Literatura científica selecionada sobre o tema "Rifts – Égée, Mer (région)"
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Artigos de revistas sobre o assunto "Rifts – Égée, Mer (région)"
Dimitropoulos, Dimitris. "Les sociétés insulaires de la Mer Égée au temps de la domination ottomane. Routes communes et trajectoires séparées". Historical Review/La Revue Historique 1 (20 de janeiro de 2005): 113. http://dx.doi.org/10.12681/hr.173.
Texto completo da fonteOuarhache, Driss, André Charriere, Françoise Chalot-prat e Mohamed EL Wartiti. "Triassic to early Liassic continental rifting chronology and process at the southwest margin of the Alpine Tethys (Middle Atlas and High Moulouya, Morocco); correlations with the Atlantic rifting, synchronous and diachronous". Bulletin de la Société Géologique de France 183, n.º 3 (1 de maio de 2012): 233–49. http://dx.doi.org/10.2113/gssgfbull.183.3.233.
Texto completo da fonteTeses / dissertações sobre o assunto "Rifts – Égée, Mer (région)"
Caroir, Fabien. "Analyse structurale du domaine Nord Eubée : rifting plio-quaternaire et décrochements actifs dans le prolongement occidental de la faille Nord-Anatolienne (Projet WATER)". Electronic Thesis or Diss., Université de Lille (2022-....), 2022. http://www.theses.fr/2022ULILR030.
Texto completo da fonteThe Aegean domain is the theatre of numerous major geodynamical events since Triassic. These divergence and convergence phases have continued to shape the landscape, the crust and the lithospheric mantle of Western Mediterranean. Today, the result is the Anatolia-Aegea microplate, bordered by the North Anatolian Fault, the Arabic Plate, the Hellenides and by the African Plate subduction beneath the Aegean Sea. The southward migration of this subduction since Eocene is responsible for the Aegean crust stretching and thinning, forming Metamorphic Core Complexes and rifts. The current extensive stresses are located in the rifts, like ones of Corinth and of the Sperchios-North Evia Gulf in continental Greece. The last one, as well as North Evia, the Oreoi Channel and the Skopelos Basin, are situated in the prolongation of the western termination of the North Anatolian Fault which marks the plate boundary between Eurasia to the north and Anatolia-Aegea to the south. These areas constitute the North Evia domain, a key-region in order to understand the deformation between Eurasia and the aegean domain. The objective of this PhD thesis is to characterize the inland deformation and especially the offshore one to place the North Evia domain in the context of continental Greece, on the scale of this diffuse plate boundary. These works are based on the interpretation of new very high resolution reflection seismic data (Sparker) acquired during the oceanography surveys “WATER” 1 and 2. The global study has been divided into two main steps: (1) analysis of structures within the North Evia domain and (2) characterization of the current deformation in this domain and its evolution since the rifting initiation.The Sparker profiles interpretation allowed to establish a tectonic detailed map which was then integrated into the regional deformation context through the compilation of inland published structural data. This map highlights four fault directions: NE-SW, NW-SE, WNW-ESE and W-E throughout the entire North Evia domain. These directions were put into perspective with the clockwise rotations recorded near to the rift, allowing thus to propose a new chronological model for the North Evia domain since the beginning of the rifting process. The last step of this model presents the current situation which is marked by numerous earthquakes of magnitudes between 4 and 7 and by numerous focal mechanisms linked to these events. The interpretation of these focal mechanisms emphasizes right-lateral strike-slip movements along NE-SW striking faults, and left-lateral strike-slip movements along NW-SE striking faults. The current deformation of the North Evia domain highlights, firstly, the complexity of fault networks which seem all active and, secondly, the complex deformation within this diffuse plate boundary where the North Anatolian Fault could have an influence on the clockwise rotations and the NE-SW striking faults. The Sperchios-North Evia Gulf has been placed into the continental Greece context, in particular from two crustal-scale cross-sections located between Peloponnese and Evia. These cross-sections show asymmetries of Corinth and Sperchios-North Evia Gulf rifts and their relationship with crustal thickness variations. Thus, the western parts of the both rifts seem to be controlled in depth by northward low-angle structures, a detachment for Corinth and the Pelagonian Thrust Front for Sperchios-North Evia Gulf. In the west, the Moho is deeper beneath the rifts and it goes up to the plumb of the reliefs located north of each rifts, thus rifts and crust show a strong asymmetry. In the East, the Moho is shallow beneath the rifts and the entire structure seems symmetrical
Pomadere, Maia. "Les enfants dans le monde égéen, du néolithique au début de l'âge du fer". Paris 1, 2007. http://www.theses.fr/2007PA010581.
Texto completo da fontePsychoyos, Olga. "Milieu naturel et sites archéologiques dans les régions côtières de la mer Egée, au néolithique et à l'âge du bronze (déplacements de la ligne de rivage et fluctuations de l'implantation humaine)". Paris 1, 1986. http://www.theses.fr/1986PA010654.
