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.

Provenienza dei sedimenti arenitici nel bacino di Tracia (eo-oligocene, Turchia nord-occidentale e Grecia nord-orientale)

The Thrace Basin is the largest and thickest Tertiary sedimentary basin of the eastern Balkans region and constitutes an important hydrocarbon province. It is located between the Rhodope-Strandja Massif to the north and west, the Marmara Sea and Biga Peninsula to the south, and the Black Sea to the est. It consists of a complex system of depocenters and uplifts with very articulate paleotopography indicated by abrupt lateral facies variations. Its southeastern margin is widely deformed by the Ganos Fault, a segment of the North Anatolian strike-slip fault system . Most of the Thrace Basin fill ranges from the Eocene to the Late Oligocene. Maximum total thickness, including the Neogene-Quaternary succession, reaches 9.000 meters in a few narrow depocenters. This sedimentary succession consists mainly of basin plain turbiditic deposits with a significant volcaniclastic component which evolves upwards to shelf deposits and continental facies, with deltaic bodies prograding towards the basin center in the Oligocene. This work deals with the provenance of Eocene-Oligocene clastic sediments of the southern and western part of Thrace Basin in Turkey and Greece. Sandstone compositional data (78 gross composition analyses and 40 heavy minerals analyses) were used to understand the change in detrital modes which reflects the provenance and geodinamic evolution of the basin. Samples were collected at six localities, which are from west to est: Gökçeada, Gallipoli and South-Ganos (south of Ganos Fault), Alexandroupolis, Korudağ and North-Ganos (north of Ganos Fault). Petrologic (framework composition and heavy-mineral analyses) and stratigraphic-sedimentologic data, (analysis of sedimentologic facies associations along representative stratigraphic sections, paleocurrents) allowed discrimination of six petrofacies; for each petrofacies the sediment dispersal system was delineated. The Thrace Basin fill is made mainly of lithic arkoses and arkosic litharenites with variable amount of low-grade metamorphic lithics (also ophiolitic), neovolcanic lithics, and carbonate grains (mainly extrabasinal). Picotite is the most widespread heavy mineral in all petrofacies. Petrological data on analyzed successions show a complex sediment dispersal pattern and evolution of the basin, indicating one principal detrital input from a source area located to the south, along both the İzmir-Ankara and Intra-Pontide suture lines, and a possible secondary source area, represented by the Rhodope Massif to the west. A significant portion of the Thrace Basin sediments in the study area were derived from ophiolitic source rocks and from their oceanic cover, whereas epimetamorphic detrital components came from a low-grade crystalline basement. An important penecontemporaneous volcanic component is widespread in late Eocene-Oligocene times, indicating widespread post-collisional (collapse?) volcanism following the closure of the Vardar ocean. Large-scale sediment mass wasting from south to north along the southern margin of the Thrace Basin is indicated (i) in late Eocene time by large olistoliths of ophiolites and penecontemporaneous carbonates, and (ii) in the mid-Oligocene by large volcaniclastic olistoliths. The late Oligocene paleogeographic scenario was characterized by large deltaic bodies prograding northward (Osmancik Formation). This clearly indicates that the southern margin of the basin acted as a major sediment source area throughout its Eocene-Oligocene history. Another major sediment source area is represented by the Rhodope Massif, in particolar the Circum-Rhodopic belt, especially for plutonic and metamorphic rocks. Considering preexisting data on the petrologic composition of Thrace Basin, silicilastic sediments in Greece and Bulgaria (Caracciolo, 2009), a Rhodopian provenance could be considered mostly for areas of the Thrace Basin outside our study area, particularly in the northern-central portions of the basin. In summary, the most important source area for the sediment of Thrace Basin in the study area was represented by the exhumed subduction-accretion complex along the southern margin of the basin (Biga Peninsula and western-central Marmara Sea region). Most measured paleocurrent indicators show an eastward paleoflow but this is most likely the result of gravity flow deflection. This is possible considered a strong control due to the east-west-trending synsedimentary transcurrent faults which cuts the Thrace Basin, generating a series of depocenters and uplifts which deeply influenced sediment dispersal and the areal distribution of paleoenvironments. The Thrace Basin was long interpreted as a forearc basin between a magmatic arc to the north and a subduction-accretion complex to the south, developed in a context of northward subduction. This interpretation was challenged by more recent data emphasizing the lack of a coeval magmatic arc in the north and the interpretation of the chaotic deposit which outcrop south of Ganos Fault as olistoliths and large submarine slumps, derived from the erosion and sedimentary reworking of an older mélange unit located to the south (not as tectonic mélange formed in an accretionary prism). The present study corroborates instead the hypothesis of a post-collisional origin of the Thrace Basin, due to a phase of orogenic collapse, which generated a series of mid-Eocene depocenters all along the İzmir-Ankara suture (following closure of the Vardar-İzmir-Ankara ocean and the ensuing collision); then the slab roll-back of the remnant Pindos ocean played an important role in enhancing subsidence and creating additional accommodation space for sediment deposition.

