15 resultados para Gilabert Jofré, Juan, 1350-1417-Biografies

em Université de Lausanne, Switzerland


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Sections through an oceanic plateau are preserved in tectonic slices in the Western Cordillera of Ecuador (South America). The San Juan section is a sequence of mafic-ultramafic cumulates. To establish that these plutonic rocks formed in an oceanic plateau setting, we have developed criteria that discriminate intrusions of oceanic plateaus from those of other tectonic settings. The mineralogy and crystallization sequence of the cumulates are similar to those of intra-plate magmas. Clinopyroxene predominates throughout, and orthopyroxene is only a minor component. Rocks of intermediate composition are absent, and hornblende is restricted to the uppermost massive gabbros within the sequence. The ultramafic cumulates are very depleted in light rare-earth elements (LREE), whereas the gabbros have flat or slightly enriched LREE patterns. The composition of the basaltic liquid in equilibrium with the peridotite, calculated using olivine compositions and REE contents of clinopyroxene, contains between 16% and 8% MgO and has a flat REE pattern. This melt is geochemically similar to other accreted oceanic plateau basalts, isotropic gabbros, and differentiated sills in western Ecuador. The Ecuadorian intrusive and extrusive rocks have a narrow range of epsilonNd(i) (+8 to +5) and have a rather large range of Pb isotopic ratios. Pb isotope systematics of the San Juan plutonic rocks and mineral separates lie along a mixing line between the depleted mantle (DMM) and the enriched-plume end members. This suggests that the Ecuadorian plutonic rocks generated from the mixing of two mantle sources, a depleted mid-oceanic ridge basalt (MORB) source and an enriched one. The latter is characterized by high (Pb-207/Pb-204)(i) ratios and could reflect a contamination by recycled either lower continental crust or oceanic pelagic sediments and (or) altered oceanic crust (enriched mantle type I, EMI). These data suggest that the San Juan sequence represents the plutonic components of an Early Cretaceous oceanic plateau, which accreted in the Late Cretaceous to the Ecuadorian margin.

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Cet article constitue une tentative de récit ethnographique qui compte rendre l'expérience vécue de la fête de San Juan/Inti Raymi dans la région d'Otavalo (Andes équatoriennes) de différents acteurs et de l'anthropologue. L'auteur s'essaie à la description minutieuse afin de montrer, à partir d'une perspective pragmatique, le développement des actions dans l'espace et dans le temps, permettant de mettre en évidence le savoir pratique et la créativité de ses interlocuteurs, ainsi que la dimension d'indétermination des situations. Par ce faire, aucune explication sous-jacente ou cachée est recherchée, le sens se trouvant dans la pratique festive même. L'abondance des détails a également pour objectif de faire vivre aux lecteurs les situations et de leur faire prendre conscience de leur caractère complexe et situé.

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Around 11.5 * 106 m3 of rock detached from the eastern slope of the Santa Cruz valley (San Juan province, Argentina) in the first fortnight of January 2005. The rockslide?debris avalanche blocked the course, resulting in the development of a lake with maximum length of around 3.5 km. The increase in the inflow rate from 47,000?74,000 m3/d between April and October to 304,000 m3/d between late October and the first fortnight of November, accelerated the growing rate of the lake. On 12 November 2005 the dam failed, releasing 24.6 * 106 m3 of water. The resulting outburst flood caused damages mainly on infrastructure, and affected the facilities of a hydropower dam which was under construction 250 km downstream from the source area. In this work we describe causes and consequences of the natural dam formation and failure, and we dynamically model the 2005 rockslide?debris avalanche with DAN3D. Additionally, as a volume ~ 24 * 106 m3of rocks still remain unstable in the slope, we use the results of the back analysis to forecast the formation of a future natural dam. We analyzed two potential scenarios: a partial slope failure of 6.5 * 106 m3 and a worst case where all the unstable volume remaining in the slope fails. The spreading of those potential events shows that a new blockage of the Santa Cruz River is likely to occur. According to their modeled morphometry and the contributing watershed upstream the blockage area, as the one of 2005, the dams would also be unstable. This study shows the importance of back and forward analysis that can be carried out to obtain critical information for land use planning, hazards mitigation, and emergency management.

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La question de savoir si la relation est différente réellement de son fondement se rencontre fréquemment dans les textes médiévaux à partir du milieu du treizième siècle. Elle se pose avant tout dans un cadre aristotélicien de discussion des catégories et revient à se demander si la catégorie de relation ajoute véritablement une chose supplémentaire, la relation, dans la réalité. Cette question s'inscrit dans une représentation réaliste des relations : pour la plupart des auteurs du treizième et du quatorzième siècle, le fait que des choses soient réellement reliées entre elles ne fait pas de doute. Deux hommes de même taille sont bel et bien égaux, c'est-à-dire réellement reliés entre eux par une relation d'égalité. La difficulté est alors de comprendre comment ces choses sont reliées entre elles, ou encore, ce qu'est exactement cette relation dont il est alors question. Faut-il dire que l'égalité dans chacun des hommes de même taille est une nouvelle chose qui s'ajoute à la substance de chacun d'eux et aux accidents de taille, appartenant à la catégorie de quantité, sur lesquels ces relations d'égalité sont fondées ? Ou faut-il dire que l'égalité est réelle d'une autre manière, c'est-à-dire sans pour autant ajouter une nouvelle chose à ce à quoi elle advient ? Ce problème, qui se rencontre déjà dans les tensions existant entre les différents exposés qu'Aristote a consacrés à cette catégorie, a reçu de multiples réponses. Celles-ci nous éclairent sur la manière dont le réel est appréhendé au Moyen-Âge et sur les débats ontologiques de l'époque. Le travail ici résumé entreprend de délimiter précisément ces réponses et propose une manière de les classer. -- Realism about relations: study of the answers given to the problem of the difference between a relation and its foundation (1250-1350) Summary Whether relation is really distinct from its foundation or not is a question that can easily be found in medieval texts from the mid-thirteenth century onwards. It comes from an aristotelian background, the discussion about the categories, and asks if the category of relation really posits another thing, i.e. a relation, in reality. It results from a realist perspective on relations. In fact, most thirteenth and fourteenth century thinkers held without doubt that things outside the mind are really connected between them. Two men sharing the same height are really equal, that is, really linked to each other by a relation of equality. What is then left to understand is how these things are linked between them, or the exact nature of the aforementioned relation. Should we say that the equality in each of the equally sized men is a new thing that adds to the substance of each of them and to the accidents of height, belonging tho the category of quantity, on which these relations are founded? Or should we say that equality is real in another way, that is, without adding a new thing to the subject acquiring it? We can already find this issue in Aristotle himself, emerging from disagreeing texts devoted to this category. It received various answers that enable us to understand better how reality was defined in the Middle Age and some of the ontological debates of the time. The work that is here summed up attempts to precisely delineate these various answers and to provide a way of classifying them.

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