Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10641
Authors: Pucci, Stefano* 
De Martini, Paolo Marco* 
Civico, Riccardo* 
Nappi, Rosa* 
Ricci, Tullio* 
Villani, Fabio* 
Brunori, Carlo Alberto* 
Caciagli, Marco* 
Sapia, Vincenzo* 
Cinti, Francesca Romana* 
Moro, Marco* 
Di Naccio, Deborah* 
Gori, Stefano* 
Falcucci, Emanuela* 
Vallone, R* 
Mazzarini, Francesco* 
Tarquini, S.* 
Del Carlo, P.* 
Kastelic, Vanja* 
Carafa, Michele Matteo C.* 
De Ritis, Riccardo* 
Gaudiosi, Germana* 
Nave, Rosella* 
Alessio, Giuliana* 
Burrato, Pierfrancesco* 
Smedile, Alessandra* 
Alfonsi, Laura* 
Vannoli, Paola* 
Pignone, Maurizio* 
Pinzi, Stefania* 
Fracassi, Umberto* 
Pizzimenti, L.* 
Mariucci, Maria Teresa* 
Pagliuca, Nicola Mauro* 
Sciarra, Alessandra* 
Carluccio, Roberto* 
Nicolosi, J.* 
Chiappini, Massimo* 
D'Ajello Caracciolo, Francesca* 
Pezzo, Giuseppe* 
Patera, Antonio* 
Azzaro, Raffaele* 
Pantosti, Daniela* 
Montone, Paola* 
Saroli, M.* 
Lo Sardo, L.* 
Lancia, M.* 
Title: Coseismic effects of the 2016 Amatrice seismic sequence: first geological results
Issue Date: 2016
Series/Report no.: FAST TRACK 5/59 (2016)
DOI: 10.4401/ag-7195
URI: http://hdl.handle.net/2122/10641
Keywords: coseismic effects
surface ruptures
fractures and faults
amatrice earthquake
Subject Classification04.06. Seismology 
Abstract: Since the beginning of the ongoing Amatrice seismic sequence on August 24, 2016, initiated by a Mw 6.0 normal faulting earthquake, the EMERGEO Working Group (an INGV team devoted to earthquake aftermath geological survey) investigated coseismic effects on the natural environment. Up to now, we surveyed about 750 km2 and collected more than 3200 geological observations including differently oriented tectonic fractures together with intermediate- to small- sized landslides. The most impressive coseismic evidence was found along the known active Mt. Vettore fault system, where surface ruptures with clear vertical/horizontal offset were observed for more than 5 km, while unclear and discontinuous coseismic features were recorded along the Laga Mts. Fault systems.
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