1,361,486 research outputs found
Whither Critical Management and Organization Studies? For a Performative Critique of Capitalist Flows in the Wake of the COVID‐19 Pandemic
Zanoni, P (corresponding author), Hasselt Univ, Hasselt, Belgium.
[email protected]
Case discussion of an immediate serious reaction to hexavalent vaccine mistaken for anaphylaxis
Giovanna Zanoni, Leonardo Gottin, Attilio Boner, Giorgio Piacentini, Diego Peroni and Michael Gol
Emozioni: parlarne, sentirle, tradurle II: Introduction
Two years after the publication of the Dossier Emozioni: sentirle, parlarne, tradurle (Zanoni and Zuccheri 2022), the contributions collected here aim to continue the interdisciplinary discussion between language, translation, and interpreting dedicated to the expression and narration of emotions. The Dossier follows a Study Day on emotions held on March 15, 2023, at the Department of Interpreting and Translation of the University of Bologna in Forlì. The interest in topics such as emotional expression in various contexts and the high participation of researchers and students in the event convinced us of the importance of producing a second dossier on the subject, involving additional scholars from diverse academic, professional, and research backgrounds. The contributions collected here should therefore be understood in this context.A due anni dalla pubblicazione del Dossier Emozioni: sentirle, parlarne, tradurle (Zanoni e Zuccheri 2022), i contributi qui raccolti intendono proseguire il confronto interdisciplinare tra lingua, traduzione e interpretazione dedicato all’espressione e alla narrazione delle emozioni. Il Dossier segue una Giornata di Studi dedicata alle emozioni e tenutasi il 15 marzo 2023 all’Università di Bologna presso il Dipartimento di Interpretazione e Traduzione di Forlì. L’interesse nei confronti di una tematica come l’espressione emotiva in diversi contesti e l’elevata partecipazione di ricercatori/trici e studenti/esse all’iniziativa ci ha convinto dell’importanza di riproporre un secondo dossier sull’argomento coinvolgendo anche altri/e studiosi/e provenienti da diversi contesti accademici, professionali e di ricerca. Sono dunque da intendersi in questo senso i contributi ivi raccolti
Testing the thermal state of Biella pluton country rocks via numerical model of magma cooling
The Biella pluton (30-31 Ma) is a Periadriatic intrusive of the Alps, emplaced in the internal part of the HP continental Sesia Lanzo Zone (Berger et al., 2012). Pluton cooling involved contact metamorphism overprinting eclogitic to greenschist facies assemblages in country rocks. Multiscale structural analysis combined with thermos-barometric estimates suggest that magma intrusion took place at shallow crustal levels (Zanoni et al., 2008; Zanoni et al., 2010; Zanoni, 2015).
The emplacement history indicates that the intrusion of Biella body occurred when the Sesia Lanzo Zone had almost completed its exhumation under low thermal state consistent with an ongoing subduction (e.g. Roda et al., 2012 and refs therein). The mechanism proposed for triggering the Periadriatic magmatism are either subduction (Tiepolo et al., 2014) or slab break-off (e.g. Von Blankenburg & Davies, 1995). However recent numerical modeling (Freeburn et al., 2015) suggests that a slab break-off related melting does not result in the widespread magmatism characterizing many collisional belts.
In order to unravel the thermal state of the Biella stock country rocks at the intrusion time we develop a preliminary 2D thermal model of pluton cooling testing four different thermal gradients of the host rocks. We compare the extent and the variation in the thermal peak of the contact aureole recorded in the country rock (Fig. 1) with the results of the numerical simulations.
