https://hdl.handle.net/2072/378192 2026-04-19T14:54:02Z 2026-04-19T14:54:02Z Artigas Raventós, Antoni Carlet, Jean Martin-Loeches, Ignacio Niederman, Michael Torres, Antoni Universitat Autònoma de Barcelona. Departament de Medicina https://hdl.handle.net/2072/489424 2026-04-14T05:27:37Z 2018-01-01T00:00:00Z

23rd International Symposium on Infections in the Critically Ill Patient Artigas Raventós, Antoni; Carlet, Jean; Martin-Loeches, Ignacio; Niederman, Michael; Torres, Antoni; Universitat Autònoma de Barcelona. Departament de Medicina This 23rd International Symposium on Infections in the Critically Ill Patient aims to review current concepts, technology and present advances in infections in critically ill patient.

2018-01-01T00:00:00Z Quintana, Lluís https://hdl.handle.net/2072/489419 2026-04-13T01:13:31Z 2013-01-01T00:00:00Z

Prosa de ficció i educació literària : notes sobre un desencontre Quintana, Lluís En aquest article ens proposem explicar per què la ficció en prosa ha tardat a introduir-se en les classes de literatura; els diferents gèneres que han estat tractats, especialment la novel·la realista; les reticències amb les quals han acollit aquesta novel·la, i les dificultats que s'hi ha trobat una vegada incorporades. Pretenem que aquest estudi aporte pautes per trobar noves aplicacions de la prosa de ficció en l'ensenyament de la literatura a la secundària.

2013-01-01T00:00:00Z Lains Amaral, João Solá, Ana Rita Bento dos Santos, Telmo M. Chichorro, Martim https://hdl.handle.net/2072/489400 2026-03-30T06:53:35Z 2022-01-01T00:00:00Z

Detrital zircon similarities and dissimilarities between the Iberian Pyrite Belt, Ossa-Morena Zone and Meguma Lains Amaral, João; Solá, Ana Rita; Bento dos Santos, Telmo M.; Chichorro, Martim Acknowledgement. We thank Ícaro Dias da Silva and an anonymous reviewer for their constructive comments and suggestions. We also acknowledged Jose Javier Álvaro Blasco and Laura Rincón for editorial handling. We acknowledge the support of FCT through PhD grant SFRH/BD/138791/2018 to João Lains Amaral and through project UIDB/50019/2020 to Instituto Dom Luiz.; Despite the so-called exotic nature of the South Portuguese Zone relatively to the other major domains of the Iberian Massif of peri-Gondwanan affinity, Devonian detrital rocks of the oldest strata in the Iberian Pyrite Belt have a remarkable resemblance with the Ossa-Morena Zone's Neoproterozoic-Cambrian rocks and the West Meguma's Cambrian-Ordovician rocks, presenting the so-called "West African signature". Using published U-Pb detrital zircon data, we discuss the similarities and dissimilarities between the Iberian Pyrite Belt, Ossa-Morena Zone and West Meguma Terrane through multidimensional scaling, comparing them with other zones of the Iberian Massif, Saxo-Thuringian Zone, Avalonia-Ganderia, and the North African cratonic regions. Our findings show that multidimensional scaling is not entirely effective in displaying the dissimilarities between the peri-Gondwanan terranes due to the background noise caused by the overwhelming number of CadomianPanafrican ages. However, it becomes a powerful tool if these ages are filtered. A dominant Meguma-type provenance (Cambro-Ordovician) for the middle-upper Devonian rocks of the Iberian Pyrite Belt is demonstrated, mainly attending to their similar Birimian-Eburnean pattern. The possibility of minor contributions from the lower Cambrian rocks of the Ossa-Morena Zone into the Iberian Pyrite Belt quartzites is unlikely, as the latter lack the 1.9Ga peak that characterises the Ossa-Morena Zone sediments. Additionally, the remarkable similarities between Ossa-Morena Zone and West Meguma's detrital rocks strongly suggest a similar paleogeographic setting (but diachronic?) for both terrains from the Ediacaran to Lower Ordovician times relative to the North African blocks.

2022-01-01T00:00:00Z Chichorro, Martim Solá, Ana Rita Bento dos Santos, Telmo M. Lains Amaral, João Crispim, Lourenço https://hdl.handle.net/2072/489399 2026-03-30T06:53:28Z 2022-01-01T00:00:00Z

Cadomian/Pan-African consolidation of the Iberian Massif assessed by its detrital and inherited zircon populations : is the ~610Ma age peak a persistent Cadomian magmatic inheritance or the key to unravel its Pan-African basement? Chichorro, Martim; Solá, Ana Rita; Bento dos Santos, Telmo M.; Lains Amaral, João; Crispim, Lourenço Acknowledgement. Martim Chichorro is grateful for the funding provided by GeoBioTec (UIDB/04035/2020). We acknowledge the support of Portuguese Fundação para a Ciência e a Tecnologia (FCT) through PhD grant SFRH/BD/138791/2018 to João Lains Amaral. This work was funded by the FCT I.P./MCTES through national funds (PIDDAC) - UIDB/50019/2020 to Telmo M. Bento dos Santos via IDL - Instituto Dom Luiz. Geopark Naturtejo is also gratefully acknowledged for long-term logistic support. Insightful comments, suggestions and corrections provided by Josep Maria Casas and an anonymous reviewer are kindly acknowledged. Finally, the authors would like to express their gratitude to the Guest Editor; This work assessed the age distribution of Cadomian/Pan-African orogenic events (550-590 and 605-790Ma, respectively) in several zones of Iberian Massif by means of detrital and inherited zircon analysis compilation. Detrital zircon age spectra show that throughout the late Neoproterozoic-to-Early Ordovician era (~120Ma sedimentary record), the main systematic peak occurs at ~610Ma, followed by peaks at typical Cadomian ages (~590-550Ma). Inherited zircons incorporated in Cambrian-to-Lower Ordovician igneous rocks show typical Cadomian ages (~590-550Ma) but, once again, a remarkably consistent Pan-African ~610Ma peak occurs. In accordance with compiled zircon data and taking into account the evidence of North African peri-cratonic inliers, Ediacaran (~610Ma) zircons incorporated in Paleozoic magmas provide indirect evidence of Pan-African magmatism, suggesting that these magmas and synorogenic sediments are likely to constitute the cryptic stratigraphic infrastructure of most of the Iberian Massif. The main source of ~610Ma inherited zircons may be the lateral chrono-equivalents of the Saghro and Bou Salda-M'Gouna Groups (Anti-Atlas, Morocco) and/or coeval igneous rocks from West African Craton or Trans-Sahara Belt, emplaced at a stratigraphic level below the lateEdiacaran sediments of the Ossa Morena Zone and the Central Iberian Zone. Assuming that the Iberian crust is a fragment of the Pan-African orogen, a relative paleoposition situated between the West African Craton and the Trans-Saharan Belt during the Late Neoproterozoic is proposed. The closed-system behaviour of Stenian-Tonian detrital zircon ages in the Trans-Sahara Belt suggests that this mega-cordillera acted as a barrier, in paleogeographic terms, to separating the Sahara Metacraton from Iberia. In Iberia, the opening of the system to Stenian-Tonian detrital zircon during the Ordovician indicates that, at that time, the Trans-Saharan Belt had already become a vast peneplain, which favoured a large drainage system with a long-distance transport mechanism that fed the passive continental margins.

2022-01-01T00:00:00Z