The goal of this thesis is to analyze the textual composition of René Goscinny’s Astérix and Le petit Nicolas, demonstrating how they differ and why. Taking a statistical look at the comparative qualities of each series of works, the structural differences and similarities in language use in these two series and their respective media are highlighted and compared. Though one might expect more complicated language use in traditional text by virtue of its format, analysis of average word length, average sentence length, lexical diversity, the prevalence of specific forms (the passé composé, possessive pronouns, etc.), and preferred collocations (ils sont fous, ces romains !) shows interesting results. Though Le petit Nicolas has longer sentences and more relative pronouns (and hence more clauses per sentence on average), Astérix has longer words and more lexical diversity. A similar comparison of the albums of Astérix written by Goscinny to those of Uderzo, paying additional attention to the structural elements of each album (usage of narration and sound effects, for example) shows that Goscinny's love of reusing phrases is far greater than Uderzo's, and that the two have very different ideas of timing as expressed in narration boxes.

In this review study, we ask ourselves if decoherence theory can solve the problems of measurement in quantum mechanics. After an introduction to decoherence theory, we present the problem of preferred basis, the problem of non-observability of interference and the problem of definite outcomes. We present Zurek's theory of environment induced superselection rules and find that the problem of preferred basis and the problem of non-observability of interference can be solved through decoherence theory, but not the problem of outcomes, if we accept the eigenstate-eigenvalue link and the Born statistical interpretation. We reveal that these two concepts are essential in the Copenhagen interpretations of quantum mechanics, and give an account for von Neumann's and Wigner's conscious collapse interpretation as well as a detailed description of Bohr's and Heisenberg's interpretation. We discuss how Bohr's and Heisenberg's interpretation relates to decoherence with a special emphasis on the irreducibility of classical concepts as interpreted by Don Howard. During the discussion, we critique Wigner's use of the word "consciousness" as opposed to von Neumann's use, as well as Howard's decisively ontological approach to Bohr through an antithetical Kantian approach. We conclude by stating that decoherence theory cannot decisively solve the problem of definite outcomes of quantum mechanics, even when considering it in relation to the Copenhagen interpretation.

Continental rifting is an important geodynamic process during which the Earth's outer-most rigid shell undergoes continuous stretching resulting in continental break-up and theformation of new oceanic basins. The East African Rift System, which has two continentalsegments comprising largely of the East African Rift (EAR) to the West and the easternmostsegment Madagascar, is the largest narrow rift on Earth. However, the driving mechanismsof continental rifting remain poorly understood due to a lack of numerical infrastructure tosimulate rifting, the lack of knowledge of the underlying mantle dynamics, and poor knowl-edge of mantle rheology. Here, we use state-of-art computational modeling of the upper660 km of the Earth to: 1) provide a better understanding of mantle flow patterns and themantle rheology beneath Madagascar, 2) to elucidate the main driving forces of observedpresent-day∼E-W opening in the EAR, and 3) to investigate the role of multiple plumesor a superplume in driving surface deformation in the EAR. In chapter 1, we simulate EdgeDriven convection (EDC), constrained by a lithospheric thickness model beneath Madagas-car. The mantle flow associated with the EDC is used to calculate induced olivine aggregates'Lattice Preferred Orientation (LPO), known as seismic anisotropy. The predicted LPO isthen used to calculate synthetic seismic anisotropy, which were compared with observationsacross the island. Through a series of comparisons, we found that asthenospheric flow result-ing from undulations in lithospheric thickness variations is the dominant source of the seismicanisotropy, but fossilized structures from an ancient shear zone may play a role in southern Madagascar. Our results suggest that the rheological conditions needed for the formationof seismic anisotropy, dislocation creep, dominates the upper asthenosphere beneath Mada-gascar and likely other continental regions. In chapter 2, we use a 3D numerical model ofthe lithosphere-asthenosphere system to simulate instantaneous lithospheric deformation inthe EAR and surroundings. We test the hypothesis that the∼E-W extension of the EAR isdriven by large scale forces arising from topography and internal density gradients, known aslithospheric buoyancy forces. We calculate surface deformation