The computed thermal boundary of the aureole is between 300 and 400°C and is wider than the mapped one due to the difficulty to distinguish between contact and greenschists regional metamorphism at such low temperatures. The best fit occurs for the simulation accounting for temperatures between 427 and 527°C (700 and 800 K) at 8 km depth (Fig. 2), assuming conduction as the only effective heat transfer mechanism. This indicates that the emplacement occurred under thermal gradients between 55 and 65°C/km that would exclude a syn-subductive magmatism. The suggested thermal gradient for the country rock of the Biella pluton would represent the constraint for testing different scenarios responsible for the generation of Periadriatic magmatism
The thermal state of Biella pluton country rocks as a tool to unravel the late orogenic tectonics of the Western Alps
Crustal level and timing of late-orogenic plutons represent powerful tools for constraining the late exhumation history of tectonic units, within collisional belts. This work aims to contribute to this topic by quantitatively determining the thermal state of Biella Periadriatic pluton country rocks during its emplacement within the continental HP metamorphic rocks of the Sesia-Lanzo Zone (SLZ), in the western Austroalpine domain (Zanoni et al., 2008, 2010; Zanoni, 2016 and refs. therein). During the Alpine subduction and exhumation, the Sesia-Lanzo Zone records a polyphasic tectono-metamorphic evolution. Pluton cooling involved contact metamorphism overprinting eclogitic to greenschist facies assemblages in the country rocks. On the basis of the amount and type of contact metamorphic assemblages the aureole extent was mapped and the variation of recorded thermal peak validated by comparison with numerical modelling of the heat transfer during magma crystallisation. Thus, this work aims constraining the late exhumation history of the internal western Alps by determining the crustal level of pluton emplacement and the thermal gradient of its country rocks at the time of intrusion.
The Alps developed during subduction and closure of the Mesozoic Tethys and subsequent continental collision over Cretaceous–Oligocene times (e.g. Dal Piaz, 2010; Handy et al., 2010; Spalla et al., 2010). The Alpine convergent system involved the subduction of the European lithosphere underneath the Adria plate. The Periadriatic line is a main crustal break of the Alpine bounding the Southalpine continental crust acting as backstop wall of the orogenic wedge during the convergence (Polino et al., 1990). This lineament (Fig. 1) separates tectonic units that during the Alpine convergence experimented intense deformation and metamorphism (i.e. Austroalpine and Penninic domains) from rocks that recorded only shallow structural level deformation (i.e. Southalpine domain). The Periadriatic line is interpreted as the ascent path for the late collisional Oligocene magmas, which emplaced to form the Periadriatic plutons (Rosenberg, 2004). The Periadriatic plutons are traditionally considered as derived from the Alpine slab breakoff (Von Blanckenburg and Davies, 1995). However recently the Tertiary magmatic rocks south of the Periadriatic line, such as the southern Adamello pluton, Veneto Volcanic province, and dykes in the central Southalpine, are supposed to be generated during Alpine subduction (Tiepolo et al., 2011; Bartoli et al., 2013; Bergomi et al., 2015). The Austroalpine domain of the western Alps consists of continental rocks tectonically sampled by the margin of Adria plate during subduction (e.g. Roda et al., 2012) and is actually divided into two main tectonic units, namely the Sesia-Lanzo Zone (SLZ) and Dent Blanche nappe. Both tectonic units were subducted and exhumed during the Alpine cycle when the oceanic subduction was still active (Spalla et al., 1996; Babist et al., 2006; Roda et al., 2012). Between 60 and 80 Ma the SLZ reached the P-peak during subduction (Bussy et al., 1998; Cenki-Tok et al., 2011), corresponding to eclogite conditions at about 550°C and ≥ 2 GPa (Zucali et al., 2002; Zucali and Spalla, 2011). Eclogite metamorphism is followed by