A study of singular integral operators with shift

Nesta tese, consideram-se operadores integrais singulares com a acção extra de um operador de deslocacamento de Carleman e com coeficientes em diferentes classes de funções essencialmente limitadas. Nomeadamente, funções contínuas por troços, funções quase-periódicas e funções possuíndo factorização generalizada. Nos casos dos operadores integrais singulares com deslocamento dado pelo operador de reflexão ou pelo operador de salto no círculo unitário complexo, obtêm-se critérios para a propriedade de Fredholm. Para os coeficientes contínuos, uma fórmula do índice de Fredholm é apresentada. Estes resultados são consequência das relações de equivalência explícitas entre aqueles operadores e alguns operadores adicionais, tais como o operador integral singular, operadores de Toeplitz e operadores de Toeplitz mais Hankel. Além disso, as relações de equivalência permitem-nos obter um critério de invertibilidade e fórmulas para os inversos laterais dos operadores iniciais com coeficientes factorizáveis. Adicionalmente, aplicamos técnicas de análise numérica, tais como métodos de colocação de polinómios, para o estudo da dimensão do núcleo dos dois tipos de operadores integrais singulares com coeficientes contínuos por troços. Esta abordagem permite também a computação do inverso no sentido Moore-Penrose dos operadores principais. Para operadores integrais singulares com operadores de deslocamento do tipo Carleman preservando a orientação e com funções contínuas como coeficientes, são obtidos limites superiores da dimensão do núcleo. Tal é implementado utilizando algumas estimativas e com a ajuda de relações (explícitas) de equivalência entre operadores. Focamos ainda a nossa atenção na resolução e nas soluções de uma classe de equações integrais singulares com deslocamento que não pode ser reduzida a um problema de valor de fronteira binomial. De forma a atingir os objectivos propostos, foram utilizadas projecções complementares e identidades entre operadores. Desta forma, as equações em estudo são associadas a sistemas de equações integrais singulares. Estes sistemas são depois analisados utilizando um problema de valor de fronteira de Riemann. Este procedimento tem como consequência a construção das soluções das equações iniciais a partir das soluções de problemas de valor de fronteira de Riemann. Motivados por uma grande diversidade de aplicações, estendemos a definição de operador integral de Cauchy para espaços de Lebesgue sobre grupos topológicos. Assim, são investigadas as condições de invertibilidade dos operadores integrais neste contexto.

Física e contemporaneidade no ensino secundário: um contributo no âmbito da formação de professores

O presente trabalho versa a problemática da abordagem da Física Moderna e Contemporânea (FMC) no Ensino Secundário no quadro dos desafios que se colocam à educação científica actual. Num mundo em mudança em que o futuro não está garantido, o esforço educativo deve incluir a dimensão da importância do conhecimento na transformação dos indivíduos com vista à intervenção. A literatura tem apresentado a transposição para a sala de aula da Física desenvolvida ao longo do século XX, como relevante neste domínio. Esta relevância prende-se com a actualidade do conhecimento, com a associação a grande parte da tecnologia actual e ainda com a ligação ao conhecimento mais profundo da natureza e, supostamente, ao sentido do universo. Porém, uma escola de cariz essencialmente transmissivo e desencorajadora de itinerâncias pessoais, tornará muito limitativa a referida transposição. Vários são os constrangimentos da abordagem da FMC neste nível de ensino. Trata-se de um conhecimento contra-intuitivo, que suscita interpretações diversificadas e que se desenvolve formalmente com base em ferramentas matemáticas, em grande parte, não acessíveis a alunos do Ensino Secundário. A formação de professores é uma vertente essencial dentro desta problemática, podendo ser considerada, em muitos casos, deficiente ou desadequada por via do mesmo tipo de constrangimentos referidos. Este trabalho propõe-se estudar as possibilidades e potencialidades da formação de professores no contexto apresentado, a partir de um cenário alternativo que consideramos inovador. Para isso foi concebido, implementado e avaliado um Círculo de Estudos no âmbito da formação em FMC. Utilizando uma estratégia de investigação/ acção/ formação, ensaiou-se a integração de uma certa transdisciplinaridade e multidimensionalidade humana num percurso de natureza complexa, procurando-se a emergência a partir da interacção. À partida eram procurados indicadores de construção identitária e desenvolvimento da profissionalidade. Era ainda esperada a participação dos professores formandos na construção de materiais didácticos. Utilizando uma metodologia de cariz qualitativo na tipologia de estudo de caso, os dados foram recolhidos a partir de instrumentos preparados para o efeito como questionários, mas também de outras fontes como textos reflexivos dos professores e materiais didácticos elaborados pelos mesmos. Os resultados obtidos são de dois tipos. Em primeiro lugar mostram que o percurso efectuado produziu alterações ao nível do discurso dos professores, que revela valorização da itinerância e abertura à incerteza na abordagem da FMC, bem como uma maior familiarização com os conceitos. Por outro lado, os materiais de utilização em sala de aula produzidos foram considerados de interesse como contributos didácticos para utilização futura. Pensamos ainda poder afirmar que são apresentados elementos importantes para a definição de um desenho de formação de professores em FMC, com vista a um ensino e a uma aprendizagem pertinentes.