solely driven by lithosphericbuoyancy forces and compare them with surface velocity observations. The lithosphericbuoyancy forces are implemented by imposing observed topography at the model surfaceand lateral density variations in the crust and mantle down to a compensation depth of 100km. Our results indicate that the large-scale∼E-W extension across East Africa is driven bylithospheric buoyancy forces, but not along-rift surface motions in deforming zones. In chap-ter 3, we test the hypothesis that the anomalous northward rift-parallel deformation observedin the deforming zones of the EAR is driven by viscous coupling between the lithosphereand deep upwelling mantle material, known as a superplume, flowing northward. We testtwo end-member plume models including a multiple plumes model simulated using high res-olution shear wave tomography-derived thermal anomaly and a superplume model (Africansuperplume) simulated by imposing a northward mantle-wind on the multiple plumes model.Our results suggest that the horizontal tractions from northward mantle flow associated withthe African Superplume is needed to explain observations of rift-parallel surface motions indeforming zones from GNSS/GPS data and northward oriented seismic anisotropy beneaththe EAR. Overall, this work yields a better understanding of the geodynamics of Africa. / Doctor of Philosophy / Continental rifting is an important geodynamic process during which the Earth's outer-most rigid shell undergoes continuous stretching resulting in continental break-up and theformation of new oceanic basins. The East African Rift System, which has two continentalsegments comprising largely of the East African Rift (EAR) to the West and the easternmostsegment Madagascar, is the largest narrow rift on Earth. However, the driving mechanismsof continental rifting remain poorly understood due to a lack of numerical infrastructure tosimulate rifting, the lack of knowledge of the underlying mantle dynamics, and poor knowl-edge of mantle rheology. Here, we use state-of-art computational modeling of the upper660 km of the Earth to: 1) provide a better understanding of mantle flow patterns and themantle rheology beneath Madagascar, 2) to elucidate the main driving forces of observedpresent-day∼E-W opening in the EAR, and 3) to investigate the role of multiple plumesor a superplume in driving surface deformation in the EAR. In chapter 1, we simulate EdgeDriven convection (EDC), constrained by a lithospheric thickness model beneath Madagas-car. The mantle flow associated with the EDC is used to calculate induced olivine aggregates'Lattice Preferred Orientation (LPO), known as seismic anisotropy. The predicted LPO isthen used to calculate synthetic seismic anisotropy, which were compared with observationsacross the island. Through a series of comparisons, we found that asthenospheric flow result-ing from undulations in lithospheric thickness variations is the dominant source of the seismicanisotropy, but fossilized structures from an ancient shear zone may play a role in southern Madagascar. Our results suggest that the rheological conditions needed for the formationof seismic anisotropy, dislocation creep, dominates the upper asthenosphere beneath Mada-gascar and likely other continental regions. In chapter 2, we use a 3D numerical model ofthe lithosphere-asthenosphere system to simulate instantaneous lithospheric deformation inthe EAR and surroundings. We test the hypothesis that the∼E-W extension of the EAR isdriven by large scale forces arising from topography and internal density gradients, known aslithospheric buoyancy forces. We calculate surface deformation solely driven by lithosphericbuoyancy forces and compare them with surface velocity observations. The lithosphericbuoyancy forces are implemented by imposing observed topography at the model surfaceand lateral density variations in the crust and mantle down to a compensation depth of 100km. Our results indicate that the large-scale∼E-W extension across East Africa is driven bylithospheric buoyancy forces, but not along-rift surface motions in deforming zones. In chap-ter 3, we test the hypothesis that the anomalous northward rift-parallel deformation observedin the deforming zones of the EAR is driven by viscous coupling between the lithosphereand deep upwelling mantle material, known as a superplume, flowing northward. We testtwo end-member plume models including a multiple plumes model simulated using high res-olution shear wave tomography-derived thermal anomaly and a superplume model (Africansuperplume) simulated by imposing a northward mantle-wind on the multiple plumes model.Our results suggest that the horizontal tractions from northward mantle flow associated withthe African Superplume is needed to explain observations of rift-parallel surface motions indeforming zones from GNSS/GPS data and northward oriented seismic anisotropy beneaththe EAR. Overall, this work yields a better understanding of the geodynamics of Africa.

