10.15778/RESIF.YP2014
Cornou,C
Bard,P.-Y.
RESIF
Seismic network YP:French part of the Argostoli (Greece) aftershock experiment (RESIF-SISMOB)
RESIF - Réseau Sismologique et géodésique Français
2014
RESIF Information System
RESIF Data Centre
Université Grenoble Alpes, Grenoble, France (UGA)
Institut des Sciences de la Terre, Grenoble, France (ISTERRE)
National Institute of Geophysics and Volcanology, Italy (INGV)
Institute of Engineering Seismology and Earthquake Engineering, Research and Technical Institute, Greece (ITSAK)
German Research Centre for Geosciences , Germany (GFZ)
Network of European Research Infrastructures for Earthquake Risk Assessment and Mitigation , FP7-INFRASTRUCTURES-2010-1 (NERA)
European Commission - CORDIS
dense array
site effects
spatial variability
2014-04-10/2015-02-28
2028-04-10/
en
Seismic Network
10.1080/13632469.2018.1453398
10.1007/s10518-018-0320-1
10.1007/s10518-018-0313-0
10.1007/s10518-017-0225-4
10.1007/s10518-017-0225-4
10.1007/s10518-017-0270-z
10.1093/gji/ggx161
http:www.resif.fr
57 Gb;8 stations
miniseed data
stationXML metadata
Open Access
Creative Commons By 4.0 Universal
Within the framework of the JRA1 work packages (Waveform modelling and site coefficients for basin response and topography) of the FP7 EU-NERA 2010-2014 project (Network of European Research Infrastructures for Earthquake Risk Assessment and Mitigation), a dense seismological temporary network was deployed in the Argostoli sedimentary basin (Cephalonia island, Greece) in order to investigate basin effects and spatial variation of ground motion. Tooking place during the period September 15th, 2011 to April 20th, 2012, the seismological experiment comprised 62 seismological stations (mid-band velocimeters, eventually coupled with accelerometers) deployed across the Argostoli basin with inter-station of about 50 meters. 2 mid-band velocimeters were installed at the eastern- and western-most part of the island in order to improve hypocentral location of earthquakes recorded during the experiment. Finally, two dense seismic arrays (with inter-station distance from 5 m to 160 m) were also deployed inside the basin to thoroughly understand seismic wave field composition. More than 3000 seismic events were recorded by this seismological network, among which 817 event with a signal-to-noise ratio above 3.
Greece
Argostoli
20.487400
20.531300
38.151100
38.183600