Neuropeptide und die Regulation des Kohlenhydratstoffwechsels im Fettkörper der Argentinischen Schabe (Blaptica dubia)

Trehalose ist der Hauptblutzucker in der Hämolymphe der meisten Insekten. Trehalose wird im Fettkörper synthetisiert, dem wichtigsten Organ des Intermediärstoffwechsels bei Insekten. Wie die Homöostase des Blutzuckers reguliert wird, ist nicht vollständig geklärt. Die Produktion von Trehalose erfordert eine grundlegende Umschaltung im Stoffwechsel des Fettkörpers, die mehrere wichtige Stoffwechselwege betrifft, so dass die Fettkörperzellen (Trophocyten) von der Speicherung und Katabolisierung von Zucker zur Mobilisierung von Reservestoffen (Glykogen, Fett, Protein) und Trehalosesynthese umschalten. Am Fettkörper und isolierten Trophocyten der Argentinischen Schabe (Blaptica dubia) wurden Stoffwechseleffekte und Elemente der Signalkette des hypertrehalosämischen Hormons Bld HrTH untersucht. Inkubation isolierter Fettkörperloben mit Bld HrTH verringerte innerhalb von 60 min den Glykogengehalt (um 13,4 %) und steigerte die Konzentration der Hexosephosphate Glucose-6-phosphat und Fructose-6-phosphat, die Substrat sowohl für die Trehalosesynthese als auch für die Glykolyse sind. Pyruvat, Glycerin-3-phosphat, Citrat und insbesondere Fructose-1,6-bisphosphat (+750 %) waren ebenfalls erhöht. Der Glykolyseaktivator/Gluconeogeneseinhibitor Fructose-2,6-bisphosphat wird durch Bld HrTH vermindert. Da Trehalosesynthese und Glykolyse um dieselben Substrate (Glucosephosphate) konkurrieren, fördert der hormoninduzierte Abfall des Glykolyseaktivators Fructose-2,6-bisphosphat die Trehalogenese.Es ist gelungen, Trophocyten zu isolieren und die Signaltransduktion von Bld HrTH an einheitlichen Zellen und auch an Einzelzellen zu studieren. Hauptziel dieser Arbeit war es, die Funktion von Ca2+ im Signalweg des Bld HrTH genauer zu untersuchen. Die isolierten Zellen reagierten auf das Neuropeptid mit einer deutlichen Steigerung der Trehalosesynthese (+133,7 %) und einer Senkung des Fructose-2,6-bisphosphat-Gehaltes (-30,2 %). Sie bieten somit ein geeignetes System zur Untersuchung der Wirkungsmechanismen von Bld HrTH auf zellulärem Niveau. Ca2+ aus dem Extrazellulärraum und aus intrazellulären Speichern spielen bei der Signaltransduktion eine Rolle. Während extrazelluläres Ca2+ insbesondere für die Senkung des Fructose-2,6-bisphosphat-Gehaltes wichtig war, wurde Ca2+ aus zellulären Speichern insbesondere für die Trehalosesynthese benötigt, wobei sich jedoch beide Wege wechselseitig beeinflussen. Erstmals konnten an isolierten Trophocyten Änderungen von Ca2+ mikrofluorometrisch an Einzelzellen studiert werden. Das hypertrehalosämische Hormon ruft einen schnellen und starken Anstieg der intrazellulären Ca2+-Konzentration ([Ca2+]i) hervor. Die Untersuchungen deuten auf einen Signalweg über IP3 und Diacylglycerin hin, entsprechend der Phosphoinositidkaskade. Eine Beteiligung des biogenen Amins Octopamin, von cAMP oder von Stickstoffmonoxid (NO) an der Signaltransduktion scheint hingegen unwahrscheinlich. Der Zuckergehalt im Medium scheint ebenfalls auf die Trehalogenese zu wirken. Bei hohen Konzentrationen von Glucose oder Trehalose wurde eine Hemmung der Trehalosesynthese beobachtet, die als Rückkopplungshemmung gedeutet werden kann. Bei Hunger wird das im Fettkörper gespeicherte Glykogen stark reduziert. Außerdem scheint die Zahl der symbiontischen Mikroorganismen in den Mycetocyten verringert.

Tectonic geomorphology and active strain of the Northern Apennines mountain front