La réserve générale interdite de partage entre les membres est un avoir obligatoire, impartageable tout au long de l’existence de la coopérative et sujet à la «dévolution désintéressée en cas de liquidation ou de dissolution». Cette réserve fonctionne comme un levier de soutien au développement de la coopérative et du mouvement coopératif dans son ensemble. Le principe de l’impartageabilité de la réserve est l’interdiction faite à toutes les coopératives du Québec de partager la réserve générale entre tous les membres et l’interdiction de la diminuer, notamment par l’attribution d’une ristourne tout au long de l’existence de la coopérative. En effet, l’impartageabilité de la réserve se fonde sur l’idée que la coopérative n’a pas pour but l’accumulation des capitaux afin de les répartir entre les membres, mais il s’agit de la création d’un capital collectif qui bénéficie à tous les adhérents présents et futurs. Si le concept de l’impartageabilité de la réserve interdit donc le partage de la réserve tout au long de l’existence de la coopérative, cette même interdiction prend le nom de la dévolution désintéressée de l’actif net au moment de la disparition de la coopérative. Cette dévolution désintéressée signifie l’interdiction faite à toutes les coopératives non financières de partager le solde de l’actif lors de la disparition (dissolution ou liquidation) de la coopérative à l’exception des coopératives agricoles qui peuvent décider dans ce cas, de distribuer le solde de l’actif aux membres sans qu’on sache les raisons de cette exception. Par ailleurs, l’impartageabilité de la réserve est considérée comme un simple inconvénient juridique pour les membres et a connu quelques réécritures dans les législations sur les coopératives sans qu’on connaisse vraiment les raisons de ces modifications. L’objectif de notre thèse est d’engager une discussion critique autour du questionnement central suivant : au regard du cadre juridique actuel sur les coopératives, le principe de l’impartageabilité de la réserve doit être maintenu comme tel dans la Loi sur les coopératives, ou être tout simplement supprimé, comme dans la société par actions, où il est inexistant sans que cette suppression ne porte atteinte à la notion juridique de la coopérative? Plus précisément, quel est ce cadre juridique et quels sont les motifs qui peuvent plaider en faveur du maintien ou de la suppression du principe de l’impartageabilité de la réserve? Pour répondre à cette question, cette thèse se divise en deux parties. La première partie explore le cadre juridique des coopératives non financières au Québec en comparaison avec certains concepts juridiques issus d’autres législations. Elle étudie les fondements juridiques sous-jacents à l’impartageabilité de la réserve en droit québécois des coopératives non financières. La deuxième partie réalise une discussion critique autour de l’histoire du principe de l’impartageabilité de la réserve (ch. 3), des différents arguments juridiques disponibles (ch. 4) et d’hypothèses articulées autour des effets concrets disponibles (ch. 5). Elle explore ces dimensions au soutien du maintien ou non de l’impartageabilité de la réserve de la législation actuelle sur les coopératives non financières. Bien que la recherche effectuée conduise à une réponse nuancée, l'ensemble des résultats milite plutôt en faveur du maintien du principe de l'impartageabilité de la réserve. Au préalable, l’observation des fondements juridiques des concepts sous-jacents à l’impartageabilité de la réserve en droit québécois des coopératives non financières a permis de comprendre les concepts sous-jacents à ce principe avant de répondre à la question autour de son maintien ou de sa suppression de la législation actuelle sur les coopératives. La discussion réalisée a permis de souligner l’importance d’une réalité de base assez évidente : ce principe permet de préserver la réserve, utile au développement de la coopérative et du mouvement coopératif dans son ensemble. De plus, ce principe de l’impartageabilité de la réserve s’inscrit dans le cadre de la vocation sociale de la coopérative, qui n’a pas pour but la maximisation du profit pécuniaire. L’impartageabilité de la réserve s’inscrit également dans le cadre de la cohérence du droit québécois des coopératives avec la notion de coopérative telle que définie par le mouvement coopératif québécois et l’ACI tout en répondant aux finalités historiques d’équité entre les générations et de solidarité. Enfin, même si la discussion des arguments tirés des illustrations de données comptables et de quelques entretiens réalisés avec certains membres actifs du mouvement coopératif ne permet pas de mener à toute conclusion ferme, il ressort que l’impartageabilité de la réserve ne freinerait pas la tendance à la hausse des investissements et du chiffre d’affaires des coopératives non financières. Cette interdiction constituerait même un mécanisme d’autofinancement de la coopérative et un symbole de solidarité. / Forbidden general reserve sharing among members is mandatory to have, indivisible throughout the existence of the cooperative and subject to the "disinterested distribution upon liquidation or dissolution". The reserve functions as a support lever for the development of the cooperative and the cooperative movement as a whole. The principle of nondivisibility of the reserve is the prohibition to all cooperatives in Quebec to share the general reserve of all members and the prohibition of the decline, including the allocation of any rebate along the existence of the cooperative. Indeed, the nondivisibility of the reserve is based on the idea that the cooperative is not