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Cephalonia Fault

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(a) The <span class="search-highlight">Cephalonia</span> transform <span class="search-highlight">fault</span> ( CTF ) marks the western edge of the Ae...
Published: 01 September 2015
Figure 1. (a) The Cephalonia transform fault ( CTF ) marks the western edge of the Aegean (Hellenic) arc (Generic Mapping Tools–based bathymetry). A shear zone between the trace of the CTF is shown, and the 2008 fault is inferred. (b) Tectonic pattern in the vicinity of Leucas and Cephalonia
Journal Article
Published: 01 February 2005
Bulletin of the Seismological Society of America (2005) 95 (1): 159–172.
... mechanisms of the two main subevents are predominantly right-lateral strike slip of south-southwest–north-northeast orientation. The Cephalonia subevent occurred on a less steeply dipping fault with a small thrust component. Large deviations from pure double couple were found but interpreted as artifacts...
FIGURES | View All (9)
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(a) Geodynamic map of the broader southeastern Mediterranean and location (...
Published: 06 June 2018
(1989 , 2006) , Stiros et al. (1994) , Lekkas et al. (2001) , and our geological survey. AEF, Agia Effimia fault; AeT, Aenos thrust; ArF and MF, Argostoli fault (east) and Minies fault (west); CTFZ, Cephalonia transform fault zone; IT, Ionian thrust; KAF, Kontogourata‐Agon fault; LT, Livadi
Image
(a) General map with the prevailing seismotectonic features in western Gree...
Published: 10 March 2020
Figure 1. (a) General map with the prevailing seismotectonic features in western Greece (Cephalonia transform fault zone [CTFZ]); the frame marks the location of Cephalonia, (b) map of Cephalonia showing the exact location of the ARGOstoli Network (ARGONET) array, and (c) rough description
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Prevailing directions of maximum horizontal extension (black arrows) for al...
Published: 01 February 2009
; AE, Apulia Escarpment; KF, Cephalonia Fault; SAP, southern Apennines; GP, Gargano promontory. White stars: selected break-out data (σ hmin ) from M ontone et alii (2004) . Direzioni prevalenti di massima estensione orizzontale (frecce nere) per i siti investigati. Le direzioni di massimo
Journal Article
Published: 20 December 2016
Bulletin of the Seismological Society of America (2017) 107 (1): 433–444.
... and Global Positioning System (GPS) slip vectors. Detailed fault modeling in this region, characterized by intense seismicity and deformation rates, usually assigned to the Cephalonia Transform fault, is a challenge because of the unfavorable observation system. To overcome this problem, we independently...
FIGURES | View All (7)
Journal Article
Published: 01 February 2007
Bulletin of the Seismological Society of America (2007) 97 (1B): 35–51.
...Christoforos Benetatos; Douglas Dreger; Anastasia Kiratzi Abstract The 14 August 2003 ( M w 6.2) Lefkada earthquake ruptured the Lefkada Segment of the Cephalonia transform fault zone ( ctfz ), a major structure along the Ionian Islands of Greece. We invert 30 P and 9 S waves recorded by the Global...
FIGURES | View All (15)
Journal Article
Published: 01 September 2015
Bulletin of the Seismological Society of America (2015) 105 (5): 2510–2520.
...Figure 1. (a) The Cephalonia transform fault ( CTF ) marks the western edge of the Aegean (Hellenic) arc (Generic Mapping Tools–based bathymetry). A shear zone between the trace of the CTF is shown, and the 2008 fault is inferred. (b) Tectonic pattern in the vicinity of Leucas and Cephalonia...
FIGURES | View All (4)
Journal Article
Published: 06 June 2018
Seismological Research Letters (2018) 89 (4): 1555–1565.
... (1989 , 2006) , Stiros et al. (1994) , Lekkas et al. (2001) , and our geological survey. AEF, Agia Effimia fault; AeT, Aenos thrust; ArF and MF, Argostoli fault (east) and Minies fault (west); CTFZ, Cephalonia transform fault zone; IT, Ionian thrust; KAF, Kontogourata‐Agon fault; LT, Livadi...