Digital storytelling: student ID in higher education

Identity achievement is related to personality, as well as cognitive and interpersonal development. In tandem with the deep structural changes that have taken place in society, education must also shift towards a teaching approach focused on learning and the overall development of the student. The integration of technology may be the drive to foster the needed changes. We draw on the literature of multiple subject areas as basis for our work, namely: identity construction and self-representation, within a psychological and social standpoint; Higher Education (HE) in Portugal after Bologna, college student development and other intrinsic relationships, namely the role of emotions and interpersonal relationships in the learning process; the technological evolution of storytelling towards Digital Storytelling (DS) – the Californian model – and its connections to identity and education. Ultimately we propose DS as the aggregator capable of humanizing HE while developing essential skills and competences. Grounded on an interpretative/constructivist paradigm, we implemented a qualitative case study to explore DS in HE. In three attempts to collect student data, we gathered detailed observation notes from two Story Circles; twelve student written reflections; fourteen Digital Stories and detailed observation notes from one Story Show. We carried out three focus groups with teachers where we discussed their perceptions of each student prior to and after watching the Digital Stories, in addition to their opinion on DS in HE as a teaching and learning method and its influence on interpersonal relationships. We sought understandings of the integration of DS to analyze student selfperception and self-representation in HE contexts and intersected our findings with teachers’ perceptions of their students. We compared teachers’ and students’ perspectives, through the analysis of data collected throughout the DS process – Story Circle, Story Creation and Story Show – and triangulated that information with the students’ personal reflections and teacher perceptions. Finally we questioned if and how DS may influence teachers’ perceptions of students. We found participants to be the ultimate gatekeepers in our study. Very few students and teachers voluntarily came forth to take part in the study, confirming the challenge remains in getting participants to see the value and understand the academic rigor of DS. Despite this reluctance, DS proved to be an asset for teachers and students directly and indirectly involved in the study. DS challenges HE contexts, namely teacher established perception of students; student’s own expectations regarding learning in HE; the emotional realm, the private vs. public dichotomy and the shift in educational roles.

Population dynamics and fisheries assessment of the bigeye thresher (Alopias superciliosus) in the Atlantic: a comparison between North Atlantic and South Atlantic stocks

Tese de doutoramento, Ciências do Mar, da Terra e do Ambiente (Biologia Pesqueira), Faculdade de Ciências e Tecnologia, Universidade do Algarve, 2015

Interrelation entre déficits métaboliques et neuropathologie associée à la maladie d’Alzheimer chez la souris 3xTg-AD

