Résumé : Depuis 1999, l’Union européenne a inauguré une nouvelle approche dans ses relations avec l’Amérique latine et les Caraïbes. A cet égard, le premier sommet Union européenne – Amérique latine – Caraïbes, dit « sommet de Rio » marque un tournant grâce au lancement du « partenariat stratégique ». Dans ce cadre, toutes les organisations régionales d’intégration économique situées dans cette zone géographique, et non pas uniquement le MERCOSUR, apparaissent comme des partenaires importants. Le changement obéit autant à des contraintes externes qu’à une stratégie extérieure. Dans le domaine des échanges commerciaux, le but déclaré est d’atteindre « une libéralisation mutuelle des échanges » sur une base équitable et mutuellement profitable tout en défendant certaines valeurs communes. Cependant, le cadre juridique longtemps en vigueur s’est avéré inadapté à l’avènement d’une ambition économique et politique d’une telle ampleur. Par conséquent, l’Union européenne se trouve confrontée au défi de réformer les cadres juridiques de ses relations avec les organisations régionales d’intégration économique d’Amérique latine et des Caraïbes. La thèse analyse l’évolution et la restructuration actuelles des instruments juridiques des relations entre l’Union européenne l’Amérique latine et les Caraïbes.
Since 1999, the European Union began a new competitive approach in its relationships with Latin America and the Caribbean. In this respect, the first step has been made in the European Union-Latin America and Caribbean’ Summit [Rio Summit (1999)] with the launch of a new partnership called “Strategic Partnership”. In this context, all organisations of regional economic integration – not only the MERCOSUR the most competitive one – are considered as important partners. The change is due to external constraints as well as an external strategy. In the field of commercial exchanges, the goal is to attempt “mutual liberalisation of exchanges” on a fair and mutually profitable basis, defending at the same time “common values”. However, the traditional legal framework of the relations is obviously unsuitable for such an ambitious economic and political project. So, from a legal aspect, the European Union is confronted with the challenge of reforming the contractual frameworks of its relations with regional economic integrations in Latin America and in the Caribbean. The issue concerns an analysis of the evolution and restructuring of existing legal instruments of the European Union’s relations with Latin America and the Caribbean.
Desde 1999, la Unión Europea instauró un nuevo enfoque en sus relaciones con América Latina y el Caribe. En este enfoque llamado “estratégico”, todas las organiza-ciones comarcales de integración económicas ubicadas en esta zona geográfica y no úni-camente el MERCOSUR, se pueden ver como interlocutores importantes. La primera cumbre Unión Europea /América latina/Caribe (cumbre de Rio) es una fecha importante en la evolución de las relaciones gracias al lanzamiento “de la colaboración estratégica”. En lo que toca a los intercambios comerciales, la meta declarada es alcanzar una “liberalización mutual de los intercambios” a partir de una base equitativa y mutualmente provechosa de-fendiendo a la vez ciertos valores comunes. Sin embargo, el marco jurídico en vigor durante una larga temporada se ha reve-lado inadecuado para el advenimiento de una ambición económica y política de esta impor-tancia. Por consiguiente, la Unión Europea se enfrenta hoy en día al desafío jurídico de la renovación del marco convencional de sus relaciones con las organizaciones de integración económica de América Latina y del Caribe. El asunto se refiere a un análisis de las rela-ciones exteriores de la Unión Europea desde el punto de vista de los desafíos jurídicos. Utilizamos el análisis sistémico para poner de relieve los factores explicativos de la evolu-ción y de la reestructuración actuales de los instrumentos jurídicos de las relaciones entre la Unión Europea y América-Latina Caribe.

http://www.theses.fr/2011AGUY0495/document

Éditeur(s) : HAL CCSD American Geophysical Union (AGU)
Résumé : International audience
The Calabro-Peloritan belt constitutes the eastward termination of the southern segment of the Alpine Mediterranean belt. This orogenic system was built up during the convergence between the Eurasian and the African plates, roughly directed North-South since the Upper Cretaceous. It was subsequently fragmented during the opening of the Western Mediterranean basins since Oligocene times. The curved shape of the Calabro-Peloritan belt was acquired during the opening of the Tyrrhenian basin since Tortonian. The origin, kinematics and significance of the Calabro-Peloritan tectonic pile are still debated. Our data in the Aspromonte Massif of Southern Calabria reveal an Alpine history marked by two main superimposed kinematic regimes. (i) A first phase corresponds to the piling up of basement nappes with a top-to-the-SE vergence, i.e in a direction orthogonal to the belt trend and towards the Adriatic foreland. This external vergence is similar to what is observed in both Northeastern Sicily and Northern Calabria. In Sicily, the age of nappe piling is Alpine, as evidenced by pinched slices of Mesozoïc sediments. In the Aspromonte Massif, thrusting age is less constrained. Our data suggest remnants of late Hercynian structuration before the Alpine stacking. (ii) A second phase corresponds to the thinning of the continental crust, dated at around 30 Ma by both geochronological and stratigraphical data. This extension is mainly localized on two low-angle detachment contacts, with top-to-the-NE displacement. The lower one corresponds to the reworking of the former main nappe contact. The upper one is a large detachment fault cutting across the pile from upper sedimentary levels down to metamorphic basement. Extension of similar Alpine age and similar internal vergence has been already recognized in other parts of the Calabro-Peloritan Arc: in the basement nappes of Northeastern Sicily and in the ophiolitic units of Northern Calabria. Coming back to the original geometry and position of the Calabro-Peloritan belt, before its bending and the opening of the Liguro-Provençal and Tyrrhenian basins, we evidence a homogeneous Oligocene NE-SW extension all along the Calabro-Peloritan segment of the Alpine Mediterranean belt. This tectonometamorphic history is best explained within the framework of the continuous Tertiary westward dipping subduction of the Tethyan oceanic domain below the European active margin and the progressive eastward retreat of the Apennine trench since Oligocene times.
ISSN: 0278-7407

hal-00283182
https://hal.archives-ouvertes.fr/hal-00283182
https://hal.archives-ouvertes.fr/hal-00283182/document
https://hal.archives-ouvertes.fr/hal-00283182/file/Heymes_et_al_2008.pdf
DOI : 10.1029/2007TC002157