decompression blueschist and greenschist re-equilibrations (Pognante et al., 1980; Zucali et al., 2002), related to later exhumation stages (e.g. Spalla et al., 1991). The shallower levels of the exhumation path took place between 45 and 30 Ma (Inger et al., 1996; Cortiana et al., 1998; Babist et al., 2006; Zanoni et al., 2010). To the east the SLZ is delimited by the Periadriatic line and in its inner part hosts the Biella and Traversella plutons (Zanoni et al., 2008; Zanoni 2010, 2016). The Biella pluton shows concentric zoning with the outer part constituted by monzonite and the inner part by syenite and granite and a calc- alkaline composition (Bigioggero et al., 1994). The pluton has been dated at about 30 Ma (Romer et al., 1996; Berger et al., 2012) and its country rocks belong to the Eclogitic Micaschists Complex (Fig. 2). Along the northeaster and southwester margins of the
Biella pluton country rocks consist of metapelites, meta-aplites and metagranitods with minor metabasites. During the Alpine convergence country rocks recorded up to six ductile deformation stages that predated the intrusion of the pluton. Only locally syn-intrusive folding and faulting are recorded in the country rocks. Generally brittle structures post-date pluton emplacement. The igneous rocks record a magmatic foliation that in place is parallel to the pluton margin. During the emplacement the country rocks recorded different type of contact metamorphism assemblages that vary with the country rock type and the distance from the pluton margin. The contact metamorphism parageneses form ne-grained coronitic structures that overprinted eclogite parageneses and local greenschist parageneses. With the distance from the pluton the amount of contact metamorphism parageneses decrease. Close to the pluton margin the contact metamorphic mineral assemblages are characterised by plagioclase, K-feldspar, cordierite, biotite, spinel, Al-silicate (sillimanite closer and andalusite farer from the pluton), and locally corundum, orthopyroxene and garnet. Locally, up to about 10 m far from the pluton margin, partial melting is recorded. With the distance from the pluton corundum, orthopyroxene, garnet, spinel, and sillimanite disappear. The contact metamorphic minerals are detected up to about 900 m far from the pluton in plain view (Fig. 2). In igneous rocks interstitial amphibole has an Al content compatible with intrusion depth variable between 4 and 7 km. Ti content in amphibole and equilibrium between amphibole and plagioclase are consistent with intrusion temperature between 670 and 720°C (Zanoni et al., 2010). In the country rocks temperature peak, reached during pluton crystallisation, vary between about 700°C at the pluton margin, and 550°C at about 600 m far from the pluton (Zanoni et al., 2010). The comparison of thermal estimates in the country rocks with a 2D conductive thermal model for pluton cooling shows that the best t is for initial temperature in the country rocks between 430 and 530°C at 8 km depth (Fig. 3). That involves a thermal gradient of the country rock at time of intrusion ranging between 55 and 65°C/km. The crustal level of Biella pluton emplacement is as shallow as a few kilometres and this is consistent with magmatic rocks intersecting all ductile structures in the country rocks and with contact metamorphism assemblages replacing greenschist facies assemblages. The computed extent of the aureole for the simulations is wider than the mapped one because the computed thermal boundary of the aureole is between 300 and 400°C. Finally, the thermal gradient of the country rocks at the time of pluton intrusion is suf ciently high to justify the emplacement of Biella pluton during the accomplishment of the break-off of the Alpine slab
Zanoni, la inspiración oculta de Alexandre Dumas