The Northern Apennines (NA) chain is the expression of the active plate margin between Europe and Adria. Given the low convergence rates and the moderate seismic activity, ambiguities still occur in defining a seismotectonic framework and many different scenarios have been proposed for the mountain front evolution. Differently from older models that indicate the mountain front as an active thrust at the surface, a recently proposed scenario describes the latter as the frontal limb of a long-wavelength fold (> 150 km) formed by a thrust fault tipped around 17 km at depth, and considered as the active subduction boundary. East of Bologna, this frontal limb is remarkably very straight and its surface is riddled with small, but pervasive high- angle normal faults. However, west of Bologna, some recesses are visible along strike of the mountain front: these perturbations seem due to the presence of shorter wavelength (15 to 25 km along strike) structures showing both NE and NW-vergence. The Pleistocene activity of these structures was already suggested, but not quantitative reconstructions are available in literature. This research investigates the tectonic geomorphology of the NA mountain front with the specific aim to quantify active deformations and infer possible deep causes of both short- and long-wavelength structures. This study documents the presence of a network of active extensional faults, in the foothills south and east of Bologna. For these structures, the strain rate has been measured to find a constant throw-to-length relationship and the slip rates have been compared with measured rates of erosion. Fluvial geomorphology and quantitative analysis of the topography document in detail the active tectonics of two growing domal structures (Castelvetro - Vignola foothills and the Ghiardo plateau) embedded in the mountain front west of Bologna. Here, tilting and river incision rates (interpreted as that long-term uplift rates) have been measured respectively at the mountain front and in the Enza and Panaro valleys, using a well defined stratigraphy of Pleistocene to Holocene river terraces and alluvial fan deposits as growth strata, and seismic reflection profiles relationships. The geometry and uplift rates of the anticlines constrain a simple trishear fault propagation folding model that inverts for blind thrust ramp depth, dip, and slip. Topographic swath profiles and the steepness index of river longitudinal profiles that traverse the anti- clines are consistent with stratigraphy, structures, aquifer geometry, and seismic reflection profiles. Available focal mechanisms of earthquakes with magnitude between Mw 4.1 to 5.4, obtained from a dataset of the instrumental seismicity for the last 30 years, evidence a clear vertical separation at around 15 km between shallow extensional and deeper compressional hypocenters along the mountain front and adjacent foothills. In summary, the studied anticlines appear to grow at rates slower than the growing rate of the longer- wavelength structure that defines the mountain front of the NA. The domal structures show evidences of NW-verging deformation and reactivations of older (late Neogene) thrusts. The reconstructed river incision rates together with rates coming from several other rivers along a 250 km wide stretch of the NA mountain front and recently available in the literature, all indicate a general increase from Middle to Late Pleistocene. This suggests focusing of deformation along a deep structure, as confirmed by the deep compressional seismicity. The maximum rate is however not constant along the mountain front, but varies from 0.2 mm/yr in the west to more than 2.2 mm/yr in the eastern sector, suggesting a similar (eastward-increasing) trend of the apenninic subduction.

Detailed study of the seismotectonic setting in the Lucanian Apennines and surrounding areas (Southern Italy)

In this research work I analyzed the instrumental seismicity of Southern Italy in the area including the Lucanian Apennines and Bradano foredeep, making use of the most recent seismological database available so far. I examined the seismicity occurred during the period between 2001 and 2006, considering 514 events with magnitudes M ≥ 2.0. In the first part of the work, P- and S-wave arrival times, recorded by the Italian National Seismic Network (RSNC) operated by the Istituto Nazionale di Geofisica e Vulcanologia (INGV), were re-picked along with those of the SAPTEX temporary array (2001–2004). For some events located in the Upper Val d'Agri, I also used data from the Eni-Agip oil company seismic network. I computed the VP/VS ratio obtaining a value of 1.83 and I carried out an analysis for the one-dimensional (1D) velocity model that approximates the seismic structure of the study area. After this preliminary analysis, making use of the records obtained in the SeSCAL experiment, I incremented the database by handpicking new arrival times. My final dataset consists of 15,666 P- and 9228 S-arrival times associated to 1047 earthquakes with magnitude ML ≥ 1.5. I computed 162 fault-plane solutions and composite focal mechanisms for closely located events. I investigated stress field orientation inverting focal mechanism belonging to the Lucanian Apennine and the Pollino Range, both areas characterized by more concentrated background seismicity. Moreover, I applied the double difference technique (DD) to improve the earthquake locations. Considering these results and different datasets available in the literature, I carried out a detailed analysis of single sub-areas and of a swarm (November 2008) recorded by SeSCAL array. The relocated seismicity appears more concentrated within the upper crust and it is mostly clustered along the Lucanian Apennine chain. In particular, two well-defined clusters were located in the Potentino and in the Abriola-Pietrapertosa sector (central Lucanian region). Their hypocentral depths are slightly deeper than those observed beneath the chain. I suggest that these two seismic features are representative of the transition from the inner portion of the chain with NE-SW extension to the external margin characterized by dextral strike-slip kinematics. In the easternmost part of the study area, below the Bradano foredeep and the Apulia foreland, the seismicity is generally deeper and more scattered and is associated to the Murge uplift and to the small structures present in the area. I also observed a small structure NE-SW oriented in the Abriola-Pietrapertosa area (activated with a swarm in November 2008) that could be considered to act as a barrier to the propagation of a potential rupture of an active NW-SE striking faults system. Focal mechanisms computed in this study are in large part normal and strike-slip solutions and their tensional axes (T-axes) have a generalized NE-SW orientation. Thanks to denser coverage of seismic stations and the detailed analysis, this study is a further contribution to the comprehension of the seismogenesis and state of stress of the Southern Apennines region, giving important contributions to seismotectonic zoning and seismic hazard assessment.

