FN Archimer Export Format
PT C
TI Earthquake monitoring in Italy: integration of a temporary seismic experiment into national real-time surveillance, the example of FocusX temporary land-network
BT 
AF Margheriti, Lucia
   Moretti, Milena
   Piccinini, Davide
   Latorre, Diana
   Alparone, Salvatore
   Cocina, Ornella
   Costanzo, antonio
   GUTSCHER, Marc-Andre
   La Rocca, Mario
   Marchetti, Alessandro
   MURPHY, Shane
   Nardi, Anna
   Pastori, Marina
AS 1:1;2:1;3:2;4:1;5:4;6:4;7:1;8:6;9:5;10:1;11:3;12:1;13:1;14:;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:PDG-REM-GEOOCEAN-ALMA;12:;13:;14:;
C1 Istituto Nazionale di Geofisica e Vulcanologia, INGV, Osservatorio Nazionale Terremoti, Italy
   Istituto Nazionale di Geofisica e Vulcanologia, INGV, Sezione di Pisa, Italy
   Geo-Ocean UMR6538, Univ. Brest, CNRS, IFREMER, France
   Istituto Nazionale di Geofisica e Vulcanologia, INGV, Osservatorio Etneo, Italy
   Laboratorio di Sismologia, Università Della Calabria, Italy
   Geo-Ocean UMR6538, Univ. Brest, CNRS, IFREMER, France
C2 INGV, ITALY
   INGV, ITALY
   IFREMER, FRANCE
   INGV, ITALY
   UNIV CALLABRIA, ITALY
   CNRS, FRANCE
SI BREST
SE PDG-REM-GEOOCEAN
   PDG-REM-GEOOCEAN-ALMA
UM GEO-OCEAN
UR https://archimer.ifremer.fr/doc/00847/95887/103792.pdf
LA English
DT Poster
CR FocusX3
BO L'Atalante
AB The INGV is the operational center for earthquake monitoring in Italy, https://www.ingv.it/en/monitoraggio-e-infrastrutture/sorveglianza/servizio-di-sorveglianza-sismica, it operates the Italian National Seismic Network and other networks at different scales and is a primary node of EIDA for archiving and distributing seismic recordings. INGV provides earthquake information to the Department of Civil Protection and to the public. In the frame of the FOCUS (Fiber Optic Cable Use for seafloor studies of earthquake hazard and deformation) project, https://www.geo-ocean.fr/Recherche/Projets-de-Recherche/ERC-FOCUS, we deployed a temporary seismic network, FXLand (1J), for a passive seismological experiment to record regional seismicity and teleseismic events. This experiment aims to improve the detection of seismicity; the accuracy of earthquake locations, and to define the crustal structure of the region. The seismicity in the Ionian area is possibly the result of two types of tectonic activity at different depths: a gently NW dipping subduction interface of the Calabrian subduction zone, and the strike-slip fault systems in the Ionian Sea, well expressed in the morpho-bathymetry and observed in previous seismic profiles. 
PY 2023
PD JUN
ID 95887
ER

EF