En esta tesis he demostrado que la novela de Edward Bulwer-Lytton (1803-1873), Zanoni (1842), fue la fuente de inspiración de Dumas padre (1802-1870) para un sinfín de personajes y elementos argumentales de Le Comte de Monte-Cristo (1844-1846); para cuatro obras de la pentalogía sobre la Revolución Francesa Mémoires d'un médecin (1846-1851) (Joseph Balsamo, Le collier de la reine, Ange Pitou y La Comtesse de Charny) y para La femme au collier de velours (1849). He analizado la intertextualidad de Zanoni y las novelas de Dumas comenzando con la influencia de Zanoni en Le Comte de Monte-Cristo y Mémoires d'un médecin en el plano de las ideas, ya que la ideología política de Zanoni (sobre la Revolución Francesa y la aristocracia del s. XIX y su regeneración, el dandismo) influyó, sin duda, en la de Dumas. Asimismo, las similitudes entre los argumentos, entre Zanoni y Montecristo y entre otros personajes (Mejnour/Faria, Albert/Glyndon, Viola/Haydée) o el que ambas obras tengan un mismo mensaje colonialista y una teoría artística idéntica prueban que Dumas se basó en Zanoni para crear Le Comte de Monte-Cristo. A su vez, he mostrado que las diferencias entre ambas novelas (Filide/Haydée, la figura de Napoleón, presente en la obra de Dumas...) se deben a modas e intereses comerciales. A su vez, los envenenamientos en Zanoni han influido en los de Le Comte de Monte-Cristo y la vindicta de Zanoni y la de Montecristo y Cagliostro están basadas en la venganza templaria de Cagliostro; en este aspecto, la influencia de Zanoni se extiende a Mémoires d'un médecin. Además, muchos elementos de Zanoni se encuentran en Le Comte de Monte-Cristo, Joseph Balsamo, Le collier de la reine, Ange Pitou y La Comtesse de Charny. Por otro lado, he demostrado que los personajes Gottlieb Murr y Antonia, de La femme au collier de velours, están basados en los de Rath Krespel, de E.T.A. Hoffmann, pero, también, en Gaetano Pisani y Viola, lo que, junto a otros aspectos, prueban la influencia de Zanoni. Por todo ello, he rebatido la explicación de Dumas sobre el origen de Le Comte de Monte-Cristo en su obra Causeries (1854) y he impugnado dos certezas comúnmente aceptadas, demostrando la gran influencia de Zanoni, una obra relegada al olvido, y la gran complejidad de Le Comte de Monte-Cristo, una novela desdeñada como superficial.376 p
Armamentario anestesiologico (XIX-XX SECOLO)
Se si perde la memoria del passato, il presente diventa offuscato, ed oscuro il futuro: spinti da questa considerazione, ci siamo imposti di raccogliere, identificare e catalogare la vecchia strumentazione e le vecchie attrezzature anestesiologiche che, ora, sono esposte alla “curiosità” (e si spera non solo dei curiosi) degli addetti e non addetti ai lavori presso l’ Istituto di Anestesia e Rianimazione del Policlinico S.Orsola.
Crediamo che il lavoro, al quale spontaneamente ci siamo obbligati, sia stato utile soprattutto per evitare la dispersione ulteriore del materiale “storico” della nostra Disciplina: come è accaduto in quasi tutti gli Ospedali, il materiale e gli strumenti, sorpassati e pressati dalle successive nuove tecnologie, sono stati dichiarati “obsoleti e disinventariabili”, accantonati in luoghi sempre meno accessibili e successivamente allontanati. Una dispersione deplorevole, irrimediabile ed amara che può essere parzialmente addolcita dal pensiero che, in alcuni casi, il materiale dismesso è stato inviato nei Paesi poveri; la maggior parte, purtroppo, rottamata (senza incentivi..).
Un’altra considerazione è da porre: rispetto ad altre Discipline che affondano la loro storia in tempi più antichi, la storia della nostra Anestesia, specie quella della moderna Anestesia, è più recente, per cui lo strumentario da raccogliere non poteva essere particolarmente abbondante.
Purtuttavia la raccolta del materiale, effettuata negli ultimi 25 anni, ha prodotto un soddisfacente risultato: almeno quello di aggiungere qualcosa al lavoro certosino e prezioso al quale si dedicò, anni orsono, un grande Maestro dell’Anestesia, lo Storico della nostra Disciplina e Amico e Collega Prof. Gualtiero Bellucci, al quale idealmente facciamo omaggio della nostra fatica.
Sul solco e sull’esempio del Prof. Bellucci, ora l’Anestesia italiana può contare su due Sedi nelle quali sono stati salvati ed esposti i nostri “strumenti del mestiere”: la sede di Siena, più ricca e preziosa, e, ora, quella di Bologna; con la speranza che anche in altre Sedi si realizzino analoghe iniziative.