FIGURES | View All (5)
Journal Article
Published: 24 January 2018
Seismological Research Letters (2018) 89 (2A): 678–687.
... ABSTRACT Cephalonia Island is one of the most seismic zones of the Euro‐Mediterranean area due to the activity of the Cephalonia transform fault connecting the Hellenic subduction to the northwest Greece collision. Following the two M w 6+ earthquakes that occurred in early 2014, a postseismic survey...
FIGURES | View All (5)
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Location of the study site and sensors. (a) <span class="search-highlight">Cephalonia</span> Island with respect ...
Published: 24 January 2018
Figure 1. Location of the study site and sensors. (a) Cephalonia Island with respect to Greece, with the main tectonic features (from Karakostas et al. , 2015 ; CTF, Cephalonian transform fault; NAT, North Anatolian trough). (b) The Argostoli area with respect to Kefalonia Island
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Main seismotectonic properties of the Aegean and surrounding regions. The s...
Published: 01 October 2004
Figure 1. Main seismotectonic properties of the Aegean and surrounding regions. The study area is indicated by a rectangle. CTF = Cephalonia Transform Fault.
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Western Greece, major <span class="search-highlight">faults</span>, and seismic stations. Hellenic subduction (li...
Published: 01 February 2005
Figure 1. Western Greece, major faults, and seismic stations. Hellenic subduction (line with teeth), the Cephalonia transform fault (arrows), and the continental collision (line with dots) are shown. The patnet short-period stations used in location are denoted by triangles. The broadband
Image
(a) The 2015 Leucas earthquake in relation to recent earthquakes (stars) in...
Published: 20 December 2016
et al. , 2005 ; Saltogianni and Stiros, 2015 ). The two main faults of the 2014 Cephalonia sequence (after Merryman Boncori et al. , 2015 ; Sokos et al. , 2015 ), the 1953 thrusts (after Stiros et al. , 1994 ), and the 1983 earthquake data (after Kiratzi and Langston, 1991 ) are also shown
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Geographical distribution of the NOANET stations. The color of the symbols ...
Published: 17 March 2021
Figure 1. Geographical distribution of the NOANET stations. The color of the symbols denotes the year of installation. CG, Corinth Gulf; IS, Ionian Sea; HT, Hellenic trench; CTFZ, Cephalonia transform fault zone; NAT, North Aegean trough; BF, Backstop front; MR, Mediterranean ridge. The color
Journal Article
Published: 19 November 2014
Seismological Research Letters (2015) 86 (1): 124–137.
... of the latter effects took place in the aftermath of the 26 January 2014 event and were reactivated one week later by the 3 February earthquake. Figure 1. Location map showing the tectonic context of the Aegean Sea and the main faults on the island of Cephalonia. Colored rectangles and magenta triangles...
FIGURES | View All (8)
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Schematic seismotectonic map of the broader Aegean, showing the main crusta...
Published: 01 June 2019
Figure 1. Schematic seismotectonic map of the broader Aegean, showing the main crustal thickness variations in km (black contours) and extensional stresses (double vectors) derived from crustal earthquake fault plane solution data. The southern Aegean Wadati–Benioff zone isodepths (blue dashed
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Horizontal global positioning system velocities (gray arrows) and correspon...
Published: 15 September 2020
are simplified as red lines. Details on the Nubia–Eurasia rotation pole are in Pérouse et al. (2012) . CTF = Cephalonia transform fault; FYROM = former Yugoslav Republic of Macedonia.
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Morphological map of the Aegean Sea and surrounding areas with major active...
Published: 01 October 2013
and Eurasian plates along with the Rhodes transform fault (RTF) and the Cephalonia transform fault (CTF) at the southeastern and western termination of the Hellenic arc, respectively, are also indicated along with the Cyprus arc at the southeast corner of the map. The white rectangle indicates the study site
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(a) Seismicity ( M  ≥ 5) of the broader Aegean area
                       ...
Published: 01 April 2024
relative to Eurasia (solid arrows), and major strike‐slip zones (CTF, Cephalonia Transform fault; NAF, North Anatolia fault; NAT, North Aegean trough; and RTF, Rhodes Transform fault). We also present two indicative Benioff zone