed segmentation model for KTFZ is available. Each fault segment considered in this study is modeled using the standard source characterization approach, promoting specific fault segments with fixed endpoints [44,45].…”
Section: Fault Segmentation Model Of Kefalonia Transform Fault Zone A...mentioning
confidence: 99%
“…A few years later, on 17 November 2015, another strong earthquake (Mw 6.4) struck the western inland part of the island. Since then, a large body of studies has been carried out concerning the analysis of the co-seismic deformation, the slip distribution, the source parameters, and the slip model [37][38][39][40][41][42]. In addition to the seismotectonic perspective, other researchers have examined the macro-seismic effects of these events via the recording of different types of mass movements as well as the identification and assessment of ground failures [43][44][45].…”
Section: Study Areamentioning
confidence: 99%
“…DInSAR Analysis: SAR interferometry is a well-established method for mapping co-seismic surface deformation [27][28][29] .…”
Section: Optical Satellite Dataset and Processingmentioning
confidence: 99%