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Статті в журналах з теми "Sebtides":
Homonnay, Emmanuelle, Jean-Marc Lardeaux, Michel Corsini, Asmae El Bakili, Delphine Bosch, Olivier Bruguier, and Mohamed Ouazzani-Touhami. "Arc-related high-K magmatism in the Ceuta Peninsula (Internal Rif, Spain): discovery and consequences." Geological Magazine 156, no. 08 (October 30, 2018): 1385–99. http://dx.doi.org/10.1017/s0016756818000717.
Farah, Aboubaker, André Michard, Omar Saddiqi, Ahmed Chalouan, Christian Chopin, Pilar Montero, Michel Corsini, and Fernando Bea. "The Beni Bousera marbles, record of a Triassic-Early Jurassic hyperextended margin in the Alpujarrides-Sebtides units (Rif belt, Morocco)." BSGF - Earth Sciences Bulletin 192 (2021): 26. http://dx.doi.org/10.1051/bsgf/2021015.
Homonnay, Emmanuelle, Michel Corsini, Jean-Marc Lardeaux, Adrien Romagny, Philippe Münch, Delphine Bosch, Bénédicte Cenki-Tok, and Mohamed Ouazzani-Touhami. "Miocene crustal extension following thrust tectonic in the Lower Sebtides units (internal Rif, Ceuta Peninsula, Spain): Implication for the geodynamic evolution of the Alboran domain." Tectonophysics 722 (January 2018): 507–35. http://dx.doi.org/10.1016/j.tecto.2017.11.028.
El Bakili, Asmae, Michel Corsini, Jean-Marc Lardeaux, Sylvain Gallet, Philippe Münch, and Ahmed Chalouan. "Amphibolite facies metamorphic event within the Upper Sebtides tectonic units (Internal Rif, Morocco): a record of a hyperextended margin at the border of the western Tethys." Comptes Rendus. Géoscience 353, no. 1 (July 5, 2021): 193–208. http://dx.doi.org/10.5802/crgeos.59.
Bessière, Eloïse, Laurent Jolivet, Romain Augier, Stéphane Scaillet, Jacques Précigout, José-Miguel Azañón, Ana Crespo-Blanc, Emmanuel Masini, and Damien Do Couto. "Lateral variations of pressure-temperature evolution in non-cylindrical orogens and 3-D subduction dynamics: the Betic-Rif Cordillera example." BSGF - Earth Sciences Bulletin 192 (2021): 8. http://dx.doi.org/10.1051/bsgf/2021007.
Janots, Emilie, François Negro, Fabrice Brunet, Bruno Goffé, Martin Engi, and Mohamed L. Bouybaouène. "Evolution of the REE mineralogy in HP–LT metapelites of the Sebtide complex, Rif, Morocco: Monazite stability and geochronology." Lithos 87, no. 3-4 (April 2006): 214–34. http://dx.doi.org/10.1016/j.lithos.2005.06.008.
Marrone, Sara, Patrick Monié, Federico Rossetti, Federico Lucci, Thomas Theye, Mohamed L. Bouybaouene, and Mohamed Najib Zaghloul. "The Pressure‐Temperature‐time‐deformation history of the Beni Mzala unit (Upper Sebtides, Rif belt, Morocco): Refining the Alpine tectono‐metamorphic evolution of the Alboran Domain of the Western Mediterranean." Journal of Metamorphic Geology, December 25, 2020. http://dx.doi.org/10.1111/jmg.12587.
Дисертації з теми "Sebtides":
El, Bakili Asmae. "Evolution tectono-metamorphique et chronologique des unités métamorphiques du Rif interne (Beni Bousera, Nord du Maroc)." Thesis, Université Côte d'Azur, 2021. http://www.theses.fr/2021COAZ4034.
Located at the extreme tip of the western Mediterranean, the Betic-Rif orogenic system is built through a complex alpine orogenic history involving processes of subduction related to convergence between Africa and Eurasia since the Cretaceous. A remarkable discovery during the last four decades of geological investigations, has been the remains of a variscan event in the internal zones of the belt. These results underline the presence of two superimposed orogenic systems, the internal zones of the belt thus remain a privileged area to study the importance of the structural and the metamorphic heritage in the partial or total reactivation by the most recent events. This work is located in the Beni Bousera sector, where crustal and mantle rocks that form the innermost units of the chain are exposed. Based on structural and petrological analyses, U-Th-Pb dating on monazite and 40Ar-39Ar dating on micas and amphiboles. The history of the Betic-Rif belt can be summarized as it follows: 1) a HP-HT event affects the base of the internal domain at around 281 ± 3 Ma. These new petrological and geochronological data obtained in the internal Rif, are correlated with the Betics, the Kabyle, the Edough massif of Algeria, the Mauritanian, and the Appalachian belts, attesting a convergent domain during the late Carboniferous – early Permian. All of these orogenic segments are part of the North African Variscides built at the north-western margin of Gondwana in response to convergence between the later and Laurentia. 2) at around 29-26 Ma, a Barrovian to Abukuma metamorphic event affects the Sebtides (the innermost units of the chain) and interpreted as the evolution of the upper plate of a subduction zone. This alpine event is typically characterized by a prograde metamorphic path marked by heating affecting the base of the Sebtides between 26 to 22 Ma, such conditions reflect thinning and heating of the crust related to the asthenosphere upwelling due to slab roll-back. This event marks the beginning of a major extensive event. 3) In the Miocene around 22-20 Ma, the internal zones are affected by an E-W extension contemporary to the opening of the Alboran Basin in a back-arc context, and the intrusion of granitic dykes into the peridotites and crustal metamorphic units, the exhumation of the Sebtides was complete at this time. 4) From early to middle Miocène, the Betic-Rif belt acquired its arcuate geometry (the Gibraltar Arc) during the collision between the Internal and the external zones, attested by de NE-SW to E-W shortening phases across the arc. 5) more lately prior to Pliocene, the Gibraltar arc was subjected to contractional possess related to a N-S shortening phase, which drastically altered its geometry