“Rimarrà solo, attorno, un lieve odore di bruciato”: la distruzione dell’esperienza in Quaderno proibito di Alba de Céspedes

In this essay, using Agamben work on The destruction of experience as a frame, I analyse the role that the acquisition of life experience plays in one of the main works of Alba de Cespedes, Quaderno proibito. I will show how the protagonist’s point of view works as a bridge between traditional experience, which became unattainable in contemporary societies, and a modern one, and I will show how the fascination that the book still has on readers is mainly related to the description of the process of destruction of the traditional form of experience

Introduzione / Introduction

Identità Italiane In Moviment

The so called "triassic breccias" of the Ionian zone in Greece and Albania: Their stratigraphie position and the ensuing tectonic implications

Field observations are reported which show that: 1) at least part of the so called "Triassic breccias" of the Ionian isopic zone actually represent a local variant of the basal breccias of a Middle-Upper Miocene marine terrigenous sequence; 2) other portions of the same Miocenic basal breccias have been often mistaken in the past for some other looking-like terrane of different age (from Jurassic to Quaternary!). Since some currently accepted inferences on the time-sequence of both sedimentary and tectonic events ensuing from the above misunderstandings become questionable, new field investigation should be extended to the entire Ionian zone with due regard to the above terranes

Quale futuro per il referendum? Considerazioni sul giudizio di ammissibilità e possibili svolte ermeneutiche de jure condito

Nella recente tornata di richieste referendarie, i vari giudizi di ammissibilità compi uti dalla Corte costituzionale hanno suscitato an cora una volta l’interrogativo se ormai, nei fatti, essi non si siano trasformati in veri e propri giudizi anticipati di legittimità costituzionale e se dunque la ricorrente affermazione in senso contrario d a pa rte del giudice costituzionale non si vada risolvendo in una mera clausola di stile . L’interrogativo riguarda in particolare la questione se giudizio di ammissibilità e giudizio di legittimità costituzionale, al di là delle ovvie differenze processuali e di latitudine, possano d irsi qualitativamente distinti. È un’opinione che, anche a parere di chi sc rive, dovrebbe essere respinta. Un diverso approccio ricostruttivo consentirebbe, invece, di collocare la distinzione tra i due giudizi su un piano divers o e forse consentire di definire il confine tra di essi in modo più chiaro. Inoltre, accogliere una tale prospettiva permetterebbe anche, come si cercherà di suggerire, di applicare lo strumentario elaborato dalla Corte costituzionale nell’ambito del giudi zio sulle leggi, anche, in quanto possibile, al giudizio di ammissibilità

INTRA-CULTIVAR DIVERSITY IN SOUTHERN ITALY OLIVE CULTIVARS DEPICTED BY MORPHOLOGICAL TRAITS AND SSR MARKERS

In this study, SSR analysis was performed on a large number of putative clones of the main olive cultivars from two Italian regions, Sicily and Calabria, in order to study the genetic relatedness, and to detect any degree of genetic diversity, which can be used to unambiguously identify possible superior clones. These putative clones have been collected and observed in the last ten years, following an extensive investigation carried out in traditional olive growing areas, thanks to the reports of farmers, millers, technician, growers and nurseries. The set of microsatellite (SSR) markers used allowed the detection of the genetic diversity, resulting from somatic mutation, indicating the presence of polyclonal cultivars, or having gametic origin, indicating a seedling origin of many clones, which thus share sibling relationships. The presence of superior clones or superior genotypes is discussed

Upper limb children action-observation training (UP-CAT): a randomised controlled trial in Hemiplegic Cerebral Palsy

BACKGROUND: Rehabilitation for children with hemiplegic cerebral palsy (HCP) aimed to improve function of the impaired upper limb (UL) uses a wide range of intervention programs. A new rehabilitative approach, called Action-Observation Therapy, based on the recent discovery of mirror neurons, has been used in adult stroke but not in children. The purpose of the present study is to design a randomised controlled trial (RCT) for evaluating the efficacy of Action-Observation Therapy in improving UL activity in children with HCP.METHODS/DESIGN: The trial is designed according to CONSORT Statement. It is a randomised, evaluator-blinded, match-pair group trial. Children with HCP will be randomised within pairs to either experimental or control group. The experimental group will perform an Action-Observation Therapy, called UP-CAT (Upper Limb-Children Action-Observation Training) in which they will watch video sequences showing goal-directed actions, chosen according to children UL functional level, combined with motor training with their hemiplegic UL. The control group will perform the same tailored actions after watching computer games. A careful revision of psychometric properties of UL outcome measures for children with hemiplegia was performed. Assisting Hand Assessment was chosen as primary measure and, based on its calculation power, a sample size of 12 matched pairs was established. Moreover, Melbourne and ABILHAND-Kids were included as secondary measures. The time line of assessments will be T0 (in the week preceding the onset of the treatment), T1 and T2 (in the week after the end of the treatment and 8 weeks later, respectively). A further assessment will be performed at T3 (24 weeks after T1), to evaluate the retention of effects. In a subgroup of children enrolled in both groups functional Magnetic Resonance Imaging, exploring the mirror system and sensory-motor function, will be performed at T0, T1 and T2.DISCUSSION: The paper aims to describe the methodology of a RCT for evaluating the efficacy of Action-Observation Therapy in improving UL activity in children with hemiplegia. This study will be the first to test this new type of treatment in childhood. The paper presents the theoretical background, study hypotheses, outcome measures and trial methodology

