A database of the coseismic effects following the 30 October 2016 Norcia earthquake in Central Italy
- Villani, F
- Civico, R
- Pucci, S
- Pizzimenti, L
- Nappi, R
- De Martini, PM
- Agosta, F
- Alessio, G
- Alfonsi, L
- Amanti, M
- Amoroso, S
- Aringoli, D
- Auciello, E
- Azzaro, R
- Baize, S
- Bello, S
- Benedetti, L
- Bertagnini, A
- Binda, G
- Bisson, M
- Blumetti, AM
- Bonadeo, L
- Boncio, P
- Bornemann, P
- Branca, S
- Braun, T
- Brozzetti, F
- Brunori, CA
- Burrato, P
- Caciagli, M
- Campobasso, C
- Carafa, M
- Cinti, FR
- Cirillo, D
- Comerci, V
- Cucci, L
- De Ritis, R
- Deiana, G
- Del Carlo, P
- Del Rio, L
- Delorme, A
- Di Manna, P
- Di Naccio, D
- Falconi, L
- Falcucci, E
- Farabollini, P
- Faure Walker, JP
- Ferrarini, F
- Ferrario, MF
- Ferry, M
- Feuillet, N
- Fleury, J
- Fracassi, U
- Frigerio, C
- Galluzzo, F
- Gambillara, R
- Gaudiosi, G
- Goodall, H
- Gori, S
- Gregory, LC
- Guerrieri, L
- Hailemikael, S
- Hollingsworth, J
- Iezzi, F
- Invernizzi, C
- Jablonská, D
- Jacques, E
- Jomard, H
- Kastelic, V
- Klinger, Y
- Lavecchia, G
- Leclerc, F
- Liberi, F
- Lisi, A
- Livio, F
- Sardo, L
- Malet, JP
- Mariucci, MT
- Materazzi, M
- Maubant, L
- Mazzarini, F
- McCaffrey, KJW
- Michetti, AM
- Mildon, ZK
- Montone, P
- Moro, M
- Nave, R
- Odin, M
- Pace, B
- Paggi, S
- Pagliuca, N
- Pambianchi, G
- Pantosti, D
- Patera, A
- Pérouse, E
- Pezzo, G
- Piccardi, L
- Pierantoni, PP
- Pignone, M
- Pinzi, S
DOIAbstract
© 2018 The Author(s). We provide a database of the coseismic geological surface effects following the Mw 6.5 Norcia earthquake that hit central Italy on 30 October 2016. This was one of the strongest seismic events to occur in Europe in the past thirty years, causing complex surface ruptures over an area of > 400 km 2. The database originated from the collaboration of several European teams (Open EMERGEO Working Group; about 130 researchers) coordinated by the Istituto Nazionale di Geofisica e Vulcanologia. The observations were collected by performing detailed field surveys in the epicentral region in order to describe the geometry and kinematics of surface faulting, and subsequently of landslides and other secondary coseismic effects. The...
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