Surface Ruptures Following The 30 October 2016 M-W 6.5 Norcia Earthquake, Central Italy

R. Civico,S. Pucci,F. Villani,L. Pizzimenti,P. M. De Martini,R. Nappi,F. Agosta,G. Alessio,L. Alfonsi, M. Amanti,S. Amoroso,D. Aringoli, E. Auciello,R. Azzaro,S. Baize,S. Bello,L. Benedetti,A. Bertagnini,G. Binda, M. Bisson, A. M. Blumetti, L. Bonadeo, P. Boncio, P. Bornemann,S. Branca,T. Braun, F. Brozzetti,C. A. Brunori,P. Burrato,M. Caciagli, C. Campobasso,M. Carafa,F. R. Cinti,D. Cirillo, V. Comerci,L. Cucci,R. De Ritis, G. Deiana,P. Del Carlo,L. Del Rio,A. Delorme,P. Di Manna,D. Di Naccio, L. Falconi,E. Falcucci,P. Farabollini,J. P. Faure Walker,F. Ferrarini,M. F. Ferrario,M. Ferry, N. Feuillet, J. Fleury,U. Fracassi, C. Frigerio, F. Galluzzo, R. Gambillara, G. Gaudiosi, H. Goodall,S. Gori,L. C. Gregory,L. Guerrieri,S. Hailemikael,F. Iezzi, C. Invernizzi, D. Jablonska,E. Jacques, H. Jomard,V. Kastelic,Y. Klinger, G. Lavecchia,F. Leclerc,F. Liberi, A. Lisi,F. Livio, L. Lo Sardo,J. P. Malet,M. T. Mariucci, M. Materazzi,F. Mazzarini, K. J. W. Mccaffrey,A. M. Michetti,Z. K. Mildon,P. Montone,M. Moro, R. Nave, M. Odin,B. Pace, S. Paggi, N. Pagliuca, G. Pambianchi,D. Pantosti,A. Patera, E. Perouse, G. Pezzo,L. Piccardi,P. P. Pierantoni,M. Pignone, S. Pinzi, E. Pistolesi, J. Point,A. Pozzi,M. Proposito,C. Puglisi,I. Puliti,T. Ricci, L. Ripamonti, M. Rizza,G. P. Roberts, M. Roncoroni,V. Sapia,M. Saroli,A. Sciarra,O. Scotti, G. Skupinski, A. Smedile,G. Tarabusi,S. Tarquini, S. Terrana, J. Tesson,E. Tondi,A. Valentini,R. Vallone, J. Van Der Woerd,P. Vannoli,A. Venuti, E. Vittori,T. Volatili,L. N. J. Wedmore,M. Wilkinson,M. Zambrano

JOURNAL OF MAPS(2018)

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摘要
We present a 1:25,000 scale map of the coseismic surface ruptures following the 30 October 2016 M-w 6.5 Norcia normal-faulting earthquake, central Italy. Detailed rupture mapping is based on almost 11,000 oblique photographs taken from helicopter flights, that has been verified and integrated with field data (>7000 measurements). Thanks to the common efforts of the Open EMERGEO Working Group (130 people, 25 research institutions and universities from Europe), we were able to document a complex surface faulting pattern with a dominant strike of N135 degrees-160 degrees (SW-dipping) and a subordinate strike of N320 degrees-345 degrees (NE-dipping) along about 28km of the active Mt. Vettore-Mt. Bove fault system. Geometric and kinematic characteristics of the rupture were observed and recorded along closely spaced, parallel or subparallel, overlapping or step-like synthetic and antithetic fault splays of the activated fault systems, comprising a total surface rupture length of approximately 46km when all ruptures were considered.
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关键词
Surface faulting, coseismic ruptures, normal faulting, geological prompt surveys, 2016-2017 seismic sequence, central Italy
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