La maladie d’Alzheimer (MA) est la maladie neurodégénérative qui cause le plus important nombre de cas de démence. On estime que près de 15% des canadiens âgés de plus de 65 ans sont atteints de la MA. Avec le vieillissement de la population, le nombre de cas augmentera de manière substantielle dans les prochaines années. À l’heure actuelle, aucun traitement ne permet de ralentir la progression de la maladie. Pour plus de 99% des cas, ses causes exactes demeurent indéterminées. Toutefois, de nombreux facteurs de risque ont été identifiés. Parmi eux, on retrouve plusieurs facteurs liés au métabolisme énergétique dont l’obésité et le diabète de type 2 (DT2). De manière intéressante, des modifications du métabolisme, telles qu’une résistance à l’insuline centrale et périphérique, sont également observées chez les patients Alzheimer. Afin de mieux comprendre l’interaction entre le DT2 et la MA, nous avons d’abord étudié les altérations métaboliques chez la souris triple transgénique (3xTg-AD), un modèle murin de la MA. Nous avons, en premier lieu, observé une intolérance au glucose qui progresse avec l’âge, qui est plus importante chez les femelles et qui semble liée à l’accumulation du peptide beta-amyloïde (Aβ) humain dans le pancréas. Ensuite, nous avons nourri cette souris avec une diète riche en gras pour vérifier l’impact d’une aggravation des déficits métaboliques sur la pathologie Alzheimer. L’aggravation de l’intolérance au glucose chez les souris 3xTg-AD semblait liée à l’atrophie des îlots de Langerhans et, en conséquence, à une réduction de la production d’insuline en réponse à l’injection de glucose. En plus de l’aggravation des déficits métaboliques, la diète riche en gras a augmenté de manière drastique l’accumulation de la forme soluble du peptide Aβ dans le cortex et a déterioré la mémoire des souris 3xTg-AD. De manière intéressante, l’élévation du peptide Aβ et les troubles de la mémoire ont été rétablis par l’administration d’une seule dose d’insuline. Aussi, nous avons observé une augmentation du peptide Aβ dans le plasma 30 minutes à la suite de l’injection d’insuline, suggérant qu’il est possible que la baisse rapide du peptide soit en partie causée par une élévation de la clairance du peptide au cerveau. Ces résultats renforcent les évidences supportant le potentiel thérapeutique de l’insuline dans le traitement de la MA. Toutefois, les résultats chez les patients mettent en lumière l’inefficacité de l’administration intranasale d’insuline chez les porteurs de l’allèle 4 du gène de l’apolipoprotéine E (APOE4). Afin de comprendre les raisons qui expliquent cette différence de réponse à l’insuline chez les porteurs de l’APOE4, nous avons injecté des souris exprimant l’APOE3 et l’APOE4 humain avec de l’insuline dans le but de vérifier l’effet central et périphérique de l’insuline chez ces animaux. Les souris APOE4 montrent une plus importante élévation de la signalisation de l’insuline au cerveau comparativement aux souris APOE3. Cette plus haute réponse est aussi associée à une élévation plus importante de la phosphorylation de la protéine tau, un marqueur neuropathologique de la MA. En somme, ces résultats suggèrent qu’il existe un cercle vicieux entre la MA et le DT2. L’administration d’insuline a un potentiel thérapeutique intéressant pour la MA, malgré des effets limités chez les patients APOE4 en raison de son impact probable sur la phosphorylation de la protéine tau.

The Professional Legitimacy of the Taiwan-educated versus US-educated Taiwanese English Teachers

Thesis (Ph.D.)--University of Washington, 2015

Muslims in Public and Media Discourse in Western Europe: The Reproduction of Aporia and Exclusion

This chapter scrutinizes the dominant public discourse in Western Europe. Drawing on examples from the UK, Germany, and France but also from the Netherlands, Denmark and Spain it illustrates the gradual transformation of discourse from an “exotic Islam” to a “threatening Islam” that endangers European values and safety and suggests that the combination of this “securitization” of Islam and the monopoly of the “Muslim voice” by radical Muslim activists leads to a vicious circle of misrecognition and enhancing the aporia of Europe's Muslims.

