Von der Bezeugung zur narrativen Vergegenwärtigung. Fokalisierung im Reisebuch des Syrers Ḥanna Dyāb (1764)

Travelogues involve different truth claims, depending on whether their authors attempt on the one hand to convey received knowledge about entities and places, or on the other hand, present accounts of the traveler character’s own experiences. This study focuses on a travelogue from 1764 written by the Arabian Nights’ Syrian storyteller, Ḥanna Dyāb. Having written his travelogue more than 50 years after his trip to Paris, he evidently conceived of his narrative as a means to re-enact his experiences as a young traveler. To describe his particular self-staging in this autodiegetic narration “before fiction” (Paige 2011), I argue that an understanding of focalization as a graded visual mediation between the character’s inner life and the reader is needed. This approach helps one grasp how, with reference to Dyāb’s travelogue, truth is not something the traveler witnesses, but rather something the reader is invited to realize. I conclude that, with this shift from witnessing to visualization (Vergegenwärtigung), Dyāb’s travelogue fulfills a core function of literature.

Les experiences de retour des sans-papiers rentrés en Equateur: Ressources et defies, mesures proposes pour un retour viable

Notre compréhension de la migration du retour est encore très limitée. Ce sujet n’a que peu retenu l’attention des spécialistes de la migration et il existe peu d’études qui donnent une vision différenciée sur les divers types de « retourné-e-s », leurs motivations à retourner dans leurs pays, les défis qu’ils/elles affrontent et les ressources dont ils/elles disposent pour parvenir à se réinsérer dans les pays d’origine. Il existe en particulier un manque important d’études qui examinent en détail la situation spécifique du retour des migrant-e-s sans-papiers et l’impact de l’aide de programmes gouvernementaux pour leur réinsertion socio-économique. Cette lacune est particulièrement marquée dans le cas de la Suisse. Confronté à la situation d’absence d’évaluations des programmes d’appui au retour des sans-papiers, et dans le but d’y apporter des améliorations possibles à son propre programme, le Service de la Population du canton de Vaud a chargé Yvonne Riaño de mener une recherche sur la situation de retour des sans-papiers retournés en Équateur entre 2008-2010 avec l’appui du programme. La recherche présentée ici se base sur un travail de terrain réalisé en Équateur en 2010. Nous avons rencontré 25 familles (70% du total des familles rentrées avec l’aide du Canton de Vaud) habitant dans diverses régions du pays et avons recueilli leurs expériences de retour. La méthodologie choisie pour la récolte des données est qualitative et combine entretiens narratifs et semi-directifs. La recherche examine les raisons d'émigration et du retour des personnes interviewées ainsi que la situation actuelle de leurs projets de réinsertion, leurs ressources disponibles et le défis auxquels elles font face pour la réalisation de leurs projets. Six principes clés sont proposés pour repenser l’aide au retour de façon à pouvoir garantir un retour viable.

Optimal Confidence Bands for Shape-Restricted Curves

Let Y be a stochastic process on [0,1] satisfying dY(t)=n 1/2 f(t)dt+dW(t) , where n≥1 is a given scale parameter (`sample size'), W is standard Brownian motion and f is an unknown function. Utilizing suitable multiscale tests, we construct confidence bands for f with guaranteed given coverage probability, assuming that f is isotonic or convex. These confidence bands are computationally feasible and shown to be asymptotically sharp optimal in an appropriate sense.

The behaviour of incompatible elements during hydrous melting of metasomatized peridotite at 4–6 GPa and 1000 °C–1200 °C

Trace element behavior during hydrous melting of a metasomatized garnet–peridotite was examined at pressures of 4–6 GPa and temperatures of 1000 °C–1200 °C, conditions appropriate for fluid penetrating the mantle wedge atop the subducting slab. Experiments were performed in a rocking multi-anvil apparatus using a diamond-trap setup. The compositions of the fluid and melt phases were measured using the cryogenic LA-ICP-MS technique. The water-saturated solidus of the K-lherzolite composition is located between 900 °C and 1000 °C at 4 GPa and between 1000 °C and 1100 °C at 5 and 6 GPa. The partition coefficients between fluid or melt and clinopyroxene reveal an asymmetric MREE trough with a minimum at Dy. The clinopyroxene in equilibrium with aqueous fluids is characterized by DUfluid–cpx > DThfluid–cpx while DUmelt–cpx tends to be similar to DThmelt–cpx. The partition coefficients between fluid or melt and garnet reveal very strong light to heavy REE fractionation, DLa/DLu from 95 (hydrous melt) to 1600 (aqueous fluid). The LILE are highly incompatible with partition coefficients > 50. The behavior of HFSE are decoupled, with DZr,Hf close to 1 while DNb,Ta > 10. Garnet is characterized by DUmelt/fluid–garnet < DThmelt/fluid–garnet. A comparison of our experimental partitioning results for trivalent cations as well as the results from the literature and the calculations carried out using the lattice strain model adapted to the presence of water in the bulk system indicates that H2O in the fluid or melt phase has a prominent effect on trace element partitioning. Garnet in mantle rocks in equilibrium with an aqueous fluid is characterized by significantly higher Do(3 +) for REE in the X site of the garnet compared with the partitioning values of the optimal cation in garnet in equilibrium with hydrous melts. Our data show for the first time that the change in the nature of the mobile phase (fluid vs. melt) does affect the affinities of trace elements into the garnet crystal at conditions below the second critical endpoint of the system. The same also applies for clinopyroxene, although this is less clear. Consequently, our new data allow for refinements in predictive modeling of element transfer from the slab to the mantle wedge and of possible compositions of metasomatized mantle that sources OIB magmatism.