Estimating crustal deformation from geodetic data

By the end of the 19th century, geodesy has contributed greatly to the knowledge of regional tectonics and fault movement through its ability to measure, at sub-centimetre precision, the relative positions of points on the Earth’s surface. Nowadays the systematic analysis of geodetic measurements in active deformation regions represents therefore one of the most important tool in the study of crustal deformation over different temporal scales [e.g., Dixon, 1991]. This dissertation focuses on motion that can be observed geodetically with classical terrestrial position measurements, particularly triangulation and leveling observations. The work is divided into two sections: an overview of the principal methods for estimating longterm accumulation of elastic strain from terrestrial observations, and an overview of the principal methods for rigorously inverting surface coseismic deformation fields for source geometry with tests on synthetic deformation data sets and applications in two different tectonically active regions of the Italian peninsula. For the long-term accumulation of elastic strain analysis, triangulation data were available from a geodetic network across the Messina Straits area (southern Italy) for the period 1971 – 2004. From resulting angle changes, the shear strain rates as well as the orientation of the principal axes of the strain rate tensor were estimated. The computed average annual shear strain rates for the time period between 1971 and 2004 are γ˙1 = 113.89 ± 54.96 nanostrain/yr and γ˙2 = -23.38 ± 48.71 nanostrain/yr, with the orientation of the most extensional strain (θ) at N140.80° ± 19.55°E. These results suggests that the first-order strain field of the area is dominated by extension in the direction perpendicular to the trend of the Straits, sustaining the hypothesis that the Messina Straits could represents an area of active concentrated deformation. The orientation of θ agree well with GPS deformation estimates, calculated over shorter time interval, and is consistent with previous preliminary GPS estimates [D’Agostino and Selvaggi, 2004; Serpelloni et al., 2005] and is also similar to the direction of the 1908 (MW 7.1) earthquake slip vector [e.g., Boschi et al., 1989; Valensise and Pantosti, 1992; Pino et al., 2000; Amoruso et al., 2002]. Thus, the measured strain rate can be attributed to an active extension across the Messina Straits, corresponding to a relative extension rate ranges between < 1mm/yr and up to ~ 2 mm/yr, within the portion of the Straits covered by the triangulation network. These results are consistent with the hypothesis that the Messina Straits is an important active geological boundary between the Sicilian and the Calabrian domains and support previous preliminary GPS-based estimates of strain rates across the Straits, which show that the active deformation is distributed along a greater area. Finally, the preliminary dislocation modelling has shown that, although the current geodetic measurements do not resolve the geometry of the dislocation models, they solve well the rate of interseismic strain accumulation across the Messina Straits and give useful information about the locking the depth of the shear zone. Geodetic data, triangulation and leveling measurements of the 1976 Friuli (NE Italy) earthquake, were available for the inversion of coseismic source parameters. From observed angle and elevation changes, the source parameters of the seismic sequence were estimated in a join inversion using an algorithm called “simulated annealing”. The computed optimal uniform–slip elastic dislocation model consists of a 30° north-dipping shallow (depth 1.30 ± 0.75 km) fault plane with azimuth of 273° and accommodating reverse dextral slip of about 1.8 m. The hypocentral location and inferred fault plane of the main event are then consistent with the activation of Periadriatic overthrusts or other related thrust faults as the Gemona- Kobarid thrust. Then, the geodetic data set exclude the source solution of Aoudia et al. [2000], Peruzza et al. [2002] and Poli et al. [2002] that considers the Susans-Tricesimo thrust as the May 6 event. The best-fit source model is then more consistent with the solution of Pondrelli et al. [2001], which proposed the activation of other thrusts located more to the North of the Susans-Tricesimo thrust, probably on Periadriatic related thrust faults. The main characteristics of the leveling and triangulation data are then fit by the optimal single fault model, that is, these results are consistent with a first-order rupture process characterized by a progressive rupture of a single fault system. A single uniform-slip fault model seems to not reproduce some minor complexities of the observations, and some residual signals that are not modelled by the optimal single-fault plane solution, were observed. In fact, the single fault plane model does not reproduce some minor features of the leveling deformation field along the route 36 south of the main uplift peak, that is, a second fault seems to be necessary to reproduce these residual signals. By assuming movements along some mapped thrust located southward of the inferred optimal single-plane solution, the residual signal has been successfully modelled. In summary, the inversion results presented in this Thesis, are consistent with the activation of some Periadriatic related thrust for the main events of the sequence, and with a minor importance of the southward thrust systems of the middle Tagliamento plain.

La produzione cinematografica nel sistema economico-industriale italiano tra il 1908 e il 1914. Il caso della Milano Films

La tesi riguarda il processo evolutivo dell’industria cinematografica italiana dal momento della sua prima espansione (biennio1906-1908) fino allo scoppio della I guerra mondiale. In particolare il lavoro si è concentrato sulle vicende societarie e produttive di una delle maggiori case di produzioni attive in Italia nel periodo preso in esame: la Milano Films. Le ricerche relative alla società milanese hanno portato al rinvenimento di una cospicua quantità di documenti finora inediti, attraverso i quali è stato possibile ricostruire nel dettaglio la vicenda societaria e produttiva della casa di produzione. Lo studio ha inoltre analizzato le peculiarità specifiche che, tra il 1908 e il 1914, contraddistinguono la cinematografia italiana dal punto di vista degli assetti societari e finanziari, dell’organizzazione produttiva, delle strategie distributive e commerciali, attraverso un costante confronto con il complessivo quadro industriale italiano coevo e, in particolare, con quei settori produttivi considerati più all’avanguardia nei primi anni del Novecento.

La strage di Ustica nell'opinione pubblica italiana (1980-1992): analisi di un caso politico e mediatico

Questa ricerca indaga come il “caso Ustica” si è articolato nell’opinione pubblica italiana negli anni compresi tra il 1980 e il 1992. Con l'espressione “caso Ustica” ci si riferisce al problema politico determinato dalle vicende legate all’abbattimento dell’aereo civile DC-9 dell’Itavia, avvenuto il 27 giugno 1980 in circostanze che, come noto, furono chiarite solamente a distanza di molti anni dal fatto. L’analisi intende cogliere le specificità del processo che ha portato la vicenda di Ustica ad acquisire rilevanza politica nell’ambito della sfera pubblica italiana, in particolare prendendo in considerazione il ruolo svolto dall’opinione pubblica in un decennio, quale quello degli anni ’80 e dei primi anni ’90 italiani, caratterizzato da una nuova centralità dei media rispetto alla sfera politica. Attraverso l’analisi di un’ampia selezione di fonti a stampa (circa 1500 articoli dei principali quotidiani italiani e circa 700 articoli tratti dagli organi dei partiti politici italiani) si sono pertanto messe in luce le dinamiche mediatiche e politiche che hanno portato alla tematizzazione di una vicenda che era rimasta fino al 1986 totalmente assente dall’agenda politica nazionale. L’analisi delle fonti giudiziarie ha permesso inoltre di verificare come la politicizzazione del caso Ustica, costruita intorno alla tensione opacità/trasparenza del potere politico e all’efficace quanto banalizzante paradigma delle “stragi di Stato”, sia risultata funzionale al raggiungimento, dopo il 1990, dei primi elementi di verità sulla tragedia e all’ampiamento del caso a una dimensione internazionale.