Journal cover Journal topic
Natural Hazards and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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: 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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Interactive discussionStatus: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version      Supplement - Supplement
 
RC1: 'Co-seismic displacements GNSS - central italy', Athanassios Ganas, 07 May 2017 Printer-friendly Version 
AC2: 'Reply to the comments', Giorgio De Guidi, 13 Jun 2017 Printer-friendly Version Supplement 
 
RC2: 'Review of ‘Co-seismic displacement on October 26 and 30, 2016 (Mw 5.9 and 6.5) – earthquakes in central Italy from the analysis of discrete GNSS network’ By De Guidi et al', John Browning, 23 May 2017 Printer-friendly Version 
AC1: 'Reply to the comments', Giorgio De Guidi, 13 Jun 2017 Printer-friendly Version Supplement 
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (further review by Editor) (02 Aug 2017) by Filippos Vallianatos  
AR by Giorgio De Guidi on behalf of the Authors (12 Aug 2017)  Author's response  Manuscript
ED: Publish subject to technical corrections (03 Sep 2017) by Filippos Vallianatos  
AR by Giorgio De Guidi on behalf of the Authors (21 Sep 2017)  Author's response  Manuscript
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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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