924 resultados para Greece Religion
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Comprend : Indice premier des matieres contenues en ce present livre [- Autre indice contenant les passages de la Bible, selon l'ordre des livres du vieil et nouveau testament]
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Abstract: Religion and democracy: Protestantism, Catholicism and Islam in comparative perspective
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L'accompagnement spirituel dans les prisons suisses est dominé par un modèle mono-culturel chrétienne. Or, la présence importante de détenus de confession musulmane dans les établissements pénitentiaires incite ceux-ci à organiser un soutien spirituel adapté à cette catégorie de leur population. Dans quel cadre légal cet accompagnement spirituel se déroule-t-il? Quelle forme prend-il ? Quels sont ceux (et plus rarement celles) qui assistent spirituellement les détenus musulmans ? Cet article propose de répondre à ces questions en énonçant les principes juridiques relatifs à l'exercice de la religion en contexte carcéral et en présentant des profils d'intervenants musulmans de prison.
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The incomplete Evros ophiolites in NE Greece form a NE-SW-oriented discontinuous belt in the Alpine orogen of the north Aegean. Field data, petrology and geochemistry are presented here for the intrusive section and associated mafic dykes of these ophiolites. Bodies of high-level isotropic gabbro and plagiogranite in the ophiolite suite are cross-cut by NE-SW-trending boninitic and tholeiitic-boninitic affinity dykes, respectively. The dykes fill tensile fractures or faults, which implies dyke emplacement in an extensional tectonic regime. The tholeiitic-transitional boninitic gabbro is REE- and HFS-depleted relative to N-MORB, indicating derivation from melting of a refractory mantle peridotite source. Associated boninitic dykes are slightly LREE-enriched, showing mineral and whole-rock geochemistry similar to the gabbro. The plagiogranite is a strongly REE-enriched high-silica trondhjemite, with textures and composition typical for an oceanic crust differentiate. Plagiogranite-hosted tholeiitic and transitional boninitic dykes are variably REE-enriched. Geochemical modelling indicates origin of the plagiogranite by up to 75% fractional crystallization of basaltic magma similar to that producing the associated tholeiitic dykes. All mafic rocks have high LILE/HFSE ratios and negative Ta-Nb-Ti and Ce anomalies, typical for subduction zone-related settings. The mafic rocks show a similar trace-element character to the mafic lavas of an extrusive section in Bulgaria, suggesting they both form genetically related intrusive and extrusive suites of the Evros ophiolites. The field occurrence, the structural context, the petrology and geochemical signature of the studied magmatic assemblage provide evidence for its origin in a proto-arc (fore-arc) tectonic setting, thus tracing the early stages of the tectono-magmatic evolution of Jurassic arc-marginal basin system that has generated the supra-subduction type Evros ophiolites.
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Collection : Les archives de la Révolution française ; 8.1306
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Collection : Les archives de la Révolution française ; 8.468