O Processo de internacionalização das empresas angolanas e o seu impacto no crescimento e desenvolvimento económico: o caso da Sonangol

Dissertação de Mestrado apresentado ao Instituto Superior de Contabilidade e Administração do Porto para a obtenção do grau de Mestre em Empreendedorismo e Internacionalização. Os orientadores: Prof. Doutor José de Freitas Santos Profª. Doutora Maria Clara Dias Pinto Ribeiro

Radiation dose rates and exposure associated to Technologically Enhanced Naturally Occurring Radioactive Materials (TENORM) at locations of a Portuguese coal-fired power plant

Coal contains trace quantities of natural radionuclides such as Th-232, U-235, U-238, as well as their radioactive decay products and 40K. These radionuclides can be released as fly ash in atmospheric emissions from coal-fired power plants, dispersed into the environment and deposited on the surrounding top soils. Therefore, the natural radiation background level is enhanced and consequently increase the total dose for the nearby population. A radiation monitoring programme was used to assess the external dose contribution to the natural radiation background, potentially resulting from the dispersion of coal ash in past atmospheric emissions. Radiation measurements were carried out by gamma spectrometry in the vicinity of a Portuguese coal-fired power plant. The radiation monitoring was achieved both on and off site, being the boundary delimited by a 20 km circle centered in the stacks of the coal plant. The measured radionuclides concentrations for the uranium and thorium series ranged from 7.7 to 41.3 Bq/kg for Ra-226 and from 4.7 to 71.6 Bq/kg for Th-232, while K-40 concentrations ranged from 62.3 to 795.1 Bq/kg. The highest values were registered near the power plant and at distances between 6 and 20 km from the stacks, mainly in the prevailing wind direction. The absorbed dose rates were calculated for each sampling location: 13.97-84.00 ηGy/h, while measurements from previous studies carried out in 1993 registered values in the range of 16.6-77.6 ηGy/h. The highest values were registered at locations in the prevailing wind direction (NW-SE). This study has been primarily done to assess the radiation dose rates and exposure to the nearby population in the surroundings of a coal-fired power plant. The results suggest an enhancement or at least an influence in the background radiation due to the coal plant past activities.

Particulate matter flux deposition in the vicinity of a coal-fired power plant

This paper describes the methodology adopted to assess local air quality impact in the vicinity of a coal power plant located in the south of Portugal. Two sampling areas were selected to assess the deposition flux of dust fallout and its potential spatial heterogeneity. The sampling area was divided into two subareas: the inner, with higher sampling density and urban and suburban characteristics, inside a 6-km circle centered on the stacks, and an outer subarea, mainly rural, with lower sampling density within a radius of 20 km. Particulate matter deposition was studied in the vicinity of the coal fired power plant during three seasonal sampling campaigns. For the first one, the average annual flux of dust fallout was 22.51 g/(m2 yr), ranging from 4.20 to 65.94 g/(m2 yr); for the second one was 9.47 g/(m2 yr), ranging from 0.78 to 32.72 g/(m2 yr) and for the last one was 38.42 g/(m2 yr), ranging from 1.41 to 117.48 g/(m2 yr). The fallout during the second campaign turned out to be much lower than for others. This was in part due to meteorological local patterns but mostly due to the fact that the power plant was not working at full power during the second sampling campaign.155

Gestão de operações de um armazém

i Gestão de Operações de um armazém Patrícia Raquel Freitas Gomes Relatório de estágio apresentado ao Instituto Superior de Contabilidade e Administração do Porto para obtenção de Grau de Mestre em Logística Orientado por: Prof. Doutora Maria Teresa Ribeiro Pereira Coorientado por: Eng.º César Emanuel Marinho Carvalho Teixeira

Drivers of participation in collaborative consumption ventures

A Work Project, presented as part of the requirements for the Award of a Masters Degree in Management from the NOVA – School of Business and Economics

