"Aber vielleicht wird erst der wahrhaft Leidende ganz frei." Freya Hobohm - Werner Krauss: Eine unbekannte Freundschaft. Unveröffentlichte Briefquellen unter Berücksichtigung ihrer literaturgeschichtlichen Implikationen

Literaturwissenschaft, Exil und Widerstand dargestellt am Beispiel von Erich Auerbach, Walter Benjamin und Werner Krauss

Kritik und Versöhnung : Beiträge im Handgemenge Kritischer Theorie

Während das Denken dem, woran es seine Synthese übt, Gewalt antut, folgt es zugleich einem Potential, das in seinem Gegenüber wartet, und gehorcht bewußtlos der Idee, an den Stücken wieder gutzumachen, was es selber verübte; der Philosophie wird dies Bewußtlose bewußt. Unversöhnlichem Denken ist die Hoffnung auf Versöhnung gesellt, weil der Widerstand des Denkens gegen das bloß Seiende, die gebieterische Freiheit des Subjekts, auch das am Objekt tendiert, was durch dessen Zurüstung zum Objekt diesem verloren ging." Getreu dieser Passage aus Adornos Negative Dialektik ließ der Kongress Kritik und Versöhnung an der Carl von Ossietzky Universität Oldenburg im Januar 2015 Studierende und Promovierende aus mehreren Universitäten zu Wort kommen, die auf je eigene Weise im genuinen Sinne der Kritischen Theorie intervenieren möchten. Der vorliegende Band dokumetiert sehr unterschiedliche Versuche, sich innerhalb der Maschen des durchfunktionalisierten akademischen Betriebs sowie darüber hinaus die Besinnung zu wahren und eine unversöhnliche Kritik gesellschaftlicher Verhältnisse zu üben

[Il barbiere di Siviglia.. Ecco ridente in cielo; arr.]

Notación musical grabada por L. Parent.Dedicatoria: "° Mademoiselle Joséphine d'Arquinvilliers"Copia digital : Biblioteca Digital Hispánica (Biblioteca Nacional de España)Copia digital. España : Ministerio de Cultura. Subdirección General de Coordinación Bibliotecaria, d2024Rústica.Título y mención de responsabilidad tomados de cubierta.Fecha de publicación 1856 según su presentación en el mes de diciembre de ese año en el Registro de la Propiedad Intelectual como consta en la Gaceta de Madrid citada.Portada litografiada firmada por A. Vialon.Registro de la Propiedad Intelectual: Ley de 1847: [sin número]; n. de solicitud de ingreso: [sin número]; fecha y datos de ingreso: [sin fecha], "137"; firma del depositante: [sin firma]Sello: "Chabal, Editeur de musique, 15, Boulevard Montmartre, Au coin de la Rue Vivienne

Traducción de hápax legómena griegos y neologismos latinos en la traducción latina interlineal del Libro de Job de la Biblia Políglota Complutense

The Complutensian Polyglot Bible (1514-1517), sponsored by the Cardinal Francisco Jiménez de Cisneros (1436-1517), reckons on interline translations for the Septuaginta column. Conceived as a Bible for research, the young man magister artium Juan de Vergara (1492-1557) accomplished the Latin interline interpretatio of the Book of Job, which has not been republished since the 16th Century and of which we make known in this article the translation procedures used with the Greek “hápax legómena” and the Latin neologisms minted by Vergara are released, as singular expressions of fidelity to the interline literalism and the interpretative realization of the Bible text.La Biblia Políglota Complutense (1514-1517), auspiciada por el Cardenal Francisco Jiménez de Cisneros (1436-1517), cuenta con traducciones interlineales para la columna de Septuaginta. Concebida como Biblia de estudio, el joven magister artium Juan de Vergara (1492-1557) realizó la interpretatio latina interlineal del libro de Job, que no se ha vuelto a publicar desde el s. XVI y de la que damos a conocer en este artículo los procedimientos de traducción usados con los hápax legómena griegos y los neologismos latinos acuñados por Juan de Vergara, como expresiones singulares de fidelidad al literalismo interlineal y de concreción interpretativa del texto bíblico

Contrasting styles of (U)HP rock exhumation along the Cenozoic Adria-Europe plate boundary (Western Alps, Calabria, Corsica)

Since the first discovery of ultrahigh pressure (UHP) rocks 30 years ago in the Western Alps, the mechanisms for exhumation of (U)HP terranes worldwide are still debated. In the western Mediterranean, the presently accepted model of synconvergent exhumation (e.g., the channel-flow model) is in conflict with parts of the geologic record. We synthesize regional geologic data and present alternative exhumation mechanisms that consider the role of divergence within subduction zones. These mechanisms, i.e., (i) the motion of the upper plate away from the trench and (ii) the rollback of the lower plate, are discussed in detail with particular reference to the Cenozoic Adria-Europe plate boundary, and along three different transects (Western Alps, Calabria-Sardinia, and Corsica-Northern Apennines). In the Western Alps, (U)HP rocks were exhumed from the greatest depth at the rear of the accretionary wedge during motion of the upper plate away from the trench. Exhumation was extremely fast, and associated with very low geothermal gradients. In Calabria, HP rocks were exhumed from shallower depths and at lower rates during rollback of the Adriatic plate, with repeated exhumation pulses progressively younging toward the foreland. Both mechanisms were active to create boundary divergence along the Corsica-Northern Apennines transect, where European southeastward subduction was progressively replaced along strike by Adriatic northwestward subduction. The tectonic scenario depicted for the Western Alps trench during Eocene exhumation of (U)HP rocks correlates well with present-day eastern Papua New Guinea, which is presented as a modern analog of the Paleogene Adria-Europe plate boundary

Etude geologique de la partie centrale du massif granitique de Gueret (Creuse, Massif Central francais)

Abstract The crystalline rocks of the Gueret plateau in the Central Massif of France consist essentially of the so-called Gueret granite and anatexites known as the Aubusson gneiss. The granite exhibits both intrusive and anatectic features. A detailed petrographic study indicates close relationships between the granite and the gneiss and, together with lead-alpha age determinations on zircon, supports the conclusion that the Gueret granite represents a local late-stage product of the Aubusson gneiss formed during remobilization of the migmatitic basement.</jats:p