Determinants of child undernutrition in India. A micro-case study to operationalize the Capability Approach

The present research aims at shedding light on the demanding puzzle characterizing the issue of child undernutrition in India. Indeed, the so called ‘Indian development paradox’ identifies the phenomenon according to which higher level of income per capita is recorded alongside a lethargic reduction in the proportion of underweight children aged below three years. Thus, in the time period occurring from 2000 to 2005, real Gross Domestic Production per capita has annually grown at 5.4%, whereas the proportion of children who are underweight has declined from 47% to 46%, a mere one point percent. Such trend opens up the space for discussing the traditionally assumed linkage between income-poverty and undernutrition as well as food intervention as the main focus of policies designed to fight child hunger. Also, it unlocks doors for evaluating the role of an alternative economic approach aiming at explaining undernutrition, such as the Capability Approach. The Capability Approach argues for widening the informational basis to account not only for resources, but also for variables related to liberties, opportunities and autonomy in pursuing what individuals value.The econometric analysis highlights the relevance of including behavioral factors when explaining child undernutrition. In particular, the ability of the mother to move freely in the community without the need of asking permission to her husband or mother-in-law is statistically significant when included in the model, which accounts also for confounding traditional variables, such as economic wealth and food security. Also, focusing on agency, results indicates the necessity of measuring autonomy in different domains and the need of improving the measurement scale for agency data, especially with regards the domain of household duties. Finally, future research is required to investigate policy venues for increasing agency in women and in the communities they live in as viable strategy for reducing the plague of child undernutrition in India.

InSAR deformation measurements of the earthquake cycle in transcurrent tectonic domains, analytical and analog modeling

I applied the SBAS-DInSAR method to the Mattinata Fault (MF) (Southern Italy) and to the Doruneh Fault System (DFS) (Central Iran). In the first case, I observed limited internal deformation and determined the right lateral kinematic pattern with a compressional pattern in the northern sector of the fault. Using the Okada model I inverted the observed velocities defining a right lateral strike slip solution for the MF. Even if it fits the data within the uncertainties, the modeled slip rate of 13-15 mm yr-1 seems too high with respect to the geological record. Concerning the Western termination of DFS, SAR data confirms the main left lateral transcurrent kinematics of this fault segment, but reveal a compressional component. My analytical model fits successfully the observed data and quantifies the slip in ~4 mm yr-1 and ~2.5 mm yr-1 of pure horizontal and vertical displacement respectively. The horizontal velocity is compatible with geological record. I applied classic SAR interferometry to the October–December 2008 Balochistan (Central Pakistan) seismic swarm; I discerned the different contributions of the three Mw > 5.7 earthquakes determining fault positions, lengths, widths, depths and slip distributions, constraining the other source parameters using different Global CMT solutions. A well constrained solution has been obtained for the 09/12/2008 aftershock, whereas I tested two possible fault solutions for the 28-29/10/08 mainshocks. It is not possible to favor one of the solutions without independent constraints derived from geological data. Finally I approached the study of the earthquake-cycle in transcurrent tectonic domains using analog modeling, with alimentary gelatins like crust analog material. I successfully joined the study of finite deformation with the earthquake cycle study and sudden dislocation. A lot of seismic cycles were reproduced in which a characteristic earthquake is recognizable in terms of displacement, coseismic velocity and recurrence time.

Fault delineation and stress orientations from the analysis of background, low magnitude seismicity in Southern Apennines (Italy)

The aim of this work was to show that refined analyses of background, low magnitude seismicity allow to delineate the main active faults and to accurately estimate the directions of the regional tectonic stress that characterize the Southern Apennines (Italy), a structurally complex area with high seismic potential. Thanks the presence in the area of an integrated dense and wide dynamic network, was possible to analyzed an high quality microearthquake data-set consisting of 1312 events that occurred from August 2005 to April 2011 by integrating the data recorded at 42 seismic stations of various networks. The refined seismicity location and focal mechanisms well delineate a system of NW-SE striking normal faults along the Apenninic chain and an approximately E-W oriented, strike-slip fault, transversely cutting the belt. The seismicity along the chain does not occur on a single fault but in a volume, delimited by the faults activated during the 1980 Irpinia M 6.9 earthquake, on sub-parallel predominant normal faults. Results show that the recent low magnitude earthquakes belongs to the background seismicity and they are likely generated along the major fault segments activated during the most recent earthquakes, suggesting that they are still active today thirty years after the mainshock occurrences. In this sense, this study gives a new perspective to the application of the high quality records of low magnitude background seismicity for the identification and characterization of active fault systems. The analysis of the stress tensor inversion provides two equivalent models to explain the microearthquake generation along both the NW-SE striking normal faults and the E- W oriented fault with a dominant dextral strike-slip motion, but having different geological interpretations. We suggest that the NW-SE-striking Africa-Eurasia convergence acts in the background of all these structures, playing a primary and unifying role in the seismotectonics of the whole region.