O Poder do Sultão e o Estado Otomano

O estado Otomano representou um dos mais complexos sistemas políticos da história do Islão. O seu sistema burocrático e militar recorria ao recrutamento (devşirme) de não-Muçulmanos composto por crianças provenientes da Romélia para evitar que qualquer membro da sociedade Otomana interviesse na política. Sem raízes estabelecidas na sociedade Otomana a sua lealdade concentrava-se numa instituição: o Sultão. No século dezoito e dezanove o exotismo Otomano cativou muitos dos Europeus, o Sultão foi descrito como o centro da sociedade Otomana com um poder absoluto sobre todos os que a compunham. O poder do Sultão era absolutista, porém, o estado Otomano estava desenhado de uma forma em que a sua estrutura não podia ser alterada, pela sua matiz Islâmica e também para não enfraquecer as bases que mantinham a cúpula de poder. Através da metodologia de process-tracing o nosso estudo analisa a forma como o Sultão obteve e legitimou o seu poder assim como os actores que serviram de contrapeso ao seu poder. No século dezanove, particularmente, nenhum Sultão possuía um poder absoluto, a dificuldade que enfrentavam por parte da sociedade Otomana para realizar reformas mostra que não podiam agir só pela sua vontade. O nosso estudo tem como objectivo criticar Karl Marx e Max Weber, consideramos que simplificam o sistema de governação Otomano. Esperamos expor como se organizava este império como estrutura política e qual o poder do Sultão, considerando o “Círculo de Equidade” como o principal modelo para o seu poder.