Seismotectonics of the active thrust front in southwestern Sicily: hints on the Belice and Selinunte seismogenic sources

We present a seismotectonic model of the active thrust front in western Sicily, which includes the area hit by the 1968 Belice earthquake sequence. The ~40 km long South-WEstern Sicilian Thrust (SWEST) is formed by two aligned albeit non-parallel fault arrays, the Granitola-Castelevetrano Thrust System (GCTS) in the west and the Partanna- Poggioreale Thrust System (PPTS) in the east. The ~NE-SW trending, NW-dipping GCTS straddles from the Pelagian coastline to Castelvetrano, is ~18 km long and composed of two segments, with the northern, ~12 km long one showing geodetic and geologic evidence of active deformation (Barreca et al., 2014). The segment is marked by a sharp gradient in Differential SAR interferometry (DinSAR and STAMPs) and GPS velocity fields. Geologic evidence include an up to 60 m high, and up to 15° steep scarp, which is the fore-limb of a broad fold involving Lower Pleistocene shore calcarenites, and cm-scale reverse displacement of an ancient road dated as early Bronze-Hellenistic age. Inversion of fault slip-lineation data from structures displacing the archaeological remains yields a ~N110°E shortening axis, consistent with the geodetic shortening direction estimated from GPS differential velocities. The ~ENE-WSW trending PPTS stretches from Partanna to the macro-seismic area of the 1968 earthquake sequence and is composed of two ~10 km long segments limited by relay ramps. Although geologic and geodetic evidence of deformation are less clear than for the GCTS, we nonetheless observe a gradient in interferometry data for the western segment, and evidence of slow deformation (creep?) in historical to recent (last ~400 yr?) man-made structures. Integration of geologic, geodetic and seismology data suggests the active folds and thrusts are the uppermost expression of steep (45°) crustal ramps (Monaco et al., 1996) which upthrust the Saccense platform at depth. Based on macroseismic and seismological evidence (Monaco et al., 1996), we contend that the PPTS was partly activated during the 1968 sequence, and that rupture stopped at the junction with the GCTS. The current geodetic strain accumulation on the GCTS, on the other hand, suggests that the fault array has been significantly loaded, and that its last important co-seismic event could have been caused the 4th–5th century A.D. destruction of Selinunte (Bottari et al., 2009)

Geodetic and geological evidence of active tectonics in south-westernSicily (Italy)

Integrated geological, geodetic and marine geophysical data provide evidence of active deformation insouth-western Sicily, in an area spatially coincident with the macroseismic zone of the destructive 1968Belice earthquake sequence. Even though the sequence represents the strongest seismic event recordedin Western Sicily in historical times, focal solutions provided by different authors are inconclusive onpossible faulting mechanism, which ranges from thrusting to transpression, and the seismogenic sourceis still undefined. Interferometric (DInSAR) observations reveal a differential ground motion on a SW–NEalignment between Campobello di Mazara and Castelvetrano (CCA), located just west of the maximummacroseismic sector. In addition, new GPS campaign-mode data acquired across the CCA alignment doc-uments NW–SE contractional strain accumulation. Morphostructural analysis allowed to associate thealignment detected through geodetic measurements with a topographic offset of Pleistocene marine sed-iments. The on-land data were complemented by new high-resolution marine geophysical surveys, whichindicate recent contraction on the offshore extension of the CCA alignment. The discovery of archaeo-logical remains displaced by a thrust fault associated with the alignment provided the first likely surfaceevidence of coseismic and/or aseismic deformation related to a seismogenic source in the area. Resultsof the integrated study supports the contention that oblique thrusting and folding in response to NW–SEoriented contraction is still active. Although we are not able to associate the CCA alignment to the 1968seismic sequence or to the historical earthquakes that destroyed the ancient Greek city of Selinunte,located on the nearby coastline, our result must be incorporated in the seismic hazard evaluation of thisdensely populated area of Sicily