Letteratura scientifica selezionata sul tema "Terre – Croûte – Extension"
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Articoli di riviste sul tema "Terre – Croûte – Extension":
Ferrière, Jacky, e Frank Chanier. "La marge Ouest-Maliaque de la Téthys (Hellénides) : une marge en hyper-extension, pauvre en magma". Annales de la Société géologique du Nord - (2e Série), Tome 28, n. 28 (1 dicembre 2021): 39–56. http://dx.doi.org/10.54563/asgn.288.
Nasri, S., J. M. Lamachère e J. Albergel. "Impact des banquettes sur le ruissellement d'un petit bassin versant". Revue des sciences de l'eau 17, n. 2 (12 aprile 2005): 265–89. http://dx.doi.org/10.7202/705534ar.
Tesi sul tema "Terre – Croûte – Extension":
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.
The 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
Thoué, Frédéric. "Quantification par imagerie tridimensionnelle de l'extension continentale et des déplacements associés : exemples au Kenya et au Yémen". Grenoble 1, 1993. http://www.theses.fr/1993GRE10200.
SATSUKAWA, Takako. "Interactions magma-roche, déformation à haute température et anisotropie sismique dans le manteau de la transition continent-océan et dans la lithosphère océanique". Phd thesis, 2012. http://tel.archives-ouvertes.fr/tel-00795505.