Regolazione delle prestazioni indispensabili e poteri della Commissione di garanzia

La legge n. 146 del 1990 ha istituito la Commissione di garanzia per l’attuazione della legge sullo sciopero nei servizi pubblici essenziali, un’authority deputata al controllo dell’effettivo bilanciamento del diritto di sciopero con gli altri diritti della persona di rango costituzionale nel caso dei servizi pubblici essenziali. Ad essa spettano alcuni poteri tra di loro eterogenei. Accanto a poteri propulsivi e sanzionatori, essa possiede poteri di tipo normativo. La legge prevede, infatti, che le prestazioni indispensabili e le altre misure necessarie al contemperamento siano determinate da accordi tra il datore di lavoro e le associazioni sindacali, mentre per il lavoro autonomo da codici di autoregolamentazione forniti da ognuna delle categorie interessate. Gli accordi e i codici di autoregolamentazione devono essere, comunque, sottoposti al vaglio della Commissione di garanzia la quale in ultimo stabilisce se essi siano idonei a realizzare il bilanciamento dei diritti in questione. Quando i soggetti indicati dalla legge non provvedano alla redazione dei suddetti atti, la Commissione interviene con l’emanazione di una provvisoria regolamentazione, la quale possiede natura di regolamento, giacchè partecipa dei caratteri della generalità ed astrattezza propri delle norme di legge. In effetti, anche altre authorities possiedono un potere normativo, che si sostanzia alle volte in un regolamento indipendente, altre in un regolamento simile ai regolamenti delegati ed altre al regolamento esecutivo. Poiché la legge n. 146 del 1990 prevede quali siano gli istituti idonei a realizzare il bilanciamento (preavviso, proclamazione scritta, procedure di raffreddamento e conciliazione, intervallo minimo, misure indicative delle prestazioni indispensabili), la provvisoria regolamentazione possiede i caratteri del regolamento esecutivo.

L’autotutela collettiva tra ipotesi di revisione della disciplina nazionale e prospettive europee

Nel presente lavoro viene trattato il delicato tema dell’autotutela collettiva, nell’intersezione tra ipotesi di revisione nazionale e prospettive europee. Dapprima viene ricostruita l’evoluzione della valutazione del conflitto collettivo nell’ordinamento giuridico italiano ed effettuata una ricognizione delle diverse manifestazioni del conflitto collettivo ivi riscontrabili. Il tentativo è quello di superare i limiti di una trattazione ristretta allo sciopero e di verificare la perdurante validità della tradizionale nozione di sciopero, intesa esclusivamente come astensione collettiva dalle prestazioni di lavoro. In un secondo capitolo vengono esaminati i disegni di legge di riforma in materia di conflitto collettivo, presentati nel corso della XVI legislatura e le clausole, incidenti sulla medesima materia, rinvenibili nell’Accordo interconfederale del 28 giugno 2011 e negli accordi FIAT del 2010, relativi agli stabilimenti di Pomigliano D’Arco e Mirafiori. Alla luce di tali materiali, si riesaminano le tematiche della titolarità individuale del diritto di sciopero, delle clausole di tregua e delle procedure arbitrali e conciliative. Successivamente, viene esaminata la produzione legislativa e giurisprudenziale comunitaria in tema di conflitto collettivo. Il confronto con l’ordinamento nazionale consente di mettere criticamente in luce il diverso rapporto tra mercato e diritti d’azione collettiva e di rilevare che nell’ordinamento comunitario la giurisprudenza della Corte di giustizia abbia introdotto limiti eccessivi al dispiegarsi dei diritti sociali in esame. Da ultimo, vengono formulate alcune considerazioni conclusive. Criticamente viene rilevato come, in tempi di globalizzazione, non viene prestata sufficiente attenzione alla valorizzazione del conflitto collettivo, come motore dell’emancipazione e del progresso sociale.

