969 resultados para Islam and state.


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Cette thèse s’ouvre avec des commentaires du siècle dernier sur les opinions de Luther à propos de l’autorité du gouvernement et de l’Église, ainsi que sur la nature humaine et la fonction de la loi. Je présente ensuite où ces critiques situent Luther par rapport à la tradition scholastique et par rapport à la tradition romaine au sein de l’Église. Puis, j’explore les œuvres de Luther pour mettre en lumière ses arguments concernant l’Église, la source de son autorité, ainsi que la relation de celle-ci avec les gouvernements, autrement dit les autorités temporelles. De là, je m’intéresse à la comparaison que le réformateur fait entre la place de l’Église dans la société et celle de l’autorité temporelle. Enfin, j’analyse les écrits de Luther à propos de deux évènements concernant la construction du Royaume de Dieu et plus précisément, dans quelle mesure l’Église dépend, ou non, des autorités temporelles pour construire ce Royaume. Nous allons trouver une réponse surprenante à la question de comment l’église est indépendante de l’autorité temporelle dans l’ouvrage spécifique au royaume de Dieu. Le but de ma thèse est de répondre à certains critiques qui reprochent à Luther de s’appuyer sur l’autorité temporelle pour établir l’Église, et par conséquent de donner au temporel le contrôle sur le spirituel. Nous découvrirons que Luther tire son autorité des Écritures. Nous découvrirons aussi les conséquences que cette autorité a sur sa philosophie politique, c'est-à-dire l’importance de la soumission aux autorités gouvernantes en même temps que la libération des individus de la tyrannie d’une fausse doctrine.

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The Relation University, Company and State UEE defined through the eight committees created in Colombia to position the investigation like central axis of the triad one, impliesthe revision of the paper that in ahead must assume the companies and the universities for the success of the nexus. The scene raises the debt that both estates show as opposed to the definition of the subjects that in particular force them to work jointly within the triad one. The systemic methodology, drawn up under the epilogue of the order of the organizations, stipulates that these can work in unison or in key when they are understood like structure, and recognize what they do to each other. However, slope has left all a leaf of conciliations, understandings and repairs that they will have to be reviewed to the light of spirit UEE.

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Cumple con los requisitos para OCR AS de Historia y su contenido, que estudia los importantes cambios producidos en la Iglesia inglesa durante el siglo XVI, se divide en seis secciones: las tres primeras tratan en orden cronológico el período de 1500 a 1558, mientras que los tres últimos ofrecen aspectos temáticos de la llamada Reforma Inglesa, entre 1558 y 1589. Incluye una selección y definición de los temas, conceptos, acontecimientos y lugares considerados más importantes, así como breves biografías de personajes clave y consejos para los exámenes.

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During the financial crisis, companies and lenders found themselves in distressed situations. Competition authorities across the globe had to deal with controversial issues such as the application of the failing firm defence in merger transactions as well as assessment of emergency aid granted by states. This article considers competition policy in periods of crisis, in particular the failing firm defence in merger control and its state aid policy.

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An assessment of the fifth Coupled Models Intercomparison Project (CMIP5) models’ simulation of the near-surface westerly wind jet position and strength over the Atlantic, Indian and Pacific sectors of the Southern Ocean is presented. Compared with reanalysis climatologies there is an equatorward bias of 3.7° (inter-model standard deviation of ± 2.2°) in the ensemble mean position of the zonal mean jet. The ensemble mean strength is biased slightly too weak, with the largest biases over the Pacific sector (-1.6±1.1 m/s, 27 -22%). An analysis of atmosphere-only (AMIP) experiments indicates that 41% of the zonal mean position bias comes from coupling of the ocean/ice models to the atmosphere. The response to future emissions scenarios (RCP4.5 and RCP8.5) is characterized by two phases: (i) the period of most rapid ozone recovery (2000-2049) during which there is insignificant change in summer; and (ii) the period 2050-2098 during which RCP4.5 simulations show no significant change but RCP8.5 simulations show poleward shifts (0.30, 0.19 and 0.28°/decade over the Atlantic, Indian and Pacific sectors respectively), and increases in strength (0.06, 0.08 and 0.15 m/s/decade respectively). The models with larger equatorward position biases generally show larger poleward shifts (i.e. state dependence). This inter-model relationship is strongest over the Pacific sector (r=-0.89) and insignificant over the Atlantic sector (r=-0.50). However, an assessment of jet structure shows that over the Atlantic sector jet shift is significantly correlated with jet width whereas over the Pacific sector the distance between the sub-polar and sub-tropical westerly jets appears to be more important.

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The chapter examines the compex roles of corruption in state-buioding environments. The first section briefly outlines how statebuilding is conceptualized in this discussion. The second section examines the concept of corruption,and argues that the organization, rather than the scale of corruption, offers a better lens through which its impact can be analyzed. The third section examines the complex relationship between corruption and statebuilding through the lenses of two key aspects of statebuilding – elite settlements, and the provision of public services – and briefly discusses both the complex relationship between corruption and security, and the impact of aid on corruption in statebuilding environments. The fourth section concludes the chapter with a reflection on the implications of the analysis for understanding contemporary statebuilding efforts and policy.

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Despite many decades investigating scalp recordable 8–13-Hz (alpha) electroencephalographic activity, no consensus has yet emerged regarding its physiological origins nor its functional role in cognition. Here we outline a detailed, physiologically meaningful, theory for the genesis of this rhythm that may provide important clues to its functional role. In particular we find that electroencephalographically plausible model dynamics, obtained with physiological admissible parameterisations, reveals a cortex perched on the brink of stability, which when perturbed gives rise to a range of unanticipated complex dynamics that include 40-Hz (gamma) activity. Preliminary experimental evidence, involving the detection of weak nonlinearity in resting EEG using an extension of the well-known surrogate data method, suggests that nonlinear (deterministic) dynamics are more likely to be associated with weakly damped alpha activity. Thus rather than the “alpha rhythm” being an idling rhythm it may be more profitable to conceive it as a readiness rhythm.

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Sea ice friction models are necessary to predict the nature of interactions between sea ice floes. These interactions are of interest on a range of scales, for example, to predict loads on engineering structures in icy waters or to understand the basin-scale motion of sea ice. Many models use Amonton's friction law due to its simplicity. More advanced models allow for hydrodynamic lubrication and refreezing of asperities; however, modeling these processes leads to greatly increased complexity. In this paper we propose, by analogy with rock physics, that a rate- and state-dependent friction law allows us to incorporate memory (and thus the effects of lubrication and bonding) into ice friction models without a great increase in complexity. We support this proposal with experimental data on both the laboratory (∼0.1 m) and ice tank (∼1 m) scale. These experiments show that the effects of static contact under normal load can be incorporated into a friction model. We find the parameters for a first-order rate and state model to be A = 0.310, B = 0.382, and μ0 = 0.872. Such a model then allows us to make predictions about the nature of memory effects in moving ice-ice contacts.