to the accumulation of capital in order to distribute them among members, but it is the creation of a collective capital that benefits all current and future members. If the concept of nondivisibility reserve therefore prohibits the sharing of reserve throughout the existence of the cooperative, the same prohibition takes the name of the disinterested distribution of net assets at the time of the disappearance of the cooperative. This disinterested distribution is in turn the ban on all non-financial cooperatives to share the remaining assets in the disappearance (dissolution or liquidation) of the cooperative except agricultural cooperatives that can decide in this case, distribute the remaining assets to members without knowing the reasons for the exception. Moreover, the nondivisibility of the reserve is considered a mere legal disadvantage for members and has had some rewrites in co-operative legislation without knowing either the reasons for these changes. The aim of our thesis is to engage a critical discussion around the following central question: given the current legal framework on cooperatives, the principle of nondivisibility the reserve must be maintained as such in the Cooperatives Act, or simply be deleted, as in the corporation, where it is nonexistent without this deletion does not affect the legal concept of the cooperative? Specifically, what is the legal framework and what are the motives which may plead in favor of maintaining or deletion of the principle of nondivisibility reserve? To answer this question, this thesis is divided into two parts. The first part explores the legal framework for non-financial cooperatives in Québec compared with certain legal concepts from other legislation. It examines the legal basis underlying the nondivisibility the Quebec law reserves of non-financial cooperatives. The second part makes a critical discussion around the history of the principle of nondivisibility Reserve (ch. 3), different legal arguments available (ch. 4) and assumptions based around concrete effects available (ch. 5). She exploire these dimensions to support maintaining or not the nondivisibility Reserve current legislation on non-financial cooperatives. Although the research lead to a nuanced response, the overall results rather militates in favor of maintaining the principle of nondivisibility reserve. Previously, the observation of the legal foundations of the underlying concepts in nondivisibility the Quebec law reserves of non-financial cooperatives helped to understand the concepts underlying this principle before answering the question about its maintenance or suppression of current legislation on cooperatives. The discussion made it possible to highlight the importance of a fairly obvious basic reality: this principle allows to preserve the reserve, useful for the development of the cooperative and the cooperative movement as a whole. Moreover, this principle of nondivisibility of the reserve part of the social mission of the cooperative, which is not intended maximizing monetary profit. The nondivisibility Reserve also part of the consistency of Quebec law cooperatives with the concept of cooperatives as defined by the Quebec cooperative movement and the ICA while addressing the historical purposes of fairness between generations and solidarity. Finally, while discussing the arguments of accounting data and illustrations of some interviews with some active members of the cooperative movement does not lead to any firm conclusion, it appears that the nondivisibility the reserve does not dampen the trend rising investment and sales of non-financial cooperatives. This prohibition even be a self-financing mechanism of the cooperative and a symbol of solidarity.

In South Africa the death of a significant caregiver is a haunting possibility. Violence, crime, road accidents, HIV/AIDS, cancer, diabetes and substance abuse are household words that describe some of the causes of "untimely deaths" of parents who still have young, school-going children. These children carry their bereavement with them to school. The challenge of standing with them lies not only with their caregivers, but also with staff and children in our school community. In co-authoring conversations with children in our school who have experienced bereavement and loss, this qualitative study used research as co-search to uncover children's preferred knowledges and spiritualities about coping, hope, care and communities of concern. This study used therapy-as-research and participatory action research-as-therapy in what developed into a network of caring communities for the participants, caregivers and therapist. / Practical Theology / M. Th. (Pastoral Therapy)

This qualitative action research was activated at the junction between three sites of operation of modern power: the site of the woman in the family, religious and cultural power discourses and the professional discourses of therapy. Using an action research design for this study focused the research on reaping benefits in real terms for the research participants. The researcher applied a postStructuralist, feminist and narrative approach to the phenomenon of failed personhood as manifested in the lives of two White Afrikaans women. Narrative therapy methodologiElS, steeped in a religious studies ethic were valuable guides on the therapy-as-research journeys, ensuring the exposure and deconstruction of dominant cultural and religious power discourses. In the course of the therapeutic and research journeys, various narrative therapy methodologies were used with positive effect on the life world of the participants. These methodologies