Texto completo da fonteThe aim of this study is to show the importance of some variations in the natural environment of the coastal regions of the aegean during the neolithic and the bronze age, that is from 6000 to 1000 bc. In the first part are exposed the main factors of the morphological evolution of the coastal regions and their consequences : the movements of the shoreline. This exposure is followed by a few morphological studies in the concerned regions. We concluded this part by stating some steps identified in the evolution of the natural environment. In the second part we describe about a hundred archaeological sites in the attempt to point out their physical surrounding and to define for each one the periods of settlement and the succession of cultural groups. In the third part we are dealing with the synthesis of the data. As far as the natural environment is concerned firstly the data proving variations gathered in the description of the archaeological sites are confronted with the results acquired in the first part. This process has brought out steps in the evolution of the natural environment in the frame of the aegean chronology. Thus in the ancient neolithic the sea-level would have been about 6 m lower than today and up to the end of the bronze age there would have been two major oscillations. Concerning the human settlement the synthesis of the archaeological data has allowed us to bring out general discontinuities in the human occupation and to observe in the cultural sequences phases of retraction and isolation or of diffusion and expansion. By comparing the results we have noticed a chronological relationship between the fluctuations of the natural environment and those of the human settlement. To conclude our study we have tried to find in what way the suggested changes in the natural environment have interracted upon the settlement
Boleti, Athina. "L' exploitation de l'émeri en Égée et en Méditerranée Orientale à l'Âge du bronze". Paris 1, 2009. http://www.theses.fr/2009PA010601.
Texto completo da fonteChabot, Jacques. "Les débuts de la sédentarisation et de l'agriculture dans le monde égéen (25 000-5 800 av. J.-C.)". Master's thesis, Université Laval, 1993. http://hdl.handle.net/20.500.11794/17754.
Texto completo da fonteDandrau, Alain. "La construction en terre dans le monde égéen protohistorique : les matériaux et leurs propriétés". Paris 1, 1997. http://www.theses.fr/1997PA010615.
Texto completo da fonteThe most part of the protohistoric aegean sites has given a lot of pieces of earth architecture (pieces of bricks or daub, wall or floor-plasters. . . ). These are usually ignored by the archaeologist. This work, placed between archaeology and archaeometry, want to demonstrate that these construction materials can serve as a source of information of the past societies. The archaeological fragments came from Dikili Tash in Macedonian Greece (5th millenium bc), and from Malia in Crete (2000-1100 bc). The materials used give us informations about architectural structures, technics of building and relations between men and the environment. The analysis have proven that the clay was choosen because of special physical characteristics (waterproof properties for roofs and floors, cohesive earth for walls. . . ). For wall-plasters, physico-chemical analysis were indispensable complements for stylistic and iconographic studies. A typology of plasters, based on function and composition, bring up technological and chronological informations
Bradfer-Burdet, Isabelle. "Les motifs marins dans l'art égéen à l'Age du Bronze". Paris 1, 2000. http://www.theses.fr/2000PA010529.
Texto completo da fonteTouchais, Gilles. "Aux marges du monde mycénien : recherches sur les origines et la diffusion de la civilisation helladique". Paris 1, 1997. http://www.theses.fr/1997PA010601.
Texto completo da fonteThis study is the synthesis of the researches carried out by the author into periods and areas situated on the fringe of mycenaean civilisation. It is organised around three main issues : 1) Cultural development of mainland Greece in the middle bronze age and the problem of the origins of mycenaean civilisation; 2) The importance of the neolithic heritage in the emergence and development of helladic civilisation; 3) The relationships between the helladic world and its north-west border areas. The first issue offers the opportunity, on the one hand, of putting up to date the comprehensive picture of middle helladic Greece drawn up by the author a few years ago in a collective work (the aegean civilisations of the neolithic and the bronze age, p. U. F. ); on the other hand, it allows to present the still unpublished documentation provided by the recently finished excavation of the middle helladic settlement on the aspis of argos. The second issue articulates around five aspects of Greek neolithic, already touched upon by the author in his previous work, but which are here put in the perspective of the current research : the occupation of caves, the nature and function of anthropomorphic figurines, the variability of ceramics, the problem of exchanges and the definition of final neolithic. The third issue, based on the excavation which the author has been in charge of for four years on the site of Sovjan (Albania), deals with the role played, in the development of helladic civilisation, by the areas situated on its north-west border (epirus, albania, western macedonia). This question, which has not yet been dealt with in a systematic way, is considered through the study of three categories of documents likely to provide evidence of contacts between greece and these areas throughout the bronze age : tumuli in the early bronze age; matt-painted ware in the middle and late bronze age; mycenaean ware and weapons in the late bronze age
Huet, Benjamin. "Rhéologie de la lithosphère continentale : l’exemple de la mer Egée". Phd thesis, Paris 6, 2010. http://www.theses.fr/2010PA066444.
Texto completo da fonteLecomte, Emmanuel. "Détachements et failles normales à faible pendage : cinématique et localisation de la déformation. Approche de terrain et modélisation numérique. Exemple des Cyclades". Paris 6, 2010. http://www.theses.fr/2010PA066470.
Texto completo da fonte