Industrial accidents triggered by lightning: causes and consequences

Natural hazards affecting industrial installations could directly or indirectly cause an accident or series of accidents with serious consequences for the environment and for human health. Accidents initiated by a natural hazard or disaster which result in the release of hazardous materials are commonly referred to as Natech (Natural Hazard Triggering a Technological Disaster) accidents. The conditions brought about by these kinds of events are particularly problematic, the presence of the natural event increases the probability of exposition and causes consequences more serious than standard technological accidents. Despite a growing body of research and more stringent regulations for the design and operation of industrial activities, Natech accidents remain a threat. This is partly due to the absence of data and dedicated risk-assessment methodologies and tools. Even the Seveso Directives for the control of risks due to major accident hazards do not include any specific impositions regarding the management of Natech risks in the process industries. Among the few available tools there is the European Standard EN 62305, which addresses generic industrial sites, requiring to take into account the possibility of lightning and to select the appropriate protection measures. Since it is intended for generic industrial installations, this tool set the requirements for the design, the construction and the modification of structures, and is thus mainly oriented towards conventional civil building. A first purpose of this project is to study the effects and the consequences on industrial sites of lightning, which is the most common adverse natural phenomenon in Europe. Lightning is the cause of several industrial accidents initiated by natural causes. The industrial sectors most susceptible to accidents triggered by lightning is the petrochemical one, due to the presence of atmospheric tanks (especially floating roof tanks) containing flammable vapors which could be easily ignited by a lightning strike or by lightning secondary effects (as electrostatic and electromagnetic pulses or ground currents). A second purpose of this work is to implement the procedure proposed by the European Standard on a specific kind of industrial plant, i.e. on a chemical factory, in order to highlight the critical aspects of this implementation. A case-study plant handling flammable liquids was selected. The application of the European Standard allowed to estimate the incidence of lightning activity on the total value of the default release frequency suggested by guidelines for atmospheric storage tanks. Though it has become evident that the European Standard does not introduce any parameters explicitly pointing out the amount of dangerous substances which could be ignited or released. Furthermore the parameters that are proposed to describe the characteristics of the structures potentially subjected to lightning strikes are insufficient to take into account the specific features of different chemical equipment commonly present in chemical plants.

Implications of regional fault distribution and kinematics for the uplift of rift flanks around the Rwenzori Mountains, Southwestern Uganda