included the externalisation of problems and the discovery of unique outcomes that constitute alternative, preferred life stories that contradict problem-saturated life stories of failed personhood. The research participants engaged in individual and communal conversations, relanguaging their self-narratives and religious narratives as part of the coconstruction of their preferred identities of moral agency and hope. Support networks were created for the research participants, Mara and Grace, to strengthen their new self- and religious narratives and to dislodge the power of the normative cultural and religious discourses of rugged individualism. In one instance, the researcher incorporated the healing power of South African bush veld, by inviting a group of women on a series of expeditions into the wilderness as part of Mara's journey. fn Grace's narrative, we utilised the modern technologies of the internet to connect her with a virtual response team and the Anti-Anorexia/Anti-Bulimia League. Storytelling and reflecting conversations formed the basis of the therapy-asresearch processes. The research participants extended therapy conversations beyond the therapy room, by actively participating in their therapy-as-research journeys. In line with narrative approaches, the researcher encouraged them to honour their skills and knowledges on their journeys: Mara extended her therapy by making resistance quilts while Grace assimilated her art, poetry and resistance writing into her healing process. / Religious Studies and Arabic / D. Litt. et Phil. (Religious Studies)

A trama de magmas graníticos alojados na crosta intermediária e superior pode-se originar pela ação de forças de corpo (ascensionais, convectivas) e/ou tectônicas. Diferentes mecanismos podem concorrer para a formação de tramas, embora a interação entre a deformação magmática e a tectônica regional seja um dos mecanismos fundamentais, notadamente nos granitos alojados em faixas orogênicas. No Domínio Apiaí da Faixa Ribeira (SP - PR), os batólitos graníticos alongados têm sido historicamente classificados como sintectônicos, ou seja, colocados durante o desenvolvimento de um arco magmático continental neoproterozóico. Os plútons menores, de forma circular a ovalada, geralmente discordantes e com típica coloração avermelhada, são considerados pós-tectônicos ou alojados após a colisão continental entre os diferentes blocos litosféricos que formaram a Faixa Ribeira. Essa classificação esquemática tem sido baseada em geoquímica e geocronologia dos granitos. Este trabalho identificou e mapeou a trama interna dos plútons sin-tectônicos (Ribeirão Branco) e pós-tectônicos (Capão Bonito e Sguário) utilizando a anisotropia de suscetibilidade magnética (ASM), de forma a inserí-los propriamente nos modelos de classificação tectônica, cujas premissas básicas são de natureza estrutural. Os granitos porfiríticos (Ribeirão Branco e Itaóca) possuem uma elevada suscetibilidade magnética (k 10-2 SI), a qual é menor (k 5 x 10-3 SI) nos granitos vermelhos (Capão Bonito e Sguário). A suscetibilidade dos granitos porfiríticos é proveniente de óxidos ferromagnéticos, notadamente magnetita pobre em Ti, que encontra-se frequentemente associada com titanita, biotita e anfibólio. Nos granitos vermelhos a suscetibilidade é gerada por magnetita, variavelmente oxidada (maghemita) e Ti-hematita (hemo-ilmenita), havendo também significativa contribuição da fração paramagnética (biotita cloritizada) à suscetibilidade total nas rochas, quando k < 10-3 SI. O grau de anisotropia magnética (P) tanto nos granitos porfiríticos como nos vermelhos é variável, porém tipicamente maior nos porfiríticos (P = 1,14, dp. 0,08), se comparado aos vermelhos (P = 1,07, dp. 0,05). A maior anisotropia de suscetibilidade no plúton Ribeirão Branco é atribuída a uma incipiente foliação detectada em vários setores do granito, que contrasta com a microestrutura aparentemente isótropa dos granitos vermelhos. O estudo da trama de silicatos no granito porfirítico Itaóca e no granito Capão Bonito mostrou que os eixos principais de anisotropia de suscetibilidade magnética e da orientação preferencial de forma (OPF) de feldspato e de biotita, são correspondentes, porém, comumente oblíquos. Essa obliquidade entre eixos é atribuída às características físicas próprias (forma, tamanho e anisotropia) dos minerais marcadores da trama. O estudo combinado da ASM e da OPF revelou ainda que P tende a crescer com a intensidade da orientação preferencial de silicatos, o que permitiu identificar os domínios de maior deformação magmática e correlacioná-los com a estrutura regional. A trama magnética do granito Ribeirão Branco organiza-se em coerência com uma tectônica regional transcorrente sinistral. Na margem ocidental deste granito, contudo, a orientação da trama é diferente do restante do maciço, tendo sido aparentemente afetada pela intrusão do granito Sguário. A trama magnética do Ribeirão Branco contrasta com a do plúton Itaóca, este último exibindo um padrão concêntrico que antecedeu ao desenvolvimento da deformação transcorrente regional. Zircões do Itaóca forneceram uma idade U-Pb (SHRIMP) concordante de 623 ± 10 Ma, atribuída à cristalização deste plúton. Dados da literatura indicam que o granito Capão Bonito é aproximadamente 15 Ma mais jovem que os batólitos de granito porfirítico. O Capão Bonito, entretanto, apresenta uma trama muito bem organizada, típica de intrusões sin-tectônicas, destacando-se excelente alinhamento da lineação magnética. No granito Sguário, o arranjo da trama é tipicamente helicoidal e, junto com a estrutura do Capão Bonito, podem ter sido organizadas em resposta a uma