Numerical models of trench migration for lateral heterogeneous subducting plates

The aim of this Thesis is to investigate the effect of heterogeneities within the subducting plate on the dynamics of subduction. In particular, I study the motion of the trench for oceanic and continental subduction, first, separately, and, then, together in the same system to understand how they interact. The understanding of these features is fundamental to reconstruct the evolution of complex subduction zones, such as the Central Mediterranean. For this purpose, I developed 2D and 3D numerical models of oceanic and continental subduction where the rheological, geometrical and compositional properties of the plates are varied. In these models, the trench and the overriding plate move self-consistently as a function of the dynamics of the system. The effect of continental subduction on trench migration is largely investigated. Results from a parametric study showed that despite different rheological properties of the plates, all models with a uniform continental crust share the same kinematic behaviour: the trench starts to advance once the continent arrives at the subduction zone. Hence, the advancing mode in continental collision scenarios is at least partly driven by an intrinsic feature of the system. Moreover, the presence of a weak lower crust within the continental plate can lead to the occurrence of delamination. Indeed, by changing the viscosity of the lower crust, both delamination and slab detachment can occur. Delamination is favoured by a low viscosity value of the lower crust, because this makes the mechanical decoupling easier between crust and lithospheric mantle. These features are observed both in 2D and 3D models, but the numerical results of the 3D models also showed that the rheology of the continental crust has a very strong effect on the dynamics of the whole system, since it influences not only the continental part of plate but also the oceanic sides.

Caratteristiche ortopediche-ortodontiche in pazienti affetti da Sindrome di Nooan

La sindrome di Noonan (SN) è una patologia a trasmissione autosomica dominante caratterizzata da bassa statura, difetti cardiaci congeniti, dismorfia facciale. In letteratura sono stati pubblicati pochi case reports riguardanti le condizioni orali-facciali in pazienti affetti da SN. Obiettivo. Individuare patologie di pertinenza ortopedico-ortodontica caratteristiche della sindrome utilizzando un campione di pazienti con diagnosi di SN. Metodi. Un gruppo di 10 pazienti affetti da SN è stato sottoposto a esame obiettivo extraorale ed intraorale, ortopantomografia, teleradiografia latero-laterale, impronte delle arcate dentarie. Le misurazioni sulle TLL sono state effettuate sulla base dell'analisi MBT; i valori palatali provengono dai modelli di studio dell’arcata superiore. È stata utilizzato il test t-Student per mettere a confronto il gruppo di studio e il gruppo di controllo riguardo le misure cefalometriche e i valori palatali. Risultati. Nel gruppo di studio sono state rilevate anomalie di numero (un dente deciduo soprannumerario e una agenesia di un dente permanente). Il test t-Student rivela differenze statisticamente significative per 7 variabili cefalometriche su 13 e per 2 variabili palatali. Conclusioni. Basandosi su questo studio è possibile concludere che i pazienti con SN mostrano II classe scheletrica di tipo mandibolare, crescita iperdivergente, tendenza al morso aperto scheletrico, palatoversione degli incisivi superiori, palato stretto. Questi risultati possono fornire informazioni utili sia per la diagnosi di SN sia per la pianificazione del corretto trattamento ortodontico.

Lateral spreading and associated slope processes in fractured rock slabs

Landslides of the lateral spreading type, involving brittle geological units overlying ductile terrains, are a common occurrence in the sandstone and limestone plateaux of the northern Apennines of Italy. These instability phenomena can become particularly risky, when historical towns and cultural heritage sites built on the top of them are endangered. Neverthless, the mechanisms controlling the developing of related instabilities, i.e. toppling and rock falls, at the edges of rock plateaux are not fully understood yet. In addition, the groundwater flow path developing at the contact between the more permeable units, i.e. the jointed rock slab, and the relatively impermeable clay-rich units have not been already studied in details, even if they may play a role in this kind of instability processes, acting as eventual predisposing and/or triggering factors. Field survey, Terrestrial Laser Scanner and Close Range Photogrammetry techniques, laboratory tests on the involved materials, hydrogeological monitoring and modelling, displacements evaluation and stability analysis through continuum and discontinuum numerical codes have been performed on the San Leo case study, with the aim to bring further insights for the understanding and the assessment of the slope processes taking place in this geological context. The current research permitted to relate the aquifer behaviour of the rocky slab to slope instability processes. The aquifer hosted in the fractured slab leads to the development of perennial and ephemeral springs at the contact between the two units. The related piping erosion phenomena, together with slope processes in the clay-shales led to the progressive undermining of the slab. The cliff becomes progressively unstable due to undermining and undergoes large-scale landslides due to fall or topple.