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Volume 17, issue 11 | Copyright
Nat. Hazards Earth Syst. Sci., 17, 1885-1892, 2017
https://doi.org/10.5194/nhess-17-1885-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Brief communication 09 Nov 2017

Brief communication | 09 Nov 2017

Brief communication: Co-seismic displacement on 26 and 30 October 2016 (Mw = 5.9 and 6.5) – earthquakes in central Italy from the analysis of a local GNSS network

Giorgio De Guidi et al.
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Cited articles
Aringoli D., Farabollini, P., Giacopetti, M., Materazzi, M., Paggi, S., Pambianchi, G., Pierantoni, P. P., Pistolesi, E., Pitts, A., and Tondi, E.: The August 24th 2016 Accumoli earthquake: surface faulting and Deep-Seated Gravitational Slope Deformation (DSGSD) in the Monte Vettore area, Ann. Geophys.-Italy, 59, Fast Track 5, https://doi.org/10.4401/ag-7199, 2016.
Blumetti, A. M.: Neotectonic investigations and evidence of paleoseismicity in the epicentral area of the January-February 1703, Central Italy, earthquakes, in: Perspectives in paleoseismology, edited by: Serva, L. and Slemmons, D. B., Association of Engeneering Geologists Special Publication, 6, 83–100, 1995.
Blumetti, A. M., Dramis, F., Gentili, B., and Pambianchi, G.: La struttura di M. Alvagnano-Castel Santa Maria nell'area nursina: aspetti geomorfologici e sismicità storica, Rend. Soc. Geol. It., 13, 71–76, 1990.
Blumetti, A. M., Guerrieri, L., and Vittori, E.: The primary role of the Paganica-San Demetrio fault system in the seismic landscape of the Middle Aterno Valley basin (Central Apennines), Quatern. Int., 288, 183–194, https://doi.org/10.1016/j.quaint.2012.04.040, 2013.
Boncio, P., Lavecchia, G., and Pace, B.: Defining a model of 3D seismogenic sources for Seismic Hazard Assessment applications: The case of central Apennines (Italy), J. Seismol., 8, 407–425, 2004.
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Short summary
In this paper we provide new and original data which show the deformation behaviour close to the seismogenic segment of the Mt Vettore normal fault system during co-seismic deformation (30 October 2016 Mw  = 5.9. This foresight allowed us to record the second (strongest) event (Mw  = 6.5) of 30 October 2016. We identified the specific fault zone that was most vulnerable to future seismic events just north of the fault segment that reactivated on 24 August.
In this paper we provide new and original data which show the deformation behaviour close to the...
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