• journal_title：Italian Journal of Geosciences
• Contributor：Andrea Manconi ; Daniele Giordan ; Paolo Allasia ; Marco Baldo ; Giorgio Lollino
• Publisher：The Electrochemical Society
• Date：2012-10-01
• Format：text/html
• Language：en
• Identifier：10.3301/IJG.2012.13
• journal_abbrev：Italian Journal of Geosciences
• issn：2038-1719
• volume：131
• issue：3
• firstpage：403
• section：Articles

We present the results of a continuous monitoring of the surface displacements following the April 6^th 2009 L’Aquila earthquake in the area of Paganica village, central Italy. We considered 3-dimensional displacements measured via Robotized Total Station (RTS) installed the April 24^th 2009 in the area of Paganica village (ca. 5 km ENE from L’Aquila town), where a water pipeline located within the urban centre was severely damaged. The monitoring system was set up in order to reveal potential post-seismic displacements that could cause further damages to the water pipeline. The RTS ran continuously for about one year, with sampling rates varying from 2 to 4 hours, and measured displacements at selected point targets. The revealed surface displacements are in agreement with the results of a DInSAR time series analysis relevant to satellite SAR data acquired over the same area and time period by the Italian satellite’s constellation Cosmo-SkyMed. Moreover, despite the RTS monitored area was spatially limited, our analyses provide detailed feedbacks on fault processes following the L’Aquila earthquake. The aftershocks temporal evolution and the post-seismic displacements measured in the area show very similar exponential decays over time, with estimated cross-correlation coefficients values ranging from 0.86 to 0.97. The results of our time dependent modelling of the RTS measurements suggest that L’Aquila earthquake post-seismic displacements were dominated by the fault afterslip and/or fault creep, while poroelastic and viscoelastic processes had negligible effects.