Vorremmo aggiungere un’ulteriore considerazione sullo spirito che ci ha animato nel ripristino e nella messa a punto dello strumentario raccolto. Con entusiasmo da neofiti e con tanto divertimento abbiamo smontato e ripulito (con la paglietta) le attrezzature di ogni traccia di ruggine ed incrostazione del passato, ne abbiamo riattivato i meccanismi, abbiamo effettuato l’identificazione (con l’ausilio di Internet e del volume catalogo di Bellucci), poi abbiamo provveduto alla catalogazione, eseguite le fotografie ed attuata l’impaginazione in un volumetto senza molte pretese: al riguardo, si è evitata la qualificazione di museo, perché, la nostra, è da considerarsi una semplice “raccolta” di materiale anestesiologico effettuata in nome e per conto della Scuola di Specializzazione di Anestesia e Rianimazione dell’Università di Bologna.
Come già verificatosi nei confronti di una analoga”impresa” attuata di recente ed inerente la raccolta dell’”Armamentario chirurgico della Scuola Bolognese”, anche il nostro Strumentario anestesiologico sarà immesso nel percorso SMA che è il Sistema Museale di Ateneo dell’Alma Mater bolognese.
L’operazione suddescritta, ovviamente, si è avvalsa, oltre che del nostro materiale, non disperso e già disponibile, anche di qualche comodato d’uso e di alcune donazioni spontanee (o “spintanee”) da parte di Colleghi ed Amici che hanno contribuito ad arricchire ed impreziosire la nostra raccolta, e di cui ci piace fare menzione (in ordine alfabetico) ringraziare sentitamente: Amigoni, Bellusci (un Chirurgo che si è dedicato alla sistematizzazione dei pannelli), Caporaloni, Chiodo, Colesanti, Di Virgilio, Maldarizzi, Mele, Merola, Preziosa, Spagnolo, e Zanoni: essi si sono privati di alcuni pezzi cui erano affezionati e li hanno offerti all’esposizione.
Operazione, infine, che si è avvalsa dell’entusiasmo di un vero amico dell’A..
Scientific Bestiarium: the Living, the Dead and the Normal
My aim is to analyse scientific literature and its representation of the animal body in relation to the disciplinary institutions of its time, namely zootechnics. I will focus on the nineteenth century as the moment of birth of a specific biological discourse and as the moment of deployment of the Industrial Revolution, which had a significant impact on animal breeding. This conjuncture produces a radical new image of the animal body and of animality in general, which plays an important role not only in science and zootechnics, but also in philosophy and the human sciences. I will frame the evolution of scientific discourses on the animal body from the Greeks to the Modern Age, in order to present their material history in relation to the concrete practices that involved animals in their time. I will finally focus on two of the most important scientific models of the nineteenth century – Pasteurism and Darwinism – as cutting-edge moments in the history of biology, precisely due to their innovative relation to the zootechnical institution and its related conceptualization of the body
Economia - XVII edizione
Traduzione italiana di Maria Teresa Musacchio (Capp. 1-3/20-34) e Carla Zanoni (Capp. 4-19
«Due fontane che di diverso effetto hanno liquore»: l’intertestualità in traduzione. Il caso ‘Zanoni’ di E. G. Bulwer-Lytton (1842)
This article deals with the all-but-forgotten literary reception of a Victorian author, Edward Bulwer-Lytton, who became famous in the nineteenth century in Italy thanks to the translations by Francesco Cusani, a famous historian of that period. Then, the author will be compared to the translator, according to the most recent studies in translational stylistics and intertextuality, focusing on the novel Zanoni (1842), translated by Cusani in 1848.L’articolo illustra la fortuna letteraria avuta dall’autore vittoriano oggi poco frequentato, Edward Bulwer-Lytton, che divenne celebre nell’Italia dell’Ottocento grazie alle traduzioni dello storico, Francesco Cusani. Si procederà, dunque, ad un confronto tra autore e traduttore, secondo i più recenti studi in stilistica traduttiva e intertestualità, focalizzando l’attenzione sulla produzione del romanzo Zanoni (1842), tradotto dal Cusani nel 1848
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