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On 24 August 2016 a strong earthquake (Mw = 6.0) affected central Italy and an intense seismic sequence started. Field observations,\udDInSAR (Differential INterferometry Synthetic-Aperture Radar) analyses and preliminary\udfocal mechanisms, as well as the distribution of aftershocks, suggested the\udreactivation of the northern sector of the Laga fault, the southern part of\udwhich was already rebooted during the 2009 L'Aquila sequence, and of the\udsouthern segment of the Mt Vettore fault system (MVFS). Based on this\udpreliminary information and following the stress-triggering concept (Stein,\ud1999; Steacy et al., 2005), we tentatively identified a potential fault zone\udthat is very vulnerable to future seismic events just north of the earlier\udepicentral area. Accordingly, we planned a local geodetic network consisting\udof five new GNSS (Global Navigation Satellite System) stations located a few\udkilometres away from both sides of the MVFS. This network was devoted to\udworking out, at least partially but in some detail, the possible northward\udpropagation of the crustal network ruptures. The building of the stations and\uda first set of measurements were carried out during a first campaign\ud(30 September and 2 October 2016). On 26 October 2016, immediately north of\udthe epicentral area of the 24 August event, another earthquake (Mw = 5.9) occurred, followed 4 days later (30 October) by the main shock\ud(Mw = 6.5) of the whole 2016 summer–autumn seismic sequence. Our\udlocal geodetic network was fully affected by the new events and therefore we\udperformed a second campaign soon after (11–13 November 2016). In this brief\udnote, we provide the results of our geodetic measurements that registered the\udco-seismic and immediately post-seismic deformation of the two major October\udshocks, documenting in some detail the surface deformation close to the fault\udtrace. We also compare our results with the available surface deformation\udfield of the broader area, obtained on the basis of the DInSAR technique, and\udshow an overall good fit

natural hazards and earth system sciences

Brief communication: Co-seismic displacement on 26 and 30 October 2016 (&amp;lt;i&amp;gt;M&amp;lt;/i&amp;gt;&amp;lt;sub&amp;gt;w&amp;lt;/sub&amp;gt; = 5.9 and 6.5) – earthquakes in central Italy from the analysis of a local GNSS network