Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7149
AuthorsSepe, V.* 
Brandi, Gi.* 
De Martino, P.* 
Dolce, M.* 
Obrizzo, F.* 
Pingue, F.* 
Tammaro, U.* 
TitleS.A.G.NET: Rete GPS dell'Appennino meridionale.
Issue DateOct-2009
Series/Report no.76/(2009)
URIhttp://hdl.handle.net/2122/7149
KeywordsGPS, Matese, SAGNet
Subject Classification04. Solid Earth::04.03. Geodesy::04.03.07. Satellite geodesy 
AbstractThe Matese carbonatic massive occupies the northernmost part of the campanian Apennine while Sannio mounts, located to the East of massive, consists primarily of quaternary deposits and represent the area of Apennine chain degrading to East towards the Bradanica foredeep. The area was affected in historical time by several destructive earthquakes. The first ground deformation studies in this area started from 1990-2000 with the definition of geodetic networks, covering all or part of the massive Matese, with the aim of evaluating seismogenic sources responsible for the seismicity of the area. In 2002, a careful inspection of the existing GPS benchmarks was carried out; those which had a good state of preservation and a good level of reliability were included into a new geodetic Matese network, consisting of 38 3D benchmarks. Several surveys were conducted in 2000, 2002 and 2004,with the aim of defining the strain field, defined by plano-altimetric components. In 2005, an intensive work of gathering and validating available data started, integrating data collected by previous surveys with those collected during the new survey carried out in 2006. This work describes in detail the various stages of implementing the final network S.A.G.NET, whose geometry was also bound to the distribution of the known seismogenic sources present in the area. We also show the first results obtained from data collected from2000 to 2006 and the resulting kinematic model for this area.
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