deformação transcorrente E-W destral. Este evento tardio estaria associado à reativação da zona de cisalhamento Ribeira, que afetou a borda sul do granito Itaóca e que contém uma componente extensional. A deformação transtensiva E-W, que favoreceu a injeção dos granitos vermelhos no Domínio Apiaí, sucederia a um evento tectonomagmático principal, que teria sido responsável pela colocação e deformação dos batólitos de granito porfirítico. A intrusão dos grandes corpos graníticos ocorreu em torno de 615 Ma e foi relacionada à convergência crustal e estiramento subparalelo à Faixa Ribeira, com a deformação localizada notadamente nas estruturas transcorrentes de direção NE-SW. / The fabric of granitic magmas emplaced in the middle and upper crustal levels can be caused by the stress action during the ascension and convection of plutons and/or tectonic strain. Several mechanisms can contribute for the previous thing, nevertheless the interaction between the distortions and tectonic is the domineering one, principally in granites located in orogenic belts. In the Apiaí domain of the Ribeira belt (SP-PR) the elongated granitic batholiths have been historically classified like syn-tectonic and them was emplaced during the development of a neoproterozoic continental magmatic arch. Small Plutons with subcircular to oval forms generally discordant with regard to the disposition of the regional structures and that in turn possess feldspars of reddish typical colour, had been considered pos-tectonic, and therefore, emplaced after the collision that joined the different litho-tectonic units that constitute the Ribeira orogenic belt. This schematic classification of these granites relicts on geochemistry and geochronology data. In this study was identified and recorded in map the internal fabric of the syn-tectonic Ribeirão Branco granite and of the pos-tectonic Capão Bonito and Sguário granites using the anisotropy of magnetic susceptibility (AMS) with the aim of inserting them appropriately in the models of tectonic classification whose basic premises are of structural nature. The porphyritic Ribeirão Branco and Itaóca granites have a high magnetic susceptibility (k = 10-2 SI), which is minor than (k = 5 x 10-3 SI) in the red granites (Capão Bonito, Sguário). In the first ones the poor Ti magnetite is the main source of susceptibility, commonly associated to titanite, biotite and amphibole. In the red granites, the susceptibility is provided by magnetite variability rusty (maghemite) and Ti - hematite (hemo-ilmenite), in addition to the significant contribution of biotite altered by hydrothermal processes. The grade of anisotropy rise (P) in the porphyritic granites (P = 1,14 SD. 0,08) and this is bigger than in the red ones (P = 1,07, SD. 0,05). In the Ribeirão Branco pluton, the high value of P is attributed to an incipient foliation detected in several sectors, which contrasts with the microstructure seemingly isotropic of the red granites. The study of the fabrics of silicates in the porphyritic granites Ribeirão Branco and Itaóca revealed that the orientations of the main axes of AMS and of shape preferred orientation (SPO) of feldspar and mafic silicates (biotite + amphibole) are congruent, nevertheless some obliquities occur. Those obliquities are attributed to the influence of the proper characteristics (form, size, anisotropy) of the marker minerals of the respective sub fabrics. In the same way, the above-mentioned study of silicates fabric demonstrated that P tends to grow up with the intensity of the SPO of silicates, which allowed to identify domains with major magmatic distortion into de granitic bodies and to correlate them with the regional structure. In general, the magnetic fabric of the Ribeirão Branco granite is organized coherently with the tectonic regional sinestral strike-slip shear zones; nevertheless, in the western sector the orientation of the magnetic fabric was likely modified by the accommodation of the Sguário granite. In the Itaóca granite, the organization of the magnetic fabric is different if compared with fabrics of the previous pluton. In Itaóca granite was recorded a fabric with a concentric organization in 623 ± 10Ma. (MSWD 0,31), according to the concordant U-Pb (SHRIMP) age in zircons obtained for the crystallization of the granite, that seems to be occurred before the strain related with the activation of the regional strike-slip shear zones. Geochronology data of the literature indicates that the Capão Bonito granite is approximately 15 Ma. younger than the batholiths of porphyritic granite. The Capão Bonito granite has an organized fabric typical of syn-tectonic intrusions that has an excellent alignment of the magnetic lineation. In the granite Sguário, the fabric has a spiral organization, in the same way as recorded in Capão Bonito, like response to a strain associated with to a small strike-slip shear zone with W-E direction. This event would be related to the reactivation of the Ribeira strike-slip shear zone, which affected the south sector of the Itaóca granite, with the participation of an extensional component. The W-E transtensive deformation that favoured the injection of the red granites in the Apiaí Domain likely was subsequent to a main tetonomagmatic event and this should have been the responsible by the emplacement and strain in the porphyritic granites. The intrusion of the big granitic bodies ~ 615 Ma. and could be it related to the convergence between crustal blocks and to the consequent stretching sub parallel of the Ribeira belt, in which the distortion was located remarkably in the strike-slip shear zones with NE-SW direction.

