AA VV (2012). La enseñanza de la historia, entre otredades y subalternidades. Cuadernos de Historia 7. Montevideo: Biblioteca Nacional. 180 páginas

Fil: De Amézola, Gonzalo Alvaro. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación. Instituto de Investigaciones en Humanidades y Ciencias Sociales (UNLP-CONICET); Argentina.

Moran J. C. y colaboradores. Proust más allá de Proust. Buenos Aires, Editorial de la Campana (Segunda edición 2005), Colección Universidad, 180 pp

Fil: Bertucci, Alejandra Isabel. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Gregory Nagy. Poetry as Performance, Homer and Beyond. Cambrige-New York-Melbourne, Cambridge University Press, 1996, ix + 254 pp. ; Gregory Nagy. Homeric Questions, Austin, University of Texas Press, 1996, ix + 180 pp.

Fil: Zecchin de Fasano, Graciela Cristina. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Ismail Kadaré. Eschyle ou le grand perdant, Paris, Fayard, 1995, 180 pp.

Fil: Pepe de Suárez, Luz Enriqueta Aurelia. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Petrography and geochemistry of lithic clasts in sediments obtained from ODP Leg 180 sites

This report includes the petrographic description and reviews the distribution of lithic clasts in sediments drilled during Leg 180 in the Woodlark Basin (southwest Pacific). The lithic clasts include (1) metamorphic rocks; (2) granites; (3) serpentinites, gabbros, dolerites, and basalts likely derived from the Papuan ophiolite belt; (4) rare alkaline volcanites reworked in middle Miocene sediments; (5) medium- to high-K calc-alkaline island arc volcanites, in part as reworked clasts, and explosive products deposited by fallout or reworked by turbiditic currents; and (6) rare sedimentary fragments. At the footwall sites the clast assemblage evidences the association of dolerites and evolved gabbroic rocks; the serpentinite likely pertaining to the same ophiolitic complex are likely derived from onland outcrops and transported by means of turbidity currents. On the whole, extensional tectonics active at least since the middle Pliocene can be inferred. The calc-alkaline volcanism is in continuity with the arc-related products from the Papua Peninsula and D'Entrecasteaux Islands and with the latest volcanics of the Miocene Trobrian arc. However, the medium- to high-K and shoshonitic products do not display a significant temporal evolution within the stratigraphic setting. Lava clasts, volcanogenic grains, and glass shards are associated with turbidity currents, whereas in the Pliocene of northern margin the increasing frequency of tephra (glass shards and vesicular silicic fragments) suggests more explosive activity and increasing contribution to the sediments from aerial fallout materials. Evidence of localized alkalic volcanism of presumable early to middle Miocene age is a new finding. It could represent a rift phase earlier than or coeval to the first opening of the Woodlark Basin or, less probably, could derive from depositional trajectories diverted from an adjacent basin.

AA VV (2012). La enseñanza de la historia, entre otredades y subalternidades. Cuadernos de Historia 7. Montevideo: Biblioteca Nacional. 180 páginas

Fil: De Amézola, Gonzalo Alvaro. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación. Instituto de Investigaciones en Humanidades y Ciencias Sociales (UNLP-CONICET); Argentina.

Moran J. C. y colaboradores. Proust más allá de Proust. Buenos Aires, Editorial de la Campana (Segunda edición 2005), Colección Universidad, 180 pp

Fil: Bertucci, Alejandra Isabel. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.