Crustal heterogeneities and complexities of fault processes

In this work we study the relation between crustal heterogeneities and complexities in fault processes. The first kind of heterogeneity considered involves the concept of asperity. The presence of an asperity in the hypocentral region of the M = 6.5 earthquake of June 17-th, 2000 in the South Iceland Seismic Zone was invoked to explain the change of seismicity pattern before and after the mainshock: in particular, the spatial distribution of foreshock epicentres trends NW while the strike of the main fault is N 7◦ E and aftershocks trend accordingly; the foreshock depths were typically deeper than average aftershock depths. A model is devised which simulates the presence of an asperity in terms of a spherical inclusion, within a softer elastic medium in a transform domain with a deviatoric stress field imposed at remote distances (compressive NE − SW, tensile NW − SE). An isotropic compressive stress component is induced outside the asperity, in the direction of the compressive stress axis, and a tensile component in the direction of the tensile axis; as a consequence, fluid flow is inhibited in the compressive quadrants while it is favoured in tensile quadrants. Within the asperity the isotropic stress vanishes but the deviatoric stress increases substantially, without any significant change in the principal stress directions. Hydrofracture processes in the tensile quadrants and viscoelastic relaxation at depth may contribute to lower the effective rigidity of the medium surrounding the asperity. According to the present model, foreshocks may be interpreted as induced, close to the brittle-ductile transition, by high pressure fluids migrating upwards within the tensile quadrants; this process increases the deviatoric stress within the asperity which eventually fails, becoming the hypocenter of the mainshock, on the optimally oriented fault plane. In the second part of our work we study the complexities induced in fault processes by the layered structure of the crust. In the first model proposed we study the case in which fault bending takes place in a shallow layer. The problem can be addressed in terms of a deep vertical planar crack, interacting with a shallower inclined planar crack. An asymptotic study of the singular behaviour of the dislocation density at the interface reveals that the density distribution has an algebraic singularity at the interface of degree ω between -1 and 0, depending on the dip angle of the upper crack section and on the rigidity contrast between the two media. From the welded boundary condition at the interface between medium 1 and 2, a stress drop discontinuity condition is obtained which can be fulfilled if the stress drop in the upper medium is lower than required for a planar trough-going surface: as a corollary, a vertically dipping strike-slip fault at depth may cross the interface with a sedimentary layer, provided that the shallower section is suitably inclined (fault "refraction"); this results has important implications for our understanding of the complexity of the fault system in the SISZ; in particular, we may understand the observed offset of secondary surface fractures with respect to the strike direction of the seismic fault. The results of this model also suggest that further fractures can develop in the opposite quadrant and so a second model describing fault branching in the upper layer is proposed. As the previous model, this model can be applied only when the stress drop in the shallow layer is lower than the value prescribed for a vertical planar crack surface. Alternative solutions must be considered if the stress drop in the upper layer is higher than in the other layer, which may be the case when anelastic processes relax deviatoric stress in layer 2. In such a case one through-going crack cannot fulfil the welded boundary conditions and unwelding of the interface may take place. We have solved this problem within the theory of fracture mechanics, employing the boundary element method. The fault terminates against the interface in a T-shaped configuration, whose segments interact among each other: the lateral extent of the unwelded surface can be computed in terms of the main fault parameters and the stress field resulting in the shallower layer can be modelled. A wide stripe of high and nearly uniform shear stress develops above the unwelded surface, whose width is controlled by the lateral extension of unwelding. Secondary shear fractures may then open within this stripe, according to the Coulomb failure criterion, and the depth of open fractures opening in mixed mode may be computed and compared with the well studied fault complexities observed in the field. In absence of the T-shaped decollement structure, stress concentration above the seismic fault would be difficult to reconcile with observations, being much higher and narrower.

Climate impact studies of sediment transport on the Adriatic coastal zone

The study of the impact of climate change on the environment has been based, until very recently, on an global approach, whose interest from a local point of view is very limited. This thesis, on the contrary, has treated the study of the impact of climate change in the Adriatic Sea basin following a twofold strategy of regionalization and integration of numerical models in order to reproduce the present and future scenarios of the system through a more and more realistic and solid approach. In particular the focus of the study was on the impact on the physical environment and on the sediment transport in the basin. This latter is a very new and original issue, to our knowledge still uninvestigated. The study case of the coastal area of Montenegro was particularly studied, since it is characterized by an important supply of sediment through the Buna/Bojana river, second most important in the Adriatic basin in terms of flow. To do this, a methodology to introduce the tidal processes in a baroclinic primitive equations Ocean General Circulation Model was applied and tidal processes were successfully reproduced in the Adriatic Sea, analyzing also the impacts they have on the mean general circulation, on salt and heat transport and on mixing and stratification of the water column in the different seasons of the year. The new hydrodynamical model has been further coupled with a wave model and with a river and sea sediment transport model, showing good results in the reproduction of sediment transport processes. Finally this complex coupled platform was integrated in the period 2001-2030 under the A1B scenario of IPCC, and the impact of climate change on the physical system and on sediment transport was preliminarily evaluated.