Contact metamorphism and emplacement of the western Adamello tonalite

The geodynamic forces acting in the Earth's interior manifest themselves in a variety of ways. Volcanoes are amongst the most impressive examples in this respect, but like with an iceberg, they only represent the tip of a more extensive system hidden underground. This system consists of a source region where melt forms and accumulates, feeder connections in which magma is transported towards the surface, and different reservoirs where it is stored before it eventually erupts to form a volcano. A magma represents a mixture of melt and crystals. The latter can be extracted from the source region, or form anywhere along the path towards their final crystallization place. They will retain information of the overall plumbing system. The host rocks of an intrusion, in contrast, provide information at the emplacement level. They record the effects of thermal and mechanical forces imposed by the magma. For a better understanding of the system, both parts - magmatic and metamorphic petrology - have to be integrated. I will demonstrate in my thesis that information from both is complementary. It is an iterative process, using constraints from one field to better constrain the other. Reading the history of the host rocks is not always straightforward. This is shown in chapter two, where a model for the formation of clustered garnets observed in the contact aureole is proposed. Fragments of garnets, older than the intrusive rocks are overgrown by garnet crystallizing due to the reheating during emplacement of the adjacent pluton. The formation of the clusters is therefore not a single event as generally assumed but the result of a two-stage process, namely the alteration of the old grains and the overgrowth and amalgamation of new garnet rims. This makes an important difference when applying petrological methods such as thermobarometry, geochronology or grain size distributions. The thermal conditions in the aureole are a strong function of the emplacement style of the pluton. therefore it is necessary to understand the pluton before drawing conclusions about its aureole. A study investigating the intrusive rocks by means of field, geochemical, geochronologi- cal and structural methods is presented in chapter three. This provided important information about the assembly of the intrusion, but also new insights on the nature of large, homogeneous plutons and the structure of the plumbing system in general. The incremental nature of the emplacement of the Western Adamello tonalité is documented, and the existence of an intermediate reservoir beneath homogeneous plutons is proposed. In chapter four it is demonstrated that information extracted from the host rock provides further constraints on the emplacement process of the intrusion. The temperatures obtain by combining field observations with phase petrology modeling are used together with thermal models to constrain the magmatic activity in the immediate intrusion. Instead of using the thermal models to control the petrology result, the inverse is done. The model parameters were changed until a match with the aureole temperatures was obtained. It is shown, that only a few combinations give a positive match and that temperature estimates from the aureole can constrain the frequency of ancient magmatic systems. In the fifth chapter, the Anisotropy of Magnetic Susceptibility of intrusive rocks is compared to 3D tomography. The obtained signal is a function of the shape and distribution of ferromagnetic grains, and is often used to infer flow directions of magma. It turns out that the signal is dominated by the shape of the magnetic crystals, and where they form tight clusters, also by their distribution. This is in good agreement with the predictions made in the theoretical and experimental literature. In the sixth chapter arguments for partial melting of host rock carbonates are presented. While at first very surprising, this is to be expected when considering the prior results from the intrusive study and experiments from the literature. Partial melting is documented by compelling microstructures, geochemical and structural data. The necessary conditions are far from extreme and this process might be more frequent than previously thought. The carbonate melt is highly mobile and can move along grain boundaries, infiltrating other rocks and ultimately alter the existing mineral assemblage. Finally, a mineralogical curiosity is presented in chapter seven. The mineral assemblage magne§site and calcite is in apparent equilibrium. It is well known that these two carbonates are not stable together in the system Ca0-Mg0-Fe0-C02. Indeed, magnesite and calcite should react to dolomite during metamorphism. The presented explanation for this '"forbidden" assemblage is, that a calcite melt infiltrated the magnesite bearing rock along grain boundaries and caused the peculiar microstructure. This is supported by isotopie disequilibrium between calcite and magnesite. A further implication of partially molten carbonates is, that the host rock drastically looses its strength so that its physical properties may be comparable to the ones of the intrusive rocks. This contrasting behavior of the host rock may ease the emplacement of the intrusion. We see that the circle closes and the iterative process of better constraining the emplacement could start again. - La Terre est en perpétuel mouvement et les forces tectoniques associées à ces mouvements se manifestent sous différentes formes. Les volcans en sont l'un des exemples les plus impressionnants, mais comme les icebergs, les laves émises en surfaces ne représentent que la pointe d'un vaste système caché dans les profondeurs. Ce système est constitué d'une région source, région où la roche source fond et produit le magma ; ce magma peut s'accumuler dans cette région source ou être transporté à travers différents conduits dans des réservoirs où le magma est stocké. Ce magma peut cristalliser in situ et produire des roches plutoniques ou alors être émis en surface. Un magma représente un mélange entre un liquide et des cristaux. Ces cristaux peuvent être extraits de la source ou se former tout au long du chemin jusqu'à l'endroit final de cristallisation. L'étude de ces cristaux peut ainsi donner des informations sur l'ensemble du système magmatique. Au contraire, les roches encaissantes fournissent des informations sur le niveau d'emplacement de l'intrusion. En effet ces roches enregistrent les effets thermiques et mécaniques imposés par le magma. Pour une meilleure compréhension du système, les deux parties, magmatique et métamorphique, doivent être intégrées. Cette thèse a pour but de montrer que les informations issues de l'étude des roches magmatiques et des roches encaissantes sont complémentaires. C'est un processus itératif qui utilise