Das Ziel dieser Arbeit bestand in der Untersuchung der Störungsverteilung und der Störungskinematik im Zusammenhang mit der Hebung der Riftschultern des Rwenzori Gebirges.rnDas Rwenzori Gebirge befindet sich im NNE-SSWbis N-S verlaufenden Albertine Rift, des nördlichsten Segments des westlichen Armes des Ostafrikanischen Grabensystems. Das Albertine Rift besteht aus Becken unterschiedlicher Höhe, die den Lake Albert, Lake Edward, Lake George und Lake Kivu enthalten. Der Rwenzori horst trennt die Becken des Lake Albert und des Lake Edward. Es erstreckt sich 120km in N-S Richtung, sowie 40-50km in E-W Richtung, der h¨ochste Punkt befindet sich 5111 ü. NN. Diese Studie untersucht einen Abschnitt des Rifts zwischen etwa 1°N und 0°30'S Breite sowie 29°30' und 30°30' östlicher Länge ersteckt. Auch die Feldarbeit konzentrierte sich auf dieses Gebiet.rnrnHauptzweck dieser Studie bestand darin, die folgende These auf ihre Richtigkeit zu überprüfen: ’Wenn es im Verlauf der Zeit tatsächlich zu wesentlichen Änderungen in der Störungskinematik kam, dann ist die starke Hebung der Riftflanken im Bereich der Rwenzoris nicht einfach durch Bewegung entlang der Graben-Hauptst¨orungen zu erklären. Vielmehr ist sie ein Resultat des Zusammenspiels mehrerer tektonische Prozesse, die das Spannungsfeld beeinflussen und dadurch Änderungen in der Kinematik hervorrufen.’ Dadurch konzentrierte sich die Studie in erster Linie auf die Störungsanalyse.rnrnDie Kenntnis regionaler Änderungen der Extensionsrichtung ist entscheidend für das Verständnis komplexer Riftsysteme wie dem Ostafrikanischen Graben. Daher bestand der Kern der Untersuchung in der Kartierung von Störungen und der Untersuchung der Störungskinematik. Die Aufnahme strukturgeologischer Daten konzentrierte sich auf die Ugandische Seite des Rifts, und Pal¨aospannungen wurden mit Hilfe von St¨orungsdaten durch Spannungsinversion rekonstruiert.rnDie unterschiedliche Orientierung spr¨oder Strukturen im Gelände, die geometrische Analyse der geologischen Strukturen sowie die Ergebnisse von Mikrostrukturen im Dünnschliff (Kapitel 4) weisen auf verschiedene Spannungsfelder hin, die auf mögliche Änderungen der Extensionsrichtung hinweisen. Die Resultate der Spannungsinversion sprechen für Ab-, Über- und Blattverschiebungen sowie für Schrägüberschiebungen (Kapitel 5). Aus der Orientierung der Abschiebungen gehen zwei verschiedene Extensionsrichtungen hervor: im Wesentlichen NW-SE Extension in fast allen Gebieten, sowie NNE-SSW Extension im östlichen Zentralbereich.rnAus der Analyse von Blattverschiebungen ergaben sich drei unterschiedliche Spannungszustände. Zum Einen NNW-SSE bis N-S Kompression in Verbindung mit ENE-WSW bzw E-W Extension wurde für die nördlichen und die zentralen Ruwenzoris ausgemacht. Ein zweiter Spannungszustand mit WNW-ESE Kompression/NNE-SSW Extension betraf die Zentralen Rwenzoris. Ein dritter Spannungszustand mit NNW-SSE Extension betraf den östlichen Zentralteil der Rwenzoris. Schrägüberschiebungen sind durch dazu schräge Achsen charakterisiert, die für N-S bis NNW-SSE Kompression sprechen und ausschließlich im östlichen Zentralabschnitt auftreten. Überschiebungen, die hauptsächlich in den zentralen und den östlichen Rwenzoris auftreten, sprechen für NE-SW orientierten σ2-Achsen und NW-SE Extension.rnrnEs konnten drei unterschiedliche Spannungseinflüsse identifiziert werden: auf die kollisionsbedingte Bildung eines Überschiebungssystem folgte intra-kratonische Kompression und schließlich extensionskontrollierte Riftbildung. Der Übergang zwischen den beiden letztgenannten Spannungszuständen erfolgte Schrittweise und erzeugte vermutlich lokal begrenzte Transpression und Transtension. Gegenw¨artig wird die Störungskinematik der Region durch ein tensiles Spannungsregime in NW-SE bis N-S Richtung bestimmt.rnrnLokale Spannungsvariationen werden dabei hauptsächlich durch die Interferenzrndes regionalen Spannungsfeldes mit lokalen Hauptst¨orungen verursacht. Weitere Faktoren die zu lokalen Veränderungen des Spannungsfeldes führen können sind unterschiedliche Hebungsgeschwindigkeiten, Blockrotation oder die Interaktion von Riftsegmenten. Um den Einfluß präexistenter Strukturen und anderer Bedingungen auf die Hebung der Rwenzoris zu ermitteln, wurde der Riftprozeß mit Hilfe eines analogen ’Sandbox’-Modells rekonstruiert (Kapitel 6). Da sich die Moho-Diskontinuität im Bereich des Arbeitsgebietes in einer Tiefe von 25 km befindet, aktive Störungen aber nur bis zu einer Tiefe von etwa 20 km beobachtet werden können (Koehn et al. 2008), wurden nur die oberen 25 km im Modell nachbebildet. Untersucht und mit Geländebeobachtungen verglichen wurden sowohl die Reihenfolge, in der Riftsegmente entstehen, als auch die Muster, die sich im Verlauf der Nukleierung und des Wachstums dieser Riftsegmente ausbilden. Das Hauptaugenmerk wurde auf die Entwicklung der beiden Subsegmente gelegt auf denen sich der Lake Albert bzw. der Lake Edward und der Lake George befinden, sowie auf das dazwischenliegende Rwenzori Gebirge. Das Ziel der Untersuchung bestand darin herauszufinden, in welcher Weise das südwärts propagierende Lake Albert-Subsegment mit dem sinistral versetzten nordwärts propagierenden Lake Edward/Lake George-Subsegment interagiert.rnrnVon besonderem Interesse war es, in welcherWeise die Strukturen innerhalb und außerhalb der Rwenzoris durch die Interaktion dieser Riftsegmente beeinflußt wurden. rnrnDrei verschiedene Versuchsreihen mit unterschiedlichen Randbedingungen wurden miteinander verglichen. Abhängig vom vorherrschenden Deformationstyp der Transferzone wurden die Reihen als ’Scherungs-dominiert’, ’Extensions-dominiert’ und als ’Rotations-dominiert’ charakterisiert. Die Beobachtung der 3-dimensionalen strukturellen Entwicklung der Riftsegmente wurde durch die Kombination von Modell-Aufsichten mit Profilschnitten ermöglicht. Von den drei genannten Versuchsreihen entwickelte die ’Rotationsdominierten’ Reihe einen rautenförmiger Block im Tranferbereich der beiden Riftsegmente, der sich um 5−20° im Uhrzeigersinn drehte. DieserWinkel liegt im Bereich des vermuteten Rotationswinkel des Rwenzori-Blocks (5°). Zusammengefasst untersuchen die Sandbox-Versuche den Einfluss präexistenter Strukturen und der Überlappung bzw. Überschneidung zweier interagierender Riftsegmente auf die Entwicklung des Riftsystems. Sie befassen sich darüber hinaus mit der Frage, welchen Einfluss Blockbildung und -rotation auf das lokale Stressfeld haben.

Induktion von Pro-Autophagie-Signalen durch einen extra- oder intrazellulären Alpha-Toxin-Angriff

