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Browsing by Author "Ahmamou, M’Fedal"
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Cinemática y paleoesfuerzos en la zona de falla transcurrente de Jebha-Chrafate (Rif septentrional, Marruecos)
Ben Makhlouf, Mohamed; Galindo Zaldívar, Jesús; Chalouan, Ahmed; Sanz de Galdeano, Carlos; Ahmamou, M’Fedal; López Garrido, Ángel Carlos (Sociedad Geológica de España, 2005)The Jebha-Chrafate is an ENE-WSW sinistral major transcurrent fault of the Rif Cordillera, formed during the southwestwards emplacement of the Internal Zones on the Flysch units and the External Zones. The analysis of ... -
Deformaciones recientes en el frente de la Cordillera Rifeña (Prerif, Marruecos)
Chalouan, Ahmed; Galindo Zaldívar, Jesús; Bargach, K.; Jabaloy, A.; Ahmamou, M’Fedal; Ruano, Patricia; Benmakhlouf, M.; Sanz de Galdeano, Carlos; Akil, Mustafa (Sociedad Geológica de España, 2000)The Prerif ridges form pari of the foreland of the Rif Mountains. They are formed by superposed slices, with folds and faults, originated during the late Miocene WSWwards displacement of the Prerif units. At present, they ... -
Edad U/Th de los travertinos de Beni Younech y correlación con las terrazas marinas cuaternarias de Ras Leona (SE del Estrecho de Gibraltar, Marruecos)
Chalouan, Ahmed; Sanz de Galdeano, Carlos; Galindo Zaldívar, Jesús; Julià, Ramón; El Kadiri, Khalil; Pedrera Parias, Antonio; Hlila, Rachid; Akil, Mustafa; Ahmamou, M’Fedal (2008)Three travertinic levels have been identified in the Beni Younech village, near the Quaternary marine terraces of Ras Leona Point, in the south-eastern coast of the Gibraltar Strait. These travertines developed probably ... -
Relaciones entre tectónica y sedimentación asociadas a las Rides Prérifaines en la Cuenca de Volubilis (frente del Rif, Marruecos)
Roldán García, Francisco Javier; Galindo Zaldívar, Jesús; Chalouan, Ahmed; Anahnah, Farida; Ahmamou, M’Fedal; Ruano, Patricia; Ruiz Constán, Ana; Sanz de Galdeano, Carlos; Ben Makhlouf, Mohamed; Marín Lechado, Carlos; López Garrido, Ángel Carlos; Pedrera Parias, Antonio (2009)The Volubilis Neogene basin (Morocco) was part of the South Rif Corridor that connected the Atlantic Ocean with the Mediterranean. This basin recorded the tectonic - sedimentary interactions of a foreland basin subjected ...