La spécificité de la tradition monétaire de Henry Thornton, Ralph George Hawtrey, John Maynard Keynes et John Richard Hicks, est de considérer le taux d'intérêt comme une variable influencée par la banque centrale. Ces auteurs peuvent être rattachés à une même tradition monétaire, différente de celle de Knut Wicksell, où le taux d'intérêt est déterminé par une variable réelle: le taux de profit. Dans la tradition de Thornton, le prêt et l'emprunt renvoient une vente et un achat de titres de dette. Ces derniers prennent une forme différente selon la période étudiée. Au dix-neuvième siècle, Thornton proposait que la Banque d'Angleterre contrôle, par des variations de son taux d'escompte, le prix de la liquidité de court-terme, étant la substituabilité des traites commerciales en monnaie. Un siècle plus tard, cette influence était effective. Cependant, au XXe siècle, avec le développement des marchés financiers, d'autre canaux de transmissions de la politique monétaire sont apparus. Bien que négligée par 1 littérature, une des controverses les plus représentatives de cette époque est celle d'Hawtre Keynes et Hicks. Ils conviennent que le taux court est un phénomène monétaire. En revanche, ils ne s'accordent pas sur la nature du taux long. Les débats portent sur la théorie pionnière d Keynes de la structure par terme des taux d'intérêt, les effets d'annonces, ainsi que les limite de l'arbitrage. / The specificity of the monetary tradition of Henry Thornton, Ralph George Hawtrey, John Maynard Keynes and John Richard Hicks is to consider the interest rate as mainly determined by the monetary policy. Those authors are part of the same monetary tradition, different that Knut Wicksell for whom the interest rate is a real variable: the rate of profit. The process of borrowing and lending, in the monetary tradition analyzed in my PhD thesis, corresponds to a sale and a purchase of debts. Debts take a different form according to the period studied. ln the nineteenth century, Thornton wrote that the Bank of England should be able to manage, by varying its discount rate, the price of short-term liquidity, which is the substitution of bills againt money. ln the twentieth century, other transmission channels of monetary policy appeared wit the evolution of financial markets. Although neglected by the literature, one of the most representative controversy at that time was between Hawtrey, Keynes and Hicks. All made a theory in which the short-term rate is a monetary phenomenon. They however disagreed on the nature of the long-term rate. The debate is on Keynes's pioneering theory of the term structur of interest rates, the announcement effects, and the limits to arbitrage.

La fovéa est la seule zone de la rétine où l’acuité visuelle est maximale. Les mécanismes qui visent à déterminer à quels endroits vont avoir lieu les prochaines fixations restent débattus. Certains auteurs suggèrent que les yeux sont principalement attirés par les zones les plus saillantes de la scène. D’autres suggèrent qu’ils sont orientés vers les objets. Les propriétés du système oculomoteur contraignent également les mouvements oculaires. L’objectif de cette thèse était de départager ces différents points de vue en examinant la contribution respective et le décours temporel des facteurs visuo-moteurs de bas niveau et des facteurs cognitifs de plus haut niveau dans la détermination des mouvements oculaires. Nous nous sommes focalisés sur trois phénomènes comportementaux clés : la tendance à bouger les yeux à proximité du centre des objets (Prefered-Viewing Location), les répercussions qu’ont ces positions d’atterrissage sur les durées initiales des fixations (Inverted Optimal-Viewing-Position) et les probabilités de refixation (Optimal-Viewing-Position). Nous avons observé que ces trois effets émergeaient, et ce, quel que soit le type de stimulus testé: des objets, des mots ou des objets sans signification. Cela suggère que ces effets reflètent les propriétés de bas niveau des systèmes visuel et oculomoteur. Par ailleurs, nous avons observé que l’endroit où les yeux atterrissaient au sein de l’objet était également influencé au fil du temps par les traitements de plus haut-niveau des propriétés du stimulus. Les saccades initiées plus tardivement atterrissaient plus proches de la zone la plus informative de l’objet. / High-quality vision is restricted to the fovea - a small region at the center of gaze. The mechanisms that determine which locations in a scene are selected for fixation remain debated. Some suggest that eye movements are mainly driven by the salient features in a scene. Others suggest that eye guidance is object based. The properties of the oculomotor system also strongly constrain eye behavior, but these have been neglected in most existing models. The purpose of this thesis was to disentangle between these different views, by investigating how low-level visuomotor factors versus higher-level cognitive factors contribute to eye movements towards and within isolated objects, and with which time course. We focused on three viewing-position effects: the tendency to move the eyes near the centers of objects (the PVL effect), and the repercussions these initial landing positions have on initial fixation durations (the I-OVP effect) and refixation probabilities (the OVP effect). We found that these three viewing-position effects emerged, and were comparable, in all stimulus types that we tested in this thesis: objects, words and even meaningless non-objects. This suggests that the effects reflect low-level properties of the visual and oculomotor systems. Furthermore, we found that where the eye moved within objects became influenced by ongoing processing of higher-level stimulus properties (e.g., object affordances) over time. Later- compared to early-triggered initial saccades, and even more so within-object refixations, were biased towards the most informative part of the objects, and away from their center of gravity.