Autophagie ist ein konservierter, kataboler Mechanismus in allen eukaryoten Zellen. Unter anderem wird ihm eine wichtige Rolle als zellautonomer Abwehrmechanismus gegen Mikroorganismen zugeschrieben; von manchen Infektionserregern wird er jedoch unterlaufen oder sogar genutzt. Der stärkste Auslöser der Autophagie ist ein Mangel an Nährstoffen, insbesondere Aminosäuren. Über die Deaktivierung der Kinase mTORC1 und die Phosphorylierung des eukaryoten Translationsinitiationsfaktors eIF2α hemmt die Nährstoffknappheit die Proteinbiosynthese und aktiviert gleichzeitig Autophagie. Wie Mikroorganismen, insbesondere Bakterien, Autophagie auslösen oder manipulieren, ist derzeit Gegenstand intensiver Forschung. Modifikationen an Mikroben oder Phagosomen und Adapterproteine, die diese Veränderungen und Komponenten des Autophagieapparates erkennen, scheinen jedenfalls bei der selektiven Erkennung durch die Autophagie-Maschinerie wichtig zu sein. rnIn der vorliegenden Dissertationsarbeit wird die Rolle des membranporenbildenden α-Toxins von Staphylococcus aureus für die Induktion von Autophagie beleuchtet. Zum einen erwies sich die Akkumulation von (EGFP)-LC3(II), einem Marker der Autophagosomen, um intrazelluläre S. aureus als abhängig von α-Toxin. Zweitens, genügt extrazellulär appliziertes α-Toxin um (EGFP)-LC3(II)-positive Endosomen zu induzieren. Während der Angriff aus dem extrazellulären Raum jedoch binnen kurzer Zeit eine fokale Kumulation von phosphoryliertem eIF2α an der Plasmamembran induziert, die an der Internalisierung des Toxins beteiligt ist, findet sich am phagosomalen Kompartiment keine Toxin-abhängige Anhäufung von p-eIF2α oder proximalen Autophagieregulatoren. Dies impliziert, dass Toxin-Angriff auf die Plasmamembran, nicht aber auf das Phagosom, zu einer Reaktion führt, wie sie bei massivem Nährstoffmangel zu beobachten ist. Obwohl keine α-Toxin-abhängige Kumulation von p-eIF2α bei einem Angriff aus dem Phagosom erfolgt, findet sich um α-Toxin-produzierende Bakterien eine massive Kumulation von LC3 und Adapterprotein p62/Sequestosome1. Dies deutet daraufhin, dass der Ort des Angriffs - Plasmamembran oder Phagosom – für den Autophagie-induzierenden Mechanismus wichtig sein könnte. Der unterschiedliche Effekt auf die zellulären Ionenkonzentrationen, den ein Angriff auf die Plasmamembran oder auf ein Phagosom auslösen würde, bietet hierfür eine mögliche Erklärung. Die Aktivierung der Autophagie über Adapterproteine könnte dann als back-up Mechanismus fungieren, der auch dann greift, wenn eine Invasion ohne Schädigung der Plasmamembran erfolgt. Ein cross-talk der beiden Induktionswege ist angesichts der Bedeutung von p62 für die selektive und die Hunger-assoziierte Autophagie gut möglich; sezerniertes Toxin könnte durch die Aktivierung der basalen Autophagie Adapter-basierte Mechanismen verstärken.

Neotettonica della faglia Nord-Anatolica nel Mare di Marmara. Analisi di dati sismici a riflessione e morfobatimetrici ad alta risoluzione

Il 17 agosto 1999 un violento terremoto di Mw 7,4 (terremoto di Izmit) ha interessato l’area del Golfo di Izmit, dove il segmento settentrionale della Faglia Nord-Anatolica (FNA) entra nel Mare di Marmara. Oltre a causare enormi danni e un numero di vittime altissimo (oltre 20000), la dislocazione orizzontale di oltre 5 metri in prossimità dell’epicentro ha caricato tettonicamente il segmento della FNA verso Istanbul. Da qui, l’importanza di un modello geologico-strutturale condiviso dalla comunità scientifica per questo ramo della Faglia Nord Anatolica, per la formulazione dei modelli di stima del rischio sismico in una zona della Turchia molto densamente popolata (oltre 12 milioni di persone). I numerosi studi di geologia e geofisica marina condotti nel Golfo di Izmit e più in generale nel Mare di Marmara, hanno avuto un grosso impulso in concomitanza del terremoto del 1999 e negli anni successivi, quando il Mare di Marmara è stato inserito tra i siti di importanza strategica. Nonostante la grande mole di dati raccolti e le pubblicazioni di lavori importanti che hanno contribuito a portare nuova luce sulla geologia di questo territorio complesso, permangono ancora incertezze e controversie sui rapporti le tra la formazione del bacino di Marmara e la FNA. Questo lavoro di tesi ha lo scopo di esaminare la cinematica della FNA nell’area del Mare di Marmara, in generale, ed in particolare lungo i vari bacini allineati lungo il ramo settentrionale: da Est verso Ovest, il Bacino di Cinarcik, il Bacino di Kumburgaz, il Bacino Centrale ed il Bacino di Tekirdag. Analizzeremo la natura e il grado di attività dei segmenti individuati da zone di trasferimento (bending o overstep) e tenteremo di cartografare la geometria, lo stile strutturale e la lunghezza di ciascun segmento, per effettuare una stima del potenziale sismogenetico di ciascun ramo utilizzando relazioni empiriche.

High numbers of DC-SIGN+ dendritic cells in lesional skin of cutaneous T-cell lymphoma

The role of dendritic cells (DCs) in disease progression of primary cutaneous T-cell lymphoma (CTCL) is not well understood. With their unique ability to induce primary immune responses as well as immunotolerance, DCs play a critical role in mediation of anti-tumor immune responses. Tumor-infiltrating DCs have been determined to represent important prognostic factors in a variety of human tumors.