les contraintes d'un domaine pour améliorer la compréhension de l'autre. Comprendre l'histoire des roches encaissantes n'est pas toujours aisé. Ceci est démontré dans le chapitre deux, où un modèle de formation des grenats observés sous forme d'agrégats dans l'auréole de contact est proposé. Des fragments de grenats plus vieux que les roches intru- sives montrent une zone de surcroissance générée par l'apport thermique produit par la mise en place du pluton adjacent. La formation des agrégats de grenats n'est donc pas le résultat d'un seul événement, comme on le décrit habituellement, mais d'un processus en deux phases, soit l'altération de vieux grains engendrant une fracturation de ces grenats, puis la formation de zone de surcroissance autour de ces différents fragments expliquant la texture en agrégats observée. Cette interprétation en deux phases est importante, car elle engendre des différences notables lorsque l'on applique des méthodes pétrologiques comme la thermobarométrie, la géochronologie ou encore lorsque l'on étudie la distribution relative de la taille des grains. Les conditions thermales dans l'auréole de contact dépendent fortement du mode d'emplacement de l'intrusion et c'est pourquoi il est nécessaire de d'abord comprendre le pluton avant de faire des conclusions sur son auréole de contact. Une étude de terrain des roches intrusives ainsi qu'une étude géochimique, géochronologique et structurale est présente dans le troisième chapitre. Cette étude apporte des informations importantes sur la formation de l'intrusion mais également de nouvelles connaissances sur la nature de grands plutons homogènes et la structure de système magmatique en général. L'emplacement incrémental est mis en évidence et l'existence d'un réservoir intermédiaire en-dessous des plutons homogènes est proposé. Le quatrième chapitre de cette thèse illustre comment utiliser l'information extraite des roches encaissantes pour expliquer la mise en place de l'intrusion. Les températures obtenues par la combinaison des observations de terrain et l'assemblage métamorphique sont utilisées avec des modèles thermiques pour contraindre l'activité magmatique au contact directe de cette auréole. Au lieu d'utiliser le modèle thermique pour vérifier le résultat pétrologique, une approche inverse a été choisie. Les paramètres du modèle ont été changés jusqu'à ce qu'on obtienne une correspondance avec les températures observées dans l'auréole de contact. Ceci montre qu'il y a peu de combinaison qui peuvent expliquer les températures et qu'on peut contraindre la fréquence de l'activité magmatique d'un ancien système magmatique de cette manière. Dans le cinquième chapitre, les processus contrôlant l'anisotropie de la susceptibilité magnétique des roches intrusives sont expliqués à l'aide d'images de la distribution des minéraux dans les roches obtenues par tomographie 3D. Le signal associé à l'anisotropie de la susceptibilité magnétique est une fonction de la forme et de la distribution des grains ferromagnétiques. Ce signal est fréquemment utilisé pour déterminer la direction de mouvement d'un magma. En accord avec d'autres études de la littérature, les résultats montrent que le signal est dominé par la forme des cristaux magnétiques, ainsi que par la distribution des agglomérats de ces minéraux dans la roche. Dans le sixième chapitre, une étude associée à la fusion partielle de carbonates dans les roches encaissantes est présentée. Si la présence de liquides carbonatés dans les auréoles de contact a été proposée sur la base d'expériences de laboratoire, notre étude démontre clairement leur existence dans la nature. La fusion partielle est documentée par des microstructures caractéristiques pour la présence de liquides ainsi que par des données géochimiques et structurales. Les conditions nécessaires sont loin d'être extrêmes et ce processus pourrait être plus fréquent qu'attendu. Les liquides carbonatés sont très mobiles et peuvent circuler le long des limites de grain avant d'infiltrer d'autres roches en produisant une modification de leurs assemblages minéralogiques. Finalement, une curiosité minéralogique est présentée dans le chapitre sept. L'assemblage de minéraux de magnésite et de calcite en équilibre apparent est observé. Il est bien connu que ces deux carbonates ne sont pas stables ensemble dans le système CaO-MgO-FeO-CO.,. En effet, la magnésite et la calcite devraient réagir et produire de la dolomite pendant le métamorphisme. L'explication présentée pour cet assemblage à priori « interdit » est que un liquide carbonaté provenant des roches adjacentes infiltre cette roche et est responsable pour cette microstructure. Une autre implication associée à la présence de carbonates fondus est que la roche encaissante montre une diminution drastique de sa résistance et que les propriétés physiques de cette roche deviennent comparables à celles de la roche intrusive. Cette modification des propriétés rhéologiques des roches encaissantes peut faciliter la mise en place des roches intrusives. Ces différentes études démontrent bien le processus itératif utilisé et l'intérêt d'étudier aussi bien les roches intrusives que les roches encaissantes pour la compréhension des mécanismes de mise en place des magmas au sein de la croûte terrestre.

Transparency and trust in government (2007-2014): a comparative study

In a 2000 report entitled "Trust in government. Ethics measures in OECD countries," OECD Secretary-General Donald J. Johnston emphasized the fact that public ethics are considered as a keystone of good governance. Moreover, public ethics are a prerequisite to public trust, which is in turn vital not only to any public service, but also to any society in general. At the same time, transparency reforms have flourished over the last few years and have several times been designed as a response to public distrust. Therefore, ethics, transparency and trust are closely linked together in a supposed virtuous circle where transparency works as a factor of better public ethics and leads to more trust in government on the citizens' side. This article explores the links between transparency and levels of trust in 10 countries between 2007 and 2014, using open data indexes and access to information requests as proxies for transparency. A national ranking of transparency, based on requests submitted by citizens to the administration and open data indexes, is then proposed. Key findings show that there is no sharp decline of trust in government in all countries considered in this article, and that transparency and trust in government are not systematically positively associated. Therefore, this article challenges the common assumption, mostly found in the normative literature, about a positive interrelation between the two, where trust in government is conceived as a beneficial effect of administrative transparency.