Deep geometry of subduction below the Andean belt of Colombia as revealed by seismic tomography

In this study new tomographic models of Colombia were calculated. I used the seismicity recorded by the Colombian seismic network during the period 2006-2009. In this time period, the improvement of the seismic network yields more stable hypocentral results with respect to older data set and allows to compute new 3D Vp and Vp/Vs models. The final dataset consists of 10813 P- and 8614 S-arrival times associated to 1405 earthquakes. Tests with synthetic data and resolution analysis indicate that velocity models are well constrained in central, western and southwestern Colombia to a depth of 160 km; the resolution is poor in the northern Colombia and close to Venezuela due to a lack of seismic stations and seismicity. The tomographic models and the relocated seismicity indicate the existence of E-SE subducting Nazca lithosphere beneath central and southern Colombia. The North-South changes in Wadati-Benioff zone, Vp & Vp/Vs pattern and volcanism, show that the downgoing plate is segmented by slab tears E-W directed, suggesting the presence of three sectors. Earthquakes in the northernmost sector represent most of the Colombian seimicity and concentrated on 100-170 km depth interval, beneath the Eastern Cordillera. Here a massive dehydration is inferred, resulting from a delay in the eclogitization of a thickened oceanic crust in a flat-subduction geometry. In this sector a cluster of intermediate-depth seismicity (Bucaramanga Nest) is present beneath the elbow of the Eastern Cordillera, interpreted as the result of massive and highly localized dehydration phenomenon caused by a hyper-hydrous oceanic crust. The central and southern sectors, although different in Vp pattern show, conversely, a continuous, steep and more homogeneous Wadati-Benioff zone with overlying volcanic areas. Here a "normalthickened" oceanic crust is inferred, allowing for a gradual and continuous metamorphic reactions to take place with depth, enabling the fluid migration towards the mantle wedge.

Le Zone Franche Urbane: Mercato europeo e Ordinamenti tributari

Lo studio delle Zone Franche Urbane all’interno del Diritto tributario europeo non ha potuto prescindere da una introduttiva delimitazione del lavoro, capace di distinguere le diverse tipologie di zone franche esistenti nei Paesi intra/extra Ue. Attraversando i casi-studio di Madeira, delle Azzorre, fino alla istituenda Zona Franca di Bruxelles, Zone d’Economie Urbaine stimulée (ZEUS), si è giunti alla constatazione dell’assenza di una definizione di Zona Franca Urbana: analizzando le esperienze normative vissute in Francia e in Italia, si è potuto tratteggiare il profilo territoriale, soggettivo e oggettivo del sistema agevolativo rivolto al recupero delle aree urbane degradate. La funzione strumentale della fiscalità, esplicitata per mezzo delle ZFU, ha condotto ad una verifica di diritto interno per controllare la legittimità delle scelte nazionali in ragione dei principi costituzionali nazionali, come anche una di diritto europeo per evitare che le scelte nazionali, anche se legittime sul piano interno, possano per gli stessi effetti incentivanti alle attività d'impresa presentarsi come una forma territoriale di aiuti di Stato fiscali. Evidenziando il rapporto tra le ZFU e il Mercato europeo si è voluto, da un lato, effettuare una ricostruzione sistemica necessaria per un’interpretazione delle ZFU che metta in luce le componenti di tale strumento orientate al perseguimento di un interesse socioeconomico, che in prima battuta generi una contraddizione, una deroga ai principi costituzionali e comunitari, per poi “sciogliersi” in una coerente applicazione degli stessi; dall’altro, tentare di elevare le ZFU a misura sistemica dell’Ordinamento europeo. Si è svolto, infine, un ragionamento in termini di federalismo fiscale con riferimento alle ZFU, trovando una adeguata collocazione nel percorso di devoluzione intrapreso dal legislatore nazionale, avendo quali interlocutori privilegiati le Regioni a Statuto Speciale.

La detenzione amministrativa degli stranieri. Nuove frontiere in materia di liberta' personale

La detenzione amministrativa degli stranieri, pur condividendo il carattere tipicamente afflittivo e stigmatizzante delle pene, non si fonda sulla commissione di un reato e non gode delle medesime garanzie previste dal sistema della giustizia penale. Nel nostro ordinamento l’inadeguatezza della legislazione, l’ampio margine di discrezionalità rimesso all’autorità di pubblica sicurezza, nonché il debole potere di sindacato giurisdizionale rimesso all’autorità giudiziaria, raggiungono il loro apice problematico nell’ambito delle pratiche di privazione della libertà personale che hanno per destinatari gli stranieri maggiormente vulnerabili, ossia quelli appena giunti sul territorio e il cui status giuridico non è ancora stato accertato (c.d. situazione di pre-admittance). E’ proprio sulla loro condizione che il presente lavoro si focalizza maggiormente. Le detenzioni de facto degli stranieri in condizione di pre-admittance sono analizzate, nel primo capitolo, a partire dal “caso Lampedusa”, descritto alla luce dell’indagine sul campo condotta dall’Autrice. Nel secondo capitolo viene ricostruito lo statuto della libertà personale dello straniero sulla base dei principi costituzionali e, nel terzo capitolo, sono analizzati i principi che informano il diritto alla libertà personale nell’ambito delle fonti sovranazionali, con particolare riferimento al diritto dell’Unione Europea e al sistema della Convenzione Europea dei Diritti dell’Uomo. Sulla scorta dei principi indagati, nel quarto capitolo è tracciata l’evoluzione legislativa in materia di detenzione amministrativa dello straniero in Italia e, nel quinto capitolo, è approfondito il tema dei Centri dell’immigrazione e delle regole che li disciplinano. Nelle conclusioni, infine, sono tirate le fila del percorso tracciato, attraverso la valutazione degli strumenti di tutela in grado di prevenire le pratiche di privazione della libertà informali e di garantire uno standard minimo nella tutela della libertà individuale, anche nelle zone di frontiera del nostro ordinamento.