La Tolérance aux pannes Byzantines (BFT) est de plus en plus cruciale avec l'évolution d'applications et en raison de la croissance de l'innovation technologique en informatique. Bien que des dizaines de protocoles BFT aient été introduites dans les années précédentes, leur mise en œuvre ne semble pas satisfaisant. Pour faire face à cette complexité, due à la dépendance d'un protocole d'une situation, nous tentons une approche qui permettra de sélectionner un protocole en fonction d'une situation. Ceci nous paraît, en s'inspirant de tout système d'encrage, comme une démarche nécessaire pour aborder la problématique de la BFT. Dans cette thèse, nous introduisons un modèle de sélection ainsi que l'algorithme qui permet de simplifier et d'automatiser le processus d'élection d'un protocole. Ce mécanisme est conçu pour fonctionner selon 3 modes : statique, dynamique et heuristique. Les deux derniers modes, nécessitent l'introduction d'un système réactif, nous ont conduits à présenter un nouveau modèle BFT: Adapt. Il réagit à tout changement et effectue, d'une manière adaptée, la commutation entre les protocoles d'une façon dynamique. Le mode statique permet aux utilisateurs de BFT de choisir un protocole BFT en une seule fois. Ceci est très utile dans les services Web et les " Clouds " où le BFT peut être fournit comme un service inclut dans le contrat (SLA). Ce mode est essentiellement conçu pour les systèmes qui n'ont pas trop d'états fluctuants. Pour ce faire, un processus d'évaluation est en charge de faire correspondre, à priori, les préférences de l'utilisateur aux profils du protocole BFT nommé, en fonction des critères de fiabilité et de performance. Le protocole choisi est celui qui réalise le meilleur score d'évaluation. Le mécanisme est bien automatisé à travers des matrices mathématiques, et produit des sélections qui sont raisonnables. D'autres systèmes peuvent cependant avoir des conditions flottantes, il s'agit de la variation des charges ou de la taille de message qui n'est pas fixe. Dans ce cas, le mode statique ne peut continuer à être efficace et risque de ne pas pouvoir s'adapter aux nouvelles conditions. D'où la nécessité de trouver un moyen permettant de répondre aux nouvelles exigences d'une façon dynamique. Adapt combine un ensemble de protocoles BFT ainsi que leurs mécanismes de commutation pour assurer l'adaptation à l'évolution de l'état du système. Par conséquent, le "Meilleur" protocole est toujours sélectionné selon l'état du système. On obtient ainsi une qualité optimisée de service, i.e., la fiabilité et la performance. Adapt contrôle l'état du système grâce à ses mécanismes d'événements, et utilise une méthode de "Support Vector Regrssion" pour conduire aux prédictions en temps réel pour l'exécution des protocoles (par exemple, débit, latence, etc.). Ceci nous conduit aussi à un mode heuristique. En utilisant des heuristiques prédéfinies, on optimise les préférences de l'utilisateur afin d'améliorer le processus de sélection. L'évaluation de notre approche montre que le choix du "meilleur" protocole est automatisé et proche de la réalité de la même façon que dans le mode statique. En mode dynamique, Adapt permet toujours d'obtenir la performance optimale des protocoles disponibles. L'évaluation démontre, en plus, que la performance globale du système peut être améliorée de manière significative. Explorer d'autres cas qui ne conduisent pas de basculer entre les protocoles. Ceci est rendu possible grâce à la réalisation des prévisions d'une grande précision qui peuvent atteindre plus de 98%dans de nombreux cas. La thèse montre que cette adaptabilité est rendue possible grâce à l'utilisation des heuristiques dans un mode dynamique.