Добірка наукової літератури з теми "Alboran Domain"
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Статті в журналах з теми "Alboran Domain":
Olivier, Philippe, and Jean-Louis Paquette. "Early Permian age of granite pebbles from an Eocene or Oligocene conglomerate of the Internal Rif belt (Alboran domain, Morocco): hypothesis on their origin." BSGF - Earth Sciences Bulletin 189, no. 3 (2018): 13. http://dx.doi.org/10.1051/bsgf/2018012.
Casciello, Emilio, Manuel Fernàndez, Jaume Vergés, Massimo Cesarano, and Montserrat Torne. "The Alboran domain in the western Mediterranean evolution: the birth of a concept." Bulletin de la Société Géologique de France 186, no. 4-5 (July 1, 2015): 371–84. http://dx.doi.org/10.2113/gssgfbull.186.4-5.371.
PLATZMAN, E., J. P. PLATT, S. P. KELLEY, and S. ALLERTON. "Large clockwise rotations in an extensional allochthon, Alboran Domain (southern Spain)." Journal of the Geological Society 157, no. 6 (November 2000): 1187–97. http://dx.doi.org/10.1144/jgs.157.6.1187.
Turner, S. P., J. P. Platt, R. M. M. George, S. P. Kelley, D. G. Pearson, and G. M. Nowell. "Magmatism Associated with Orogenic Collapse of the Betic-Alboran Domain, SE Spain." Journal of Petrology 40, no. 6 (June 1, 1999): 1011–36. http://dx.doi.org/10.1093/petroj/40.6.1011.
El Bakili, Asmae, Michel Corsini, Ahmed Chalouan, Philippe Münch, Adrien Romagny, Jean Marc Lardeaux, and Ali Azdimousa. "Neogene polyphase deformation related to the Alboran Basin evolution: new insights for the Beni Bousera massif (Internal Rif, Morocco)." BSGF - Earth Sciences Bulletin 191 (2020): 10. http://dx.doi.org/10.1051/bsgf/2020008.
Crespo-Blanc, Ana, and Dominique Frizon de Lamotte. "Structural evolution of the external zones derived from the Flysch trough and the South Iberian and Maghrebian paleomargins around the Gibraltar arc: a comparative study." Bulletin de la Société Géologique de France 177, no. 5 (September 1, 2006): 267–82. http://dx.doi.org/10.2113/gssgfbull.177.5.267.
Michard, André, Ahmed Chalouan, Hugues Feinberg, Bruno Goffé, and Raymond Montigny. "How does the Alpine belt end between Spain and Morocco ?" Bulletin de la Société Géologique de France 173, no. 1 (January 1, 2002): 3–15. http://dx.doi.org/10.2113/173.1.3.
Vissers, R. L. M., J. P. Platt, and D. van der Wal. "Late orogenic extension of the Betic Cordillera and the Alboran Domain: A lithospheric view." Tectonics 14, no. 4 (August 1995): 786–803. http://dx.doi.org/10.1029/95tc00086.
Torné, M., E. Banda, V. García-Duen˜as, and J. C. Balanyá. "Mantle-lithosphere bodies in the Alboran crustal domain (Ronda peridotites, Betic-Rif orogenic belt)." Earth and Planetary Science Letters 110, no. 1-4 (May 1992): 163–71. http://dx.doi.org/10.1016/0012-821x(92)90046-x.
Michard, André, Bruno Goffé, Mohamed Bouybaouene, and Omar Saddiqi. "Late Hercynian–Mesozoic thinning in the Alboran domain: metamorphic data from the northern Rif, Morocco." Terra Nova 9, no. 4 (December 1997): 171–74. http://dx.doi.org/10.1046/j.1365-3121.1997.d01-24.x.
Дисертації з теми "Alboran Domain":
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
Javid, Fakhr Bita. "Active tectonic analysis in the transition domain between Albortz and Kopeh Dagh (NE Iran)." Aix-Marseille 3, 2010. http://www.theses.fr/2010AIX30038.
We present results from an active tectonic study of the transition zone between Alborz and Kopeh Dagh which is an active deformation domain in relation with the Arabia-Eurasia collision. Focal mechanism and recent faulting slip-vector (fault kinematics) analyses indicate an active transpressional tectonic regime characterized by a regionally significant NNE-trending [sigma]1. We provide evidence: 1- for a drastic temporal change in the stress state during Plio-Quatemary and, 2- that there is no slip partitioning in this transition domain presently. Geomorphic and tectonic analyses combined with cosmogenic dating methods (36Cl et 10Be) led us to determine the following long-term slip rates : 2-3 mm. Yr-1, 1-2 mm. Yr-1, 3-4 mm. Yr-1 and 1-3 mm. Yr-1, for the Jajarm, Ashkhaneh, Abr and Khij Faults, respectively. These faultings can be due to the westward motion of the eastern Alborz-western Kopeh Dagh with respect to Eurasia
Частини книг з теми "Alboran Domain":
Doblas, Miguel, José López-Ruiz, and José-María Cebriá. "Cenozoic evolution of the Alboran Domain: A review of the tectonomagmatic models." In Cenozoic Volcanism in the Mediterranean Area. Geological Society of America, 2007. http://dx.doi.org/10.1130/2007.2418(15).